Misplaced Pages

Yosemite National Park: Difference between revisions

Article snapshot taken from Wikipedia with creative commons attribution-sharealike license. Give it a read and then ask your questions in the chat. We can research this topic together.
Browse history interactively← Previous editContent deleted Content addedVisualWikitext
Revision as of 13:34, 18 July 2016 editHike395 (talk | contribs)Autopatrolled, Extended confirmed users, Pending changes reviewers, Rollbackers, Template editors98,532 edits rm extra adjectives from lede← Previous edit Latest revision as of 05:37, 14 January 2025 edit undoHike395 (talk | contribs)Autopatrolled, Extended confirmed users, Pending changes reviewers, Rollbackers, Template editors98,532 edits Reverted good faith edits by Unkown13579 (talk): See MOS:SECTIONSTYLETags: Twinkle Undo 
Line 1: Line 1:
{{short description|National park in California, United States}}
{{Redirect|Yosemite}} {{Redirect|Yosemite}}
{{pp-move-indef}} {{pp-move}}
{{Use mdy dates|date=November 2013}} {{Use American English|date=March 2021}}
{{Use mdy dates|date=April 2018}}
{{Infobox protected area {{Infobox protected area
| name = Yosemite National Park | name = Yosemite National Park
| iucn_category = II | iucn_category = II
| iucn_ref = <ref>{{Cite web|url=https://www.protectedplanet.net/10908|title=Yosemite National Park|publisher=Protected Planet|website=protectedplanet.net|access-date=2020-05-29|archive-date=May 30, 2022|archive-url=https://web.archive.org/web/20220530002952/https://www.protectedplanet.net/10908|url-status=live}}</ref>
| photo = Tunnel View, Yosemite Valley, Yosemite NP - Diliff.jpg | photo = Tunnel View, Yosemite Valley, Yosemite NP - Diliff.jpg
| photo_caption = Yosemite Valley from Tunnel View | photo_caption = ] from ]
| map = USA | map = California#USA
| label = Yosemite National Park
| relief = 1
| map_caption = | map_caption = Location in California##Location in the United States
| map_width = | map_width =
| location = ], ], & ] counties, ], U.S. | location = ], ], ] and ], ], United States
| nearest_city = ] | nearest_city = ]
| coordinates = {{coord|37|44|33|N|119|32|15|W|region:US-CA|display=inline, title}}
| lat_d = 37 | lat_m = 51 | lat_NS = N
| coords_ref = <ref>{{cite gnis|255923|Yosemite National Park}}</ref>
| long_d = 119 | long_m = 33 | long_EW = W
| established = {{start date and age|1890|10|1}}
| region = US-CA
| scale = 1000000 | area_acre = 759620
| area_ref = <ref name="statistics">{{cite web |url=https://www.nps.gov/yose/learn/management/statistics.htm |title=Park Statistics |publisher=Yosemite National Park (]) |access-date=July 22, 2018 |archive-date=March 8, 2015 |archive-url=https://web.archive.org/web/20150308185200/http://www.nps.gov/yose/learn/management/statistics.htm |url-status=live }}</ref>
| coords_ref = <ref name="gnis">{{cite gnis |id=255923 |name=Yosemite National Park}}</ref>
| visitation_num = 3,897,070
| established = {{start date|1890|10|1}}
| visitation_year = 2023
| area = {{convert|747,956|acre|sqmi ha km2}}<ref name="area">{{cite web |url=http://www.nps.gov/yose/parkmgmt/statistics.htm |title=Park Statistics |publisher = Yosemite National Park (U.S. National Park Service) |accessdate=13 February 2014}}</ref>
| visitation_ref = <ref>{{cite web |title=Annual Park Ranking Report for Recreation Visits in: 2023 |url=https://irma.nps.gov/Stats/SSRSReports/National%20Reports/Annual%20Park%20Ranking%20Report%20(1979%20-%20Last%20Calendar%20Year)|website=nps.gov |publisher=National Park Service |access-date=March 23, 2024 }}</ref>
| visitation_num = 3,882,642
| visitation_year = 2014
| visitation_ref = <ref name="visits">{{NPS Visitation |accessdate=January 8, 2016}}</ref>
| governing_body = ] | governing_body = ]
| website = {{Official website}} | website = {{Official URL}}
| embedded1 = {{designation list | embed=yes | embedded1 = {{Infobox UNESCO World Heritage Site
| designation1 = WHS |child = yes
|ID = 308
| designation1_date = ] <small>(8th ])</small>
|Year = 1984
| designation1_type = Natural
| designation1_criteria = vii, viii |Criteria = Natural: vii, viii
| designation1_number =
| designation1_free1name = State Party
| designation1_free1value = United States
| designation1_free2name = Region
| designation1_free2value = ]
}} }}
}} }}


'''Yosemite National Park''' ({{IPAc-en|j|oʊ|ˈ|s|ɛ|m|ɨ|t|i}} {{respell|yoh|SEM|it-ee}}<ref>{{cite web | url=http://www.bbcamerica.com/mind-the-gap/2014/01/13/american-place-name-pronunciations-guide-brits/ | title=No, Arkansas Doesn't Sound the Way It Looks: A Guide to Pronouncing U.S. Place Names | publisher=BBC America | date=January 13, 2014 | accessdate=14 July 2014 | author=Hargis, Toni}}</ref>) is a ] spanning eastern portions of ], ] and ] counties in the central eastern portion of the ] of ].<ref name=VisitCal>, ]</ref><ref name=NPR>, ], 26 August 2013</ref> The park, which is managed by the National Park Service, covers an area of {{convert|747,956|acre|sqmi ha km2}}<ref name="area"/> and reaches across the western slopes of the ] mountain range.<ref>{{harvnb|Harris|1998|p=324}}</ref> About 3.8 million people visit Yosemite each year:<ref name="visits"/> most spend the majority of their time in the seven square miles (18&nbsp;km<sup>2</sup>) of ].<ref name="naturehistory"/> Designated a ] in 1984, Yosemite is internationally recognized for its ] cliffs, ]s, clear ]s, ] groves, lakes, mountains, glaciers, and ].<ref name = "naturehistory">{{cite web | title =Nature & History | publisher = United States National Park Service: Yosemite National Park | url = http://www.nps.gov/archive/yose/nature/nature.htm | archiveurl=https://web.archive.org/web/20070125062753/http://www.nps.gov/archive/yose/nature/nature.htm|archivedate=January 25, 2007 | date = October 13, 2006 | accessdate = January 27, 2007}}</ref> Almost 95% of the park is designated ].<ref>{{cite web | title =Yosemite Wilderness| publisher = United States National Park Service: Yosemite National Park | url = http://www.nps.gov/yose/planyourvisit/yosemitewilderness.htm | accessdate = March 15, 2008 }}</ref> Yosemite was central to the development of the national park idea. First, ] and others lobbied to protect Yosemite Valley from development, ultimately leading to President ]'s signing the ] in 1864. Later, ] led a successful movement to establish a larger national park encompassing not just the valley, but surrounding mountains and forests as well—paving the way for the United States national park system.<ref name = "historyculture"/> '''Yosemite National Park''' ({{IPAc-en|j|oʊ|ˈ|s|ɛ|m|ɪ|t|i}} {{respell|yoh|SEM|ih|tee}}<ref>{{MW|Yosemite Falls}}</ref>) is a ] in ].<ref>{{harvnb|Harris|1998|p=324}}</ref><ref name="VisitCal">{{cite web|url=http://www.visitcalifornia.com/region/discover-high-sierra|title=Discover the High Sierra|publisher=]|access-date=June 9, 2015|archive-date=June 3, 2020|archive-url=https://web.archive.org/web/20200603003117/http://www.visitcalifornia.com/region/discover-high-sierra|url-status=live}}</ref> It is bordered on the southeast by ] and on the northwest by ]. The park is managed by the ] and covers {{convert|759620|acre|sqmi km2|0}}<ref name="statistics" /> in four ]{{snd}}centered in ] and ], extending north and east to ] and south to ]. Designated a ] in 1984, Yosemite is internationally recognized for its granite cliffs, waterfalls, clear streams, groves of ], lakes, mountains, meadows, glaciers, and ].<ref name = "naturehistory">{{cite web | title =Nature & History | publisher = United States National Park Service: Yosemite National Park | url =http://www.nps.gov/archive/yose/nature/nature.htm | archive-url=https://web.archive.org/web/20070125062753/http://www.nps.gov/archive/yose/nature/nature.htm|archive-date=January 25, 2007 | date = October 13, 2006 | access-date = January 27, 2007}}</ref> Almost 95 percent of the park is designated ].<ref>{{cite web | title = Yosemite Wilderness | publisher = United States National Park Service: Yosemite National Park | url = http://www.nps.gov/yose/planyourvisit/yosemitewilderness.htm | access-date = March 15, 2008 | archive-date = December 19, 2015 | archive-url = https://web.archive.org/web/20151219025803/http://www.nps.gov/yose/planyourvisit/yosemitewilderness.htm | url-status = live }}</ref> Yosemite is one of the largest and least fragmented habitat blocks in the ].


Its ] is characterized by ] and remnants of older rock. About 10&nbsp;million years ago, the Sierra Nevada was ] and tilted to form its unique slopes, which increased the steepness of stream and river beds, forming deep, narrow canyons. About one million years ago ]s formed at higher elevations. They moved downslope, cutting and sculpting the U-shaped ].<ref name="naturehistory" />
Yosemite is one of the largest and least fragmented ] blocks in the Sierra Nevada, and the park supports a diversity of ]s and ]s. The park has an elevation range from {{convert|2127|to|13114|ft|m}} and contains five major ]: ]/] woodland, ], upper ], ], and ]. Of California's 7,000 plant species, about 50% occur in the Sierra Nevada and more than 20% within Yosemite. There is suitable habitat for more than 160 rare plants in the park, with rare local ] formations and unique ]s characterizing the restricted ranges many of these plants occupy.<ref name = "naturehistory"/>


European American settlers first entered the valley in 1851. Other travelers entered earlier, but ] is credited with discovering the area that became Yosemite National Park.<ref>{{Cite web |title=Yosemite NP: Early History of Yosemite Valley |url=https://www.nps.gov/parkhistory/online_books/yose/kuykendall/sec.htm |access-date=2022-04-21 |website=www.nps.gov |archive-date=February 18, 2022 |archive-url=https://web.archive.org/web/20220218160004/https://www.nps.gov/parkhistory/online_books/yose/kuykendall/sec.htm |url-status=live }}</ref> ] had inhabited the region for nearly 4,000 years, although humans may have first visited as long as 8,000 to 10,000 years ago.<ref>{{Cite book | title=Yosemite: Official National Park Service Handbook |publisher=National Park Service |year=1989 |series=no. 138 |location=Washington, DC |page=102}}</ref><ref name=":1" />
The ] is characterized by granitic rocks and remnants of older rock. About 10 million years ago, the Sierra Nevada was uplifted and then tilted to form its relatively gentle western slopes and the more dramatic eastern slopes. The uplift increased the steepness of stream and river beds, resulting in formation of deep, narrow ]s. About 1 million years ago, ] and ] accumulated, forming ]s at the higher alpine meadows that moved down the river valleys. Ice thickness in Yosemite Valley may have reached {{convert|4000|ft|m}} during the early glacial episode. The downslope movement of the ice masses cut and sculpted the U-shaped valley that attracts so many visitors to its scenic vistas today.<ref name="naturehistory"/>


Yosemite was critical to the development of the concept of national parks. ] and others lobbied to protect Yosemite Valley from development, ultimately leading to President ]'s signing of the Yosemite Grant of 1864 that declared Yosemite as federally preserved land.<ref name="historyculture" /> In 1890, ] led a successful movement to motivate ] to establish Yosemite Valley and its surrounding areas as a National Park. This helped pave the way for the ].<ref name="historyculture" /> Yosemite draws about four million visitors annually.<ref name="visits">{{cite web | url=https://irma.nps.gov/Stats/SSRSReports/Park%20Specific%20Reports/Annual%20Park%20Recreation%20Visitation%20(1904%20-%20Last%20Calendar%20Year) | title=Annual Park Recreation Visitation (1904&nbsp;– Last Calendar Year) | publisher=U.S. National Park Service | access-date=March 11, 2019 | archive-date=June 11, 2019 | archive-url=https://web.archive.org/web/20190611041047/https://irma.nps.gov/Stats/SSRSReports/Park%20Specific%20Reports/Annual%20Park%20Recreation%20Visitation%20(1904%20-%20Last%20Calendar%20Year) | url-status=live }}</ref> Most visitors spend the majority of their time in the valley's {{convert|7|sqmi|km2|spell=in}}.<ref name="naturehistory" /> The park set a visitation record in 2016, surpassing five million visitors for the first time.<ref>{{cite web|title=New visitation record in 2016 as over 5 million people visited Yosemite National Park.|url=http://goldrushcam.com/sierrasuntimes/index.php/news/local-news/8685-new-visitation-record-in-2016-as-over-5-million-people-visited-yosemite-national-park|website=GoldRushCam.com|date=January 13, 2017|publisher=Sierra Sun Times|access-date=February 8, 2017|archive-date=May 25, 2017|archive-url=https://web.archive.org/web/20170525092757/http://goldrushcam.com/sierrasuntimes/index.php/news/local-news/8685-new-visitation-record-in-2016-as-over-5-million-people-visited-yosemite-national-park|url-status=live}}</ref> In 2023, the park saw nearly four million visitors.<ref>{{Cite web |date=2024-03-27 |title=Top 10 most visited national parks |url=https://www.nationalgeographic.com/travel/national-parks/article/most-visited-parks-photos |access-date=2024-03-27 |website=Travel |language=en}}</ref>
The name "Yosemite" (meaning "killer" in ]) originally referred to the name of a renegade tribe which was driven out of the area (and possibly annihilated) by the ]. Before then the area was called "Ahwahnee" ("big mouth") by indigenous people.<ref>{{cite web|title = Origin of the Word Yosemite — What does Yosemite mean? Naming Yosemite Etymology: where did the place name Yosemite come from?|url = http://www.yosemite.ca.us/library/origin_of_word_yosemite.html|website = www.yosemite.ca.us|accessdate = 2015-10-04|first = Dan Anderson, Madison S.|last = Beeler}}</ref>

==Toponym==
The word ''Yosemite'' (derived from ''yohhe'meti,'' "they are killers" in ]) historically referred to the name that the ] gave to the ] People, the resident indigenous tribe.<ref name="Anderson" /><ref>{{cite web |title=Yosemite |url=http://www.etymonline.com/index.php?search=Yosemite&searchmode=none |access-date=September 10, 2010 |work=Online etymology dictionary |archive-date=May 25, 2017 |archive-url=https://web.archive.org/web/20170525092757/http://www.etymonline.com/index.php?search=Yosemite&searchmode=none |url-status=live }}</ref><ref name=":0">{{Cite book |last=Barrett |first=S. A. |title=Myths of the southern sierra miwok. |date=2010 |publisher=Nabu Press |isbn=978-1-177-40758-8 |oclc=944730381}}</ref> Previously, the region had been called "Ahwahnee" ("big mouth") by its only indigenous inhabitants, the Ahwahneechee.<ref name=Anderson>{{cite web|title = Origin of the Word Yosemite|url = http://www.yosemite.ca.us/library/origin_of_word_yosemite.html|website = www.yosemite.ca.us|access-date = October 4, 2015|first1 = Dan|last1 = Anderson|archive-date = January 5, 2007|archive-url = https://web.archive.org/web/20070105223109/http://www.yosemite.ca.us/library/origin_of_word_yosemite.html|url-status = live}}</ref> The term ''Yosemite'' in Miwok is easily confused with a similar term for "grizzly bear", and is still a common misconception.<ref name=Anderson/><ref name=Beeler>{{cite journal|title=Yosemite and Tamalpais|journal=Journal of the American Name Society|volume=3|issue=3|pages=185–86|year=1955|first=Madison Scott|last=Beeler}}</ref>


==History== ==History==
{{Main article|History of the Yosemite area}} {{Main|History of the Yosemite area}}


===Ahwahneechee and the Mariposa Wars=== ===Ahwahneechee and the Mariposa Wars===
{{multiple image {{multiple image
| align = right | align = right
| direction = horizontal | direction = horizontal
| header_align = center | header_align = center
| header = | header =
| image1 = Miwok-Paiute ceremony in 1872 at current site of Yosemite Lodge.jpeg | image1 = Miwok-Paiute ceremony in 1872 at current site of Yosemite Lodge.jpeg
| width1 = 195 | width1 = 195
| alt1 = | alt1 =
| caption1 = ] ceremony (1872) | caption1 = ] ceremony (1872)
| image2 = Lafayette Bunnell 1880.jpg | image2 = Lafayette Bunnell 1880.jpg
| width2 = 160 | width2 = 160
| alt2 = engraving of Dr Lafayette Bunnell, showing him as an older man with a craggy face, short bristly hair and a cropped grey beard. | alt2 = engraving of Dr Lafayette Bunnell, showing him as an older man with a craggy face, short bristly hair and a cropped grey beard.
| caption2 =Dr. ] gave Yosemite Valley its name. | caption2 = ] gave Yosemite Valley its name.
}} }}


The indigenous natives of Yosemite called themselves the ], meaning "dwellers" in Ahwahnee.<ref>{{Cite book |last=Runte |first=Alfred |url=https://archive.org/details/yosemiteembattle00runt |title=Yosemite: The Embattled Wilderness |publisher=University of Nebraska Press |year=1990 |isbn=0803238940 |pages=Chapter 1}}</ref> The Ahwahneechee People were the only tribe that lived within the park boundaries, but other tribes lived in surrounding areas. Together they formed a larger Indigenous population in California, called the ]<ref name="Spence">{{cite journal |last1=Spence |first1=Mark |date=1996 |title=Dispossesing the Wilderness: Yosemite Indians and the National Park Ideal, 1864–1930 |journal=Pacific Historical Review |volume=65 |issue=1 |pages=27–59 |doi=10.2307/3640826 |issn=0030-8684 |jstor=3640826}}</ref> They are related to the Northern ] and ] tribes. Other tribes like the Central ] and the ], who both lived in the ] and central California, visited Yosemite to trade and intermarry.{{sfn|Greene|1987|p=78}} This resulted in a blending of culture that helped preserve their presence in Yosemite after early American settlements and urban development threatened their survival.<ref name="Spence" /> Vegetation and game in the region were similar to modern times; acorns were a dietary staple, as well as other seeds and plants, salmon and deer.<ref name="Spence" />
As revealed by archeological finds, the Yosemite Valley has been inhabited for nearly 3,000 years, though humans may have first visited the area as long as 8,000 to 10,000 years ago.<ref>{{Cite book|title = Yosemite: Official National Park Service Handbook|last = NPS contributors|first = |publisher = National Park Service.|year = 1989|isbn = |location = Washington, D.C|page = 102|series = no. 138}}</ref> The indigenous natives called themselves the ], meaning "dwellers in Ahwahnee."<ref>{{Cite book|title = Yosemite: The Embattled Wilderness|last = Runte|first = Alfred|publisher = University of Nebraska Press|year = 1990|isbn = 0-8032-3894-0|location = |pages = Chapter 1}}</ref> They are related to the Northern ] and ] tribes. Many tribes visited the area to trade, including nearby Central ], who lived along the drainage area of the ] and ] Rivers.{{sfn|Greene|1987|p=57}} A major trading route went over Mono Pass and through ] to ], just to the east of the Yosemite area. Vegetation and game in the region was similar to that present today; acorns were a staple to their diet, as well as other seeds and plants, salmon and deer.<ref>{{cite web|url = http://www.gorp.com/parks-guide/travel-ta-yosemite-hiking-california-sidwcmdev_056853.html|archiveurl = https://web.archive.org/web/20140528045059/http://www.gorp.com/parks-guide/travel-ta-yosemite-hiking-california-sidwcmdev_056853.html|archivedate = 2014-05-28|title = The Living Yosemite—The Ahwahnechee (One Hundred Hikes in Yosemite)|date = 29 Apr 2002|accessdate = 27 May 2014|website = Great Outdoor Recreation Pages|publisher = |last = Schaffer|first = Jeffrey P.}}</ref>


The 1848–1855 ] was a major event impacting the native population. It drew more than 90,000 European Americans to the area in 1849, causing competition for resources between gold miners and residents.<ref>{{cite book |editor-last1=Starr |editor-first1=Kevin |editor-last2=Orsi |editor-first2=Richard J |year=2000 |title=Rooted in Barbarous Soil: People, Culture, and Community in Gold Rush California |publisher=University of California Press |location=Berkeley and Los Angeles |isbn=978-0-520-22496-4 |page=57 }}</ref> About 70 years before the Gold Rush, the indigenous population was estimated to be 300,000, quickly dropping to 150,000, and just ten years later, only about 50,000 remained.<ref name=":1" /> The reasons for such a decline included disease, birth rate decreases, starvation, and conflict. The conflict in Yosemite, which is known as the ], was part of the ], which was the systemic killing of indigenous peoples throughout the State between the 1840s and 1870s.<ref name="Adhikari">{{cite book |last=Adhikari |first=Mohamed |date=25 July 2022 |title=Destroying to Replace: Settler Genocides of Indigenous Peoples |url=https://books.google.com/books?id=ht9dEAAAQBAJ |location=Indianapolis |publisher=Hackett Publishing Company |pages=72–115 |isbn=978-1647920548 |access-date=March 21, 2023 |archive-date=March 26, 2023 |archive-url=https://web.archive.org/web/20230326164810/https://books.google.com/books?id=ht9dEAAAQBAJ |url-status=live }}</ref> It started in December 1850 when California funded a state militia to drive Native people from contested territory to suppress Native American resistance to the European American influx.<ref name="miwuk">{{cite web |title=Who We Are |url=https://www.southernsierramiwuknation.org/about-2 |access-date=July 23, 2021 |publisher=Southern Sierra Miwuk Nation |archive-date=August 6, 2021 |archive-url=https://web.archive.org/web/20210806040156/https://www.southernsierramiwuknation.org/about-2 |url-status=live }}</ref>
The ] in the mid-19th century dramatically increased travel by European-Americans in the area, causing competition for resources between the regional Paiute and Miwok and the miners and hangers on. In 1851 as part of the Mariposa Wars intended to suppress Native American resistance, ] Major ] led the ] into the west end of Yosemite Valley. He was pursuing forces of around 200 Ahwahneechee led by ].<ref name="GeologyNP326">{{harvnb|Harris|1998|p=326}}</ref>


Yosemite tribes often stole from settlers and miners, sometimes killing them, in retribution for the extermination/domestication of their people, and loss of their lands and resources.<ref name=":1" /> The War and formation of the ] was partially the result of a single incident involving ], a ] trader whose trading post was attacked in December, 1850. After the incident, Savage rallied other miners and gained the support of local officials to pursue a war against the Natives. He was appointed ] Major and leader of the Mariposa Battalion in the beginning of 1851.<ref name=":1" /> He and Captain John Boling were responsible for pursuing the Ahwahneechee people, led by ] and driving them west, and out of Yosemite.<ref>{{Cite web |title=Sketch of Yosemite National Park and an Account of the Origin of the Yosemite and Hetch Hetchy Valleys (History of Yosemite National Parkr) |url=https://www.nps.gov/parkhistory/online_books/yose/matthes/sec1.htm |access-date=2022-04-19 |website=www.nps.gov |archive-date=July 4, 2022 |archive-url=https://web.archive.org/web/20220704055441/https://www.nps.gov/parkhistory/online_books/yose/matthes/sec1.htm |url-status=live }}</ref><ref name=":1" /> In March 1851 under Savage's command, the Mariposa Battalion captured about 70 Ahwahneechee and planned to take them to a reservation in Fresno, but they escaped. Later in May, under the command of Boling, the battalion captured 35 Ahwahneechee, including Chief Tenaya, and marched them to the reservation. Most were allowed to eventually leave and the rest escaped.<ref name=":1" /> Tenaya and others fled across the ] and settled with the ]. Tenaya and some of his companions were ultimately killed in 1853 either over stealing horses or a gambling conflict. The survivors of Tenaya's group and other ] were absorbed into the Mono Lake Paiute tribe.<ref name=":1" /><ref name=":2">{{Cite web |last=Bingaman |first=John W. |date=1966 |title=The Ahwahneechees: A Story of the Yosemite Indians |url=https://www.yosemite.ca.us/library/the_ahwahneechees/chapter_1.html |access-date=April 11, 2022 |website=yosemite.ca.us |archive-date=June 23, 2022 |archive-url=https://web.archive.org/web/20220623094147/http://www.yosemite.ca.us/library/the_ahwahneechees/chapter_1.html |url-status=live }}</ref><ref name=":3">{{cite web |last1=Godfrey |first1=Elizabeth |title=Yosemite Indians; Yesterday and Today |url=http://www.yosemite.ca.us/library/yosemite_indians/history.html |access-date=26 August 2021 |website=Yosemite Indians |archive-date=February 19, 2020 |archive-url=https://web.archive.org/web/20200219202803/http://www.yosemite.ca.us/library/yosemite_indians/history.html |url-status=live }}</ref>
Accounts from this battalion were the first well-documented reports of ethnic Europeans entering Yosemite Valley. Attached to Savage's unit was Dr. ], the company ], who later wrote about his awestruck impressions of the valley in ''The Discovery of the Yosemite''. Bunnell is credited with naming Yosemite Valley, based on his interviews with Chief Tenaya. Bunnell wrote that Chief Tenaya was the founder of the ].<ref name="Bunnell17">{{cite book | title = Discovery of the Yosemite and the Indian War of 1851 Which Led to That Event | last= Bunnell | first= Lafayette H.| url= http://www.yosemite.ca.us/library/discovery_of_the_yosemite/17.html| archiveurl= http://www.webcitation.org/69H6QuTpJ| archivedate= 2012-07-19 | chapter=Chapter 17 | publisher = F.H. Revell | year = 1892 | accessdate=January 27, 2007 | isbn =0-939666-58-8 }}</ref> The ], a neighboring tribe, and most white settlers considered the Ahwahneechee to be especially violent because of their frequent territorial disputes. The Miwok term for the Pai-Ute band was ''yohhe'meti,'' meaning "they are killers".<ref>{{cite web | url= http://www.yosemite.ca.us/library/origin_of_word_yosemite.html | archiveurl= http://www.webcitation.org/5yUgegp1j | archivedate= 2011-05-07 | title= Origin of the Word Yosemite | last=Anderson| first=Daniel E. | publisher = The Yosemite Web |date=July 2005 |accessdate = January 27, 2007 }}</ref><ref>{{cite web|url=http://www.etymonline.com/index.php?search=Yosemite&searchmode=none|title=Yosemite|work=Online etymology dictionary|accessdate=September 10, 2010}}</ref> Correspondence and articles written by members of the battalion helped to popularize the natural wonders of the Yosemite Valley and the surrounding area.
]
Accounts from this battalion were the first well-documented reports of European Americans entering Yosemite Valley. Attached to Savage's unit was Doctor ], who later wrote about his awestruck impressions of the valley in ''The Discovery of the Yosemite''. Bunnell is credited with naming Yosemite Valley, based on his interviews with Chief Tenaya. Bunnell wrote that Chief Tenaya was the founder of the Ahwahnee colony.<ref name="Bunnell17">{{cite book|title=Discovery of the Yosemite and the Indian War of 1851 Which Led to That Event |last=Bunnell |first=Lafayette H. |url=http://www.yosemite.ca.us/library/discovery_of_the_yosemite/17.html |archive-url=https://web.archive.org/web/20121005171611/http://www.yosemite.ca.us/library/discovery_of_the_yosemite/17.html |archive-date=October 5, 2012 |chapter=Chapter 17 |publisher=F.H. Revell |year=1892 |access-date=January 27, 2007 |isbn=0939666588 |url-status=dead }}</ref> Bunnell falsely believed that the word "Yosemite" meant "full-grown grizzly bear".<ref>{{cite book|title=Discovery of the Yosemite and the Indian War of 1851 Which Led to That Event |last=Bunnell |first=Lafayette H.}}</ref>


===Indigenous peoples' continuing presence ===
Chief Tenaya and his Ahwahneechee were eventually captured and their village burned; they were removed to a ] near ]. The chief and some others were later allowed to return to Yosemite Valley. In the spring of 1852 they attacked a group of eight gold ], and then moved east to flee law enforcement.<ref name="Schaffer46">{{harvnb|Schaffer|1999|p=46}}</ref> Near Mono Lake, they took refuge with the nearby ] of Paiute. They stole horses from their hosts and moved away, but the Mono Paiutes tracked down and killed many of the Ahwahneechee, including Chief Tenaya. The Mono Paiute took the survivors as captives back to Mono Lake and absorbed them into the ] tribe.
] and ] Native American artist from the Yosemite region|163x163px]]
After the ], Native Americans continued to live in the Yosemite area in reduced numbers. The remaining Yosemite ] tribe members there were forced to relocate to a village constructed in 1851 by the state government.<ref name=":1" /> They learned to live within this camp and their limited rights, adapting to the changed environment by entering the tourism industry through employment and small businesses, manufacturing and selling goods and providing services.<ref name="Spence" /> In 1953, the National Park Service banned all non-employee Natives from residing in the Park and evicted the non-employees who had residence. In 1969, with only a few families left in the Park, the National Park Service evicted the remaining Native people living within the Park (all Park employees and their families) to a government housing area for park employees and destroyed the village as part of a fire-fighting exercise.<ref name="SpenceBookChapter8">{{cite book |last1=Spence |first1=Mark David |title=Dispossessing the wilderness: Indian removal and the making of the national parks |chapter=Yosemite Indians and the National Park Ideal, 1916-1969 |date=1999 |pages=115–132 |chapter-url=https://archive.org/details/dispossessingwil0000spen/page/114/mode/2up?view=theater |access-date=3 April 2024}}</ref><ref name="miwuk" /> A reconstructed "Indian Village of Ahwahnee" sits behind the ], located next to the Yosemite Valley Visitor Center.<ref>{{cite web |title=Indian Village of the Ahwahnee – Yosemite National Park (U.S. National Park Service) |url=https://www.nps.gov/yose/learn/historyculture/yosemite-indians.htm |access-date=1 March 2021 |archive-date=March 2, 2021 |archive-url=https://web.archive.org/web/20210302223136/https://www.nps.gov/yose/learn/historyculture/yosemite-indians.htm |url-status=live }}</ref><ref>{{cite web |title=Yosemite Indians – Yosemite National Park (U.S. National Park Service) |url=https://www.nps.gov/yose/learn/historyculture/indian-village-of-the-ahwahnee.htm |access-date=1 March 2021 |archive-date=February 21, 2021 |archive-url=https://web.archive.org/web/20210221140746/https://www.nps.gov/yose/learn/historyculture/indian-village-of-the-ahwahnee.htm |url-status=live }}</ref><ref>{{cite web |title=Yosemite Valley map |url=https://www.nps.gov/carto/hfc/carto/media/YOSEmap2.pdf |archive-url=https://web.archive.org/web/20181012171335/https://www.nps.gov/carto/hfc/carto/media/YOSEmap2.pdf |archive-date=2018-10-12 |url-status=live |access-date=1 March 2021}}</ref>


By the late 19th century, the population of all native inhabitants in Yosemite was difficult to determine, estimates ranged from thirty to several hundred. The Ahwahneechee people and their descendants were hard to identify.<ref name=":1">{{Cite book|last=Solnit|first=Rebecca|url=https://www.worldcat.org/oclc/876343009|title=Savage Dreams: a Journey into the Hidden Wars of the American West.|date=2014|publisher=]|isbn=978-0-520-95792-3|location=Berkeley|oclc=876343009|access-date=February 22, 2022|archive-date=February 5, 2024|archive-url=https://web.archive.org/web/20240205174233/https://search.worldcat.org/title/876343009|url-status=live}}</ref> The last full-blooded Ahwahneechee died in 1931. Her name was Totuya, or Maria Lebrado. She was the granddaughter of Chief ] and one of many forced out of her ancestral homelands.<ref name=":1" /><ref name="miwuk" /> The Ahwahneechee live through the memory of their descendants, their fellow Yosemite Natives, and through the Yosemite exhibit in the ] and the Yosemite Museum.<ref name=":1" /> As a method of self-preservation and resilience, the Indigenous people of California proposed treaties in 1851 and 1852 that would have established land reservations for them, but Congress refused to ratify them.<ref name=":1" /> The Southern Sierra Miwuk Nation is seeking tribal sovereignty and federal recognition.<ref name="miwuk" /><ref name=":4">{{Cite web |title=Federal Recognition {{!}} Southern Sierra Miwuk Nation |url=https://www.southernsierramiwuknation.org/federal-recognition |access-date=2022-04-21 |website=SouthernSierra Miwuk |language=en |archive-date=April 21, 2022 |archive-url=https://web.archive.org/web/20220421080511/https://www.southernsierramiwuknation.org/federal-recognition |url-status=live }}</ref> The National Park Service created policies to protect sacred sites and allow Native People to return to their homelands and use National Park resources.<ref name=":4" /><ref>{{Cite book |first=Jeanette |last=Wolfley |url=http://worldcat.org/oclc/1305864036 |title=Reclaiming a presence in ancestral lands : the return of Native Peoples to the National Parks |date=2016 |publisher= |oclc=1305864036 |access-date=April 21, 2022 |archive-date=February 5, 2024 |archive-url=https://web.archive.org/web/20240205174241/https://search.worldcat.org/title/1305864036 |url-status=live }}</ref>
A reconstructed "Indian Village of Ahwahnee" has been erected behind the ], located next to the Yosemite Valley Visitor Center.


