Malpelo Island (Isla Malpelo)
Malpelo is a small oceanic island in the eastern Pacific Ocean, located about 500 km west of the Colombian mainland with a military post manned by the Colombian Armed Forces. It consists of a sheer and barren rock with three high peaks, the highest being Cerro de la Mona with a height of 300 m. The island is about 1.5 km in length from northeast to southwest, and 700 yd in width.
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 with a length of 300 km and a width of 100 km. 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 1000 and 5000 fathom 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.
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 with a length of 300 km and a width of 100 km. 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 1000 and 5000 fathom 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.
Map - Malpelo Island (Isla Malpelo)
Map
Country - Colombia
Currency / Language
ISO | Currency | Symbol | Significant figures |
---|---|---|---|
COP | Colombian peso | $ | 2 |
ISO | Language |
---|---|
ES | Spanish language |