Isla Ángel De La Guarda
The geologically active Ballenas Fault runs along the seabed of the linear Canal de Ballenas. A 6.9 magnitude earthquake occurred on this fault in 2009.
Geography
The island is extremely dry, with no sources of freshwater other than washes following rainfall. It has an area of 931 square kilometers (359 sq mi) and a chain of mountains runs along its 69 km (43 mi) length, reaching a maximum of 1,305 m (4,281 ft) above sea level. It runs northwest to southeast. The west coast is roughly straight in that direction, but the east coast runs inward near the middle before heading outward until it reaches the island's widest point. The coast then runs south for a while before finally returning to its southeasterly direction.
Much of the island is inaccessible due to mountains at or near the shore, especially on the west coast. There are a few flat areas on the coast at the outlets of washes that were created by sediment. These alluvial fans are mostly on the east coast, but a large one is found on the west coast where the island narrows in the middle. Much of the island's geology is made up of volcanic and alluvial sand deposits.
Biology
Despite its extreme dryness, the island is relatively diverse in plant and animal life. There are many types of birds and reptiles, especially lizards. The Angel Island chuckwalla, Angel Island speckled rattlesnake (Crotalus angelensis), Angel Island mouse (Peromyscus guardia) and Angel de la Guarda woodrat (Neotoma insularis) occur only on the island. The only mammals are bats, rodents, and introduced feral cats. Plants include elephant trees, cacti, grasses, shrubs, succulents, and boojum trees.
See also
Notes
- ^ Aitchison, Stewart W. (2010-01-01). The Desert Islands of Mexico's Sea of Cortez. University of Arizona Press. ISBN 9780816527748.