===Early tourists=== ===Early tourists===
{{multiple image {{multiple image
| align = right | align = right
| direction = horizontal | direction = horizontal
| header_align = center | header_align = center
| header = | header =
| image1 = 30. The dead giant.jpg | image1 = 30. The dead giant.jpg
| width1 = 194 | width1 = 194
| alt1 = | alt1 =
| caption1 = The Dead Giant, c.1870 | caption1 = The Dead Giant ({{circa|1870s}})
| image2 = 8. The vernal fall, Yosemite valley.jpg | image2 = 8. The vernal fall, Yosemite valley.jpg
| width2 = 188 | width2 = 188
| alt2 = | alt2 =
| caption2 = ] (c. 1889) | caption2 = ] ({{circa|1870s}})
}} }}
{{multiple image
In 1855, entrepreneur ], artist ] and two others were the first to tour the area.<ref name="GeologyNP326"/> Hutchings and Ayres were responsible for much of the earliest publicity about Yosemite, writing articles and ].{{sfn|Wuerthner|1994|p=20}} Ayres' style in art was highly detailed with exaggerated angularity. His works and written accounts were distributed nationally, and an art exhibition of his drawings was held in New York City. Hutchings' publicity efforts between 1855 and 1860 led to an increase in tourism to Yosemite.<ref>{{cite web|url=http://xroads.virginia.edu/~MA96/RAILROAD/yosemite.html|title=Discovery and Invention in the Yosemite|work=The Role of Railroads in Protecting, Promoting, and Selling Yellowstone and Yosemite National Parks|first=J.S.|last=Johns|publisher=University of Virginia|year=1996}}</ref>
| align = right

| direction = horizontal
] was an Indian encampment in what is now the southwestern part of the park. Settler ] discovered the ] of ] in Wawona in 1857. He had simple lodgings built, and roads to the area. In 1879, the ] was built to serve tourists visiting Mariposa Grove. As tourism increased, so did the number of trails and hotels developed by people intending to build on the trade.

The ], also known as the Tunnel Tree, was a famous giant sequoia that stood in the Mariposa Grove. It was {{convert|227|ft|m}} tall, and was {{convert|90|ft|m|abbr=on}} in circumference. When a carriage-wide tunnel was cut through the tree in 1881, it became even more popular as a tourist photo attraction. Everything from horse-drawn carriages in the late 19th century, to automobiles in the first part of the 20th century, traveled the road which passed through that tree. The Wawona Tree fell in 1969 under a heavy load of snow. It was estimated to have been 2,300 years old.
{{multiple image
| align = right
| direction = horizontal
| header_align = center | header_align = center
| header = | header =
| image1 = Wawona Hotel.jpg | image1 = Wawona Hotel.jpg
| width1 = 252 | width1 = 252
| alt1 = | alt1 =
| caption1 =The ] | caption1 = The ] (1985)
| image2 = Mother Curry in front of Camp Curry.jpeg | image2 = Mother Curry in front of Camp Curry.jpeg
| width2 = 130 | width2 = 130
| alt2 = Woman in a long dress in front of a sign across a road. Wooden letters read "Camp Curry". | alt2 = Woman in a long dress in front of a sign across a road. Wooden letters read "Camp Curry".
| caption2 = Jennie Curry in front of Camp Curry, circa 1900 | caption2 = Jennie Curry in front of Camp Curry ({{circa|1900}})
}} }}
In 1855, entrepreneur ], artist ] and two others were the first tourists to visit.<ref name="GeologyNP326">{{harvnb|Harris|1998|p=326}}</ref> Hutchings and Ayres were responsible for much of Yosemite's earliest publicity, writing articles and ] about the valley.{{sfn|Wuerthner|1994|p=20}} Ayres' style was detailed with exaggerated angularity. His works and written accounts were distributed nationally, and an exhibition of his drawings was held in New York City. Hutchings' publicity efforts between 1855 and 1860 increased tourism to Yosemite.<ref>{{cite web|url=http://xroads.virginia.edu/~MA96/RAILROAD/yosemite.html|title=Discovery and Invention in the Yosemite|work=The Role of Railroads in Protecting, Promoting, and Selling Yellowstone and Yosemite National Parks|first=J.S.|last=Johns|publisher=University of Virginia|year=1996|access-date=August 20, 2010|archive-date=March 3, 2016|archive-url=https://web.archive.org/web/20160303200437/http://xroads.virginia.edu/~MA96/RAILROAD/yosemite.html|url-status=dead}}</ref> Natives supported the growing tourism industry by working as laborers or maids. Later, they performed dances for tourists, acted as guides, and sold handcrafted goods, notably woven baskets.<ref name="Spence" /> The Indian village and its peoples fascinated visitors, especially James Hutchings who advocated for Yosemite tourism. He and others considered the indigenous presence to be one of Yosemite's greatest attractions.<ref name="Spence" />
Yosemite's first concession was established in 1884 when John Degnan and his wife established a bakery and store.{{sfn|NPS|1989|p=58}} In 1916, the National Park Service granted a 20-year concession to the Desmond Park Service Company. It bought out or built hotels, stores, camps, a dairy, a garage, and other park services.{{sfn|Greene|1987|p=360}} Desmond changed its name to the Yosemite National Park Company in December 1917 and was reorganized in 1920.{{sfn|Greene|1987|pp=362, 364}}


] was an early Indian encampment for Nuchu and Ahwahneechee people who were captured and relocated to a reservation on the Fresno River by Savage and the Mariposa Battalion in March 1851.<ref>{{Cite web |last=Sargent |first=Shirley |date=1961 |title=Wawona's Yesterdays |url=https://www.yosemite.ca.us/library/wawonas_yesterdays/indians.html |access-date=April 14, 2022 |archive-date=June 17, 2022 |archive-url=https://web.archive.org/web/20220617221051/http://www.yosemite.ca.us/library/wawonas_yesterdays/indians.html |url-status=live }}</ref> ] discovered the ] of ] in Wawona in 1857. He had simple lodgings and roads built. In 1879, the ] was built to serve tourists visiting Mariposa Grove.<ref>{{cite book |title=Wawona Hotel Complex Cultural Landscape Report , Yosemite National Park |date=August 2012 |publisher=Mundus Bishop for National Park Service |pages=15}}</ref> As tourism increased, so did the number of trails and hotels to build on it.<ref>{{cite book |last1=Schaffer |first1=Jeffrey |title=Yosemite National Park: A complete hiker's guide |date=June 2006 |publisher=Wilderness Press |location=Berkeley, CA |isbn=0899973833 |page=11 |edition=5 |url=https://books.google.com/books?id=Z4fSi0EjFHoC |access-date=31 August 2021 |archive-date=June 27, 2023 |archive-url=https://web.archive.org/web/20230627231037/https://books.google.com/books?id=Z4fSi0EjFHoC |url-status=live }}</ref>
The Curry Company had been started in 1899 by David and Jennie Curry to provide concessions in the park. They also founded Camp Curry, formerly known as ], now known as Half Dome Village.{{sfn|Wuerthner|1994|p=40}} The Currys lobbied reluctant park supervisors to allow expansion of concession operations and development in the area.


The ], also known as the ], was a ] that grew in the ]. It was {{convert|234|ft|m}} tall, and was {{convert|90|ft|m|abbr=on}} in circumference. When a carriage-wide tunnel was cut through the tree in 1881, it became even more popular as a tourist photo attraction. Carriages and automobiles traversed the road that passed through the tree. The tree was permanently weakened by the tunnel, and it fell in 1969 under a heavy load of snow. It was estimated to have been 2,100 years old.<ref>{{cite web |title=The Myth of the Tree You Can Drive Through |url=https://www.nps.gov/seki/faqtunnel.htm |website=nps.gov |publisher=National Park Service |access-date=26 August 2021 |archive-date=August 27, 2021 |archive-url=https://web.archive.org/web/20210827150438/https://www.nps.gov/seki/faqtunnel.htm |url-status=live }}</ref>
Administrators in the National Park Service felt that limiting the number of concessionaires in each national park would be more financially sound. The Curry Company and its rival, the Yosemite National Park Company, were forced to merge in 1925 to form the ] (YP&CC).{{sfn|Greene|1987|p=387}} The company built the ] in 1927.

Yosemite's first concession was established in 1884 when John Degnan and his wife established a bakery and store.{{sfn|NPS|1989|p=58}} In 1916, the National Park Service granted a 20-year concession to the Desmond Park Service Company. It bought out or built hotels, stores, camps, a dairy, a garage, and other park facilities.{{sfn|Greene|1987|p=360}} The ] was completed in 1908 by a subsidiary of the ]. It was located at ] just outside of Yosemite.<ref>{{Cite book|title=Yosemite Valley Railroad|last=Radanovich|first=Leroy|publisher=Arcadia Publishing Incorporated|year=2010|url=https://books.google.com/books?id=0BqfELO5QsQC|page=|isbn=9781439640333|access-date=2021-12-27|archive-date=April 9, 2023|archive-url=https://web.archive.org/web/20230409043107/https://books.google.com/books?id=0BqfELO5QsQC|url-status=live}}</ref>{{sfn|Greene|1987|pp=362, 364}}

The Curry Company started in 1899, led by David and Jennie Curry to provide concessions. They founded Camp Curry, now ].{{sfn|Wuerthner|1994|p=40}}

Park service administrators felt that limiting the number of concessionaires in the park would be more financially sound. The Curry Company and its rival, the Yosemite National Park Company, were forced to merge in 1925 to form the ] (YP&CC).{{sfn|Greene|1987|p=387}} The company built the ] in 1926–27.<ref>{{cite journal|author=Gene Rose |title=The Ahwahnee: Yosemite Grandeur |journal=Skiing Heritage Journal |url=https://archive.org/details/bub_gb_x1gEAAAAMBAJ|date=March 2003|publisher=International Skiing History Association|pages=|issn=1082-2895}}</ref>


===Yosemite Grant=== ===Yosemite Grant===
] ], photographed by photographer ] in 1872.]]
Concerned by the effects of commercial interests, prominent citizens including Galen Clark and Senator ] advocated for protection of the area. A park bill was prepared with the assistance of the ] in the ].<ref>{{cite journal | title = Yosemite: The Story of an Idea |author=Huth, Hans| work=Sierra Club Bulletin |publisher = Sierra Club |issue=33 |pages=63–76| url = http://www.yosemite.ca.us/library/yosemite_story_of_an_idea.html| archiveurl = http://www.webcitation.org/69H6SI60H| archivedate = 2012-07-19 |date=March 1948 |accessdate = April 20, 2011 }}</ref> The bill passed both houses of the ], and was signed by ] ] on June 30, 1864, creating the Yosemite Grant.<ref name="Schaffer48">{{harvnb|Schaffer|1999|p=48}}</ref><ref>{{cite book|chapter-url=http://constitution.org/uslaw/sal/013_statutes_at_large.pdf|page=325|chapter=Thirty-Eighth Congress, Session I, Chap. 184 (June 30, 1864): An Act authorizing a Grant to the State of California of the "Yo-Semite Valley" and of the Land embracing the "Mariposa Big Tree Grove"|title=], Treaties, and Proclamations of the United States of America from December 1863, to December 1865|editor=]|volume=13|location=Boston|publisher=Little, Brown and Company|year=1866}}</ref> This is the first instance of park land being set aside specifically for preservation and public use by action of the U.S. federal government, and set a precedent for the 1872 creation of ] as the first ].<ref name = "historyculture">{{cite web | title = History & Culture | publisher = United States National Park Service: Yosemite National Park | url = http://www.nps.gov/yose/historyculture/index.htm | accessdate = January 27, 2007 }}</ref> Yosemite Valley and the Mariposa Grove were ceded to ] as a ], and a board of commissioners was proclaimed two years later. Concerned by the impact of commercial interests, citizens including ] and Senator ] advocated protection for the area.<ref>{{cite journal|title=Yosemite: The Story of an Idea |author=Huth, Hans |journal=Sierra Club Bulletin |publisher=Sierra Club |issue=33 |pages=63–76 |url=http://www.yosemite.ca.us/library/yosemite_story_of_an_idea.html |archive-url=https://web.archive.org/web/20120508220101/http://www.yosemite.ca.us/library/yosemite_story_of_an_idea.html |archive-date=May 8, 2012 |date=March 1948 |access-date=April 20, 2011 |url-status=dead }}</ref> The ] passed legislation that was signed by ] ] on June 30, 1864, creating the Yosemite Grant.<ref name="Schaffer48">{{harvnb|Schaffer|1999|p=48}}</ref><ref>{{cite book|chapter-url=http://constitution.org/uslaw/sal/013_statutes_at_large.pdf|page=325|chapter=Thirty-Eighth Congress, Session I, Chap. 184 (June 30, 1864): An Act authorizing a Grant to the State of California of the "Yo-Semite Valley" and of the Land embracing the "Mariposa Big Tree Grove"|title=], Treaties, and Proclamations of the United States of America from December 1863, to December 1865|editor=]|volume=13|location=Boston|publisher=Little, Brown and Company|year=1866|url-status=dead|archive-url=https://web.archive.org/web/20111116010746/http://constitution.org/uslaw/sal/013_statutes_at_large.pdf|archive-date=November 16, 2011}}</ref> This is the first time land was set aside specifically for preservation and public use by the U.S. government, and set a precedent for the 1872 creation of ] national park, the nation's first.<ref name = "historyculture">{{cite web | title = History & Culture | publisher = United States National Park Service: Yosemite National Park | url = http://www.nps.gov/yose/historyculture/index.htm | access-date = January 27, 2007 | archive-date = May 2, 2007 | archive-url = https://web.archive.org/web/20070502182407/http://www.nps.gov/yose/historyculture/index.htm | url-status = live }}</ref> Yosemite Valley and the ] were ceded to ] as a ], and a board of commissioners was established two years later.<ref>{{Cite web|url=http://www.150.parks.ca.gov/?page_id=27539|title=Yosemite "State Park"|website=www.150.parks.ca.gov|access-date=April 30, 2021|archive-date=October 16, 2020|archive-url=https://web.archive.org/web/20201016155602/http://www.150.parks.ca.gov/?page_id=27539|url-status=live}}</ref>


Galen Clark was appointed by the commission as the Grant's first guardian, but neither Clark nor the commissioners had the authority to evict ] (which included Hutchings).<ref name="Schaffer48"/> The issue was not settled until 1872 when the homesteader land holdings were invalidated by the U.S. Supreme Court.<ref>''Hutchings v. Low'' {{ussc|82|77|1872}}</ref> Clark and the reigning commissioners were ousted in 1880, this dispute also reaching the Supreme Court in 1880.<ref>''Ashburner v. California'' {{ussc|103|575|1880}}</ref> The two Supreme Court decisions affecting management of the Yosemite Grant are considered important precedents in land management law.<ref>Alfred Runte. 1990. Yosemite. The Embattled Wilderness. University of Nebraska Press.</ref> Hutchings became the new park guardian.<ref name="Schaffer49"/> Galen Clark was appointed by the commission as the Grant's first guardian, but neither Clark nor the commissioners had the authority to evict ] (which included Hutchings).<ref name="Schaffer48"/> The issue was not settled until 1872 when the homesteader land holdings were invalidated by the U.S. Supreme Court.<ref>''Hutchings v. Low'' {{ussc|82|77|1872}}</ref> Clark and the commissioners were ousted in a dispute that reached the Supreme Court in 1880.<ref>''Ashburner v. California'' {{ussc|103|575|1880}}</ref> The two Supreme Court decisions affecting management of the Yosemite Grant are considered precedents in land management law.<ref>{{cite book |first=Alfred |last=Runte |year=1990 |title=Yosemite : The Embattled Wilderness |url=https://archive.org/details/yosemiteembattle00runt |url-access=registration |location=Lincoln |publisher=University of Nebraska Press |isbn=0803289413 |pages=34–35, 50}}</ref> Hutchings became the new park guardian.<ref name="Schaffer49"/>


Access to the park by tourists improved in the early years of the park, and conditions in the Valley were made more hospitable. Tourism significantly increased after the ] was completed in 1869, but the long horseback ride to reach the area was a deterrent.<ref name="Schaffer48"/> Three ] roads were built in the mid-1870s to provide better access for the growing number of visitors to Yosemite Valley. Tourist access to the park improved, and conditions in the Valley became more hospitable. Tourism significantly increased after the ] was completed in 1869, while the long horseback ride to reach the area was a deterrent.<ref name="Schaffer48"/> Three ] roads were built in the mid-1870s to provide better access for the growing number of visitors.<ref>{{cite book|url=https://www.yosemite.ca.us/library/olmsted/report.html|title=Yosemite and the Mariposa Grove: A Preliminary Report|year=1865|first=Frederick|last=Law Olmsted|access-date=September 1, 2021|archive-date=May 29, 2021|archive-url=https://web.archive.org/web/20210529082917/http://www.yosemite.ca.us/library/olmsted/report.html|url-status=live}}</ref>


John Muir was a Scottish-born American naturalist and explorer. It was because of Muir that many National Parks were left untouched, such as Yosemite Valley National Park. One of the most significant camping trips Muir took was in 1903 with then president Theodore Roosevelt. This trip persuaded Roosevelt to return "Yosemite Valley and Mariposa Grove to federal protection as part of Yosemite National Park".<ref>{{cite web|url=http://www.pbs.org/nationalparks/people/historical/muir/|work=The National Parks: America's Best Idea|title=People - John Muir |publisher=PBS}}</ref> ] was a Scottish-born American naturalist and explorer. Muir's leadership ensured that many National Parks were left untouched, including Yosemite.<ref>{{cite web|url=https://www.pbs.org/nationalparks/people/historical/muir/|work=The National Parks: America's Best Idea|title=People&nbsp;– John Muir|publisher=PBS|access-date=September 18, 2017|archive-date=September 23, 2017|archive-url=https://web.archive.org/web/20170923104845/http://www.pbs.org/nationalparks/people/historical/muir/|url-status=live}}</ref>


] wrote articles popularizing the area and increasing scientific interest in it. Muir was one of the first to theorize that the major landforms in Yosemite Valley were created by large alpine ]s, bucking established scientists such as ], who regarded Muir as an amateur.<ref name="Schaffer49">{{harvnb|Schaffer|1999|p=49}}</ref> Muir wrote scientific papers on the area's biology. Landscape architect ] emphasized the importance of conservation of Yosemite Valley. Muir wrote articles popularizing the area and increasing scientific interest in it. Muir was one of the first to theorize that the major landforms in Yosemite Valley were created by alpine glaciers, bucking established scientists such as ].<ref name="Schaffer49">{{harvnb|Schaffer|1999|p=49}}</ref> Muir wrote scientific papers on the area's biology. Landscape architect ] emphasized the importance of conservation of Yosemite Valley.<ref>{{cite web |last1=Olmsted |first1=Frederick Law |title=Olmsted Report on Management of Yosemite, 1865 |url=https://www.nps.gov/parkhistory/online_books/anps/anps_1b.htm |website=National Park Service |access-date=1 September 2021 |archive-date=August 12, 2021 |archive-url=https://web.archive.org/web/20210812125501/https://www.nps.gov/parkhistory/online_books/anps/anps_1b.htm |url-status=live }}</ref>


===Increased protection efforts=== ===Increased protection efforts===
{{multiple image {{multiple image
| align = right | align = right
| direction = horizontal | direction = horizontal
| header_align = center | header_align = center
| header = | header =
| image1 = Galen Clark in the Big Tree Grove.jpeg | image1 = Galen Clark in the Big Tree Grove.jpeg
| width1 = 150 | width1 = 150
| alt1 = | alt1 =
| caption1 =Early settler, ] | caption1 = Early settler, ]
| image2 = Muir and Roosevelt restored.jpg | image2 = Muir and Roosevelt restored.jpg
| width2 = 170 | width2 = 170
| alt2 = | alt2 =
| caption2 = ] and ] on Glacier Point | caption2 = ] and ] on Glacier Point
}} }}


Overgrazing of ]s (especially by ]), ] of giant sequoia, and other damage caused Muir to become an advocate for further protection. Muir convinced prominent guests of the importance of putting the area under federal protection; one such guest was ], editor of '']''. Muir and Johnson lobbied Congress for the Act that created Yosemite National Park on October 1, 1890.<ref name="Schaffer50">{{harvnb|Schaffer|1999|p=50}}</ref> The State of California, however, retained control of Yosemite Valley and Mariposa Grove. Muir also helped persuade local officials to virtually eliminate grazing from the Yosemite high country. ] of meadows (especially by sheep), logging of giant sequoia, and other damage led Muir to become an advocate for further protection. Muir convinced prominent guests of the importance of putting the area under federal protection. One such guest was ], editor of '']''. Muir and Johnson lobbied Congress for the Act that created Yosemite National Park on October 1, 1890.<ref name="Schaffer50">{{harvnb|Schaffer|1999|p=50}}</ref> The State of California, however, retained control of Yosemite Valley and Mariposa Grove. Muir's writings raised awareness about the damage caused by sheep grazing, and he actively campaigned to virtually eliminate grazing from the Yosemite's high-country.<ref>{{cite web |title=Yosemite |url=https://www.nps.gov/yose/learn/historyculture/muir.htm |website=nps.gov |publisher=National Park Service |access-date=1 September 2021 |archive-date=September 3, 2021 |archive-url=https://web.archive.org/web/20210903062250/https://www.nps.gov/yose/learn/historyculture/muir.htm |url-status=live }}</ref>


The newly created national park came under the jurisdiction of the United States Army's Troop I of the ] on May 19, 1891, which set up camp in Wawona with Captain ] as acting superintendent.<ref name="Schaffer50"/> By the late 1890s, sheep grazing was no longer a problem, and the Army made many other improvements. The cavalry could not intervene to ease the worsening condition of Yosemite Valley and Mariposa Grove. The cavalry left another legacy in the park, the ranger hat. From 1899 to 1913, cavalry regiments of the Western Department, including the all Black ] (known as the "Buffalo Soldiers") and the ], stationed two troops at Yosemite and brought with them the trooper's campaign hat with its distinctive Montana Peak we recognize today as the "ranger hat." This peak had been formed into the trooper's stetson by veterans of the 1898 Spanish–American War to better shed tropical rain. The newly created national park came under the jurisdiction of the United States Army's Troop I of the ] on May 19, 1891, which set up camp in Wawona with Captain ] as acting superintendent.<ref name="Schaffer50"/> By the late 1890s, sheep grazing was no longer a problem, and the Army made other improvements. However, the cavalry could not intervene to ease the worsening conditions. From 1899 to 1913, cavalry regiments of the Western Department, including the all Black ] (known as the "Buffalo Soldiers") and the ], stationed two troops at Yosemite.


] circa 1880]] ] and ], by ] ({{circa|1880}})]]
Muir and his ] continued to lobby the government and influential people for the creation of a unified Yosemite National Park. In May 1903, President ] camped with Muir near ] for three days. On that trip, Muir convinced Roosevelt to take control of Yosemite Valley and Mariposa Grove away from California and return it to the federal government. In 1906, Roosevelt signed a bill that did precisely that. Muir and his ] continued to lobby the government and influential people for the creation of a unified Yosemite National Park. In May 1903, President ] camped with Muir near ] for three days. On that trip, Muir convinced Roosevelt to take control of Yosemite Valley and Mariposa Grove away from California and return it to the federal government. In 1906, Roosevelt signed a bill that shifted control.<ref>{{cite web|url=https://www.nps.gov/jomu/learn/historyculture/people.htm#onthisPage-2|title=John Muir and President Roosevelt|work=John Muir National Historic Site, California|publisher=National Park Service|access-date=2021-08-31|archive-date=August 19, 2021|archive-url=https://web.archive.org/web/20210819190816/https://www.nps.gov/jomu/learn/historyculture/people.htm#onthisPage-2|url-status=live}}</ref>


===National Park Service=== ===National Park Service===
The ] was formed in 1916, and Yosemite was transferred to that agency's jurisdiction. Tuolumne Meadows Lodge, ], and campgrounds at Tenaya and Merced lakes were also completed in 1916.<ref name="Schaffer52">{{harvnb|Schaffer|1999|p=52}}</ref> ]s started to enter the park in ever-increasing numbers following the construction of all-weather highways to the park. The Yosemite Museum was founded in 1926 through the efforts of ].{{sfn|NPS|1989|p=117}} The ] (NPS) was formed in 1916, and Yosemite was transferred to that agency's jurisdiction. Tuolumne Meadows Lodge, ], and campgrounds at Tenaya and Merced lakes were also completed in 1916.<ref name="Schaffer52">{{harvnb|Schaffer|1999|p=52}}</ref> Automobiles started to enter the park in ever-increasing numbers following the opening of all-weather highways to the park. The Yosemite Museum was founded in 1926 through the efforts of ].{{sfn|NPS|1989|p=117}} In the 1920s, the museum featured Native Americans practicing traditional crafts, and many Southern Sierra Miwok continued to live in Yosemite Valley until they were evicted from the park in the 1960s.<ref>{{cite web|url=http://www.fresnobee.com/news/special-reports/yosemite-at-150/article19521750.html|title=American Indians share their Yosemite story|access-date=July 12, 2017|archive-date=July 22, 2017|archive-url=https://web.archive.org/web/20170722135414/http://www.fresnobee.com/news/special-reports/yosemite-at-150/article19521750.html|url-status=live}}</ref> Although the NPS helped create a museum that included Native American culture, its early actions and organizational values were dismissive of Yosemite Natives and the Ahwahneechee.<ref name=":1" /> NPS in the early 20th century criticized and restricted the expression of indigenous culture and behavior. For example, park officials penalized Natives for playing games and drinking during the Indian Field Days of 1924.<ref name="Spence" /> In 1929, Park Superintendent Charles G. Thomson concluded that the Indian village was aesthetically unpleasant and was limiting white settler development and ordered the camp to be burned down.<ref name=":1" /> In 1969, many Native residents left in search of work as a result of the decline in tourism. NPS demolished their empty houses, evicted the remaining residents, and destroyed the entire village.<ref name=":1" /> This was the last Indigenous settlement within the park.<ref name=":1" /><ref name="miwuk" />


In 1903, a dam in the northern portion of the park was proposed. Located in the ], its purpose was to provide water and ] to ]. Muir and the Sierra Club opposed the project, while others, including ], supported it.<ref>Moseley, W. G. 2009. "Beyond Knee-Jerk Environmental Thinking: Teaching Geographic Perspectives on Conservation, Preservation and the Hetch Hetchy Valley Controversy." ''Journal of Geography in Higher Education''. 33(3): 433-451.</ref> In 1913, the U.S. Congress authorized the ] through passage of the ].<ref name="Schaffer51">{{harvnb|Schaffer|1999|p=51}}</ref> In 1903, a dam in ] in the northwestern region of the park was proposed. Its purpose was to provide water and ] to ]. Muir and the Sierra Club opposed the project, while others, including ], supported it.<ref>{{cite journal |last=Moseley |first=W. G. |year=2009 |title=Beyond Knee-Jerk Environmental Thinking: Teaching Geographic Perspectives on Conservation, Preservation and the Hetch Hetchy Valley Controversy |journal=Journal of Geography in Higher Education |volume=33 |issue=3 |pages=433–51 |doi=10.1080/03098260902982492 |s2cid=143538071 }}</ref> In 1913, the ] was approved via passage of the ].<ref name="Schaffer51">{{harvnb|Schaffer|1999|p=51}}</ref>
]]]


In 1918, ] was hired as the first female Park Ranger in Yosemite.<ref name=":6">{{Cite web
In the late 1920s, in an attempt that would be impossible to make today, a ] for Yosemite for the ] was put forward.<ref name="olympics1932">{{cite web|url=http://www.destination360.com/north-america/us/california/badger-pass-ski-resort |title=Badger Pass Ski Resort - Badger Pass - Badger Pass Yosemite |publisher=Destination360.com |date= |accessdate=April 1, 2012}}</ref> (Ultimately, ], hosted.)<ref name="olympics1932"/>
|title = Women of Yosemite
|url = https://www.nps.gov/yose/learn/historyculture/women.htm
|access-date = 2023-04-18
|year = 2022
|publisher = National Park Service
|archive-date = March 30, 2023
|archive-url = https://web.archive.org/web/20230330045408/https://www.nps.gov/yose/learn/historyculture/women.htm
|url-status = live
}}</ref> Following Hodges in 1921, ] was hired as a seasonal Park Ranger<ref name=":6" /> and continued to serve in that position for 20 years.<ref name=":6" />
] in ] Valley]]


In 1937, conservationist ], head of the Emergency Conservation Committee (ECC), successfully lobbied Congress to purchase about {{convert|8,000| acres}} of old-growth sugar pines on the perimeter of Yosemite National Park that were to be logged.<ref>{{cite book |last=Furmansky |first=Dyana Z. |year=2009 |title=Rosalie Edge, Hawk of Mercy: The Activist Who Saved Nature from the Conservationists |url=https://archive.org/details/rosalieedgehawko00zasl |url-access=registration |publisher=University of Georgia Press |isbn=978-0820336763 |pages = 200–07}}</ref>
More recently, preservationists persuaded Congress to designate {{convert|677600|acre}}, or about 89% of the park, as the Yosemite Wilderness—a highly protected ].<ref>{{cite web|url=http://www.nps.gov/legal/parklaws/1/laws1-volume1-appendix.pdf|archiveurl=http://www.webcitation.org/5z2KHC4Ck|archivedate=2011-05-29|title=California Wilderness Act of 1984|author=98th U.S. Congress|year=1984|accessdate=May 8, 2010|format=PDF}}</ref> The Park Service has reduced artificial inducements to visit the park, such as the '']'', in which red-hot embers were pushed off a cliff near Glacier Point at night. ] in Yosemite Valley during the summer months has become a concern. Two electric buses commenced service in September 1995. The buses are quiet and do not emit pollutants. Eventually, all the buses in Yosemite will be electric.<ref>{{cite web|url=http://www.energyquest.ca.gov/transportation/electric.html|title=A Student's Guide to Alternative Fuel Vehicles|work=EnergyQuest|publisher=California Energy Commission|accessdate=September 10, 2010}}</ref> The ] killed a hiker and the ] damaged many roads and several campgrounds.


