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Malpelo Island

Colombian island

  • 7 min read
  • 4 chapters
Malpelo Island, Colombia
NOAA · Public domain

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Through Island and Bird

Geography

Malpelo is the only island that rises above the surface from the Malpelo Ridge, which is a solitary volcanic submarine ridge that extends in a northeast-southwest direction for 300 km (190 mi) and has a width of 100 km (62 mi). This island is surrounded by a number of offshore rocks. Off the northeast corner are the Tres Mosqueteros. Off the southwest corner are Salomón, Saúl, La Gringa, and Escuba. All the rocks are surrounded by deep water, and most of the face of the main island is very steep. Soundings between 1,800 and 9,100 metres (1,000 and 5,000 fathoms) are obtainable within a few kilometres of the shore and the currents are strong and changeable. As an oceanic island, it has never been connected with any other islands or the mainland.

Malpelo Island is composed of Miocene pillow lavas, volcanic breccias, and basaltic dikes that have been dated as being 16 to 17 million years old. This island and the underlying and underwater Malpelo Ridge were created along with the Carnegie Ridge in the Late Miocene by a very complex interaction between the Cocos-Nazca Spreading Centre and the Galápagos hotspot.

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