. The Socorro hotspot is marked 37 on map. The island rises abruptly from the sea to in elevation at its summit. Socorro Island is the emerged summit of a massive, predominantly submarine
shield volcano. The island is part of the northern Mathematicians Ridge, a
mid-ocean ridge that became largely inactive 3.5 million years ago when activity moved to the
East Pacific Rise. All four islands along with the many
seamounts on the ridge are post-abandonment alkaline volcanoes. Socorro Island is unusual in that it is the only dominantly
silicic peralkaline volcanic island in the Pacific Ocean. It most recently erupted in late January and early February 1993, which was a submarine flank eruption off the coast from Punta Tosca. An earlier eruption was on May 21, 1951; earlier eruptions probably occurred in 1905, 1896 and 1848. The initial volcanic event probably occurred in 3090BC 500 years. Mount Evermann () is the name given to the summit dome complex, in honor of
ichthyologist Barton Warren Evermann. The island's surface is broken by furrows, small craters, and numerous ravines, and covered in
lava domes,
lava flows and
cinder cones. There is a naval station, established in 1957, with a population of 250 (staff and families), living in a village with a church, that stands on the western side of Bahía Vargas Lozano, a small cove with a rocky beach, about east of Cabo Regla, the southernmost point of the island. The station is served by a dock, a local helipad and Isla Socorro airport, located six kilometers to the north. There is a fresh water spring about northwest of Cabo Regla, at the shoreline of Ensenada Grayson (or Caleta Grayson). This is
brackish and sometimes covered by the sea at high tide. In the 1950s, a small freshwater seep was known to exist some inland at Bahía Lucio Gallardo Pavon (Binner's Cove), northwest of the naval station. ==History==