By 1968, ] and parking in Yosemite Valley during the summer months has become a concern. NPS reduced artificial inducements to visit the park, such as the '']'', in which red-hot embers were pushed off a cliff near Glacier Point at night.<ref>{{cite news|url=https://www.earthmagazine.org/article/benchmarks-january-25-1968-last-firefall-yosemite-tradition-flames-out/|magazine=Earth Magazine|title=Benchmarks: January 25, 1968: The last firefall: A Yosemite tradition flames out|first=Sara E|last=Pratt|date=December 14, 2017|access-date=December 2, 2023|archive-date=October 25, 2023|archive-url=https://web.archive.org/web/20231025083407/https://www.earthmagazine.org/article/benchmarks-january-25-1968-last-firefall-yosemite-tradition-flames-out/|url-status=live}}</ref>
==Geography==
{{Main article|Geography of the Yosemite area}}
]


In 1984, preservationists persuaded Congress to designate {{convert|677600|acre}}, or about 89 percent of the park, as the Yosemite Wilderness. As a ], it would be preserved in its natural state with humans being only temporary visitors.<ref>{{cite web |url=http://www.nps.gov/legal/parklaws/1/laws1-volume1-appendix.pdf |archive-url=https://web.archive.org/web/20120203175920/http://www.nps.gov/legal/parklaws/1/laws1-volume1-appendix.pdf |archive-date=February 3, 2012 |title=California Wilderness Act of 1984 - 98th U.S. Congress |access-date=May 8, 2010 |url-status=dead }}</ref>
Yosemite National Park is located in the central Sierra Nevada of California. Three wilderness areas are adjacent to Yosemite: the ] to the southeast, the ] to the northeast, and the ] to the north.

In 2016, ] (TPL) purchased Ackerson Meadow, a {{convert|400|acre||adj=mid| tract}} on the western edge of the park for $2.3&nbsp;million. Ackerson Meadow was originally included in the proposed 1890 park boundary, but never acquired by the federal government. The purchase and donation of the meadow was made possible through a cooperative effort by TPL, NPS, and Yosemite Conservancy. On September 7, 2016, NPS accepted the donation of the land, making the meadow the largest addition to Yosemite since 1949.<ref>{{cite web|url=https://www.nps.gov/yose/learn/news/ackersonaddition.htm|title=Ackerson Meadow Gifted to Yosemite National Park|author=National Park Service|access-date=September 8, 2016|archive-date=September 20, 2016|archive-url=https://web.archive.org/web/20160920195915/https://www.nps.gov/yose/learn/news/ackersonaddition.htm|url-status=live}}</ref> With extensive erosion from years of cattle ranching , the land is being transformed back into a healthy meadow.<ref>{{Cite web |last=Rogers |first=Paul |date=2024-08-23 |title=Yosemite National Park: Crews restore damaged landscape back to conditions not seen in 150 years |url=https://www.mercurynews.com/2024/08/23/yosemite-national-park-crews-restore-damaged-landscape-back-to-conditions-not-seen-in-150-years/ |access-date=2024-08-24 |website=The Mercury News |language=en-US}}</ref>

==Geography==
{{Main|Geography of the Yosemite area}}
]
Yosemite National Park is located in the central Sierra Nevada. Three wilderness areas are adjacent to Yosemite: the ] to the southeast, the ] to the northeast, and the ] to the north.


The {{convert|1189|mi2|km2|abbr=on}} park is roughly the size of the U.S. state of ] and contains thousands of ]s and ]s, {{convert|1600|mi|km}} of streams, {{convert|800|mi|km}} of ] trails, and {{convert|350|mi|km}} of roads.<ref name="nature">{{cite web | title =Nature & Science | publisher =United States National Park Service: Yosemite National Park | url = http://www.nps.gov/yose/naturescience/index.htm | accessdate = January 27, 2007 }}</ref> Two federally designated ]s, the ] and the Tuolumne, begin within Yosemite's borders and flow westward through the Sierra foothills, into the ]. Annual park visitation exceeds 3.5&nbsp;million, with most visitor use concentrated in the seven-square-mile (18&nbsp;km<sup>2</sup>) area of ].<ref name="nature"/> The {{convert|1189|mi2|km2|abbr=on}} park contains thousands of lakes and ponds, {{convert|1600|mi|km}} of streams, {{convert|800|mi|km}} of hiking trails, and {{convert|350|mi|km}} of roads.<ref name="nature">{{cite web | title =Nature & Science | publisher =United States National Park Service: Yosemite National Park | url =http://www.nps.gov/yose/naturescience/index.htm | access-date =January 27, 2007 | archive-date =April 22, 2007 | archive-url =https://web.archive.org/web/20070422072242/http://www.nps.gov/yose/naturescience/index.htm | url-status =live }}</ref> Two federally designated ]s, the ] and the ], begin within Yosemite's borders and flow westward through the Sierra foothills into the ].


===Rocks and erosion=== ===Rocks and erosion===
]]] ], a granite monolith on Yosemite Valley's northern escarpment]]
Almost all of the ] in the Yosemite area are cut from the ] rock of the ] (a ] is a large mass of intrusive ] that formed deep below the surface).<ref name="GeologyNP329">{{harvnb|Harris|1998|p=329}}</ref> About 5% of the park's landforms (mostly in its eastern margin near ]) are ] ] and ]s.<ref name="landforms">{{cite web | publisher = United States National Park Service: Yosemite National Park | url = http://www.nps.gov/archive/yose/nature/geo_landforms.htm | archiveurl = https://web.archive.org/web/20090514004436/http://www.nps.gov/archive/yose/nature/geo_landforms.htm | archivedate = May 14, 2009 | title = Geology: The Making of the Landscape | date = December 22, 2004 | accessdate =January 27, 2007 }}</ref> These rocks are called ''roof pendants'' because they were once the roof of the underlying granitic rock.<ref>{{cite web | publisher = United States Geological Survey | url = http://www.cr.nps.gov/history/online_books/geology/publications/pp/160/sec2a.htm | archiveurl = http://www.webcitation.org/69H5zzZyl | archivedate = 2012-07-19 | title = Geological Survey Professional Paper 160: Geologic History of the Yosemite Valley - The Sierra Block | date = November 28, 2006 |accessdate = January 27, 2007 }}</ref> Almost all of the landforms are cut from the granitic rock of the ] (a ] is a large mass of intrusive ] that formed deep below the surface).<ref name="GeologyNP329">{{harvnb|Harris|1998|p=329}}</ref> About five percent of the park's landforms (mostly in its eastern margin near ]) are ] ] and ]s.<ref name="landforms">{{cite web | publisher = United States National Park Service: Yosemite National Park | url = http://www.nps.gov/archive/yose/nature/geo_landforms.htm | archive-url = https://web.archive.org/web/20090514004436/http://www.nps.gov/archive/yose/nature/geo_landforms.htm | archive-date = May 14, 2009 | title = Geology: The Making of the Landscape | date = December 22, 2004 | access-date =January 27, 2007 }}</ref> These ] once formed the roof over the underlying granitic magma.<ref>{{cite web|publisher=United States Geological Survey |url=http://www.cr.nps.gov/history/online_books/geology/publications/pp/160/sec2a.htm |archive-url=https://web.archive.org/web/20121022231626/http://www.cr.nps.gov/history/online_books/geology/publications/pp/160/sec2a.htm |archive-date=October 22, 2012 |title=Geological Survey Professional Paper 160: Geologic History of the Yosemite Valley&nbsp;– The Sierra Block |date=November 28, 2006 |access-date=January 27, 2007 |url-status=dead }}</ref>


] acting upon different types of uplift-created joint and fracture systems is responsible for creating the valleys, canyons, ], and other features we see today. These joints and fracture systems do not move, and are therefore not ].<ref name="GeologyNP331">{{harvnb|Harris|1998|p=331}}</ref> Spacing between joints is controlled by the amount of ] in the granite and ] rocks; more silica tends to create a more resistant rock, resulting in larger spaces between joints and fractures.<ref name="GeologyUSP220">{{harvnb|Kiver|Harris|1999|p=220}}</ref> ] acting upon different types of uplift-generated joint and fracture systems is responsible for producing the valleys, canyons, ], and other features. These joints and fracture systems do not move, and are therefore not ].<ref name="GeologyNP331">{{harvnb|Harris|1998|p=331}}</ref> Spacing between joints is controlled by the amount of ] in the granite and ] rocks; more silica tends to form a more resistant rock, resulting in larger spaces between joints and fractures.<ref name="GeologyUSP220">{{harvnb|Kiver|Harris|1999|p=220}}</ref>


Pillars and columns, such as Washington Column and Lost Arrow, are created by cross joints. Erosion acting on master joints is responsible for creating valleys and later canyons.<ref name="GeologyUSP220"/> The single most erosive force over the last few million years has been large alpine glaciers, which have turned the previously V-shaped river-cut valleys into U-shaped glacial-cut canyons (such as Yosemite Valley and Hetch Hetchy Valley). ] (caused by the tendency of ]s in ]ic rocks to expand at the surface) acting on granitic rock with widely spaced joints is responsible for creating domes such as ] and ] and inset arches like Royal Arches.<ref name="GeologyNP332"/> Pillars and columns, such as ] and ], are generated by cross joints. Erosion acting on master joints is responsible for shaping valleys and later canyons.<ref name="GeologyUSP220"/> The single most erosive force over the last few million years has been large alpine ], which turned the previously V-shaped river-cut valleys into U-shaped glacial-cut canyons (such as Yosemite Valley and Hetch Hetchy Valley). ] (caused by the tendency of ]s in ]ic rocks to expand at the surface) acting on granitic rock with widely spaced joints is responsible for producing domes such as ] and ] and inset arches like Royal Arches.<ref name="GeologyNP332"/>


===Popular features=== ===Popular features===
] ]] ]]]
Yosemite Valley represents only one percent of the park area, but this is where most visitors arrive and stay. The ] is the first view of the Valley for many visitors and is extensively photographed. ], a prominent granite cliff that looms over Yosemite Valley, is one of the most popular ] destinations in the world because of its diverse range of climbing routes in addition to its year-round accessibility. ]s such as ] and Half Dome rise {{convert|3000|and|4800|ft|m}}, respectively, above the valley floor. Yosemite Valley represents only one percent of the park area. The ] gives a view of the valley. ] is a prominent granite cliff that looms over the valley, and is a rock climbing favorite because of its sheer size, diverse climbing routes, and year-round accessibility. ]s such as ] and ] rise {{convert|3000|and|4800|ft|m}}, respectively, above the valley floor. The park contains dozens of other ].<ref>{{cite news |last1=Cross |first1=Robert |title=Mountain majesty Yosemite: The California national park is home to some of the country's most scenic natural wonders. |url=https://www.baltimoresun.com/news/bs-xpm-1996-05-26-1996147114-story.html |access-date=7 September 2021 |work=The Baltimore Sun |date=26 May 1996 |archive-date=October 6, 2022 |archive-url=https://web.archive.org/web/20221006075550/https://www.baltimoresun.com/news/bs-xpm-1996-05-26-1996147114-story.html |url-status=live }}</ref>


The high country of Yosemite contains beautiful areas such as ], ], the ], the ], and the Kuna Crest. The Sierra crest and the ] run through Yosemite, with peaks of red metamorphic rock, such as Mount Dana and ], and granite peaks, such as ]. ] is the highest point in the park, standing at {{convert|13,120|ft|m}}. The Lyell Glacier is the largest glacier in Yosemite National Park and is one of the few remaining in the Sierra Nevada today. The high country of Yosemite contains other important features such as ], ], the ], the ], and the ]. The ] and the ] run through Yosemite. Mount Dana and ] are peaks of red metamorphic rock. Granite peaks include ], ], and ]. ] is the highest point in the park, standing at {{convert|13,120|ft|m}}. The ] is the largest glacier in the park and one of the few remaining in the Sierra.<ref>{{Cite web|title=Yosemite National Park's Largest Glacier Stagnant – Yosemite National Park (U.S. National Park Service)|url=https://www.nps.gov/yose/learn/news/lyellglacier.htm|access-date=2021-05-06|website=www.nps.gov|language=en|archive-date=May 6, 2021|archive-url=https://web.archive.org/web/20210506185923/https://www.nps.gov/yose/learn/news/lyellglacier.htm|url-status=live}}</ref>


The park has three groves of ancient giant sequoia (''Sequoiadendron giganteum'') ]s; the Mariposa Grove (200 trees), the ] (25 trees), and the ] (20 trees).<ref name="GeologyNP340"/> This species grows larger in volume than any other and is one of the tallest and longest-lived.<ref name="Kiver227">{{harvnb|Kiver|Harris|1999|p=227}}</ref> The park has three groves of ancient giant sequoia ('']'') trees; the ] (200 trees), the ] (25 trees), and the ] (20 trees).<ref name="GeologyNP340"/> This species grows larger in volume than any other and is one of the tallest and longest-lived.<ref name="Kiver227">{{harvnb|Kiver|Harris|1999|p=227}}</ref>


===Water and ice=== ===Water and ice===
] flowing through ], a ]]]
The ] and ] systems originate along the crest of the Sierra in the park and have carved river canyons {{convert|3000|to|4000|ft|m}} deep. The Tuolumne River drains the entire northern portion of the park, an area of approximately {{convert|680|mi2|km2}}. The Merced River begins in the park's southern peaks, primarily the Cathedral and Clark Ranges, and drains an area of approximately {{convert|511|mi2|km2}}.<ref name = "water overview">{{cite web | title = Water Overview | url = http://www.nps.gov/archive/yose/nature/water.htm | archive-url=https://web.archive.org/web/20070107180730/http://www.nps.gov/archive/yose/nature/water.htm|archive-date=January 7, 2007 | publisher = National Park Service: Yosemite National Park | date = December 22, 2004 | access-date = January 27, 2007 }}</ref>


Tuolumne and Merced River systems originate along the crest of the ] in the park and have carved river canyons {{convert|3000|to|4000|ft|m}} deep. The Tuolumne River drains the entire northern portion of the park, an area of approximately {{convert|680|mi2|km2}}. The Merced River begins in the park's southern peaks, primarily the Cathedral and Clark Ranges, and drains an area of approximately {{convert|511|mi2|km2}}.<ref name = "water overview">{{cite web | title = Water Overview | url = http://www.nps.gov/archive/yose/nature/water.htm | archiveurl=https://web.archive.org/web/20070107180730/http://www.nps.gov/archive/yose/nature/water.htm|archivedate=January 7, 2007 | publisher = National Park Service: Yosemite National Park | date = December 22, 2004 | accessdate = January 27, 2007 }}</ref> Hydrologic processes, including ], flooding, and fluvial geomorphic response, have been fundamental in creating park landforms.<ref name = "water overview"/> The park contains approximately 3,200 lakes (greater than 100 m<sup>2</sup>), two ], and {{convert|1700|mi|km}} of streams.<ref name = "hydrology">{{cite web | title = Hydrology and Watersheds | url = http://www.nps.gov/archive/yose/nature/wtr_hydrology.htm | archive-url = https://web.archive.org/web/20100728075552/http://www.nps.gov/archive/yose/nature/wtr_hydrology.htm | archive-date = July 28, 2010 | publisher = National Park Service: Yosemite National Park | date = December 22, 2004 | access-date = January 27, 2007 }}</ref> ]s flourish in valley bottoms throughout the park, and are often hydrologically linked to nearby lakes and rivers through seasonal flooding and groundwater. Meadow habitats, distributed at elevations from {{convert|3000|to|11000|ft|m}} in the park, are generally wetlands, as are the ] habitats found on the banks of Yosemite's watercourses.<ref name = "wetland vegetation">{{cite web | title = Wetland Vegetation | url = http://www.nps.gov/archive/yose/nature/veg_wetlands.htm | archive-url = https://web.archive.org/web/20100419080619/http://www.nps.gov/archive/yose/nature/veg_wetlands.htm | archive-date = April 19, 2010 | publisher = National Park Service: Yosemite National Park | date = December 22, 2004 | access-date = January 27, 2007 }}</ref>
]—Yosemite]]


] flows from a U-shaped hanging valley that was created by a tributary glacier.]]
Hydrologic processes, including ], ], and fluvial geomorphic response, have been fundamental in creating landforms in the park.<ref name = "water overview"/> The park also contains approximately 3,200 lakes (greater than 100 m<sup>2</sup>), two ], and {{convert|1700|mi|km}} of streams, all of which help form these two large ].<ref name = "hydrology">{{cite web | title = Hydrology and Watersheds | url = http://www.nps.gov/archive/yose/nature/wtr_hydrology.htm | archiveurl = https://web.archive.org/web/20100728075552/http://www.nps.gov/archive/yose/nature/wtr_hydrology.htm | archivedate = July 28, 2010 | publisher = National Park Service: Yosemite National Park | date = December 22, 2004 | accessdate = January 27, 2007 }}</ref> ]s in Yosemite occur in valley bottoms throughout the park, and are often hydrologically linked to nearby lakes and rivers through seasonal flooding and groundwater movement. Meadow habitats, distributed at elevations from {{convert|3000|to|11000|ft|m}} in the park, are generally wetlands, as are the ] habitats found on the banks of Yosemite's numerous streams and rivers.<ref name = "wetland vegetation">{{cite web | title = Wetland Vegetation | url = http://www.nps.gov/archive/yose/nature/veg_wetlands.htm | archiveurl = https://web.archive.org/web/20100419080619/http://www.nps.gov/archive/yose/nature/veg_wetlands.htm | archivedate = April 19, 2010 | publisher = National Park Service: Yosemite National Park | date = December 22, 2004 | accessdate = January 27, 2007 }}</ref>
Yosemite is famous for its ] in a small area. Numerous sheer drops, glacial steps and ]s in the park feature spectacular cascades, especially during April, May, and June (as the snow melts). Located in Yosemite Valley, ] is the fourth tallest waterfall in North America at {{convert|2425|ft|m}} according to the World Waterfall Database.<ref>{{Cite web |title=Tallest and Largest Waterfalls at the World Waterfall Database |url=https://www.worldwaterfalldatabase.com/tallest-waterfalls/total-height |access-date=2023-09-04 |website=www.worldwaterfalldatabase.com |language=en |archive-date=October 23, 2008 |archive-url=https://web.archive.org/web/20081023160017/http://www.world-waterfalls.com/database.php?s=N&t=H&orderby=height&sortLimit=300 |url-status=live }}</ref> Also in the valley is the much lower volume ]s, which has the highest single vertical drop, {{convert|1612|ft|m}}.<ref name="Kiver227"/> Perhaps the most prominent of the valley waterfalls is ]. Wapama Falls in Hetch Hetchy Valley is another notable waterfall. Hundreds of ] waterfalls become active in the park after heavy rains or melting snowpack.<ref>{{cite news |last1=Krieger |first1=Lisa |title=Waterfalls are roaring this spring at Yosemite |url=https://www.mercurynews.com/2019/05/17/waterfalls-are-roaring-this-spring-at-yosemite-and-here-are-the-best-right-now/ |access-date=9 September 2021 |work=San Jose Mercury News |date=17 May 2019 |archive-date=September 9, 2021 |archive-url=https://web.archive.org/web/20210909172152/https://www.mercurynews.com/2019/05/17/waterfalls-are-roaring-this-spring-at-yosemite-and-here-are-the-best-right-now/ |url-status=live }}</ref>
] flows from a U-shaped hanging valley that was created by a tributary glacier.]]
Yosemite is famous for its ] in a small area. Numerous sheer drops, glacial steps and ]s in the park provide many places for ]s to exist, especially during April, May, and June (the snowmelt season). Located in Yosemite Valley, the ] is the highest in North America at {{convert|2425|ft|m|adj=on}}. Also in Yosemite Valley is the much lower volume ]s, which has the highest single vertical drop, {{convert|1612|ft|m}}.<ref name="Kiver227"/> Perhaps the most prominent of the Yosemite Valley waterfalls is ], which is the waterfall seen from the Tunnel View viewpoint at the east end of the Wawona Tunnel. Wapama Falls in Hetch Hetchy Valley is another notable waterfall. Hundreds of ] waterfalls also exist in the park.
]]]


All glaciers in the park are relatively small glaciers that occupy areas that are in almost permanent shade, such as north- and northeast-facing ]. ] is the largest glacier in Yosemite (the Palisades Glaciers are the largest in the Sierra Nevada) and covers {{convert|160|acre}}.<ref name="GeologyUSP228">{{harvnb|Kiver|Harris|1999|p=228}}</ref> None of the Yosemite glaciers are a remnant of the much, much larger ] alpine glaciers responsible for sculpting the Yosemite landscape. Instead, they were formed during one of the ] episodes that have occurred since the thawing of the Ice Age (such as the ]).<ref name="GeologyNP340">{{harvnb|Harris|1998|p=340}}</ref> ] has reduced the number and size of glaciers around the world. Many Yosemite glaciers, including Merced Glacier, which was discovered by John Muir in 1871 and bolstered his glacial origins theory of the Yosemite area, have disappeared and most of the others have lost up to 75% of their surface area.<ref name="GeologyUSP228"/> Park ]s are relatively small and occupy areas that are in almost permanent shade, such as north- and northeast-facing ]. ] is the largest glacier in Yosemite (the Palisades Glaciers are the largest in the Sierra Nevada) and covers {{convert|160|acre}}.<ref name="GeologyUSP228">{{harvnb|Kiver|Harris|1999|p=228}}</ref> None of the Yosemite glaciers are a remnant of the ] alpine glaciers responsible for sculpting the Yosemite landscape. Instead, they were formed during one of the ] episodes that have occurred since the thawing of the Ice Age (such as the ]).<ref name="GeologyNP340">{{harvnb|Harris|1998|p=340}}</ref> Many Yosemite glaciers have disappeared, such as the Black Mountain Glacier that was marked in 1871 and had gone by the mid-1980s.<ref>{{cite news |last1=Sahagun |first1=Louis |title=Yosemite's largest ice mass is melting fast |url=https://www.latimes.com/local/la-xpm-2013-oct-01-la-me-glaciers-20131002-story.html |access-date=14 September 2021 |work=Los Angeles Times |date=1 October 2013 |archive-date=September 14, 2021 |archive-url=https://web.archive.org/web/20210914181402/https://www.latimes.com/local/la-xpm-2013-oct-01-la-me-glaciers-20131002-story.html |url-status=live }}</ref> Yosemite's final two glaciers – the Lyell and Maclure glaciers – have receded over the last 100 years and are expected to disappear as a result of climate change.<ref>{{cite web |title=Yosemite – Nature – Geology – Glaciers |url=https://www.nps.gov/yose/learn/nature/glaciers.htm |website=nps.gov |publisher=National Park Service |access-date=14 September 2021 |archive-date=September 14, 2021 |archive-url=https://web.archive.org/web/20210914175346/https://www.nps.gov/yose/learn/nature/glaciers.htm |url-status=live }}</ref><ref>{{cite news |last1=Liberatore |title=Glaciers in Yosemite |url=https://www.myyosemitepark.com/things-to-do/natural-wonders/mountains-landscapes/when-glaciers-ruled/ |access-date=14 September 2021 |publisher=Yosemite National Park trips |date=15 March 2013 |archive-date=September 14, 2021 |archive-url=https://web.archive.org/web/20210914175033/https://www.myyosemitepark.com/things-to-do/natural-wonders/mountains-landscapes/when-glaciers-ruled/ |url-status=live }}</ref>


===Climate=== ===Climate===
] ]] ]]]
Yosemite has a ] (] ''Csa''), meaning most precipitation falls during the mild winter, and the other seasons are nearly dry (less than three percent of precipitation falls during the long, hot summers). Because of ], precipitation increases with elevation up to {{convert|8000|ft|m}} where it slowly decreases to the crest. Precipitation amounts vary from {{convert|36|in|mm}} at {{convert|4000|ft|m}} elevation to {{convert|50|in|mm}} at {{convert|8600|ft|m}}. Snow does not typically accumulate until November in the high country. It deepens into March or early April.<ref name="climate">{{cite web | publisher = National Park Service: Yosemite National Park | url = http://www.nps.gov/archive/yose/nature/wtr_climate.htm |archive-url=https://web.archive.org/web/20070101113353/http://www.nps.gov/archive/yose/nature/wtr_climate.htm|archive-date=January 1, 2007 | title = Climate | date = December 22, 2004 | access-date = January 27, 2007 }}</ref>


Mean daily temperatures range from {{convert|25|°F|0}} to {{convert|53|°F|0}} at Tuolumne Meadows at {{convert|8600|ft|m}}. At the Wawona Entrance (elevation {{convert|5130|ft|m|disp=or}}), mean daily temperature ranges from {{convert|36|to|67|°F|°C}}. At the lower elevations below {{convert|5000|ft|m}}, temperatures are hotter; the mean daily high temperature at Yosemite Valley (elevation {{convert|3966|ft|m|disp=or}}) varies from {{convert|46|to|90|°F|°C}}. At elevations above {{convert|8000|ft|m}}, the hot, dry summer temperatures are moderated by frequent summer thunderstorms, along with snow that can persist into July. The combination of dry vegetation, low relative humidity, and thunderstorms results in frequent lightning-caused ] as well.<ref name="climate"/>
Yosemite has a ] (] ''Csa''), meaning most precipitation falls during the mild winter, and the other seasons are nearly dry (less than 3% of precipitation falls during the long, hot summers).<ref name="Wuerthner8">{{harvnb|Wuerthner|1994|p=8}}</ref> Because of ], precipitation increases with elevation up to {{convert|8000|ft|m}} where it slowly decreases to the crest. Precipitation amounts vary from {{convert|36|in|mm}} at {{convert|4000|ft|m}} elevation to {{convert|50|in|mm}} at {{convert|8600|ft|m}}. Snow does not typically persist on the ground until November in the high country. It accumulates all winter and into March or early April.<ref name="climate">{{cite web | publisher = National Park Service: Yosemite National Park | url = http://www.nps.gov/archive/yose/nature/wtr_climate.htm |archiveurl=https://web.archive.org/web/20070101113353/http://www.nps.gov/archive/yose/nature/wtr_climate.htm|archivedate=January 1, 2007 | title = Climate | date = December 22, 2004 | accessdate = January 27, 2007 }}</ref>


At park headquarters (elevation {{convert|4018|ft|disp=or|abbr=on}}), January averages {{convert|38.0|°F|1}}, while July averages {{convert|73.3|°F|1}}. In summer the nights are much cooler than the days. An average of 45.5 days have highs of {{convert|90|°F|0}} or higher and an average of 105.6 nights with freezing temperatures. Freezing temperatures have been recorded in every month of the year. The record high temperature was {{convert|112|°F|0}} on July 22 and July 24, 1915, while the record low temperature was {{convert|-7|°F|0}} on January 1, 2009. Average annual precipitation is nearly {{convert|37|in|0}}, falling on 67 days. The wettest year was 1983 with {{convert|66.06|in|mm}} and the driest year was 1976 with {{convert|14.84|in|mm}}. The most precipitation in one month was {{convert|29.61|in|mm}} in December 1955 and the most in one day was {{convert|6.92|in|mm}} on December 23, 1955. Average annual snowfall is {{convert|39.4|in|m}}. The snowiest winter was 1948–1949 with {{convert|176.5|in|m}}. The most snow in one month was {{convert|175.0|in|m}} in January 1993.
Mean daily temperatures range from {{convert|25|°F|0}} to {{convert|53|°F|0}} at Tuolumne Meadows at {{convert|8600|ft|m}}. At the Wawona Entrance (elevation {{convert|5130|ft|m|disp=or}}), mean daily temperature ranges from {{convert|36|to|67|°F|°C}}. At the lower elevations below {{convert|5000|ft|m}}, temperatures are hotter; the mean daily high temperature at Yosemite Valley (elevation {{convert|3966|ft|m|disp=or}}) varies from {{convert|46|to|90|°F|°C}}. At elevations above {{convert|8000|ft|m}}, the hot, dry summer temperatures are moderated by frequent summer ]s, along with snow that can persist into July. The combination of dry ], low relative ], and thunderstorms results in frequent ]-caused ] as well.<ref name="climate"/>

