Geology of Anguilla - Misplaced Pages

The geology of Anguilla consists of Lesser Antilles island arc volcanic rocks overlain by Oligocene, Miocene and Pliocene reef limestone. Older tuff and basalt outcrops in only two places on the island, which are tilted. During the Pliocene and Pleistocene, the underlying Anguilla Bank likely connected Saint Bartholomew and Saint Martin as one island.

References

Budd, A. F.; Johnson, K. G.; Edwards, J. C. (1995). "Caribbean reef coral diversity during the early to middle Miocene: an example from the Anguilla Formation". Coral Reefs. 14 (2): 109–117. Bibcode:1995CorRe..14..109B. doi:10.1007/BF00303432. S2CID 22827668.
Christman, Robert A. (1953). "Geology of St. Bartholomew, St. Martin, and Anguilla, Lesser Antilles | GSA Bulletin". Geological Society of America Bulletin. 64: 85. doi:10.1130/0016-7606(1953)64[85:GOSBSM]2.0.CO;2. Retrieved 2018-11-09.

v t e Geology of North America
Sovereign states	Antigua and Barbuda Bahamas Barbados Belize Canada Costa Rica Cuba Dominica Dominican Republic El Salvador Grenada Guatemala Haiti Honduras Jamaica Mexico Nicaragua Panama Saint Kitts and Nevis Saint Lucia Saint Vincent and the Grenadines Trinidad and Tobago United States
Dependencies and other territories	Anguilla Aruba Bermuda Bonaire British Virgin Islands Cayman Islands Curaçao Greenland Guadeloupe Martinique Montserrat Puerto Rico Saint Barthélemy Saint Martin Saint Pierre and Miquelon Saba Sint Eustatius Sint Maarten Turks and Caicos Islands United States Virgin Islands