Malpelo Ridge

The Malpelo Ridge (Spanish: Dorsal de Malpelo) is an elevated part of Nazca Plate off the Pacific coast of Colombia. It is a faulted chain of volcanic rock of tholeiitic composition.[1] The Malpelo Ridge may have originated simultaneously as Carnegie Ridge, and thus represent an old continuation of Cocos Ridge.[2] It is thought to have acquired it present position due to tectonic movements along the Panama Fracture Zone.[2]

References
  1. Lonsdale, Peter; Fornari, Daniel (1980). "Submarine geology of Malpelo Ridge, Panama Basin". Marine Geology. 36 (1–2): 65–83. Bibcode:1980MGeol..36...65L. doi:10.1016/0025-3227(80)90041-9.
  2. Marcaillou, Boris; Charvis, Philippe; Collot, Jean-Yves (2006). "Structure of the Malpelo Ridge (Colombia) from seismic and gravity modelling". Marine Geophysical Researches. 27 (4): 289–300. Bibcode:2006MarGR..27..289M. doi:10.1007/s11001-006-9009-y. S2CID 129634673.

This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.