At the park headquarters, with an elevation of {{convert|3966|ft}}, January averages {{convert|38.2|°F|1}}, while July averages {{convert|73.0|°F|1}}, though in summer the nights are much cooler than the hot days.<ref name= NCDC2 >{{cite web
|url = http://www.nws.noaa.gov/climate/xmacis.php?wfo=hnx
|title = NOWData - NOAA Online Weather Data
|publisher =]
|accessdate = June 9, 2013
}}</ref> There are an average of 39.5 days with highs of {{convert|90|°F|0}} or higher and an average of 97.9 nights with freezing temperatures.<ref name= NCDC2 /> Freezing temperatures have been recorded in every month of the year. The record high temperature was {{convert|115|°F|0}} on July 20, 1915, while the record low temperature was {{convert|-6|°F|0}} on January 2, 1924 and on January 21, 1937.<ref name= NCDC2 /><ref name = WRCC>{{cite web |url = http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?ca9855 |title = Yosemite Park HDQTRS, California |publisher= Western Regional Climate Center |accessdate = June 9, 2013}}</ref> Average annual precipitation is nearly {{convert|37|in|0}}, falling on 65 days. The wettest year was 1983 with {{convert|68.94|in|mm}} and the driest year was 1976 with {{convert|14.84|in|mm}}.<ref name= WRCC/> The most precipitation in one month was {{convert|29.61|in|mm}} in December 1955 and the most in one day was {{convert|6.92|in|mm}} on December 23, 1955.<ref name= WRCC/> Average annual snowfall is {{convert|65.6|in|m}}. The snowiest year was 1967 with {{convert|154.9|in|m}}. The most snow in one month was {{convert|140.8|in|m}} in January 1993.<ref name= WRCC/>


{{Weather box {{Weather box
|location = Yosemite Park Headquarters, California, 1991–2020 normals, extremes 1905–present
|single line = Y
|collapsed = Y |collapsed = Y
|width=100%
|location = Yosemite Park Headquarters, elev. {{convert|3966|ft|0}}
|single line = Y
|Jan record high F = 72 |Jan record high F = 72
|Feb record high F = 82 |Feb record high F = 82
Line 220: Line 232:
|May record high F = 99 |May record high F = 99
|Jun record high F = 103 |Jun record high F = 103
|Jul record high F = 115 |Jul record high F = 112
|Aug record high F = 110 |Aug record high F = 110
|Sep record high F = 108 |Sep record high F = 108
Line 226: Line 238:
|Nov record high F = 86 |Nov record high F = 86
|Dec record high F = 73 |Dec record high F = 73
|year record high F = 115 |year record high F =
|Jan high F = 47.2 |Jan avg record high F = 58.7
|Feb high F = 53.1 |Feb avg record high F = 64.2
|Mar high F = 58.7 |Mar avg record high F = 70.4
|Apr high F = 65.9 |Apr avg record high F = 77.0
|May high F = 72.8 |May avg record high F = 83.3
|Jun high F = 81.4 |Jun avg record high F = 91.3
|Jul high F = 89.9 |Jul avg record high F = 97.4
|Aug high F = 89.5 |Aug avg record high F = 97.5
|Sep high F = 83.5 |Sep avg record high F = 93.7
|Oct high F = 73.5 |Oct avg record high F = 85.1
|Nov high F = 57.7 |Nov avg record high F = 70.9
|Dec high F = 47.5 |Dec avg record high F = 59.3
|year high F = 68.3 |year avg record high F = 99.1
|Jan low F = 25.6 | Jan high F = 47.5
|Feb low F = 28.1 | Feb high F = 51.2
|Mar low F = 31.0 | Mar high F = 56.7
|Apr low F = 35.9 | Apr high F = 63.1
|May low F = 41.6 | May high F = 70.5
|Jun low F = 47.3 | Jun high F = 80.5
|Jul low F = 53.2 | Jul high F = 89.2
|Aug low F = 52.0 | Aug high F = 89.0
|Sep low F = 46.7 | Sep high F = 83.0
|Oct low F = 38.3 | Oct high F = 70.9
|Nov low F = 30.2 | Nov high F = 56.0
|Dec low F = 26.2 | Dec high F = 45.9
|year low F = 38.0 |year high F = 67.0
|Jan record low F = -6 |Jan mean F = 38.0
|Feb mean F = 40.7
|Mar mean F = 45.1
|Apr mean F = 50.4
|May mean F = 57.5
|Jun mean F = 65.8
|Jul mean F = 73.3
|Aug mean F = 72.9
|Sep mean F = 67.2
|Oct mean F = 56.1
|Nov mean F = 44.3
|Dec mean F = 36.8
|year mean F = 54.0
| Jan low F = 28.5
| Feb low F = 30.2
| Mar low F = 33.5
| Apr low F = 37.6
| May low F = 44.5
| Jun low F = 51.0
| Jul low F = 57.4
| Aug low F = 56.8
| Sep low F = 51.4
| Oct low F = 41.3
| Nov low F = 32.5
| Dec low F = 27.8
|year low F = 41.0
|Jan avg record low F = 19.2
|Feb avg record low F = 22.0
|Mar avg record low F = 25.2
|Apr avg record low F = 28.4
|May avg record low F = 35.2
|Jun avg record low F = 40.8
|Jul avg record low F = 49.8
|Aug avg record low F = 48.9
|Sep avg record low F = 42.0
|Oct avg record low F = 31.6
|Nov avg record low F = 25.4
|Dec avg record low F = 20.7
|year avg record low F = 15.7
|Jan record low F = -7
|Feb record low F = 1 |Feb record low F = 1
|Mar record low F = 9 |Mar record low F = 9
|Apr record low F = 12 |Apr record low F = 12
|May record low F = 15 |May record low F = 15
|Jun record low F = 14 |Jun record low F = 22
|Jul record low F = 32 |Jul record low F = 32
|Aug record low F = 32 |Aug record low F = 32
Line 265: Line 316:
|Nov record low F = 10 |Nov record low F = 10
|Dec record low F = -1 |Dec record low F = -1
|year record low F = -6 |year record low F =
|precipitation colour = green |precipitation colour = green
|Jan precipitation inch = 6.51 | Jan precipitation inch = 6.98
|Feb precipitation inch = 6.17 | Feb precipitation inch = 6.49
|Mar precipitation inch = 5.39 | Mar precipitation inch = 5.47
|Apr precipitation inch = 3.04 | Apr precipitation inch = 3.17
|May precipitation inch = 1.47 | May precipitation inch = 1.92
|Jun precipitation inch = 0.70 | Jun precipitation inch = 0.46
|Jul precipitation inch = 0.31 | Jul precipitation inch = 0.29
|Aug precipitation inch = 0.20 | Aug precipitation inch = 0.16
|Sep precipitation inch = 0.66 | Sep precipitation inch = 0.40
|Oct precipitation inch = 1.91 | Oct precipitation inch = 1.56
|Nov precipitation inch = 3.93 | Nov precipitation inch = 4.05
|Dec precipitation inch = 5.97 | Dec precipitation inch = 5.60
|year precipitation inch = 36.55

| unit precipitation days = 0.01 in
|Jan snow inch = 16.2
| Jan precipitation days = 8.9
|Feb snow inch = 14.6
| Feb precipitation days = 9.0
|Mar snow inch = 12.9
| Mar precipitation days = 11.0
|Apr snow inch = 5.1
|May snow inch = 0.2 | Apr precipitation days = 7.2
| May precipitation days = 6.4
|Jun snow inch = 0
| Jun precipitation days = 2.2
|Jul snow inch = 0
| Jul precipitation days = 1.1
|Aug snow inch = 0
|Sep snow inch = 0 | Aug precipitation days = 0.9
| Sep precipitation days = 2.0
|Oct snow inch = 0.2
|Nov snow inch = 3.6 | Oct precipitation days = 3.5
| Nov precipitation days = 5.9
|Dec snow inch = 12.5
| Dec precipitation days = 8.5
|year snow inch = 65.6
|unit precipitation days = 0.01 in | year precipitation days = 66.6
|Jan precipitation days = 9 |Jan snow inch = 16.8
|Feb precipitation days = 9 |Feb snow inch = 4.2
|Mar precipitation days = 10 |Mar snow inch = 5.2
|Apr precipitation days = 7 |Apr snow inch = 0.8
|May precipitation days = 5 |May snow inch = 0.0
|Jun precipitation days = 3 |Jun snow inch = 0.0
|Jul precipitation days = 1 |Jul snow inch = 0.0
|Aug precipitation days = 1 |Aug snow inch = 0.0
|Sep precipitation days = 2 |Sep snow inch = 0.0
|Oct precipitation days = 4 |Oct snow inch = 0.0
|Nov precipitation days = 6 |Nov snow inch = 3.4
|Dec precipitation days = 8 |Dec snow inch = 5.1
|year snow inch =

|unit snow days = 0.1 in
|source 1= WRCC (1905-2012)<ref name= WRCC/>
|Jan snow days = 2.5
|date=December 2015}}
|Feb snow days = 1.4
|Mar snow days = 1.5
|Apr snow days = 0.4
|May snow days = 0.0
|Jun snow days = 0.0
|Jul snow days = 0.0
|Aug snow days = 0.0
|Sep snow days = 0.0
|Oct snow days = 0.0
|Nov snow days = 0.5
|Dec snow days = 1.5
|year snow days =
|Jan light = 10.0
|Feb light = 11.0
|Mar light = 12.0
|Apr light = 13.0
|May light = 14.0
|Jun light = 15.0
|Jul light = 14.0
|Aug light = 14.0
|Sep light = 12.0
|Oct light = 11.0
|Nov light = 10.0
|Dec light = 10.0
|year light = 12.0
|Jan uv = 2
|Feb uv = 4
|Mar uv = 6
|Apr uv = 7
|May uv = 9
|Jun uv = 10
|Jul uv = 11
|Aug uv = 10
|Sep uv = 8
|Oct uv = 5
|Nov uv = 3
|Dec uv = 2
|source 1 = NOAA (snow/snow days 1981&ndash;2010)<ref>{{cite web
| url = https://w2.weather.gov/climate/xmacis.php?wfo=hnx
| title = NOWData – NOAA Online Weather Data
| publisher = ]
| access-date = June 8, 2021
| archive-date = May 11, 2021
| archive-url = https://web.archive.org/web/20210511112537/https://w2.weather.gov/climate/xmacis.php?wfo=hnx
| url-status = live
}}</ref><ref>{{cite web
| url = https://www.ncei.noaa.gov/access/services/data/v1?dataset=normals-monthly-1991-2020&startDate=0001-01-01&endDate=9996-12-31&stations=USC00049855&format=pdf
| title = Summary of Monthly Normals 1991–2020
| publisher = ]
| access-date = June 8, 2021
| archive-date = June 9, 2021
| archive-url = https://web.archive.org/web/20210609001602/https://www.ncei.noaa.gov/access/services/data/v1?dataset=normals-monthly-1991-2020&startDate=0001-01-01&endDate=9996-12-31&stations=USC00049855&format=pdf
| url-status = live
}}</ref><ref>{{cite web
|url = https://www.ncei.noaa.gov/access/services/data/v1?dataset=normals-monthly&stations=USC00049855&format=pdf&dataTypes=MLY-TMAX-NORMAL,MLY-TMIN-NORMAL,MLY-TAVG-NORMAL,MLY-PRCP-NORMAL,MLY-SNOW-NORMAL
|publisher = National Oceanic and Atmospheric Administration
|title = U.S. Climate Normals Quick Access – Station: Yosemite Park Headquarters, CA (1981&ndash;2010)
|access-date = May 27, 2023
|archive-date = May 27, 2023
|archive-url = https://web.archive.org/web/20230527180047/https://www.ncei.noaa.gov/access/services/data/v1?dataset=normals-monthly&stations=USC00049855&format=pdf&dataTypes=MLY-TMAX-NORMAL,MLY-TMIN-NORMAL,MLY-TAVG-NORMAL,MLY-PRCP-NORMAL,MLY-SNOW-NORMAL
|url-status = live
}}</ref>
|source 2 = Weather Atlas<ref name="Weather Atlas">{{cite web |url=https://www.weather-us.com/en/california-usa/yosemite-national-park-climate |title=Yosemite National Park, California, USA – Monthly weather forecast and Climate data |publisher=Weather Atlas |access-date=26 January 2019 |archive-date=September 29, 2019 |archive-url=https://web.archive.org/web/20190929020825/https://www.weather-us.com/en/california-usa/yosemite-national-park-climate |url-status=live }}</ref>}}


{{Clear}} {{Clear}}


==Geology== ==Geology==
{{Main article|Geology of the Yosemite area}} {{Main|Geology of the Yosemite area}}
] image)]]

===Tectonic and volcanic activity=== ===Tectonic and volcanic activity===
{{See also|Tioga Pass caldera}}
] image)]]
The location of the park was a ] during the ] and early ].<ref name="GeologyNP328"/> Sediment was derived from continental sources and was deposited in shallow water. These rocks became deformed and metamorphosed.<ref>{{cite journal |title=Review of Late Jurassic-early Miocene sedimentationand plate-tectonic evolution of northern California: illuminatingexample of an accretionary margin |first=WG |last=Ernst |journal=Chin. J. Geochem. |year=2015 |volume=34 |issue=2 |pages=123–42 |doi=10.1007/s11631-015-0042-x |bibcode=2015Geoch..34..123E |s2cid=55662231 |url=http://english.gyig.cas.cn/pu/papers_CJG/201505/P020150515379493168537.pdf |archive-url=https://web.archive.org/web/20200321144527/http://english.gyig.cas.cn/pu/papers_CJG/201505/P020150515379493168537.pdf |archive-date=2020-03-21 |url-status=live}}</ref><ref>{{cite conference|title=Paleotectonic and paleogeographic significance of the Calaveras Complex, western Sierra Nevada, California|last1=Schweickert|first1=Richard A|last2=Saleeby|first2=Jason B|last3=Tobisch|first3=Othmar T|last4=Wright|first4=William H. III|year=1977|conference=Paleozoic paleogeography of the western United States : Pacific Coast Paleogeography Symposium I|publisher=Society of Economic Paleontologists and Mineralogists|location=Los Angeles, California|pages=381–94|url=https://authors.library.caltech.edu/53867/|access-date=November 3, 2020|archive-date=September 17, 2020|archive-url=https://web.archive.org/web/20200917180152/https://authors.library.caltech.edu/53867/|url-status=live}}</ref>


Heat generated from the ] ] below the ] led to the creation of an ] of volcanoes on the west coast of proto-North America between the late ] and ] periods.<ref name="GeologyNP328">{{harvnb|Harris|1998|p=328}}</ref> Material accreted onto the western edge of North America, and mountains were raised to the east in Nevada.<ref>{{cite web|title=Yosemite National Park Geologic Resources Inventory Report|url=http://npshistory.com/publications/yose/nrr-2012-560.pdf |archive-url=https://web.archive.org/web/20190109062212/http://npshistory.com/publications/yose/nrr-2012-560.pdf |archive-date=2019-01-09 |url-status=live|publisher=National Park Service|id=Natural Resource Report NPS/NRSS/GRD/NRR—2012/560|pages=43–44}}</ref>
The area of the park was astride a ] during the ] and early ].<ref name="GeologyNP328"/> Sediment was derived from continental sources and was deposited in shallow water. These rocks have since been metamorphosed.


The first phase of regional ] started 210&nbsp;million years ago in the late Triassic and continued throughout the Jurassic to about 150&nbsp;million years before present (]), which led to the creation of the ].<ref name="GeologyNP329"/> The resulting rocks were mostly granitic in composition and lay about {{convert|6|mi|km}} below the surface.<ref name="GeologyNP337">{{harvnb|Harris|1998|p=337}}</ref> Around the same time, the ] built the Nevadan mountain range (also called the Ancestral Sierra Nevada) to a height of {{convert|15000|ft|m}}.
Heat generated from the ] ] below the ] led to the creation of an ] of volcanoes on the west coast of proto-North America between the late ] and ] periods.<ref name="GeologyNP328">{{harvnb|Harris|1998|p=328}}</ref> Later volcanism in the ] intruded and covered these rocks in what may have been magmatic activity associated with the early stages of the creation of the Sierra Nevada Batholith. 95% of these rocks were eventually removed by uplifted-accelerated erosion.


The second major pluton emplacement phase lasted from about 120&nbsp;million to 80&nbsp;million years ago during the ].<ref name="GeologyNP329"/> This was part of the ].<ref>{{Cite journal|last1=Yonkee|first1=W. Adolph|last2=Weil|first2=Arlo Brandon|date=2015-11-01|title=Tectonic evolution of the Sevier and Laramide belts within the North American Cordillera orogenic system|journal=Earth-Science Reviews|language=en|volume=150|pages=531–93|doi=10.1016/j.earscirev.2015.08.001|bibcode=2015ESRv..150..531Y|issn=0012-8252|doi-access=}}</ref>
The first phase of regional ] started 210 million years ago in the late Triassic and continued throughout the Jurassic to about 150 million years before present (]).<ref name="GeologyNP329"/> Around the same time, the ] built the Nevadan mountain range (also called the Ancestral Sierra Nevada) to a height of {{convert|15000|ft|m}}. This was directly part of the creation of the Sierra Nevada Batholith, and the resulting rocks were mostly granitic in composition and emplaced about {{convert|6|mi|km}} below the surface.<ref name="GeologyNP337">{{harvnb|Harris|1998|p=337}}</ref> The second major pluton emplacement phase lasted from about 120 million to 80 million years ago during the ].<ref name="GeologyNP329"/> This was part of the ].


Starting 20 million years ago (in the ]) and lasting until 5 million years ago, a now-extinct extension of ] ]es erupted, bringing large amounts of igneous material in the area. These igneous deposits blanketed the region north of the Yosemite region. Volcanic activity persisted past 5 million years BP east of the current park borders in the Mono Lake and ] areas. Starting 20&nbsp;million years ago (in the ]) and lasting until 5&nbsp;million years ago, a now-extinct extension of ] volcanoes erupted, bringing large amounts of igneous material in the area. These igneous deposits blanketed the region north of the Yosemite region. Volcanic activity persisted past 5&nbsp;million years BP east of the current park borders in the Mono Lake and ] areas.<ref>{{cite book|title = Geology of the Sierra Nevada|last = Hill|first = Mary|location = Berkeley, California|publisher = University of California Press|year = 2006|page=270}}</ref>


===Uplift and erosion=== ===Uplift and erosion===
]s cause erosion in granitic rocks, creating many ] including ].]]
Starting 10 million years ago, vertical movement along the Sierra fault started to uplift the Sierra Nevada. Subsequent tilting of the Sierra block and the resulting accelerated uplift of the Sierra Nevada increased the ] of western-flowing streams.<ref name="GeologyNP339">{{harvnb|Harris|1998|p=339}}</ref> The streams consequently ran faster and thus cut their valleys more quickly. Additional uplift occurred when major faults developed to the east, especially the creation of ] from ]-associated extensional forces. Uplift of the Sierra accelerated again about two million years ago during the ].
Starting 10&nbsp;million years ago, vertical movement along the Sierra fault started to uplift the Sierra Nevada. Subsequent tilting of the Sierra block and the resulting accelerated uplift of the Sierra Nevada increased the ] of western-flowing streams.<ref name="GeologyNP339">{{harvnb|Harris|1998|p=339}}</ref> The streams consequently ran faster and thus cut their valleys more quickly. Additional uplift occurred when major faults developed to the east, forming ] from ]-associated extensional forces. Sierra uplift accelerated again about two million years ago during the ].<ref>{{cite book |last1=Konigsmark |first1=Ted |title=Geologic Trips, Sierra Nevada |year=2002 |publisher=GeoPress |isbn=0966131657 |page=234 |url=http://www.geologictrips.com/sn/snttyv.pdf |archive-url=https://web.archive.org/web/20120515201942/http://www.geologictrips.com/sn/snttyv.pdf |archive-date=2012-05-15 |url-status=live |access-date=22 September 2021}}</ref>
] joints have modified the near-surface portions of massive granitic rocks in the park, helping create the many spectacular domes, including Half Dome shown here.]]
The uplifting and increased erosion exposed granitic rocks in the area to surface pressures, resulting in exfoliation (responsible for the rounded shape of the many domes in the park) and mass wasting following the numerous fracture joint planes (cracks; especially vertical ones) in the now solidified plutons.<ref name="GeologyNP332">{{harvnb|Harris|1998|p=332}}</ref> Pleistocene glaciers further accelerated this process and the larger ones transported the resulting ] and ] from valley floors.


The uplifting and increased erosion exposed granitic rocks to surface pressures, resulting in exfoliation (responsible for the rounded shape of the many domes in the park) and mass wasting following the numerous fracture joint planes (cracks; especially vertical ones) in the now solidified plutons.<ref name="GeologyNP332">{{harvnb|Harris|1998|p=332}}</ref> ] glaciers further accelerated this process, while glacial meltwater transported the resulting ] and ] from valley floors.<ref name=Huber>{{cite book|first=N. King|last=Huber|title=The Geologic Story of Yosemite National Park|location=Washington|publisher=Government Printing Office|year=1987|id=USGS Bulletin 1595|chapter=Final Evolution of the Landscape|chapter-url=https://www.yosemite.ca.us/library/geologic_story_of_yosemite/final_evolution.html|access-date=July 5, 2022|archive-date=March 31, 2022|archive-url=https://web.archive.org/web/20220331161402/http://www.yosemite.ca.us/library/geologic_story_of_yosemite/final_evolution.html|url-status=live}}</ref>
Numerous vertical joint planes controlled where and how fast erosion took place. Most of these long, linear and very deep cracks trend northeast or northwest and form parallel, often regularly spaced sets. They were created by uplift-associated pressure release and by the unloading of overlying rock via erosion.


Numerous vertical joint planes controlled where and how fast erosion took place. Most of these long, linear and very deep cracks trend northeast or northwest and form parallel, often regularly spaced sets.<ref name=Huber/>
===Sculpting by glaciers===

A series of glaciations further modified the region starting about 2 to 3 million years ago and ending sometime around 10,000 BP. At least four major glaciations have occurred in the Sierra Nevada, locally called the Sherwin (also called the pre-Tahoe), Tahoe, Tenaya, and Tioga.<ref name="GeologyNP339"/> The Sherwin glaciers were the largest, filling Yosemite and other valleys, while later stages produced much smaller glaciers. A Sherwin-age glacier was almost surely responsible for the major excavation and shaping of Yosemite Valley and other canyons in the area.
===Glacial sculpting===
]
] in upper ]]]
Glacial systems reached depths of up to {{convert|4000|ft|m}} and left their marks in the Yosemite area. The longest glacier in the Yosemite area ran down the Grand Canyon of the Tuolumne River for {{convert|60|mi|km}}, passing well beyond Hetch Hetchy Valley. Merced Glacier flowed out of Yosemite Valley and into the Merced River Gorge. Lee Vining Glacier carved Lee Vining Canyon and emptied into Lake Russel (the much-enlarged ice age version of Mono Lake). Only the highest peaks, such as Mount Dana and Mount Conness, were not covered by glaciers. Retreating glaciers often left recessional ]s that impounded lakes such as the {{convert|5.5|mi|km|0}} long Lake Yosemite (a shallow lake that periodically covered much of the floor of Yosemite Valley).<ref name="GeologyNP333">{{harvnb|Harris|1998|p=333}}</ref>
A series of glaciations further modified the region starting about 2 to 3&nbsp;million years ago and ending sometime around 10,000 BP. At least four major glaciations occurred in the Sierra, locally called the Sherwin (also called the pre-Tahoe), Tahoe, Tenaya, and Tioga.<ref name="GeologyNP339"/> The Sherwin glaciers were the largest, filling Yosemite and other valleys, while later stages produced much smaller glaciers. A Sherwin-age glacier was almost surely responsible for the major excavation and shaping of Yosemite Valley and other canyons in the area.<ref>{{Cite web|title=Volcanoes of the Eastern Sierra Nevada|url=https://sierra.sitehost.iu.edu/papers/2012/klapperich.html|access-date=2021-06-28|website=sierra.sitehost.iu.edu|archive-date=June 28, 2021|archive-url=https://web.archive.org/web/20210628032933/https://sierra.sitehost.iu.edu/papers/2012/klapperich.html|url-status=live}}</ref>

Glacial systems reached depths of up to {{convert|4000|ft|m}} and left their marks. The longest glacier ran down the Grand Canyon of the Tuolumne River for {{convert|60|mi|km}}, passing well beyond Hetch Hetchy Valley. Merced Glacier flowed out of Yosemite Valley and into the Merced River Gorge. Lee Vining Glacier carved Lee Vining Canyon and emptied into Lake Russel (the much-enlarged ice age version of Mono Lake). Only the highest peaks, such as Mount Dana and Mount Conness, were not covered by glaciers. Retreating glaciers often left recessional ]s that impounded lakes such as the {{convert|5.5|mi|km|0}} long Lake Yosemite (a shallow lake that periodically covered much of the floor of Yosemite Valley).<ref name="GeologyNP333">{{harvnb|Harris|1998|p=333}}</ref>


==Ecology== ==Ecology==
Line 342: Line 459:


===Habitats=== ===Habitats===
] in Yosemite Valley]] ] in Yosemite Valley]]
The park has an elevation range from {{convert|2127|to|13114|ft|m}} and contains five major ]: ] and ] woodland, ], upper ], ], and ]. Of California's 7,000 plant species, approximately 50 percent occur in the Sierra Nevada and more than 20 percent within the park. The park contains suitable habitat for more than 160 rare plants, with rare local ] formations and unique ]s characterizing the restricted ranges many of these plants occupy.<ref name="naturehistory" />
With its scrubby sun-baked ], stately groves of pine, fir, and sequoia, and expanses of alpine woodlands and meadows, Yosemite National Park preserves a Sierra Nevada landscape as it prevailed before Euro-American settlement.<ref name = "snepLateSuccessional">{{Cite book

| first = Jerry, F
With its scrubby sun-baked ], stately groves of pine, fir, and sequoia, and expanses of alpine woodlands and meadows, Yosemite National Park preserves a Sierra landscape as it prevailed before Euro-American settlement.<ref name="snepLateSuccessional">{{Cite book
| last = Franklin
| first1 = Jerry F.
| last1 = Franklin
| first2 = Jo Ann | first2 = Jo Ann
| last2 = Fites-Kaufmann | last2 = Fites-Kaufmann
| chapter = 21: Assessment of Late-Successional Forests of the Sierra Nevada | chapter = 21: Assessment of Late-Successional Forests of the Sierra Nevada
| year = 1996 | year = 1996
| pages = 627–671 | pages = 627–71
| title = Sierra Nevada Ecosystem Project. Final Report to Congress. Status of the Sierra Nevada Volume II: Assessments and Scientific Basis for Management Options | title = Sierra Nevada Ecosystem Project. Final Report to Congress. Status of the Sierra Nevada
| volume = II: Assessments and Scientific Basis for Management Options
| publisher = Centers for Water and Wildland Resources, University of California
| url = http://pubs.usgs.gov/dds/dds-43/VOL_II/VII_C21.PDF | format=PDF
| chapter-url = http://pubs.usgs.gov/dds/dds-43/VOL_II/VII_C21.PDF
| isbn=1-887673-01-6}}</ref> In contrast to surrounding lands, which have been significantly altered by logging, the park still contains some {{convert|225510|acre}} of ].<ref name = "1993OldGrowthEstimates">{{Cite journal
| isbn = 1887673016
| last1 = Bolsinger | first1 = Charles L.
| access-date = December 10, 2014
| last2 = Waddell | first2 = Karen L.
| archive-date = May 13, 2019
| archive-url = https://web.archive.org/web/20190513155027/https://pubs.usgs.gov/dds/dds-43/VOL_II/VII_C21.PDF
| url-status = live
}}</ref> In contrast to surrounding lands, which have been significantly altered by logging, the park contains some {{convert|225510|acre}} of ].<ref name="1993OldGrowthEstimates">{{Cite journal
| last1 = Bolsinger
| first1 = Charles L.
| last2 = Waddell
| first2 = Karen L.
| year = 1993 | year = 1993
| title = Area of old-growth forests in California, Oregon, and Washington | title = Area of old-growth forests in California, Oregon, and Washington
| url = http://www.fs.fed.us/pnw/pubs/pnw_rb197.pdf | url = http://www.fs.fed.us/pnw/pubs/pnw_rb197.pdf
| publisher = ], Pacific Northwest Research Station | publisher = ], Pacific Northwest Research Station
| id = Resource Bulletin PNW-RB-197 | journal = Resource Bulletin
| postscript = <!--None--> | issue = 197
| id = PNW-RB-197
}}</ref> Taken together, the park's varied ] support over 250 species of ]s, which include fish, ]ns, ]s, birds, and mammals.<ref name = "wildlife">{{NPS|source={{cite web | title = Wildlife Overview | url = http://www.nps.gov/archive/yose/nature/wildlife.htm | archiveurl=https://web.archive.org/web/20070127153544/http://www.nps.gov/archive/yose/nature/wildlife.htm|archivedate=January 27, 2007 | publisher = National Park Service: Yosemite Park Service | date = December 22, 2004 }} }}</ref>
| access-date = February 10, 2009
]
| archive-date = October 23, 2020
Along much of Yosemite's western boundary, habitats are dominated by ]s of ], ], ], ], ], and a few stands of giant sequoia, interspersed by areas of ] and ]. A relatively high diversity of wildlife species is supported by these habitats, because of relatively mild, lower-elevation climate and the mixture of habitat types and plant species. Wildlife species typically found in these habitats include ], ], ], ], ], ], ], ], ], ], ], two species of ], ], ], and a wide variety of bat species.<ref name="wildlife"/>
| archive-url = https://web.archive.org/web/20201023223431/https://www.fs.fed.us/pnw/pubs/pnw_rb197.pdf
| url-status = live
}}</ref> Taken together, the park's varied ] support over 250 species of ]s, which include fish, amphibians, reptiles, birds, and mammals.<ref name="wildlife">{{NPS| title = Wildlife Overview | url = http://www.nps.gov/archive/yose/nature/wildlife.htm | archive-url=https://web.archive.org/web/20070127153544/http://www.nps.gov/archive/yose/nature/wildlife.htm|archive-date=January 27, 2007 | publisher = National Park Service: Yosemite Park Service | date = December 22, 2004 }}</ref>

Yosemite's western boundary has habitats dominated by ]s of ], ], ], ], ], and a few stands of giant sequoia, interspersed by areas of ] and ]. These habitats support relatively high wildlife diversity. Wildlife include ], ], ], ], ], ], ], ], ], ], ], two species of skunk, ], ], and bats.<ref name="wildlife"/>

At higher elevation, the coniferous forests become purer stands of ], ], ], ], and the occasional ]. Fewer wildlife species tend to be found in these habitats, because of their higher elevation and lower complexity. Animals include ], ], ], ], ], and ]. Reptiles are not common, but include ], ], and ].<ref name = "wildlife"/>


] in ]]]
Going higher in elevation, the coniferous forests become purer stands of ], ], ], ], and the occasional ]. Fewer wildlife species tend to be found in these habitats, because of their higher elevation and lower complexity. Species likely to be found include ], ], ], ], ], and ]. Reptiles are not common, but include ], ], and ].<ref name = "wildlife"/>
As the landscape rises, trees become smaller and more sparse, with stands broken by areas of exposed granite. These include lodgepole pine, ], and ] that, at highest elevations, give way to vast expanses of granite as treeline is reached. The climate in these habitats is harsh and the growing season is short, but species such as ], ], white-tailed ], ], and ] are adapted to these conditions. Treeless alpine habitats are favored by ]. This species is found in the Yosemite area only around Tioga Pass, where a small, reintroduced population exists.<ref name = "wildlife"/>
] in ].]]
As the landscape rises, trees become smaller and more sparse, with stands broken by areas of exposed granite. These include lodgepole pine, ], and ] that, at highest elevations, give way to vast expanses of granite as treeline is reached. The climate in these habitats is harsh and the growing season is short, but species such as ], ], white-tailed ], ], and ] are adapted to these conditions. Also, the treeless alpine habitats are the areas favored by ]. This species, however, is now found in the Yosemite area only around Tioga Pass, where a small, reintroduced population exists.<ref name = "wildlife"/>


At a variety of elevations, meadows provide important, productive habitat for wildlife. Animals come to feed on the green ] and use the flowing and standing water found in many meadows. ], in turn, are attracted to these areas. The interface between meadow and forest is also favored by many animal species because of the proximity of open areas for foraging and cover for protection. Species that are highly dependent upon meadow habitat include ], ], ], and ].<ref name = "wildlife"/> At a variety of elevations, meadows provide important habitat. Animals come to feed on the green ] and use the flowing and standing water found in many meadows. Predators follow these animals. The interface between meadow and forest is favored by many animal species because of the proximity of open areas for foraging and cover for protection. Species that are highly dependent upon meadow habitat include ], ], ], and ].<ref name = "wildlife"/>


===Management issues=== ===Management issues===
] with a conspicuous ear tag browsing on its natural foods in Yosemite Valley]] ] with an ear tag in Yosemite Valley]]
The black bears of Yosemite were once famous for breaking into parked cars to steal food. They were an encouraged tourist sight for many years at the park's garbage dumps, where they congregated to eat garbage, and tourists gathered to photograph them. Increasing bear/human encounters and increasing property damage led to an aggressive campaign to discourage bears from interacting with people and their stuff. The open-air dumps were closed; trash receptacles were replaced with ] receptacles; campgrounds were equipped with bear-proof food lockers so that people would not leave food in their vehicles. Because bears who show aggression towards people usually are destroyed, park personnel have come up with innovative ways to lead bears to associate humans and their property with experiences such as getting hit with a ]. {{as of|2001}}, about 30 bears a year were captured and ] and their ] sampled so that, when bear damage occurs, rangers can ascertain which bear was causing the problem.<ref>{{cite magazine | url= http://news.nationalgeographic.com/news/2001/04/0423_wirebears.html | archive-url= https://web.archive.org/web/20010430063837/http://news.nationalgeographic.com/news/2001/04/0423_wirebears.html | url-status= dead | archive-date= April 30, 2001 | title= DNA to Help Identify "Problem" Bears at Yosemite | magazine= National Geographic | date = April 23, 2001 | access-date=January 4, 2007}}</ref>{{update inline|date=November 2020}}
Despite the richness of high-quality habitats in Yosemite, the ], ], and ] have become ] in the park within historical time,<ref name = "snepTerrestrialVertebrates">{{Cite book | first = David M. | last = Graber | chapter = 25: Status of Terrestrial Vertebrates | year = 1996 | pages = 709–734 | title = Sierra Nevada Ecosystem Project. Final Report to Congress. Status of the Sierra Nevada Volume II: Assessments and Scientific Basis for Management Options | url = http://pubs.usgs.gov/dds/dds-43/VOL_II/VII_C25.PDF | format=PDF|isbn=1-887673-01-6}}</ref> and another 37 species currently have special status under either California or federal ] legislation. The most serious current threats to Yosemite's wildlife and the ecosystems they occupy include loss of a natural fire regime, ], ], ], and climate change. On a more local basis, factors such as ]s and the availability of human food have affected some wildlife species.


Despite the richness of high-quality habitats in Yosemite, the ], ], and ] have become extinct in the park within historical time,<ref name = "snepTerrestrialVertebrates">{{Cite book | first = David M. | last = Graber | chapter = 25: Status of Terrestrial Vertebrates | year = 1996 | pages = 709–34 | title = Sierra Nevada Ecosystem Project. Final Report to Congress. Status of the Sierra Nevada Volume II: Assessments and Scientific Basis for Management Options | publisher = Centers for Water and Wildland Resources, University of California | url = http://pubs.usgs.gov/dds/dds-43/VOL_II/VII_C25.PDF | isbn = 1887673016 | access-date = December 10, 2014 | archive-date = June 20, 2020 | archive-url = https://web.archive.org/web/20200620143941/https://pubs.usgs.gov/dds/dds-43/VOL_II/VII_C25.PDF | url-status = live }}</ref> and another 37 species currently have special status under either California or federal ] legislation. The most serious current threats include loss of a natural fire regime, ], air pollution, ], and climate change. On a more local basis, factors such as ]s and the availability of human food have affected some wildlife species.<ref>{{Cite web |last=Stephens |first=Tim |title=Yosemite bears and human food: Study reveals changing diets over past century |url=https://news.ucsc.edu/2014/03/yosemite-bears.html |access-date=2022-06-27 |website=UC Santa Cruz News |language=en |archive-date=June 18, 2022 |archive-url=https://web.archive.org/web/20220618204900/https://news.ucsc.edu/2014/03/yosemite-bears.html |url-status=live }}</ref><ref>{{Cite web |last=Hughes |first=Trevor |title=National park visitors leave roadkill in their wake |url=https://www.usatoday.com/story/news/nation/2013/07/27/national-park-road-kill/2587753/ |access-date=2022-06-27 |website=USA TODAY |language=en-US |archive-date=June 27, 2022 |archive-url=https://web.archive.org/web/20220627011811/https://www.usatoday.com/story/news/nation/2013/07/27/national-park-road-kill/2587753/ |url-status=live }}</ref>
] are competing with native plants in Yosemite.]]
The black bears of Yosemite were once famous for breaking into parked cars to steal food. They were also an encouraged tourist sight for many years at the park's ]s, where bears congregated to eat park visitors' garbage and tourists gathered to photograph the bears. Increasing encounters between bears and humans and increasing damage to property led to an aggressive campaign to discourage bears from relying on human food or interacting with people and their property. The open-air dumps were closed; all trash receptacles were replaced with ] receptacles; all campgrounds were equipped with bear-proof food lockers so that people would not leave food in their vehicles, which were easy targets for the powerful and resourceful bears. Because bears who show aggression towards people usually are eventually destroyed, park personnel have continued to come up with innovative ways to have bears associate humans and their property with unpleasant experiences, such as being hit with ]s. Today, about 30 bears a year are captured and ] and their ] is sampled so that, when bear damage occurs, rangers can ascertain which bear is causing the problem.<ref>{{cite news | url= http://news.nationalgeographic.com/news/2001/04/0423_wirebears.html | title= DNA to Help Identify "Problem" Bears at Yosemite | publisher= National Geographic | date = April 23, 2001 | accessdate=January 4, 2007}}</ref>


] competes with Yosemite's native plants.<ref name = "exotic"/>]]
Increasing ] pollution is causing tissue damage to the massive giant sequoia trees in the park. This makes them more vulnerable to ] infestation and ]. Since the ] of these trees require fire-touched soil to ], historic ] has reduced these trees' ability to reproduce. The current policy of setting ]s is expected to help the germination issue.
Yosemite National Park has documented the presence of more than 130 non-native plant species within park boundaries. They were introduced into Yosemite following the migration of early ] settlers in the late 1850s. Natural and human-caused disturbances, such as wildland fires and construction activities, have contributed to a rapid increase in the spread of non-native plants. Some of these species invade and displace the native plant communities, impacting park resources. Non-native plants can bring about significant ecosystem changes by altering native plant communities and the processes that support them. Some non-native species may cause an increase in fire frequency or increase the available soil nitrogen that allow other non-native plants to establish. Many non-native species, such as ] (''Centaurea solstitialis''), are able to produce a long ] that allows them to out-compete the native plants for available water.<ref name = "exotic">{{cite web | url= http://www.nps.gov/archive/yose/nature/veg_exotics.htm | archive-url=https://web.archive.org/web/20070102234435/http://www.nps.gov/archive/yose/nature/veg_exotics.htm|archive-date=January 2, 2007 | title= Exotic Plants | date = December 22, 2004| publisher= National Park Service: Yosemite National Park | access-date= January 4, 2007 }}</ref>


Bull thistle ('']''), common mullein ('']''), and Klamath weed ('']'') have been identified as noxious ] in Yosemite since the 1940s. More recently recognized species are yellow star thistle (''Centaurea solstitialis''), sweet clover ('']'' spp.), Himalayan blackberry ('']''), cut-leaved blackberry ('']'') and large periwinkle ('']'').<ref name = "exotic"/>
Yosemite National Park has documented more than 130 non-native plant ] within park boundaries. These non-native plants were introduced into Yosemite following the migration of early ] settlers in the late 1850s. Natural and human-caused disturbances, such as wildland fires and construction activities, have contributed to a rapid increase in the spread of non-native plants. A number of these species aggressively invade and displace the native plant communities, resulting in impacts on the park's resources. Non-native plants can bring about significant changes in park ecosystems by altering the native plant communities and the processes that support them. Some non-native species may cause an increase in the fire frequency of an area or increase the available ] in the soil that may allow more non-native plants to become established. Many non-native species, such as ] (''Centaurea solstitialis''), are able to produce a long ] that allows them to out-compete the native plants for available water.<ref name = "exotic">{{cite web | url= http://www.nps.gov/archive/yose/nature/veg_exotics.htm | archiveurl=https://web.archive.org/web/20070102234435/http://www.nps.gov/archive/yose/nature/veg_exotics.htm|archivedate=January 2, 2007 | title= Exotic Plants | date = December 22, 2004| publisher= National Park Service: Yosemite National Park | accessdate= January 4, 2007 }}</ref>


Increasing ] pollution causes tissue damage to sequoia trees, making them more vulnerable to insect infestation and disease. Since the ] of these trees require fire-touched soil to ], historic ] has reduced their ability to reproduce. Planned ]s may help the germination issue.<ref>{{Cite web|title=Giant Sequoias and Fire – Sequoia & Kings Canyon National Parks (U.S. National Park Service)|url=https://www.nps.gov/seki/learn/nature/giant-sequoias-and-fire.htm|access-date=2021-04-08|website=www.nps.gov|language=en|archive-date=August 24, 2021|archive-url=https://web.archive.org/web/20210824004759/https://www.nps.gov/seki/learn/nature/giant-sequoias-and-fire.htm|url-status=live}}</ref>
Bull thistle ('']''), common mullein ('']''), and Klamath weed ('']'') have been identified as noxious ] in Yosemite since the 1940s. Additional species that have been recognized more recently as aggressive and requiring control are yellow star thistle (''Centaurea solstitialis''), sweet clover ('']'' spp.), Himalayan blackberry ('']''), cut-leaved blackberry ('']'') and large periwinkle ('']'').<ref name = "exotic"/>
{{Clear}}


===Wildfires=== ===Wildfires ===
] burns in Little Yosemite Valley, 2014]] ] burns in Little Yosemite Valley, 2014]]
Indigenous residents intentionally set small fires in the early 1860s and before to clear the ground of brush as part as their farming practices.<ref name="Spence" /> These fires are comparable to contemporary practices such as ]s that are done by the U.S. Forest Service and others. Although it was not their primary reason, Yosemite Natives helped preserve biodiversity and resilience by lighting these small fires. Native Americans used fire as an early ] tool to keep certain lands clear, resulting in more food for large animals and decreasing the chance of large forest fires which that now devastate forest ecosystems.<ref name=":5">{{Cite web |last=Johnson |first=Eric Michael |title=How John Muir's Brand of Conservation Led to the Decline of Yosemite |url=https://blogs.scientificamerican.com/primate-diaries/how-john-muir-s-brand-of-conservation-led-to-the-decline-of-yosemite/ |access-date=2022-04-21 |website=Scientific American Blog Network |language=en |archive-date=May 22, 2022 |archive-url=https://web.archive.org/web/20220522193645/https://blogs.scientificamerican.com/primate-diaries/how-john-muir-s-brand-of-conservation-led-to-the-decline-of-yosemite/ |url-status=live }}</ref> Some early uncontrolled forest fires were set accidentally by the militia group led by Major John Savage when the group burned down the Ahwahneechee camp in an attempt to expel them. The house fires eventually spread to a large section of the forest and the militia group ended up having to abandon their raid to save their own camp from the conflagration.<ref name=":5" />
Forest fires seasonally clear the park of dead vegetation, making way for new growth.<ref name = "Evergreen Magazine">{{cite web | url= http://evergreenmagazine.com/magazine/article/Are_there_good_forest_fires_.html | archiveurl= https://web.archive.org/web/20140315012328/http://evergreenmagazine.com/magazine/article/Are_there_good_forest_fires_.html | archivedate= 2014-03-15 | title= Are There Good Forest Fires? | date = Summer 2002| publisher= Evergreen Magazine | accessdate= 14 March 2014 }}</ref> These fires are detrimental to the ecology of the park,<ref name = "Evergreen Magazine"/> and also damage the income generated by tourism. The Summer of Fire saw more resources dedicated to the subject of wildfire than ever before or since in the United States. The most recent fire, the ], which destroyed nearly $2 billion in assets and revenue, closed off much of the park to tourists.<ref name = "National Park Service Fires">{{cite web | url= http://www.nps.gov/yell/naturescience/wildlandfire.htm | archiveurl= http://www.webcitation.org/6Vq3bJUPi | archivedate= 2015-01-25 | title= History of Wildland Fire in Yosemite Park | date = 14 March 2014| publisher= National Park Service | accessdate= 14 March 2014 }}</ref> This rim fire was the third largest on record, and burned nearly 500 acres of wild habitat.<ref name = "National Park Service Fires"/>

Forest fires clear the park of dead vegetation, making way for new growth.<ref name="Evergreen Magazine">{{cite web | url= http://evergreenmagazine.com/magazine/article/Are_there_good_forest_fires_.html | archive-url= https://web.archive.org/web/20140315012328/http://evergreenmagazine.com/magazine/article/Are_there_good_forest_fires_.html | archive-date= 2014-03-15 | title= Are There Good Forest Fires? | date = Summer 2002| publisher= Evergreen Magazine | access-date= 14 March 2014 }}</ref> Small fires damage the income generated by tourism. During late July and early August, 2018, the Valley and other sections of the park, temporarily closed due to the ] at its western boundary.<ref>{{Cite news|url=https://www.fresnobee.com/news/local/article215400735.html|title=Yosemite Valley will close due to fire. 'Get yourself out of here,' official says|work=fresnobee|access-date=2018-07-24|archive-date=July 24, 2018|archive-url=https://web.archive.org/web/20180724213643/https://www.fresnobee.com/news/local/article215400735.html|url-status=live}}</ref> The closing was the largest in almost thirty years.<ref>{{Cite news |url=https://www.nytimes.com/2018/07/25/us/yosemite-national-park-fire.html |title=Yosemite National Park Evacuated Amid Threat From Fire |newspaper=The New York Times |date=July 25, 2018 |access-date=2018-07-30 |last1=Branch |first1=John |last2=Medina |first2=Jennifer |last3=Fountain |first3=Henry |archive-date=July 30, 2018 |archive-url=https://web.archive.org/web/20180730140726/https://www.nytimes.com/2018/07/25/us/yosemite-national-park-fire.html |url-status=live }}</ref>


==Activities== ==Activities==
] Shuttle, Yosemite's free ] system]] ]
]]]


===Public access===
Yosemite Valley is open year-round and numerous activities are available through the ], Yosemite Conservancy, and ] at Yosemite, including nature walks, photography and art classes, stargazing programs, tours, bike rentals, rafting, mule and horseback rides, and rock climbing classes. Many people enjoy short walks and longer hikes to waterfalls in Yosemite Valley, or walks among giant sequoias in the Mariposa, Tuolumne, or Merced Groves. Others like to drive or take a tour bus to Glacier Point (summer–fall) to see a spectacular view of Yosemite Valley and the high country, or drive along the scenic ] to Tuolumne Meadows (May–October) and go for a walk or hike.
Yosemite National Park is open year-round, though certain roads close during snowy months, usually from November through May or June.<ref>{{Cite web|title=Operating Hours & Seasons|work=Yosemite National Park|publisher=U.S. National Park Service|url=https://www.nps.gov/yose/planyourvisit/hours.htm|access-date=2023-12-02|language=en|archive-date=December 2, 2023|archive-url=https://web.archive.org/web/20231202200909/https://www.nps.gov/yose/planyourvisit/hours.htm|url-status=live}}</ref> Certain trails also close during winter, including The 4-Mile Trail and part of The Mist Trail.<ref>{{Cite web |title=Yosemite in Winter |url=https://www.yosemitehikes.com/yosemite-info/yosemite-in-winter.htm |access-date=2023-12-02 |website=www.yosemitehikes.com |archive-date=October 29, 2023 |archive-url=https://web.archive.org/web/20231029030722/https://www.yosemitehikes.com/yosemite-info/yosemite-in-winter.htm |url-status=live }}</ref>


Traffic congestion in the valley is heavy during peak summer season (June to August) and a free ] operates in the valley. Parking in the valley during the summer is often full.<ref>{{cite web | url = http://www.nps.gov/yose/planyourvisit/bus.htm | publisher = National Park Service: Yosemite National Park | title = Bus | date = May 27, 2009 | access-date = May 8, 2010 | archive-date = October 24, 2020 | archive-url = https://web.archive.org/web/20201024201830/https://www.nps.gov/yose/planyourvisit/bus.htm | url-status = live }}</ref> Transit options are available from ] and ].<ref name=Marshall>{{cite magazine | last1=Marshall | first1=Aarian | title=Hiking or Camping? Take the Bus to the Trail This Summer | url=https://www.wired.com/story/hiking-camping-take-bus-trail-summer/ | magazine=] | date=May 24, 2019 | access-date=June 9, 2019 | archive-date=May 24, 2019 | archive-url=https://web.archive.org/web/20190524124352/https://www.wired.com/story/hiking-camping-take-bus-trail-summer/ | url-status=live }}</ref>
Most park visitors stay just for the day, and only visit locations within Yosemite Valley that are easily accessible by automobile. There is a ]25-30 per automobile user fee to enter the park, depending on the season.<ref>{{cite web | url = http://www.nps.gov/yose/planyourvisit/feesandreservations.htm | title = Fees and Reservations}} National Park Service: Yosemite National Park. Retrieved on October 27, 2007.</ref> Traffic congestion in the valley is a serious problem during peak season, in summer. A free ] operates year-round in the valley, and ]s encourage people to use this system since parking within the valley during the summer is often nearly impossible to find.<ref>{{cite web | url = http://www.nps.gov/yose/planyourvisit/bus.htm | publisher = National Park Service: Yosemite National Park | title = Bus | date = May 27, 2009 }}</ref>


In addition to exploring the natural features of the park, visitors can also learn about the ] and ] history of Yosemite Valley at a number of facilities in the valley: the Yosemite Valley Visitor Center, the adjoining Yosemite Museum, and the Nature Center at Happy Isles. There are also two ]s: the ]'s ] (Yosemite's first public visitor center), and the world-famous Ahwahnee Hotel. Camp 4 was added to the ] in 2003.<ref>{{cite web |title = Camp 4 Listed With National Register of Historic Places The natural and cultural history of Yosemite Valley is presented at the Yosemite Valley Visitor Center, the adjoining Yosemite Museum, and the Nature Center at Happy Isles. The parks' two ]s are the ]'s ] (Yosemite's first public visitor center), and the Ahwahnee Hotel. Camp 4 is on the ].<ref>{{cite web |title = Camp 4 Listed With National Register of Historic Places
| work = NPS Press Release | publisher =National Park Service | date = February 27, 2003 |url = http://www.nps.gov/archive/yose/news/2003/camp0227.htm |archiveurl = https://web.archive.org/web/20070316120511/http://www.nps.gov/archive/yose/news/2003/camp0227.htm |archivedate = 2007-03-16 |accessdate = December 14, 2008 }}</ref> | work = NPS Press Release | publisher =National Park Service | date = February 27, 2003 |url = http://www.nps.gov/archive/yose/news/2003/camp0227.htm |archive-url = https://web.archive.org/web/20070316120511/http://www.nps.gov/archive/yose/news/2003/camp0227.htm |archive-date = 2007-03-16 |access-date = December 14, 2008 }}</ref>


===Hiking=== ===Hiking===
]]] ] cables on a busy summer day in 2008]]
Over {{convert|800|mi|km}} of trails are available to hikers<ref name="naturehistory"/>—everything from an easy stroll to a challenging mountain hike, or ]. The popular Half Dome hike to the summit of ] requires a permit whenever the cables are up (usually from ] weekend to ]).<ref>{{Cite web|title=Half Dome Day Hike|work=Yosemite National Park|publisher=U.S. National Park Service|url=https://www.nps.gov/yose/planyourvisit/halfdome.htm|access-date=2023-01-02|archive-date=October 30, 2018|archive-url=https://web.archive.org/web/20181030101332/https://www.nps.gov/yose/planyourvisit/halfdome.htm|url-status=live}}</ref> A maximum of 300 hikers, selected by lottery, are permitted to advance beyond the base of the subdome each day, including 225 day hikers and 75 backpackers.<ref>{{Cite web|title=Half Dome Permits for Day Hikers|work=Yosemite National Park|publisher=U.S. National Park Service|url=https://www.nps.gov/yose/planyourvisit/hdpermits.htm|access-date=2023-01-02|archive-date=November 18, 2018|archive-url=https://web.archive.org/web/20181118095956/https://www.nps.gov/yose/planyourvisit/hdpermits.htm|url-status=live}}</ref>
Over {{convert|800|mi|km}} of trails are available to hikers<ref name="naturehistory"/>—anything from the easy stroll, to the grueling hikes up several park mountains, to multiple-day ].


The park can be divided into 5 sections for the day-user—Yosemite Valley, Wawona/Mariposa Grove/Glacier Point, Tuolumne Meadows, Hetch Hetchy, and ]/White Wolf.<ref>{{cite web|url = http://www.yosemitehikes.com/hikes.htm|title = Yosemite Hikes|first = Russ|last = Cary}}</ref> Numerous books describe park trails, and free information is available from the Park Service in Yosemite. Park rangers encourage visitors to experience portions of the park in addition to Yosemite Valley. The park can be divided into five sections—Yosemite Valley, Wawona/Mariposa Grove/Glacier Point, Tuolumne Meadows, Hetch Hetchy, and ]/White Wolf.<ref>{{cite web|url = http://www.yosemitehikes.com/hikes.htm|title = Yosemite Hikes|first = Russ|last = Cary|access-date = May 27, 2009|archive-date = November 14, 2020|archive-url = https://web.archive.org/web/20201114062806/https://www.yosemitehikes.com/hikes.htm|url-status = live}}</ref> Numerous books describe park trails, while the National Park Service provides free information.


Between late spring and early fall, much of the park can be accessed for multiple-day backpacking trips. All overnight trips into the back country require a wilderness permit<ref name = "permits"/> and most require approved bear-resistant food storage.<ref name = "food storage">{{cite web | publisher = National Park Service: National Park Service | url = http://www.nps.gov/yose/planyourvisit/bears.htm| title = Bear and food storage | date = February 10, 2010}}</ref> Between late spring and early fall, much of the park can be accessed for backpacking trips. All overnight trips into the back country require a wilderness permit<ref name = "permits"/> and most require approved bear-resistant food storage.<ref name = "food storage">{{cite web | publisher = National Park Service: National Park Service | url = http://www.nps.gov/yose/planyourvisit/bears.htm | title = Bear and food storage | date = February 10, 2010 | access-date = May 8, 2010 | archive-date = November 11, 2020 | archive-url = https://web.archive.org/web/20201111191930/https://www.nps.gov/yose/planyourvisit/bears.htm | url-status = live }}</ref>


===Driving destinations=== ===Driving===
{{Further|List of Yosemite destinations}} {{Further|List of Yosemite destinations}}
While some locations in Yosemite require hiking, other locations can be reached via automobile transportation. Driving locations also allow guests to observe the night sky in locations other than their campsite or lodge. All of the roads in Yosemite are scenic, but the most famous is the Tioga Road, typically open from late May or early June through November.<ref name = "auto touring">{{cite web | publisher = National Park Service: Yosemite National Park | title = Auto Touring | url =http://www.nps.gov/yose/planyourvisit/touring.htm | date = December 22, 2004 | accessdate = January 27, 2007 }}</ref> While some locations in Yosemite are accessible only on foot, other locations can be reached via road. The most famous road is ].<ref name = "auto touring">{{cite web | publisher = National Park Service: Yosemite National Park | title = Auto Touring | url = http://www.nps.gov/yose/planyourvisit/touring.htm | date = December 22, 2004 | access-date = January 27, 2007 | archive-date = October 28, 2020 | archive-url = https://web.archive.org/web/20201028214728/https://www.nps.gov/yose/planyourvisit/touring.htm | url-status = live }}</ref>


As an alternative to driving, bicycles are allowed on the roads. However, bicycles are only allowed off-road on {{convert|12|mi|km}} of paved trails in Yosemite Valley itself; mountain biking is not allowed.<ref name="bike">{{cite web | title= Biking | url = http://www.nps.gov/yose/planyourvisit/biking.htm | publisher = National Park Service: Yosemite National Park |date=March 2007 | accessdate = March 23, 2007 }}</ref> Bicycles are allowed on the roads, but only {{convert|12|mi|km}} of paved off-road trails are available in Yosemite Valley itself; mountain biking is not allowed.<ref name="bike">{{cite web | title = Biking | url = http://www.nps.gov/yose/planyourvisit/biking.htm | publisher = National Park Service: Yosemite National Park | date = March 2007 | access-date = March 23, 2007 | archive-date = November 11, 2020 | archive-url = https://web.archive.org/web/20201111223459/https://www.nps.gov/yose/planyourvisit/biking.htm | url-status = live }}</ref>


===Climbing=== ===Climbing===
] ]] ]]]
Rock climbing is an important part of Yosemite.<ref name="climbing">{{cite web | title = Climbing | url = http://www.nps.gov/yose/planyourvisit/climbing.htm | publisher = National Park Service: Yosemite National Park | date = December 11, 2008}}</ref> ], a walk-in campground in Yosemite Valley, was instrumental in the development of rock climbing as a sport, and is listed on the National Register of Historic Places.<ref name = "camp4">{{cite press release | title = Camp 4 Listed With National Register of Historic Places | publisher = National Park Service: Yosemite National Park | date = February 27, 2003 | url = http://www.nps.gov/archive/yose/news/2003/camp0227.htm | archiveurl = https://web.archive.org/web/20070316120511/http://www.nps.gov/archive/yose/news/2003/camp0227.htm | archivedate = 2007-03-16 | accessdate = January 27, 2007 }}</ref> Climbers can generally be spotted in the snow-free months on anything from ten-foot-high (3&nbsp;m) boulders to the {{convert|3300|ft|km|adj=on}} face of El Capitan. Classes are offered by numerous groups on rock climbing. Rock climbing is an important part of Yosemite.<ref name="climbing">{{cite web | title = Climbing | url = http://www.nps.gov/yose/planyourvisit/climbing.htm | publisher = National Park Service: Yosemite National Park | date = December 11, 2008 | access-date = May 8, 2010 | archive-date = October 29, 2020 | archive-url = https://web.archive.org/web/20201029191818/https://www.nps.gov/yose/planyourvisit/climbing.htm | url-status = live }}</ref> In particular the valley is surrounded by summits such as Half Dome and El Capitan. ] is a walk-in campground in the Valley that was instrumental in the development of rock climbing as a sport, and is listed on the ].<ref name = "camp4">{{cite press release | title = Camp 4 Listed With National Register of Historic Places | publisher = National Park Service: Yosemite National Park | date = February 27, 2003 | url = http://www.nps.gov/archive/yose/news/2003/camp0227.htm | archive-url = https://web.archive.org/web/20070316120511/http://www.nps.gov/archive/yose/news/2003/camp0227.htm | archive-date = 2007-03-16 | access-date = January 27, 2007 }}</ref> Climbers can generally be spotted in the snow-free months on anything from ten-foot-high (3&nbsp;m) boulders to the {{convert|3300|ft|km|adj=on}} face of El Capitan. Classes on rock climbing are offered there.

] is well known for ].


===Winter activities=== ===Winter activities===
] walk in the park]] ] walk in the park]]
Yosemite Valley is open all year, although some roads within the park close in winter. ] is available at the ]—the oldest downhill skiing area in California, offering downhill skiing from mid-December through early April.<ref name="skiing">{{cite web |url = http://www.nps.gov/yose/planyourvisit/wintersports.htm | title= Skiing | publisher = National Park Service: Yosemite National Park | date = September 21, 2006 | accessdate = January 27, 2007 }}</ref> Much of the park is open to ] and ]ing, with several backcountry ski huts open for use.<ref name = "TuolumneWinter">{{cite web | publisher = National Park Service: Yosemite National Park | title = Tuolumne Meadows Winter Conditions Update | url = http://www.nps.gov/yose/planyourvisit/tm.htm | accessdate = January 27, 2007 }}</ref><ref name="winter">{{cite web | publisher = National Park Service: Yosemite National Park | title = Winter Wilderness Travel | url = http://www.nps.gov/yose/planyourvisit/wildwinter.htm | date = March 2, 2010}}</ref> Wilderness permits are required for backcountry overnight ski trips.<ref name = "permits">{{cite web | title = Wilderness Permits | publisher = National Park Service: Yosemite National Park | url = http://www.nps.gov/yose/planyourvisit/wildpermits.htm| date = February 12, 2010 }}</ref> Away from the Valley, the park is snowed in during the winter months, with many roads closed. ] is available at the ]—the oldest downhill skiing area in California, operating from mid-December through early April.<ref name="skiing">{{cite web | url = http://www.nps.gov/yose/planyourvisit/wintersports.htm | title = Skiing | publisher = National Park Service: Yosemite National Park | date = September 21, 2006 | access-date = January 27, 2007 | archive-date = December 4, 2020 | archive-url = https://web.archive.org/web/20201204132654/https://www.nps.gov/yose/planyourvisit/wintersports.htm | url-status = live }}</ref> Much of the park is open to ] and ]ing, and backcountry ski huts are available.<ref name = "TuolumneWinter">{{cite web | publisher = National Park Service: Yosemite National Park | title = Tuolumne Meadows Winter Conditions Update | url = http://www.nps.gov/yose/planyourvisit/tm.htm | access-date = January 27, 2007 | archive-date = October 21, 2020 | archive-url = https://web.archive.org/web/20201021224249/https://www.nps.gov/yose/planyourvisit/tm.htm | url-status = live }}</ref><ref name="winter">{{cite web | publisher = National Park Service: Yosemite National Park | title = Winter Wilderness Travel | url = http://www.nps.gov/yose/planyourvisit/wildwinter.htm | date = March 2, 2010 | access-date = May 8, 2010 | archive-date = November 12, 2020 | archive-url = https://web.archive.org/web/20201112010734/https://www.nps.gov/yose/planyourvisit/wildwinter.htm | url-status = live }}</ref> Wilderness permits are required for backcountry overnight ski trips.<ref name = "permits">{{cite web | title = Wilderness Permits | publisher = National Park Service: Yosemite National Park | url = http://www.nps.gov/yose/planyourvisit/wildpermits.htm | date = February 12, 2010 | access-date = May 8, 2010 | archive-date = December 15, 2020 | archive-url = https://web.archive.org/web/20201215221816/https://www.nps.gov/yose/planyourvisit/wildpermits.htm | url-status = live }}</ref>


The ] is an annual holiday event, held since 1927 at the Ahwahnee Hotel, inspired by ]'s descriptions of Squire Bracebridge and English ] traditions of the 18th century in his ''Sketch Book''. Between 1929 and 1973, the show was organized by ].<ref name="Bracebridge">{{cite web | title = History | work = The Bracebridge Dinner at Yosemite| url = http://www.bracebridgedinners.com/history.html| archiveurl = http://www.webcitation.org/69H6AhPtm| archivedate = 2012-07-19 | accessdate = May 8, 2010}}</ref> The ] is an annual holiday event, held since 1927 at the Ahwahnee Hotel, inspired by ]'s descriptions of Squire Bracebridge and English ] traditions of the 18th century in his ''Sketch Book''. Between 1929 and 1973, the show was organized by ].<ref name="Bracebridge">{{cite web|title=History |work=The Bracebridge Dinner at Yosemite |url=http://www.bracebridgedinners.com/history.html |archive-url=https://web.archive.org/web/20120312225909/http://www.bracebridgedinners.com/history.html |archive-date=March 12, 2012 |access-date=May 8, 2010 |url-status=dead }}</ref>


===Other=== ===Other===
Yosemite has 13 official campgrounds.<ref>{{cite web | url = https://spkcamping.com/camping-in-yosemite-national-park/ | title = Yosemite camping | access-date = January 16, 2023 | archive-date = January 16, 2023 | archive-url = https://web.archive.org/web/20230116110719/https://spkcamping.com/camping-in-yosemite-national-park/ | url-status = live }}</ref>
Bicycle rentals are available in Yosemite Valley spring through fall. Over {{convert|12|mi|km}} of paved bike paths are available in Yosemite Valley. In addition, bicyclists can ride on regular roads. ] are required by law for children under 18 years of age. Off-trail riding and ] are not permitted in Yosemite National Park.<ref>{{cite web|url=http://www.nps.gov/archive/yose/pphtml/planyourvisit.html|archiveurl=https://web.archive.org/web/20090221050244/http://www.nps.gov/archive/yose/pphtml/planyourvisit.html|archivedate=February 21, 2009|title=Plan Your Visit|work=Yosemite National Park|publisher=U.S. National Park Service}}</ref>


Bicycle rentals are available from spring through fall. Over {{convert|12|mi|km}} of paved bike paths are available in Yosemite Valley. In addition, bicyclists can ride on roads. Helmets are required for children under 18 years of age. Off-trail riding and ] are not permitted in the park.<ref>{{cite web|url=http://www.nps.gov/archive/yose/pphtml/planyourvisit.html|archive-url=https://web.archive.org/web/20090221050244/http://www.nps.gov/archive/yose/pphtml/planyourvisit.html|archive-date=February 21, 2009|title=Plan Your Visit|work=Yosemite National Park|publisher=U.S. National Park Service}}</ref>
Water activities are plentiful during warmer months. Rafting can be done through the Yosemite Valley on the Merced River. There are also swimming pools available at Yosemite Lodge and Curry Village.
{{Clear}}


Water activities are plentiful during warmer months. Rafting can be done through the valley on the Merced River from late May to July.<ref>{{cite book |last1=Brown |first1=Ann Marie |title=Moon Yosemite, Sequoia & Kings Canyon Hiking, Camping, Waterfalls & Big Trees |date=2015 |publisher=Avalon Publishing |isbn=9781640494459|at=Rafting}}</ref> Swimming pools are available at Yosemite Lodge and Curry Village.
In 2010, Yosemite National Park was honored with its own quarter under the ] program.<ref>{{cite web|url=http://www.americathebeautifulquarters.gov/coins/2010/yosemite|archiveurl=https://web.archive.org/web/20110721032931/http://www.americathebeautifulquarters.gov/coins/2010/yosemite|archivedate=July 21, 2011|title=Yosemite National Parks Quarter|publisher=U.S. Mint}}</ref>

===Horsetail Fall===
] flows over the eastern edge of El Capitan. This small waterfall usually flows only during winter and is easy to miss. On rare occasions during mid- to late February, it can glow orange when backlit by sunset. This unique lighting effect happens only on evenings with a clear sky. Minor haze or cloudiness can spoil the effect. Although entirely natural, the phenomenon is reminiscent of the human-caused Firefall that historically occurred from Glacier Point.

==In popular culture==
] sign advising young visitors to not feed the bears at Yosemite National Park.]]
The opening scenes of '']'' (1989) were filmed in Yosemite National Park. Films such as '']'' (1920) and '']'' (1994) have also been shot there.<ref>Maddrey, Joseph (2016). ''The Quick, the Dead and the Revived: The Many Lives of the Western Film''. McFarland. p. 175. {{ISBN|978-1476625492}}.</ref> The 2014 documentary '']'' is centered around Yosemite Valley and its history with an emphasis on climbing culture.<ref>{{Citation|last1=Mortimer|first1=Peter|title=Valley Uprising|date=2014-09-01|url=https://www.imdb.com/title/tt3784160/|type=Documentary|others=Peter Sarsgaard, Alex Honnold, Yvon Chouinard, Royal Robbins|publisher=Sender Films, Big UP Productions|access-date=2021-04-26|last2=Rosen|first2=Nick|last3=Lowell|first3=Josh|archive-date=June 13, 2019|archive-url=https://web.archive.org/web/20190613102243/https://www.imdb.com/title/tt3784160/|url-status=live}}</ref> The Academy Award-winning 2018 documentary '']'' was filmed in Yosemite.<ref>{{Cite news|last=Catsoulis|first=Jeannette|date=September 27, 2018|title=Review: In 'Free Solo,' Braving El Capitan With Only Fingers and Toes|work=The New York Times|url=https://www.nytimes.com/2018/09/27/movies/free-solo-review-alex-honnold-el-capitan.html|access-date=2020-09-04|archive-date=April 21, 2022|archive-url=https://web.archive.org/web/20220421222107/https://www.nytimes.com/2018/09/27/movies/free-solo-review-alex-honnold-el-capitan.html|url-status=live}}</ref> ''],'' a 2017 documentary, was filmed there.<ref>{{Citation|last1=Lowell|first1=Josh|title=The Dawn Wall|date=2018-07-17|url=https://www.imdb.com/title/tt7286916/|type=Documentary, Biography, Sport|others=John Branch, Tommy Caldwell, Kevin Jorgeson|publisher=Red Bull Media House, Sender Films|access-date=2021-04-26|last2=Mortimer|first2=Peter|archive-date=April 21, 2022|archive-url=https://web.archive.org/web/20220421222117/https://www.imdb.com/title/tt7286916/|url-status=live}}</ref>


==See also== ==See also==
{{columns-list|colwidth=30em|
{{Portal|California}}
* ]
* ]
* ]
* ]
* ]
* ] * ]
* ] * ]
* ]
* ]
* ]
* ] for further reading about the ]
* ] * ]
* ] * ]
* ]
* ]
* ]
* ] – Warner Bros. theatrical cartoon character
* ]
* ], a community inside the gates of the park
* ], a short-line railroad that replaced stagecoach travel to the park
}}


==Notes== ==Citations==
{{Reflist|33em}} {{clear right}}
{{reflist}}


==General references==
==References==
{{refbegin}} {{refbegin}}
* {{cite book|last=Berkowitz|first=Paul D.|title=Legacy of the Yosemite Mafia: Noble Cause Corruption in the National Park Service|publisher=Trine Day Publishing|location=Walterville Oregon|year=2017|isbn=978-1-63424-126-7}}
* {{Cite book|title = Yosemite: the Park and its Resources|last = Greene|first = Linda Wedel|publisher = U.S. Department of the Interior / National Park Service|year = 1987|isbn = |location = |url = http://www.yosemite.ca.us/library/yosemite_resources/yosemite_resources.pdf|archiveurl = https://web.archive.org/web/20110606144808/http://www.yosemite.ca.us/library/yosemite_resources/yosemite_resources.pdf|archivedate = 2011-06-06|ref=harv}}
* Diamant, Rolf and Carr, Ethan (2022). ''Olmsted and Yosemite: Civil War, Abolition, and The National Park Idea''. Amherst, Massachusetts: Library of American Landscape History {{ISBN|9781952620348}}
* {{cite book|last=Harris|first=Ann G.|title=Geology of National Parks|edition=Fifth|location=Kendall, Iowa|publisher=Hunt Publishing|year=1998|isbn=0-7872-5353-7|ref=harv}}
* {{Cite book|title = Yosemite: the Park and its Resources|last = Greene|first = Linda Wedel|publisher = U.S. Department of the Interior / National Park Service|year = 1987|url = http://www.yosemite.ca.us/library/yosemite_resources/yosemite_resources.pdf|archive-url = https://web.archive.org/web/20110606144808/http://www.yosemite.ca.us/library/yosemite_resources/yosemite_resources.pdf|archive-date = 2011-06-06}}
* {{cite book|last1=Kiver|first1=Eugene P.|first2=David V.|last2=Harris|title=Geology of U.S. Parklands|edition=Fifth|publisher=John Wiley & Sons|location=New York|year=1999|isbn= 0-471-33218-6|ref=harv}}
* {{cite book|last=Harris|first=Ann G.|title=Geology of National Parks|edition=Fifth|location=Kendall, Iowa|publisher=Hunt Publishing|year=1998|isbn=0787253537}}
* Muir, John. "" ''The Century; a popular quarterly'' (Sept. 1890) 40#5
* {{cite book|last=Schaffer|first=Jeffrey P.|title=Yosemite National Park: A Natural History Guide to Yosemite and Its Trails|publisher=Wilderness Press|location=Berkeley|year=1999|isbn=0-89997-244-6|ref=harv}} * {{cite book|last1=Kiver|first1=Eugene P.|first2=David V.|last2=Harris|title=Geology of U.S. Parklands|edition=Fifth|publisher=John Wiley & Sons|location=New York|year=1999|isbn= 0471332186}}
* Muir, John. " {{Webarchive|url=https://web.archive.org/web/20170917105738/http://ebooks.library.cornell.edu/cgi/t/text/pageviewer-idx?c=cent;cc=cent;rgn=full%20text;idno=cent0040-5;didno=cent0040-5;view=image;seq=0666;node=cent0040-5%3A2 |date=September 17, 2017 }}" ''The Century; a popular quarterly'' (Sept. 1890) 40#5
* {{cite book|last=Wuerthner|first=George|title=Yosemite: A Visitor's Companion|publisher=Stackpole Books|year=1994|isbn=0-8117-2598-7|ref=harv}}
* {{cite book|last=Schaffer|first=Jeffrey P.|title=Yosemite National Park: A Natural History Guide to Yosemite and Its Trails|publisher=Wilderness Press|location=Berkeley|year=1999|isbn=0899972446}}
* {{cite book|last=Wuerthner|first=George|title=Yosemite: A Visitor's Companion|publisher=Stackpole Books|year=1994|isbn=0811725987|url=https://archive.org/details/yosemitevisitors00wuer}}
* {{cite book|title=Yosemite: Official National Park Service Handbook|volume=138|publisher=Division of Publications, National Park Service|year=1989|ref={{harvid|NPS|1989}}}} * {{cite book|title=Yosemite: Official National Park Service Handbook|volume=138|publisher=Division of Publications, National Park Service|year=1989|ref={{harvid|NPS|1989}}}}
* {{NPS}} * {{NPS}}
** {{cite web|url=http://www.nps.gov/archive/yose/nature/wtr_climate.htm|title=Climate|date=December 22, 2004|accessdate=January 27, 2007|archiveurl=https://web.archive.org/web/20070101113353/http://www.nps.gov/archive/yose/nature/wtr_climate.htm|archivedate=January 1, 2007|publisher=National Park Service}} ** {{cite web|url=http://www.nps.gov/archive/yose/nature/wtr_climate.htm|title=Climate|date=December 22, 2004|access-date=January 27, 2007|archive-url=https://web.archive.org/web/20070101113353/http://www.nps.gov/archive/yose/nature/wtr_climate.htm|archive-date=January 1, 2007|publisher=National Park Service}}
** {{cite web|url=http://www.nps.gov/archive/yose/nature/veg_exotics.htm|title=Exotic Vegetation|date=December 22, 2004|accessdate=January 27, 2007|archiveurl=https://web.archive.org/web/20070102234435/http://www.nps.gov/archive/yose/nature/veg_exotics.htm|archivedate=January 2, 2007|publisher=National Park Service}} ** {{cite web|url=http://www.nps.gov/archive/yose/nature/veg_exotics.htm|title=Exotic Vegetation|date=December 22, 2004|access-date=January 27, 2007|archive-url=https://web.archive.org/web/20070102234435/http://www.nps.gov/archive/yose/nature/veg_exotics.htm|archive-date=January 2, 2007|publisher=National Park Service}}
** {{cite web|url=http://www.nps.gov/archive/yose/nature/nature.htm|title=Nature & History|date=October 13, 2006|accessdate=January 27, 2007|archiveurl=https://web.archive.org/web/20070125062753/http://www.nps.gov/archive/yose/nature/nature.htm|archivedate=January 25, 2007|publisher=National Park Service}} ** {{cite web|url=http://www.nps.gov/archive/yose/nature/nature.htm|title=Nature & History|date=October 13, 2006|access-date=January 27, 2007|archive-url=https://web.archive.org/web/20070125062753/http://www.nps.gov/archive/yose/nature/nature.htm|archive-date=January 25, 2007|publisher=National Park Service}}
** {{cite web|url=http://www.nps.gov/archive/yose/nature/water.htm|title=Water Overview|date=December 22, 2004|accessdate=January 27, 2007|archiveurl=https://web.archive.org/web/20070107180730/http://www.nps.gov/archive/yose/nature/water.htm|archivedate=January 7, 2007|publisher=National Park Service}} ** {{cite web|url=http://www.nps.gov/archive/yose/nature/water.htm|title=Water Overview|date=December 22, 2004|access-date=January 27, 2007|archive-url=https://web.archive.org/web/20070107180730/http://www.nps.gov/archive/yose/nature/water.htm|archive-date=January 7, 2007|publisher=National Park Service}}
** {{cite web|url=http://www.nps.gov/archive/yose/nature/wildlife.htm|title=Wildlife Overview|date=December 22, 2004|accessdate=January 27, 2007|archiveurl=https://web.archive.org/web/20070127153544/http://www.nps.gov/archive/yose/nature/wildlife.htm|archivedate=January 27, 2007|publisher=National Park Service}} ** {{cite web|url=http://www.nps.gov/archive/yose/nature/wildlife.htm|title=Wildlife Overview|date=December 22, 2004|access-date=January 27, 2007|archive-url=https://web.archive.org/web/20070127153544/http://www.nps.gov/archive/yose/nature/wildlife.htm|archive-date=January 27, 2007|publisher=National Park Service}}
{{refend}} {{refend}}


==External links== ==External links==
{{Spoken Misplaced Pages-2|2005-06-18|Yosemite_National_Park_(Part_1).ogg|Yosemite_Natinal_Park_(Part_2).ogg}} {{Spoken Misplaced Pages|date=2005-06-18|Yosemite_National_Park_(Part_1).ogg|Yosemite National Park (Part 2).oga}}
* {{Official website|https://www.nps.gov/yose/index.htm}} of the
{{Sister project links| wikt=no | commons=Yosemite National Park | b=no | n=no | q=no | s=Yosemite | v=no | voy=Yosemite National Park | species=no | d=no | display=Yosemite National Park}}
* {{Cite web |date=2019-03-18 |title=Providing for Yosemite's Future — Yosemite Conservancy |url=https://yosemite.org/ |access-date=2023-06-28 |website=yosemite.org |language=en-US}}
*
* {{Cite web |title=The Role of the Railroads in Yellowstone and Yosemite National Parks |url=http://xroads.virginia.edu/~MA96/RAILROAD/home.html |archive-url=https://web.archive.org/web/19971108063855/http://xroads.virginia.edu/~MA96/RAILROAD/home.html |url-status=dead |archive-date=November 8, 1997 |access-date=2023-06-28 |website=xroads.virginia.edu}} from American Studies at the University of Virginia
*
* *
* {{Cite web |url=http://thehive.modbee.com/?q=node%2F153 |title=Historic Yosemite Indian Chiefs – with photos |access-date=April 6, 2019 |archive-url=https://web.archive.org/web/20060521032840/http://thehive.modbee.com/?q=node%2F153 |archive-date=May 21, 2006 |url-status=dead}}
*
* {{Cite web |title=Edith Irvine's Historic Photographs of Yosemite National Park|url=https://contentdm.lib.byu.edu/digital/collection/EdithIrvine/search/searchterm/yosemite%20national%20park%20(calif.)/field/subjec/mode/all/conn/and/order/title/ad/asc |access-date=2023-06-28 |website=contentdm.lib.byu.edu}}
*
*
* from American Studies at the University of Virginia
* {{Cite book |last=Muir |first=John |url=http://dx.doi.org/10.5962/bhl.title.19229 |title=My first summer in the Sierra |date=1911 |publisher=Houghton Mifflin |location=Boston, Mass|doi=10.5962/bhl.title.19229 }} {{cite web|url=https://archive.org/details/my_first_summer_in_the_sierra_ap_0906_librivox/ |title=Audio recording |website=LibriVox.org|date=June 3, 2009 }}
;Media specific
{{Sister bar| wikt=no | commons=Yosemite National Park | b=no | n=no | q=no | s=Yosemite | v=no | voy=Yosemite National Park | species=no | d=no | display=Yosemite National Park}}
*
* {{wayback|url=http://thehive.modbee.com/?q=node/153 |title=Historic Yosemite Indian Chiefs—with photos |date=20060521032840}}
*
*
*
* by John Muir. Free MP3 audio recording from LibriVox.org

{{featured article}}
{{Yosemite National Park}} {{Yosemite National Park}}
{{Navboxes|title=Related links
|list1=
{{Sierra Nevada}}
{{National parks of the United States}} {{National parks of the United States}}
{{World Heritage Sites in the United States of America}} {{World Heritage Sites in the United States of America}}
{{Protected areas of California|NPS}} {{Protected areas of California|NPS}}
{{California}} {{California}}}}

{{Authority control}}


] ]
] ]
]
] ]
]
] ]
] ]
Line 497: Line 650:
] ]
] ]
] ]
] ]
] ]
]
]

Latest revision as of 05:37, 14 January 2025

National park in California, United States "Yosemite" redirects here. For other uses, see Yosemite (disambiguation).

Yosemite National Park
IUCN category II (national park)
Yosemite Valley from Tunnel View
Map showing the location of Yosemite National ParkMap showing the location of Yosemite National ParkYosemite National ParkLocation in CaliforniaShow map of CaliforniaMap showing the location of Yosemite National ParkMap showing the location of Yosemite National ParkYosemite National ParkLocation in the United StatesShow map of the United States
LocationTuolumne, Mariposa, Mono and Madera Counties, California, United States
Nearest cityMariposa, California
Coordinates37°44′33″N 119°32′15″W / 37.74250°N 119.53750°W / 37.74250; -119.53750
Area759,620 acres (3,074.1 km)
EstablishedOctober 1, 1890; 134 years ago (1890-10-01)
Visitors3,897,070 (in 2023)
Governing bodyNational Park Service
Websitenps.gov/yose Edit this at Wikidata
UNESCO World Heritage Site
CriteriaNatural: vii, viii
Reference308
Inscription1984 (8th Session)

Yosemite National Park (/joʊˈsɛmɪti/ yoh-SEM-ih-tee) is a national park of the United States in California. It is bordered on the southeast by Sierra National Forest and on the northwest by Stanislaus National Forest. The park is managed by the National Park Service and covers 759,620 acres (1,187 sq mi; 3,074 km) in four counties – centered in Tuolumne and Mariposa, extending north and east to Mono and south to Madera. Designated a World Heritage Site in 1984, Yosemite is internationally recognized for its granite cliffs, waterfalls, clear streams, groves of giant sequoia, lakes, mountains, meadows, glaciers, and biological diversity. Almost 95 percent of the park is designated wilderness. Yosemite is one of the largest and least fragmented habitat blocks in the Sierra Nevada.

Its geology is characterized by granite and remnants of older rock. About 10 million years ago, the Sierra Nevada was uplifted and tilted to form its unique slopes, which increased the steepness of stream and river beds, forming deep, narrow canyons. About one million years ago glaciers formed at higher elevations. They moved downslope, cutting and sculpting the U-shaped Yosemite Valley.

European American settlers first entered the valley in 1851. Other travelers entered earlier, but James D. Savage is credited with discovering the area that became Yosemite National Park. Native Americans had inhabited the region for nearly 4,000 years, although humans may have first visited as long as 8,000 to 10,000 years ago.

Yosemite was critical to the development of the concept of national parks. Galen Clark and others lobbied to protect Yosemite Valley from development, ultimately leading to President Abraham Lincoln's signing of the Yosemite Grant of 1864 that declared Yosemite as federally preserved land. In 1890, John Muir led a successful movement to motivate Congress to establish Yosemite Valley and its surrounding areas as a National Park. This helped pave the way for the National Park System. Yosemite draws about four million visitors annually. Most visitors spend the majority of their time in the valley's seven square miles (18 km). The park set a visitation record in 2016, surpassing five million visitors for the first time. In 2023, the park saw nearly four million visitors.

Toponym

The word Yosemite (derived from yohhe'meti, "they are killers" in Miwok) historically referred to the name that the Miwok gave to the Ahwahneechee People, the resident indigenous tribe. Previously, the region had been called "Ahwahnee" ("big mouth") by its only indigenous inhabitants, the Ahwahneechee. The term Yosemite in Miwok is easily confused with a similar term for "grizzly bear", and is still a common misconception.

History

Main article: History of the Yosemite area

Ahwahneechee and the Mariposa Wars

Paiute ceremony (1872)engraving of Dr Lafayette Bunnell, showing him as an older man with a craggy face, short bristly hair and a cropped grey beard.Lafayette Bunnell gave Yosemite Valley its name.

The indigenous natives of Yosemite called themselves the Ahwahneechee, meaning "dwellers" in Ahwahnee. The Ahwahneechee People were the only tribe that lived within the park boundaries, but other tribes lived in surrounding areas. Together they formed a larger Indigenous population in California, called the Southern Sierra Miwok. They are related to the Northern Paiute and Mono tribes. Other tribes like the Central Sierra Miwoks and the Yokuts, who both lived in the San Joaquin Valley and central California, visited Yosemite to trade and intermarry. This resulted in a blending of culture that helped preserve their presence in Yosemite after early American settlements and urban development threatened their survival. Vegetation and game in the region were similar to modern times; acorns were a dietary staple, as well as other seeds and plants, salmon and deer.

The 1848–1855 California Gold Rush was a major event impacting the native population. It drew more than 90,000 European Americans to the area in 1849, causing competition for resources between gold miners and residents. About 70 years before the Gold Rush, the indigenous population was estimated to be 300,000, quickly dropping to 150,000, and just ten years later, only about 50,000 remained. The reasons for such a decline included disease, birth rate decreases, starvation, and conflict. The conflict in Yosemite, which is known as the Mariposa War, was part of the California genocide, which was the systemic killing of indigenous peoples throughout the State between the 1840s and 1870s. It started in December 1850 when California funded a state militia to drive Native people from contested territory to suppress Native American resistance to the European American influx.

Yosemite tribes often stole from settlers and miners, sometimes killing them, in retribution for the extermination/domestication of their people, and loss of their lands and resources. The War and formation of the Mariposa Battalion was partially the result of a single incident involving James Savage, a Fresno trader whose trading post was attacked in December, 1850. After the incident, Savage rallied other miners and gained the support of local officials to pursue a war against the Natives. He was appointed United States Army Major and leader of the Mariposa Battalion in the beginning of 1851. He and Captain John Boling were responsible for pursuing the Ahwahneechee people, led by Chief Tenaya and driving them west, and out of Yosemite. In March 1851 under Savage's command, the Mariposa Battalion captured about 70 Ahwahneechee and planned to take them to a reservation in Fresno, but they escaped. Later in May, under the command of Boling, the battalion captured 35 Ahwahneechee, including Chief Tenaya, and marched them to the reservation. Most were allowed to eventually leave and the rest escaped. Tenaya and others fled across the Sierra Nevada and settled with the Mono Lake Paiutes. Tenaya and some of his companions were ultimately killed in 1853 either over stealing horses or a gambling conflict. The survivors of Tenaya's group and other Ahwahneechee were absorbed into the Mono Lake Paiute tribe.

Sculpture of Chief Tenaya made by Sal Maccarone for the Tenaya Lodge in Yosemite National Park

Accounts from this battalion were the first well-documented reports of European Americans entering Yosemite Valley. Attached to Savage's unit was Doctor Lafayette Bunnell, who later wrote about his awestruck impressions of the valley in The Discovery of the Yosemite. Bunnell is credited with naming Yosemite Valley, based on his interviews with Chief Tenaya. Bunnell wrote that Chief Tenaya was the founder of the Ahwahnee colony. Bunnell falsely believed that the word "Yosemite" meant "full-grown grizzly bear".

Indigenous peoples' continuing presence

Basket woven by Lucy Telles (1885–1955), a Mono Lake Paiute and Southern Sierra Miwok Native American artist from the Yosemite region

After the Mariposa War, Native Americans continued to live in the Yosemite area in reduced numbers. The remaining Yosemite Ahwahneechee tribe members there were forced to relocate to a village constructed in 1851 by the state government. They learned to live within this camp and their limited rights, adapting to the changed environment by entering the tourism industry through employment and small businesses, manufacturing and selling goods and providing services. In 1953, the National Park Service banned all non-employee Natives from residing in the Park and evicted the non-employees who had residence. In 1969, with only a few families left in the Park, the National Park Service evicted the remaining Native people living within the Park (all Park employees and their families) to a government housing area for park employees and destroyed the village as part of a fire-fighting exercise. A reconstructed "Indian Village of Ahwahnee" sits behind the Yosemite Museum, located next to the Yosemite Valley Visitor Center.

By the late 19th century, the population of all native inhabitants in Yosemite was difficult to determine, estimates ranged from thirty to several hundred. The Ahwahneechee people and their descendants were hard to identify. The last full-blooded Ahwahneechee died in 1931. Her name was Totuya, or Maria Lebrado. She was the granddaughter of Chief Tenaya and one of many forced out of her ancestral homelands. The Ahwahneechee live through the memory of their descendants, their fellow Yosemite Natives, and through the Yosemite exhibit in the Smithsonian and the Yosemite Museum. As a method of self-preservation and resilience, the Indigenous people of California proposed treaties in 1851 and 1852 that would have established land reservations for them, but Congress refused to ratify them. The Southern Sierra Miwuk Nation is seeking tribal sovereignty and federal recognition. The National Park Service created policies to protect sacred sites and allow Native People to return to their homelands and use National Park resources.

Early tourists

The Dead Giant (c. 1870s)Vernal Fall (c. 1870s) The Wawona Hotel (1985)Woman in a long dress in front of a sign across a road. Wooden letters read "Camp Curry".Jennie Curry in front of Camp Curry (c. 1900)

In 1855, entrepreneur James Mason Hutchings, artist Thomas Ayres and two others were the first tourists to visit. Hutchings and Ayres were responsible for much of Yosemite's earliest publicity, writing articles and special issues about the valley. Ayres' style was detailed with exaggerated angularity. His works and written accounts were distributed nationally, and an exhibition of his drawings was held in New York City. Hutchings' publicity efforts between 1855 and 1860 increased tourism to Yosemite. Natives supported the growing tourism industry by working as laborers or maids. Later, they performed dances for tourists, acted as guides, and sold handcrafted goods, notably woven baskets. The Indian village and its peoples fascinated visitors, especially James Hutchings who advocated for Yosemite tourism. He and others considered the indigenous presence to be one of Yosemite's greatest attractions.

Wawona was an early Indian encampment for Nuchu and Ahwahneechee people who were captured and relocated to a reservation on the Fresno River by Savage and the Mariposa Battalion in March 1851. Galen Clark discovered the Mariposa Grove of giant sequoia in Wawona in 1857. He had simple lodgings and roads built. In 1879, the Wawona Hotel was built to serve tourists visiting Mariposa Grove. As tourism increased, so did the number of trails and hotels to build on it.

The Wawona Tree, also known as the Tunnel Tree, was a giant sequoia that grew in the Mariposa Grove. It was 234 feet (71 m) tall, and was 90 ft (27 m) in circumference. When a carriage-wide tunnel was cut through the tree in 1881, it became even more popular as a tourist photo attraction. Carriages and automobiles traversed the road that passed through the tree. The tree was permanently weakened by the tunnel, and it fell in 1969 under a heavy load of snow. It was estimated to have been 2,100 years old.

Yosemite's first concession was established in 1884 when John Degnan and his wife established a bakery and store. In 1916, the National Park Service granted a 20-year concession to the Desmond Park Service Company. It bought out or built hotels, stores, camps, a dairy, a garage, and other park facilities. The Hotel Del Portal was completed in 1908 by a subsidiary of the Yosemite Valley Railroad. It was located at El Portal, California just outside of Yosemite.

The Curry Company started in 1899, led by David and Jennie Curry to provide concessions. They founded Camp Curry, now Curry Village.

Park service administrators felt that limiting the number of concessionaires in the park would be more financially sound. The Curry Company and its rival, the Yosemite National Park Company, were forced to merge in 1925 to form the Yosemite Park & Curry Company (YP&CC). The company built the Ahwahnee Hotel in 1926–27.

Yosemite Grant

A view of the park and Vernal Fall, photographed by photographer Eadweard Muybridge in 1872.

Concerned by the impact of commercial interests, citizens including Galen Clark and Senator John Conness advocated protection for the area. The 38th United States Congress passed legislation that was signed by President Abraham Lincoln on June 30, 1864, creating the Yosemite Grant. This is the first time land was set aside specifically for preservation and public use by the U.S. government, and set a precedent for the 1872 creation of Yellowstone national park, the nation's first. Yosemite Valley and the Mariposa Grove were ceded to California as a state park, and a board of commissioners was established two years later.

Galen Clark was appointed by the commission as the Grant's first guardian, but neither Clark nor the commissioners had the authority to evict homesteaders (which included Hutchings). The issue was not settled until 1872 when the homesteader land holdings were invalidated by the U.S. Supreme Court. Clark and the commissioners were ousted in a dispute that reached the Supreme Court in 1880. The two Supreme Court decisions affecting management of the Yosemite Grant are considered precedents in land management law. Hutchings became the new park guardian.

Tourist access to the park improved, and conditions in the Valley became more hospitable. Tourism significantly increased after the first transcontinental railroad was completed in 1869, while the long horseback ride to reach the area was a deterrent. Three stagecoach roads were built in the mid-1870s to provide better access for the growing number of visitors.

John Muir was a Scottish-born American naturalist and explorer. Muir's leadership ensured that many National Parks were left untouched, including Yosemite.

Muir wrote articles popularizing the area and increasing scientific interest in it. Muir was one of the first to theorize that the major landforms in Yosemite Valley were created by alpine glaciers, bucking established scientists such as Josiah Whitney. Muir wrote scientific papers on the area's biology. Landscape architect Frederick Law Olmsted emphasized the importance of conservation of Yosemite Valley.

Increased protection efforts

Early settler, Galen ClarkTheodore Roosevelt and John Muir on Glacier Point

Overgrazing of meadows (especially by sheep), logging of giant sequoia, and other damage led Muir to become an advocate for further protection. Muir convinced prominent guests of the importance of putting the area under federal protection. One such guest was Robert Underwood Johnson, editor of Century Magazine. Muir and Johnson lobbied Congress for the Act that created Yosemite National Park on October 1, 1890. The State of California, however, retained control of Yosemite Valley and Mariposa Grove. Muir's writings raised awareness about the damage caused by sheep grazing, and he actively campaigned to virtually eliminate grazing from the Yosemite's high-country.

The newly created national park came under the jurisdiction of the United States Army's Troop I of the 4th Cavalry on May 19, 1891, which set up camp in Wawona with Captain Abram Epperson Wood as acting superintendent. By the late 1890s, sheep grazing was no longer a problem, and the Army made other improvements. However, the cavalry could not intervene to ease the worsening conditions. From 1899 to 1913, cavalry regiments of the Western Department, including the all Black 9th Cavalry (known as the "Buffalo Soldiers") and the 1st Cavalry, stationed two troops at Yosemite.

Bridalveil Fall and El Capitan, by Carleton Watkins (c. 1880)

Muir and his Sierra Club continued to lobby the government and influential people for the creation of a unified Yosemite National Park. In May 1903, President Theodore Roosevelt camped with Muir near Glacier Point for three days. On that trip, Muir convinced Roosevelt to take control of Yosemite Valley and Mariposa Grove away from California and return it to the federal government. In 1906, Roosevelt signed a bill that shifted control.

National Park Service

The National Park Service (NPS) was formed in 1916, and Yosemite was transferred to that agency's jurisdiction. Tuolumne Meadows Lodge, Tioga Pass Road, and campgrounds at Tenaya and Merced lakes were also completed in 1916. Automobiles started to enter the park in ever-increasing numbers following the opening of all-weather highways to the park. The Yosemite Museum was founded in 1926 through the efforts of Ansel Franklin Hall. In the 1920s, the museum featured Native Americans practicing traditional crafts, and many Southern Sierra Miwok continued to live in Yosemite Valley until they were evicted from the park in the 1960s. Although the NPS helped create a museum that included Native American culture, its early actions and organizational values were dismissive of Yosemite Natives and the Ahwahneechee. NPS in the early 20th century criticized and restricted the expression of indigenous culture and behavior. For example, park officials penalized Natives for playing games and drinking during the Indian Field Days of 1924. In 1929, Park Superintendent Charles G. Thomson concluded that the Indian village was aesthetically unpleasant and was limiting white settler development and ordered the camp to be burned down. In 1969, many Native residents left in search of work as a result of the decline in tourism. NPS demolished their empty houses, evicted the remaining residents, and destroyed the entire village. This was the last Indigenous settlement within the park.

In 1903, a dam in Hetch Hetchy Valley in the northwestern region of the park was proposed. Its purpose was to provide water and hydroelectric power to San Francisco. Muir and the Sierra Club opposed the project, while others, including Gifford Pinchot, supported it. In 1913, the O'Shaughnessy Dam was approved via passage of the Raker Act.

In 1918, Clare Marie Hodges was hired as the first female Park Ranger in Yosemite. Following Hodges in 1921, Enid Michael was hired as a seasonal Park Ranger and continued to serve in that position for 20 years.

O'Shaughnessy Dam in Hetch Hetchy Valley

In 1937, conservationist Rosalie Edge, head of the Emergency Conservation Committee (ECC), successfully lobbied Congress to purchase about 8,000 acres (3,200 ha) of old-growth sugar pines on the perimeter of Yosemite National Park that were to be logged.

By 1968, traffic congestion and parking in Yosemite Valley during the summer months has become a concern. NPS reduced artificial inducements to visit the park, such as the Firefall, in which red-hot embers were pushed off a cliff near Glacier Point at night.

In 1984, preservationists persuaded Congress to designate 677,600 acres (274,200 ha), or about 89 percent of the park, as the Yosemite Wilderness. As a wilderness area, it would be preserved in its natural state with humans being only temporary visitors.

In 2016, The Trust for Public Land (TPL) purchased Ackerson Meadow, a 400-acre tract (160 ha) on the western edge of the park for $2.3 million. Ackerson Meadow was originally included in the proposed 1890 park boundary, but never acquired by the federal government. The purchase and donation of the meadow was made possible through a cooperative effort by TPL, NPS, and Yosemite Conservancy. On September 7, 2016, NPS accepted the donation of the land, making the meadow the largest addition to Yosemite since 1949. With extensive erosion from years of cattle ranching , the land is being transformed back into a healthy meadow.

Geography

Main article: Geography of the Yosemite area
Park map

Yosemite National Park is located in the central Sierra Nevada. Three wilderness areas are adjacent to Yosemite: the Ansel Adams Wilderness to the southeast, the Hoover Wilderness to the northeast, and the Emigrant Wilderness to the north.

The 1,189 sq mi (3,080 km) park contains thousands of lakes and ponds, 1,600 miles (2,600 km) of streams, 800 miles (1,300 km) of hiking trails, and 350 miles (560 km) of roads. Two federally designated Wild and Scenic Rivers, the Merced and the Tuolumne, begin within Yosemite's borders and flow westward through the Sierra foothills into the Central Valley of California.

Rocks and erosion

El Capitan, a granite monolith on Yosemite Valley's northern escarpment

Almost all of the landforms are cut from the granitic rock of the Sierra Nevada Batholith (a batholith is a large mass of intrusive igneous rock that formed deep below the surface). About five percent of the park's landforms (mostly in its eastern margin near Mount Dana) are metamorphosed volcanic and sedimentary rocks. These roof pendants once formed the roof over the underlying granitic magma.

Erosion acting upon different types of uplift-generated joint and fracture systems is responsible for producing the valleys, canyons, domes, and other features. These joints and fracture systems do not move, and are therefore not faults. Spacing between joints is controlled by the amount of silica in the granite and granodiorite rocks; more silica tends to form a more resistant rock, resulting in larger spaces between joints and fractures.

Pillars and columns, such as Washington Column and Lost Arrow, are generated by cross joints. Erosion acting on master joints is responsible for shaping valleys and later canyons. The single most erosive force over the last few million years has been large alpine glaciers, which turned the previously V-shaped river-cut valleys into U-shaped glacial-cut canyons (such as Yosemite Valley and Hetch Hetchy Valley). Exfoliation (caused by the tendency of crystals in plutonic rocks to expand at the surface) acting on granitic rock with widely spaced joints is responsible for producing domes such as Half Dome and North Dome and inset arches like Royal Arches.

Popular features

Cathedral Peak

Yosemite Valley represents only one percent of the park area. The Tunnel View gives a view of the valley. El Capitan is a prominent granite cliff that looms over the valley, and is a rock climbing favorite because of its sheer size, diverse climbing routes, and year-round accessibility. Granite domes such as Sentinel Dome and Half Dome rise 3,000 and 4,800 feet (910 and 1,460 m), respectively, above the valley floor. The park contains dozens of other granite domes.

The high country of Yosemite contains other important features such as Tuolumne Meadows, Dana Meadows, the Clark Range, the Cathedral Range, and the Kuna Crest. The Sierra Crest and the Pacific Crest Trail run through Yosemite. Mount Dana and Mount Gibbs are peaks of red metamorphic rock. Granite peaks include Mount Conness, Cathedral Peak, and Matterhorn Peak. Mount Lyell is the highest point in the park, standing at 13,120 feet (4,000 m). The Lyell Glacier is the largest glacier in the park and one of the few remaining in the Sierra.

The park has three groves of ancient giant sequoia (Sequoiadendron giganteum) trees; the Mariposa Grove (200 trees), the Tuolumne Grove (25 trees), and the Merced Grove (20 trees). This species grows larger in volume than any other and is one of the tallest and longest-lived.

Water and ice

The Merced River flowing through Yosemite Valley, a U-shaped valley

The Tuolumne and Merced River systems originate along the crest of the Sierra in the park and have carved river canyons 3,000 to 4,000 feet (910 to 1,220 m) deep. The Tuolumne River drains the entire northern portion of the park, an area of approximately 680 square miles (1,800 km). The Merced River begins in the park's southern peaks, primarily the Cathedral and Clark Ranges, and drains an area of approximately 511 square miles (1,320 km).

Hydrologic processes, including glaciation, flooding, and fluvial geomorphic response, have been fundamental in creating park landforms. The park contains approximately 3,200 lakes (greater than 100 m), two reservoirs, and 1,700 miles (2,700 km) of streams. Wetlands flourish in valley bottoms throughout the park, and are often hydrologically linked to nearby lakes and rivers through seasonal flooding and groundwater. Meadow habitats, distributed at elevations from 3,000 to 11,000 feet (910 to 3,350 m) in the park, are generally wetlands, as are the riparian habitats found on the banks of Yosemite's watercourses.

Bridalveil Fall flows from a U-shaped hanging valley that was created by a tributary glacier.

Yosemite is famous for its high concentration of waterfalls in a small area. Numerous sheer drops, glacial steps and hanging valleys in the park feature spectacular cascades, especially during April, May, and June (as the snow melts). Located in Yosemite Valley, Yosemite Falls is the fourth tallest waterfall in North America at 2,425 feet (739 m) according to the World Waterfall Database. Also in the valley is the much lower volume Ribbon Falls, which has the highest single vertical drop, 1,612 feet (491 m). Perhaps the most prominent of the valley waterfalls is Bridalveil Fall. Wapama Falls in Hetch Hetchy Valley is another notable waterfall. Hundreds of ephemeral waterfalls become active in the park after heavy rains or melting snowpack.

Park glaciers are relatively small and occupy areas that are in almost permanent shade, such as north- and northeast-facing cirques. Lyell Glacier is the largest glacier in Yosemite (the Palisades Glaciers are the largest in the Sierra Nevada) and covers 160 acres (65 ha). None of the Yosemite glaciers are a remnant of the Ice Age alpine glaciers responsible for sculpting the Yosemite landscape. Instead, they were formed during one of the neoglacial episodes that have occurred since the thawing of the Ice Age (such as the Little Ice Age). Many Yosemite glaciers have disappeared, such as the Black Mountain Glacier that was marked in 1871 and had gone by the mid-1980s. Yosemite's final two glaciers – the Lyell and Maclure glaciers – have receded over the last 100 years and are expected to disappear as a result of climate change.

Climate

Yosemite in autumn

Yosemite has a Mediterranean climate (Köppen climate classification Csa), meaning most precipitation falls during the mild winter, and the other seasons are nearly dry (less than three percent of precipitation falls during the long, hot summers). Because of orographic lift, precipitation increases with elevation up to 8,000 feet (2,400 m) where it slowly decreases to the crest. Precipitation amounts vary from 36 inches (910 mm) at 4,000 feet (1,200 m) elevation to 50 inches (1,300 mm) at 8,600 feet (2,600 m). Snow does not typically accumulate until November in the high country. It deepens into March or early April.

Mean daily temperatures range from 25 °F (−4 °C) to 53 °F (12 °C) at Tuolumne Meadows at 8,600 feet (2,600 m). At the Wawona Entrance (elevation 5,130 feet or 1,560 metres), mean daily temperature ranges from 36 to 67 °F (2 to 19 °C). At the lower elevations below 5,000 feet (1,500 m), temperatures are hotter; the mean daily high temperature at Yosemite Valley (elevation 3,966 feet or 1,209 metres) varies from 46 to 90 °F (8 to 32 °C). At elevations above 8,000 feet (2,400 m), the hot, dry summer temperatures are moderated by frequent summer thunderstorms, along with snow that can persist into July. The combination of dry vegetation, low relative humidity, and thunderstorms results in frequent lightning-caused fires as well.

At park headquarters (elevation 4,018 ft or 1,225 m), January averages 38.0 °F (3.3 °C), while July averages 73.3 °F (22.9 °C). In summer the nights are much cooler than the days. An average of 45.5 days have highs of 90 °F (32 °C) or higher and an average of 105.6 nights with freezing temperatures. Freezing temperatures have been recorded in every month of the year. The record high temperature was 112 °F (44 °C) on July 22 and July 24, 1915, while the record low temperature was −7 °F (−22 °C) on January 1, 2009. Average annual precipitation is nearly 37 inches (940 mm), falling on 67 days. The wettest year was 1983 with 66.06 inches (1,678 mm) and the driest year was 1976 with 14.84 inches (377 mm). The most precipitation in one month was 29.61 inches (752 mm) in December 1955 and the most in one day was 6.92 inches (176 mm) on December 23, 1955. Average annual snowfall is 39.4 inches (1.00 m). The snowiest winter was 1948–1949 with 176.5 inches (4.48 m). The most snow in one month was 175.0 inches (4.45 m) in January 1993.

Climate data for Yosemite Park Headquarters, California, 1991–2020 normals, extremes 1905–present
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °F (°C) 72
(22)
82
(28)
90
(32)
96
(36)
99
(37)
103
(39)
112
(44)
110
(43)
108
(42)
98
(37)
86
(30)
73
(23)
112
(44)
Mean maximum °F (°C) 58.7
(14.8)
64.2
(17.9)
70.4
(21.3)
77.0
(25.0)
83.3
(28.5)
91.3
(32.9)
97.4
(36.3)
97.5
(36.4)
93.7
(34.3)
85.1
(29.5)
70.9
(21.6)
59.3
(15.2)
99.1
(37.3)
Mean daily maximum °F (°C) 47.5
(8.6)
51.2
(10.7)
56.7
(13.7)
63.1
(17.3)
70.5
(21.4)
80.5
(26.9)
89.2
(31.8)
89.0
(31.7)
83.0
(28.3)
70.9
(21.6)
56.0
(13.3)
45.9
(7.7)
67.0
(19.4)
Daily mean °F (°C) 38.0
(3.3)
40.7
(4.8)
45.1
(7.3)
50.4
(10.2)
57.5
(14.2)
65.8
(18.8)
73.3
(22.9)
72.9
(22.7)
67.2
(19.6)
56.1
(13.4)
44.3
(6.8)
36.8
(2.7)
54.0
(12.2)
Mean daily minimum °F (°C) 28.5
(−1.9)
30.2
(−1.0)
33.5
(0.8)
37.6
(3.1)
44.5
(6.9)
51.0
(10.6)
57.4
(14.1)
56.8
(13.8)
51.4
(10.8)
41.3
(5.2)
32.5
(0.3)
27.8
(−2.3)
41.0
(5.0)
Mean minimum °F (°C) 19.2
(−7.1)
22.0
(−5.6)
25.2
(−3.8)
28.4
(−2.0)
35.2
(1.8)
40.8
(4.9)
49.8
(9.9)
48.9
(9.4)
42.0
(5.6)
31.6
(−0.2)
25.4
(−3.7)
20.7
(−6.3)
15.7
(−9.1)
Record low °F (°C) −7
(−22)
1
(−17)
9
(−13)
12
(−11)
15
(−9)
22
(−6)
32
(0)
32
(0)
24
(−4)
19
(−7)
10
(−12)
−1
(−18)
−7
(−22)
Average precipitation inches (mm) 6.98
(177)
6.49
(165)
5.47
(139)
3.17
(81)
1.92
(49)
0.46
(12)
0.29
(7.4)
0.16
(4.1)
0.40
(10)
1.56
(40)
4.05
(103)
5.60
(142)
36.55
(928)
Average snowfall inches (cm) 16.8
(43)
4.2
(11)
5.2
(13)
0.8
(2.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
0.0
(0.0)
3.4
(8.6)
5.1
(13)
35.5
(90.6)
Average precipitation days (≥ 0.01 in) 8.9 9.0 11.0 7.2 6.4 2.2 1.1 0.9 2.0 3.5 5.9 8.5 66.6
Average snowy days (≥ 0.1 in) 2.5 1.4 1.5 0.4 0.0 0.0 0.0 0.0 0.0 0.0 0.5 1.5 7.8
Mean daily daylight hours 10.0 11.0 12.0 13.0 14.0 15.0 14.0 14.0 12.0 11.0 10.0 10.0 12.0
Average ultraviolet index 2 4 6 7 9 10 11 10 8 5 3 2 6
Source 1: NOAA (snow/snow days 1981–2010)
Source 2: Weather Atlas

Geology

Main article: Geology of the Yosemite area
Generalized geologic map of the Yosemite area (based on a USGS image)

Tectonic and volcanic activity

See also: Tioga Pass caldera

The location of the park was a passive continental margin during the Precambrian and early Paleozoic. Sediment was derived from continental sources and was deposited in shallow water. These rocks became deformed and metamorphosed.

Heat generated from the Farallon Plate subducting below the North American Plate led to the creation of an island arc of volcanoes on the west coast of proto-North America between the late Devonian and Permian periods. Material accreted onto the western edge of North America, and mountains were raised to the east in Nevada.

The first phase of regional plutonism started 210 million years ago in the late Triassic and continued throughout the Jurassic to about 150 million years before present (BP), which led to the creation of the Sierra Nevada Batholith. The resulting rocks were mostly granitic in composition and lay about 6 miles (9.7 km) below the surface. Around the same time, the Nevadan orogeny built the Nevadan mountain range (also called the Ancestral Sierra Nevada) to a height of 15,000 feet (4,600 m).

The second major pluton emplacement phase lasted from about 120 million to 80 million years ago during the Cretaceous. This was part of the Sevier orogeny.

Starting 20 million years ago (in the Cenozoic) and lasting until 5 million years ago, a now-extinct extension of Cascade Range volcanoes erupted, bringing large amounts of igneous material in the area. These igneous deposits blanketed the region north of the Yosemite region. Volcanic activity persisted past 5 million years BP east of the current park borders in the Mono Lake and Long Valley areas.

Uplift and erosion

Exfoliation joints cause erosion in granitic rocks, creating many domes including Half Dome.

Starting 10 million years ago, vertical movement along the Sierra fault started to uplift the Sierra Nevada. Subsequent tilting of the Sierra block and the resulting accelerated uplift of the Sierra Nevada increased the gradient of western-flowing streams. The streams consequently ran faster and thus cut their valleys more quickly. Additional uplift occurred when major faults developed to the east, forming Owens Valley from Basin and Range-associated extensional forces. Sierra uplift accelerated again about two million years ago during the Pleistocene.

The uplifting and increased erosion exposed granitic rocks to surface pressures, resulting in exfoliation (responsible for the rounded shape of the many domes in the park) and mass wasting following the numerous fracture joint planes (cracks; especially vertical ones) in the now solidified plutons. Pleistocene glaciers further accelerated this process, while glacial meltwater transported the resulting talus and till from valley floors.

Numerous vertical joint planes controlled where and how fast erosion took place. Most of these long, linear and very deep cracks trend northeast or northwest and form parallel, often regularly spaced sets.

Glacial sculpting

Glacially polished granite cirque in upper Tenaya Canyon

A series of glaciations further modified the region starting about 2 to 3 million years ago and ending sometime around 10,000 BP. At least four major glaciations occurred in the Sierra, locally called the Sherwin (also called the pre-Tahoe), Tahoe, Tenaya, and Tioga. The Sherwin glaciers were the largest, filling Yosemite and other valleys, while later stages produced much smaller glaciers. A Sherwin-age glacier was almost surely responsible for the major excavation and shaping of Yosemite Valley and other canyons in the area.

Glacial systems reached depths of up to 4,000 feet (1,200 m) and left their marks. The longest glacier ran down the Grand Canyon of the Tuolumne River for 60 miles (97 km), passing well beyond Hetch Hetchy Valley. Merced Glacier flowed out of Yosemite Valley and into the Merced River Gorge. Lee Vining Glacier carved Lee Vining Canyon and emptied into Lake Russel (the much-enlarged ice age version of Mono Lake). Only the highest peaks, such as Mount Dana and Mount Conness, were not covered by glaciers. Retreating glaciers often left recessional moraines that impounded lakes such as the 5.5 miles (9 km) long Lake Yosemite (a shallow lake that periodically covered much of the floor of Yosemite Valley).

Ecology

Further information: Ecology of the Sierra Nevada and List of plants of the Sierra Nevada (U.S.)

Habitats

Mule deer in Yosemite Valley

The park has an elevation range from 2,127 to 13,114 feet (648 to 3,997 m) and contains five major vegetation zones: chaparral and oak woodland, lower montane forest, upper montane forest, subalpine zone, and alpine. Of California's 7,000 plant species, approximately 50 percent occur in the Sierra Nevada and more than 20 percent within the park. The park contains suitable habitat for more than 160 rare plants, with rare local geologic formations and unique soils characterizing the restricted ranges many of these plants occupy.

With its scrubby sun-baked chaparral, stately groves of pine, fir, and sequoia, and expanses of alpine woodlands and meadows, Yosemite National Park preserves a Sierra landscape as it prevailed before Euro-American settlement. In contrast to surrounding lands, which have been significantly altered by logging, the park contains some 225,510 acres (91,260 ha) of old-growth forest. Taken together, the park's varied habitats support over 250 species of vertebrates, which include fish, amphibians, reptiles, birds, and mammals.

Yosemite's western boundary has habitats dominated by mixed coniferous forests of ponderosa pine, sugar pine, incense cedar, white fir, Douglas fir, and a few stands of giant sequoia, interspersed by areas of black oak and canyon live oak. These habitats support relatively high wildlife diversity. Wildlife include black bear, coyote, raccoon, mountain kingsnake, Gilbert's skink, white-headed woodpecker, bobcat, river otter, gray fox, red fox, brown creeper, two species of skunk, cougar, spotted owl, and bats.

At higher elevation, the coniferous forests become purer stands of red fir, western white pine, Jeffrey pine, lodgepole pine, and the occasional foxtail pine. Fewer wildlife species tend to be found in these habitats, because of their higher elevation and lower complexity. Animals include golden-mantled ground squirrel, chickaree, fisher, Steller's jay, hermit thrush, and American goshawk. Reptiles are not common, but include rubber boa, western fence lizard, and northern alligator lizard.

Marmot in Tuolumne Meadows

As the landscape rises, trees become smaller and more sparse, with stands broken by areas of exposed granite. These include lodgepole pine, whitebark pine, and mountain hemlock that, at highest elevations, give way to vast expanses of granite as treeline is reached. The climate in these habitats is harsh and the growing season is short, but species such as pika, yellow-bellied marmot, white-tailed jackrabbit, Clark's nutcracker, and black rosy finch are adapted to these conditions. Treeless alpine habitats are favored by Sierra Nevada bighorn sheep. This species is found in the Yosemite area only around Tioga Pass, where a small, reintroduced population exists.

At a variety of elevations, meadows provide important habitat. Animals come to feed on the green grasses and use the flowing and standing water found in many meadows. Predators follow these animals. The interface between meadow and forest is favored by many animal species because of the proximity of open areas for foraging and cover for protection. Species that are highly dependent upon meadow habitat include great grey owl, willow flycatcher, Yosemite toad, and mountain beaver.

Management issues

A black bear with an ear tag in Yosemite Valley

The black bears of Yosemite were once famous for breaking into parked cars to steal food. They were an encouraged tourist sight for many years at the park's garbage dumps, where they congregated to eat garbage, and tourists gathered to photograph them. Increasing bear/human encounters and increasing property damage led to an aggressive campaign to discourage bears from interacting with people and their stuff. The open-air dumps were closed; trash receptacles were replaced with bear-proof receptacles; campgrounds were equipped with bear-proof food lockers so that people would not leave food in their vehicles. Because bears who show aggression towards people usually are destroyed, park personnel have come up with innovative ways to lead bears to associate humans and their property with experiences such as getting hit with a rubber bullet. As of 2001, about 30 bears a year were captured and ear-tagged and their DNA sampled so that, when bear damage occurs, rangers can ascertain which bear was causing the problem.

Despite the richness of high-quality habitats in Yosemite, the brown bear, California condor, and least Bell's vireo have become extinct in the park within historical time, and another 37 species currently have special status under either California or federal endangered species legislation. The most serious current threats include loss of a natural fire regime, exotic species, air pollution, habitat fragmentation, and climate change. On a more local basis, factors such as road kills and the availability of human food have affected some wildlife species.

The yellow star thistle competes with Yosemite's native plants.

Yosemite National Park has documented the presence of more than 130 non-native plant species within park boundaries. They were introduced into Yosemite following the migration of early Euro-American settlers in the late 1850s. Natural and human-caused disturbances, such as wildland fires and construction activities, have contributed to a rapid increase in the spread of non-native plants. Some of these species invade and displace the native plant communities, impacting park resources. Non-native plants can bring about significant ecosystem changes by altering native plant communities and the processes that support them. Some non-native species may cause an increase in fire frequency or increase the available soil nitrogen that allow other non-native plants to establish. Many non-native species, such as yellow star thistle (Centaurea solstitialis), are able to produce a long tap root that allows them to out-compete the native plants for available water.

Bull thistle (Cirsium vulgare), common mullein (Verbascum thapsus), and Klamath weed (Hypericum perforatum) have been identified as noxious pests in Yosemite since the 1940s. More recently recognized species are yellow star thistle (Centaurea solstitialis), sweet clover (Melilot spp.), Himalayan blackberry (Rubus armeniacus), cut-leaved blackberry (Rubus laciniatus) and large periwinkle (Vinca major).

Increasing ozone pollution causes tissue damage to sequoia trees, making them more vulnerable to insect infestation and disease. Since the cones of these trees require fire-touched soil to germinate, historic fire suppression has reduced their ability to reproduce. Planned prescribed fires may help the germination issue.

Wildfires

The Meadow Fire burns in Little Yosemite Valley, 2014

Indigenous residents intentionally set small fires in the early 1860s and before to clear the ground of brush as part as their farming practices. These fires are comparable to contemporary practices such as controlled burns that are done by the U.S. Forest Service and others. Although it was not their primary reason, Yosemite Natives helped preserve biodiversity and resilience by lighting these small fires. Native Americans used fire as an early wildlife management tool to keep certain lands clear, resulting in more food for large animals and decreasing the chance of large forest fires which that now devastate forest ecosystems. Some early uncontrolled forest fires were set accidentally by the militia group led by Major John Savage when the group burned down the Ahwahneechee camp in an attempt to expel them. The house fires eventually spread to a large section of the forest and the militia group ended up having to abandon their raid to save their own camp from the conflagration.

Forest fires clear the park of dead vegetation, making way for new growth. Small fires damage the income generated by tourism. During late July and early August, 2018, the Valley and other sections of the park, temporarily closed due to the Ferguson Fire at its western boundary. The closing was the largest in almost thirty years.

Activities

Tunnel tree at Yosemite National Park in May 2022
Yosemite Valley Shuttle System bus, a free bus service

Public access

Yosemite National Park is open year-round, though certain roads close during snowy months, usually from November through May or June. Certain trails also close during winter, including The 4-Mile Trail and part of The Mist Trail.

Traffic congestion in the valley is heavy during peak summer season (June to August) and a free shuttle bus system operates in the valley. Parking in the valley during the summer is often full. Transit options are available from Fresno and Merced.

The natural and cultural history of Yosemite Valley is presented at the Yosemite Valley Visitor Center, the adjoining Yosemite Museum, and the Nature Center at Happy Isles. The parks' two National Historic Landmarks are the Sierra Club's LeConte Memorial Lodge (Yosemite's first public visitor center), and the Ahwahnee Hotel. Camp 4 is on the National Register of Historic Places.

Hiking

Hikers line the Half Dome cables on a busy summer day in 2008

Over 800 miles (1,300 km) of trails are available to hikers—everything from an easy stroll to a challenging mountain hike, or backpacking trips. The popular Half Dome hike to the summit of Half Dome requires a permit whenever the cables are up (usually from Memorial Day weekend to Columbus Day). A maximum of 300 hikers, selected by lottery, are permitted to advance beyond the base of the subdome each day, including 225 day hikers and 75 backpackers.

The park can be divided into five sections—Yosemite Valley, Wawona/Mariposa Grove/Glacier Point, Tuolumne Meadows, Hetch Hetchy, and Crane Flat/White Wolf. Numerous books describe park trails, while the National Park Service provides free information.

Between late spring and early fall, much of the park can be accessed for backpacking trips. All overnight trips into the back country require a wilderness permit and most require approved bear-resistant food storage.

Driving

Further information: List of Yosemite destinations

While some locations in Yosemite are accessible only on foot, other locations can be reached via road. The most famous road is Tioga Road.

Bicycles are allowed on the roads, but only 12 miles (19 km) of paved off-road trails are available in Yosemite Valley itself; mountain biking is not allowed.

Climbing

Climbing the Narrows in Sentinel Rock

Rock climbing is an important part of Yosemite. In particular the valley is surrounded by summits such as Half Dome and El Capitan. Camp 4 is a walk-in campground in the Valley that was instrumental in the development of rock climbing as a sport, and is listed on the National Register of Historic Places. Climbers can generally be spotted in the snow-free months on anything from ten-foot-high (3 m) boulders to the 3,300-foot (1.0 km) face of El Capitan. Classes on rock climbing are offered there.

Tuolumne Meadows is well known for rock and mountain climbing.

Winter activities

A ranger-guided snowshoe walk in the park

Away from the Valley, the park is snowed in during the winter months, with many roads closed. Downhill skiing is available at the Badger Pass Ski Area—the oldest downhill skiing area in California, operating from mid-December through early April. Much of the park is open to cross-country skiing and snowshoeing, and backcountry ski huts are available. Wilderness permits are required for backcountry overnight ski trips.

The Bracebridge dinner is an annual holiday event, held since 1927 at the Ahwahnee Hotel, inspired by Washington Irving's descriptions of Squire Bracebridge and English Christmas traditions of the 18th century in his Sketch Book. Between 1929 and 1973, the show was organized by Ansel Adams.

Other

Yosemite has 13 official campgrounds.

Bicycle rentals are available from spring through fall. Over 12 miles (19 km) of paved bike paths are available in Yosemite Valley. In addition, bicyclists can ride on roads. Helmets are required for children under 18 years of age. Off-trail riding and mountain biking are not permitted in the park.

Water activities are plentiful during warmer months. Rafting can be done through the valley on the Merced River from late May to July. Swimming pools are available at Yosemite Lodge and Curry Village.

Horsetail Fall

Horsetail Fall flows over the eastern edge of El Capitan. This small waterfall usually flows only during winter and is easy to miss. On rare occasions during mid- to late February, it can glow orange when backlit by sunset. This unique lighting effect happens only on evenings with a clear sky. Minor haze or cloudiness can spoil the effect. Although entirely natural, the phenomenon is reminiscent of the human-caused Firefall that historically occurred from Glacier Point.

In popular culture

A Yogi Bear sign advising young visitors to not feed the bears at Yosemite National Park.

The opening scenes of Star Trek V: The Final Frontier (1989) were filmed in Yosemite National Park. Films such as The Last of the Mohicans (1920) and Maverick (1994) have also been shot there. The 2014 documentary Valley Uprising is centered around Yosemite Valley and its history with an emphasis on climbing culture. The Academy Award-winning 2018 documentary Free Solo was filmed in Yosemite. The Dawn Wall, a 2017 documentary, was filmed there.

See also

Citations

  1. "Yosemite National Park". protectedplanet.net. Protected Planet. Archived from the original on May 30, 2022. Retrieved May 29, 2020.
  2. "Yosemite National Park". Geographic Names Information System. United States Geological Survey, United States Department of the Interior.
  3. ^ "Park Statistics". Yosemite National Park (U.S. National Park Service). Archived from the original on March 8, 2015. Retrieved July 22, 2018.
  4. "Annual Park Ranking Report for Recreation Visits in: 2023". nps.gov. National Park Service. Retrieved March 23, 2024.
  5. "Yosemite Falls". Merriam-Webster.com Dictionary. Merriam-Webster.
  6. Harris 1998, p. 324
  7. "Discover the High Sierra". California Office of Tourism. Archived from the original on June 3, 2020. Retrieved June 9, 2015.
  8. ^ "Nature & History". United States National Park Service: Yosemite National Park. October 13, 2006. Archived from the original on January 25, 2007. Retrieved January 27, 2007.
  9. "Yosemite Wilderness". United States National Park Service: Yosemite National Park. Archived from the original on December 19, 2015. Retrieved March 15, 2008.
  10. "Yosemite NP: Early History of Yosemite Valley". www.nps.gov. Archived from the original on February 18, 2022. Retrieved April 21, 2022.
  11. Yosemite: Official National Park Service Handbook. no. 138. Washington, DC: National Park Service. 1989. p. 102.
  12. ^ Solnit, Rebecca (2014). Savage Dreams: a Journey into the Hidden Wars of the American West. Berkeley: University of California Press. ISBN 978-0-520-95792-3. OCLC 876343009. Archived from the original on February 5, 2024. Retrieved February 22, 2022.
  13. ^ "History & Culture". United States National Park Service: Yosemite National Park. Archived from the original on May 2, 2007. Retrieved January 27, 2007.
  14. "Annual Park Recreation Visitation (1904 – Last Calendar Year)". U.S. National Park Service. Archived from the original on June 11, 2019. Retrieved March 11, 2019.
  15. "New visitation record in 2016 as over 5 million people visited Yosemite National Park". GoldRushCam.com. Sierra Sun Times. January 13, 2017. Archived from the original on May 25, 2017. Retrieved February 8, 2017.
  16. "Top 10 most visited national parks". Travel. March 27, 2024. Retrieved March 27, 2024.
  17. ^ Anderson, Dan. "Origin of the Word Yosemite". www.yosemite.ca.us. Archived from the original on January 5, 2007. Retrieved October 4, 2015.
  18. "Yosemite". Online etymology dictionary. Archived from the original on May 25, 2017. Retrieved September 10, 2010.
  19. Barrett, S. A. (2010). Myths of the southern sierra miwok. Nabu Press. ISBN 978-1-177-40758-8. OCLC 944730381.
  20. Beeler, Madison Scott (1955). "Yosemite and Tamalpais". Journal of the American Name Society. 3 (3): 185–86.
  21. Runte, Alfred (1990). Yosemite: The Embattled Wilderness. University of Nebraska Press. pp. Chapter 1. ISBN 0803238940.
  22. ^ Spence, Mark (1996). "Dispossesing the Wilderness: Yosemite Indians and the National Park Ideal, 1864–1930". Pacific Historical Review. 65 (1): 27–59. doi:10.2307/3640826. ISSN 0030-8684. JSTOR 3640826.
  23. Greene 1987, p. 78.
  24. Starr, Kevin; Orsi, Richard J, eds. (2000). Rooted in Barbarous Soil: People, Culture, and Community in Gold Rush California. Berkeley and Los Angeles: University of California Press. p. 57. ISBN 978-0-520-22496-4.
  25. Adhikari, Mohamed (July 25, 2022). Destroying to Replace: Settler Genocides of Indigenous Peoples. Indianapolis: Hackett Publishing Company. pp. 72–115. ISBN 978-1647920548. Archived from the original on March 26, 2023. Retrieved March 21, 2023.
  26. ^ "Who We Are". Southern Sierra Miwuk Nation. Archived from the original on August 6, 2021. Retrieved July 23, 2021.
  27. "Sketch of Yosemite National Park and an Account of the Origin of the Yosemite and Hetch Hetchy Valleys (History of Yosemite National Parkr)". www.nps.gov. Archived from the original on July 4, 2022. Retrieved April 19, 2022.
  28. Bingaman, John W. (1966). "The Ahwahneechees: A Story of the Yosemite Indians". yosemite.ca.us. Archived from the original on June 23, 2022. Retrieved April 11, 2022.
  29. Godfrey, Elizabeth. "Yosemite Indians; Yesterday and Today". Yosemite Indians. Archived from the original on February 19, 2020. Retrieved August 26, 2021.
  30. Bunnell, Lafayette H. (1892). "Chapter 17". Discovery of the Yosemite and the Indian War of 1851 Which Led to That Event. F.H. Revell. ISBN 0939666588. Archived from the original on October 5, 2012. Retrieved January 27, 2007.
  31. Bunnell, Lafayette H. Discovery of the Yosemite and the Indian War of 1851 Which Led to That Event.
  32. Spence, Mark David (1999). "Yosemite Indians and the National Park Ideal, 1916-1969". Dispossessing the wilderness: Indian removal and the making of the national parks. pp. 115–132. Retrieved April 3, 2024.
  33. "Indian Village of the Ahwahnee – Yosemite National Park (U.S. National Park Service)". Archived from the original on March 2, 2021. Retrieved March 1, 2021.
  34. "Yosemite Indians – Yosemite National Park (U.S. National Park Service)". Archived from the original on February 21, 2021. Retrieved March 1, 2021.
  35. "Yosemite Valley map" (PDF). Archived (PDF) from the original on October 12, 2018. Retrieved March 1, 2021.
  36. ^ "Federal Recognition | Southern Sierra Miwuk Nation". SouthernSierra Miwuk. Archived from the original on April 21, 2022. Retrieved April 21, 2022.
  37. Wolfley, Jeanette (2016). Reclaiming a presence in ancestral lands : the return of Native Peoples to the National Parks. . OCLC 1305864036. Archived from the original on February 5, 2024. Retrieved April 21, 2022.
  38. Harris 1998, p. 326
  39. Wuerthner 1994, p. 20.
  40. Johns, J.S. (1996). "Discovery and Invention in the Yosemite". The Role of Railroads in Protecting, Promoting, and Selling Yellowstone and Yosemite National Parks. University of Virginia. Archived from the original on March 3, 2016. Retrieved August 20, 2010.
  41. Sargent, Shirley (1961). "Wawona's Yesterdays". Archived from the original on June 17, 2022. Retrieved April 14, 2022.
  42. Wawona Hotel Complex Cultural Landscape Report , Yosemite National Park. Mundus Bishop for National Park Service. August 2012. p. 15.
  43. Schaffer, Jeffrey (June 2006). Yosemite National Park: A complete hiker's guide (5 ed.). Berkeley, CA: Wilderness Press. p. 11. ISBN 0899973833. Archived from the original on June 27, 2023. Retrieved August 31, 2021.
  44. "The Myth of the Tree You Can Drive Through". nps.gov. National Park Service. Archived from the original on August 27, 2021. Retrieved August 26, 2021.
  45. NPS 1989, p. 58.
  46. Greene 1987, p. 360.
  47. Radanovich, Leroy (2010). Yosemite Valley Railroad. Arcadia Publishing Incorporated. ISBN 9781439640333. Archived from the original on April 9, 2023. Retrieved December 27, 2021.
  48. Greene 1987, pp. 362, 364.
  49. Wuerthner 1994, p. 40.
  50. Greene 1987, p. 387.
  51. Gene Rose (March 2003). "The Ahwahnee: Yosemite Grandeur". Skiing Heritage Journal. International Skiing History Association: 21. ISSN 1082-2895.
  52. Huth, Hans (March 1948). "Yosemite: The Story of an Idea". Sierra Club Bulletin (33). Sierra Club: 63–76. Archived from the original on May 8, 2012. Retrieved April 20, 2011.
  53. ^ Schaffer 1999, p. 48
  54. Sanger, George P., ed. (1866). "Thirty-Eighth Congress, Session I, Chap. 184 (June 30, 1864): An Act authorizing a Grant to the State of California of the "Yo-Semite Valley" and of the Land embracing the "Mariposa Big Tree Grove"" (PDF). The Statutes At Large, Treaties, and Proclamations of the United States of America from December 1863, to December 1865. Vol. 13. Boston: Little, Brown and Company. p. 325. Archived from the original (PDF) on November 16, 2011.
  55. "Yosemite "State Park"". www.150.parks.ca.gov. Archived from the original on October 16, 2020. Retrieved April 30, 2021.
  56. Hutchings v. Low 82 U.S. 77 (1872)
  57. Ashburner v. California 103 U.S. 575 (1880)
  58. Runte, Alfred (1990). Yosemite : The Embattled Wilderness. Lincoln: University of Nebraska Press. pp. 34–35, 50. ISBN 0803289413.
  59. ^ Schaffer 1999, p. 49
  60. Law Olmsted, Frederick (1865). Yosemite and the Mariposa Grove: A Preliminary Report. Archived from the original on May 29, 2021. Retrieved September 1, 2021.
  61. "People – John Muir". The National Parks: America's Best Idea. PBS. Archived from the original on September 23, 2017. Retrieved September 18, 2017.
  62. Olmsted, Frederick Law. "Olmsted Report on Management of Yosemite, 1865". National Park Service. Archived from the original on August 12, 2021. Retrieved September 1, 2021.
  63. ^ Schaffer 1999, p. 50
  64. "Yosemite". nps.gov. National Park Service. Archived from the original on September 3, 2021. Retrieved September 1, 2021.
  65. "John Muir and President Roosevelt". John Muir National Historic Site, California. National Park Service. Archived from the original on August 19, 2021. Retrieved August 31, 2021.
  66. Schaffer 1999, p. 52
  67. NPS 1989, p. 117.
  68. "American Indians share their Yosemite story". Archived from the original on July 22, 2017. Retrieved July 12, 2017.
  69. Moseley, W. G. (2009). "Beyond Knee-Jerk Environmental Thinking: Teaching Geographic Perspectives on Conservation, Preservation and the Hetch Hetchy Valley Controversy". Journal of Geography in Higher Education. 33 (3): 433–51. doi:10.1080/03098260902982492. S2CID 143538071.
  70. Schaffer 1999, p. 51
  71. ^ "Women of Yosemite". National Park Service. 2022. Archived from the original on March 30, 2023. Retrieved April 18, 2023.
  72. Furmansky, Dyana Z. (2009). Rosalie Edge, Hawk of Mercy: The Activist Who Saved Nature from the Conservationists. University of Georgia Press. pp. 200–07. ISBN 978-0820336763.
  73. Pratt, Sara E (December 14, 2017). "Benchmarks: January 25, 1968: The last firefall: A Yosemite tradition flames out". Earth Magazine. Archived from the original on October 25, 2023. Retrieved December 2, 2023.
  74. "California Wilderness Act of 1984 - 98th U.S. Congress" (PDF). Archived from the original (PDF) on February 3, 2012. Retrieved May 8, 2010.
  75. National Park Service. "Ackerson Meadow Gifted to Yosemite National Park". Archived from the original on September 20, 2016. Retrieved September 8, 2016.
  76. Rogers, Paul (August 23, 2024). "Yosemite National Park: Crews restore damaged landscape back to conditions not seen in 150 years". The Mercury News. Retrieved August 24, 2024.
  77. "Nature & Science". United States National Park Service: Yosemite National Park. Archived from the original on April 22, 2007. Retrieved January 27, 2007.
  78. ^ Harris 1998, p. 329
  79. "Geology: The Making of the Landscape". United States National Park Service: Yosemite National Park. December 22, 2004. Archived from the original on May 14, 2009. Retrieved January 27, 2007.
  80. "Geological Survey Professional Paper 160: Geologic History of the Yosemite Valley – The Sierra Block". United States Geological Survey. November 28, 2006. Archived from the original on October 22, 2012. Retrieved January 27, 2007.
  81. Harris 1998, p. 331
  82. ^ Kiver & Harris 1999, p. 220
  83. ^ Harris 1998, p. 332
  84. Cross, Robert (May 26, 1996). "Mountain majesty Yosemite: The California national park is home to some of the country's most scenic natural wonders". The Baltimore Sun. Archived from the original on October 6, 2022. Retrieved September 7, 2021.
  85. "Yosemite National Park's Largest Glacier Stagnant – Yosemite National Park (U.S. National Park Service)". www.nps.gov. Archived from the original on May 6, 2021. Retrieved May 6, 2021.
  86. ^ Harris 1998, p. 340
  87. ^ Kiver & Harris 1999, p. 227
  88. ^ "Water Overview". National Park Service: Yosemite National Park. December 22, 2004. Archived from the original on January 7, 2007. Retrieved January 27, 2007.
  89. "Hydrology and Watersheds". National Park Service: Yosemite National Park. December 22, 2004. Archived from the original on July 28, 2010. Retrieved January 27, 2007.
  90. "Wetland Vegetation". National Park Service: Yosemite National Park. December 22, 2004. Archived from the original on April 19, 2010. Retrieved January 27, 2007.
  91. "Tallest and Largest Waterfalls at the World Waterfall Database". www.worldwaterfalldatabase.com. Archived from the original on October 23, 2008. Retrieved September 4, 2023.
  92. Krieger, Lisa (May 17, 2019). "Waterfalls are roaring this spring at Yosemite". San Jose Mercury News. Archived from the original on September 9, 2021. Retrieved September 9, 2021.
  93. Kiver & Harris 1999, p. 228
  94. Sahagun, Louis (October 1, 2013). "Yosemite's largest ice mass is melting fast". Los Angeles Times. Archived from the original on September 14, 2021. Retrieved September 14, 2021.
  95. "Yosemite – Nature – Geology – Glaciers". nps.gov. National Park Service. Archived from the original on September 14, 2021. Retrieved September 14, 2021.
  96. Liberatore (March 15, 2013). "Glaciers in Yosemite". Yosemite National Park trips. Archived from the original on September 14, 2021. Retrieved September 14, 2021.
  97. ^ "Climate". National Park Service: Yosemite National Park. December 22, 2004. Archived from the original on January 1, 2007. Retrieved January 27, 2007.
  98. "NOWData – NOAA Online Weather Data". National Oceanic and Atmospheric Administration. Archived from the original on May 11, 2021. Retrieved June 8, 2021.
  99. "Summary of Monthly Normals 1991–2020". National Oceanic and Atmospheric Administration. Archived from the original on June 9, 2021. Retrieved June 8, 2021.
  100. "U.S. Climate Normals Quick Access – Station: Yosemite Park Headquarters, CA (1981–2010)". National Oceanic and Atmospheric Administration. Archived from the original on May 27, 2023. Retrieved May 27, 2023.
  101. "Yosemite National Park, California, USA – Monthly weather forecast and Climate data". Weather Atlas. Archived from the original on September 29, 2019. Retrieved January 26, 2019.
  102. ^ Harris 1998, p. 328
  103. Ernst, WG (2015). "Review of Late Jurassic-early Miocene sedimentationand plate-tectonic evolution of northern California: illuminatingexample of an accretionary margin" (PDF). Chin. J. Geochem. 34 (2): 123–42. Bibcode:2015Geoch..34..123E. doi:10.1007/s11631-015-0042-x. S2CID 55662231. Archived (PDF) from the original on March 21, 2020.
  104. Schweickert, Richard A; Saleeby, Jason B; Tobisch, Othmar T; Wright, William H. III (1977). Paleotectonic and paleogeographic significance of the Calaveras Complex, western Sierra Nevada, California. Paleozoic paleogeography of the western United States : Pacific Coast Paleogeography Symposium I. Los Angeles, California: Society of Economic Paleontologists and Mineralogists. pp. 381–94. Archived from the original on September 17, 2020. Retrieved November 3, 2020.
  105. "Yosemite National Park Geologic Resources Inventory Report" (PDF). National Park Service. pp. 43–44. Natural Resource Report NPS/NRSS/GRD/NRR—2012/560. Archived (PDF) from the original on January 9, 2019.
  106. Harris 1998, p. 337
  107. Yonkee, W. Adolph; Weil, Arlo Brandon (November 1, 2015). "Tectonic evolution of the Sevier and Laramide belts within the North American Cordillera orogenic system". Earth-Science Reviews. 150: 531–93. Bibcode:2015ESRv..150..531Y. doi:10.1016/j.earscirev.2015.08.001. ISSN 0012-8252.
  108. Hill, Mary (2006). Geology of the Sierra Nevada. Berkeley, California: University of California Press. p. 270.
  109. ^ Harris 1998, p. 339
  110. Konigsmark, Ted (2002). Geologic Trips, Sierra Nevada (PDF). GeoPress. p. 234. ISBN 0966131657. Archived (PDF) from the original on May 15, 2012. Retrieved September 22, 2021.
  111. ^ Huber, N. King (1987). "Final Evolution of the Landscape". The Geologic Story of Yosemite National Park. Washington: Government Printing Office. USGS Bulletin 1595. Archived from the original on March 31, 2022. Retrieved July 5, 2022.
  112. "Volcanoes of the Eastern Sierra Nevada". sierra.sitehost.iu.edu. Archived from the original on June 28, 2021. Retrieved June 28, 2021.
  113. Harris 1998, p. 333
  114. Franklin, Jerry F.; Fites-Kaufmann, Jo Ann (1996). "21: Assessment of Late-Successional Forests of the Sierra Nevada" (PDF). Sierra Nevada Ecosystem Project. Final Report to Congress. Status of the Sierra Nevada. Vol. II: Assessments and Scientific Basis for Management Options. Centers for Water and Wildland Resources, University of California. pp. 627–71. ISBN 1887673016. Archived (PDF) from the original on May 13, 2019. Retrieved December 10, 2014.
  115. Bolsinger, Charles L.; Waddell, Karen L. (1993). "Area of old-growth forests in California, Oregon, and Washington" (PDF). Resource Bulletin (197). United States Forest Service, Pacific Northwest Research Station. PNW-RB-197. Archived (PDF) from the original on October 23, 2020. Retrieved February 10, 2009.
  116. ^ Public Domain This article incorporates public domain material from Wildlife Overview. National Park Service: Yosemite Park Service. December 22, 2004. Archived from the original on January 27, 2007.
  117. "DNA to Help Identify "Problem" Bears at Yosemite". National Geographic. April 23, 2001. Archived from the original on April 30, 2001. Retrieved January 4, 2007.
  118. Graber, David M. (1996). "25: Status of Terrestrial Vertebrates". Sierra Nevada Ecosystem Project. Final Report to Congress. Status of the Sierra Nevada Volume II: Assessments and Scientific Basis for Management Options (PDF). Centers for Water and Wildland Resources, University of California. pp. 709–34. ISBN 1887673016. Archived (PDF) from the original on June 20, 2020. Retrieved December 10, 2014.
  119. Stephens, Tim. "Yosemite bears and human food: Study reveals changing diets over past century". UC Santa Cruz News. Archived from the original on June 18, 2022. Retrieved June 27, 2022.
  120. Hughes, Trevor. "National park visitors leave roadkill in their wake". USA TODAY. Archived from the original on June 27, 2022. Retrieved June 27, 2022.
  121. ^ "Exotic Plants". National Park Service: Yosemite National Park. December 22, 2004. Archived from the original on January 2, 2007. Retrieved January 4, 2007.
  122. "Giant Sequoias and Fire – Sequoia & Kings Canyon National Parks (U.S. National Park Service)". www.nps.gov. Archived from the original on August 24, 2021. Retrieved April 8, 2021.
  123. ^ Johnson, Eric Michael. "How John Muir's Brand of Conservation Led to the Decline of Yosemite". Scientific American Blog Network. Archived from the original on May 22, 2022. Retrieved April 21, 2022.
  124. "Are There Good Forest Fires?". Evergreen Magazine. Summer 2002. Archived from the original on March 15, 2014. Retrieved March 14, 2014.
  125. "Yosemite Valley will close due to fire. 'Get yourself out of here,' official says". fresnobee. Archived from the original on July 24, 2018. Retrieved July 24, 2018.
  126. Branch, John; Medina, Jennifer; Fountain, Henry (July 25, 2018). "Yosemite National Park Evacuated Amid Threat From Fire". The New York Times. Archived from the original on July 30, 2018. Retrieved July 30, 2018.
  127. "Operating Hours & Seasons". Yosemite National Park. U.S. National Park Service. Archived from the original on December 2, 2023. Retrieved December 2, 2023.
  128. "Yosemite in Winter". www.yosemitehikes.com. Archived from the original on October 29, 2023. Retrieved December 2, 2023.
  129. "Bus". National Park Service: Yosemite National Park. May 27, 2009. Archived from the original on October 24, 2020. Retrieved May 8, 2010.
  130. Marshall, Aarian (May 24, 2019). "Hiking or Camping? Take the Bus to the Trail This Summer". Wired. Archived from the original on May 24, 2019. Retrieved June 9, 2019.
  131. "Camp 4 Listed With National Register of Historic Places". NPS Press Release. National Park Service. February 27, 2003. Archived from the original on March 16, 2007. Retrieved December 14, 2008.
  132. "Half Dome Day Hike". Yosemite National Park. U.S. National Park Service. Archived from the original on October 30, 2018. Retrieved January 2, 2023.
  133. "Half Dome Permits for Day Hikers". Yosemite National Park. U.S. National Park Service. Archived from the original on November 18, 2018. Retrieved January 2, 2023.
  134. Cary, Russ. "Yosemite Hikes". Archived from the original on November 14, 2020. Retrieved May 27, 2009.
  135. ^ "Wilderness Permits". National Park Service: Yosemite National Park. February 12, 2010. Archived from the original on December 15, 2020. Retrieved May 8, 2010.
  136. "Bear and food storage". National Park Service: National Park Service. February 10, 2010. Archived from the original on November 11, 2020. Retrieved May 8, 2010.
  137. "Auto Touring". National Park Service: Yosemite National Park. December 22, 2004. Archived from the original on October 28, 2020. Retrieved January 27, 2007.
  138. "Biking". National Park Service: Yosemite National Park. March 2007. Archived from the original on November 11, 2020. Retrieved March 23, 2007.
  139. "Climbing". National Park Service: Yosemite National Park. December 11, 2008. Archived from the original on October 29, 2020. Retrieved May 8, 2010.
  140. "Camp 4 Listed With National Register of Historic Places" (Press release). National Park Service: Yosemite National Park. February 27, 2003. Archived from the original on March 16, 2007. Retrieved January 27, 2007.
  141. "Skiing". National Park Service: Yosemite National Park. September 21, 2006. Archived from the original on December 4, 2020. Retrieved January 27, 2007.
  142. "Tuolumne Meadows Winter Conditions Update". National Park Service: Yosemite National Park. Archived from the original on October 21, 2020. Retrieved January 27, 2007.
  143. "Winter Wilderness Travel". National Park Service: Yosemite National Park. March 2, 2010. Archived from the original on November 12, 2020. Retrieved May 8, 2010.
  144. "History". The Bracebridge Dinner at Yosemite. Archived from the original on March 12, 2012. Retrieved May 8, 2010.
  145. "Yosemite camping". Archived from the original on January 16, 2023. Retrieved January 16, 2023.
  146. "Plan Your Visit". Yosemite National Park. U.S. National Park Service. Archived from the original on February 21, 2009.
  147. Brown, Ann Marie (2015). Moon Yosemite, Sequoia & Kings Canyon Hiking, Camping, Waterfalls & Big Trees. Avalon Publishing. Rafting. ISBN 9781640494459.
  148. Maddrey, Joseph (2016). The Quick, the Dead and the Revived: The Many Lives of the Western Film. McFarland. p. 175. ISBN 978-1476625492.
  149. Mortimer, Peter; Rosen, Nick; Lowell, Josh (September 1, 2014), Valley Uprising (Documentary), Peter Sarsgaard, Alex Honnold, Yvon Chouinard, Royal Robbins, Sender Films, Big UP Productions, archived from the original on June 13, 2019, retrieved April 26, 2021
  150. Catsoulis, Jeannette (September 27, 2018). "Review: In 'Free Solo,' Braving El Capitan With Only Fingers and Toes". The New York Times. Archived from the original on April 21, 2022. Retrieved September 4, 2020.
  151. Lowell, Josh; Mortimer, Peter (July 17, 2018), The Dawn Wall (Documentary, Biography, Sport), John Branch, Tommy Caldwell, Kevin Jorgeson, Red Bull Media House, Sender Films, archived from the original on April 21, 2022, retrieved April 26, 2021

General references

External links

Listen to this article
(2 parts, 40 minutes)
Spoken Misplaced Pages iconThese audio files were created from a revision of this article dated 18 June 2005 (2005-06-18), and do not reflect subsequent edits.(Audio help · More spoken articles) Yosemite National Park at Misplaced Pages's sister projects:
Yosemite National Park
Attractions
Valley
attractions
Half Dome
Hiking
trails
Rock
climbs
People
Lodging
and camping
Natural disasters
Transportation
Nearby
municipalities
Additional
information
Related links
Sierra Nevada
Mountains
Peaks >14,000 ft
Northern peaks
Central peaks
Southern peaks
Climbing
Passes
Rivers
Lakes
Protected
areas
National parks
and monuments
National forests
Wilderness areas
State parks
Communities
Ski areas
Trails
National parks of the United States
List of national parks of the United States (by elevation)
World Heritage Sites in the United States
Northeast
Midwest
South
West
Multiple locations
Territories
Shared with Canada
Protected areas of California
National Park System
Parks
PreservesMojave
Monuments
Seashores
Historical Parks
Historic Sites
Memorials
Recreation Areas
California State Parks
Parks
Natural Reserves
Marine Reserves
Historic Parks
Beaches
Recreation Areas
Vehicular
Recreation Areas
Other
National Forests and Grasslands
National Forests
and Grasslands
National Wilderness
Preservation System
National Monuments
and Recreation Areas
State Forests
National Wildlife Refuges
State Wildlife Areas
Wildlife
Areas
Ecological
Reserves
Marine
Protected
Areas
Bureau of Land Management National Conservation Lands
National Monuments
National
Conservation Areas
Wilderness Areas
National Marine Sanctuaries
National Estuarine Research Reserves
University of California Natural Reserve System
Private Conservation Land Trusts
Heritage registers
National Natural Landmarks
State of California
Sacramento (capital)
Topics
Regions
Metro regions
Counties
Most populous
cities
flag California portal
Categories: