| Cayman Ridge | |
|---|---|
 Cayman Ridge and
Cayman Trough. | |
| Highest point | |
| Coordinates |
86°30′N 17°30′W / 86.500°N 17.500°W 77°45′N 20°00′W / 77.750°N 20.000°W |
| Geography | |
  Cayman Ridge Location of Cayman Ridge in Caribbean Sea | |
| Location |
Caribbean Sea
Cuba
Cayman Islands
Honduras |
| Parent range |
Sierra Maestra Cayman Islands Misteriosa Bank Rosario Bank |
| Geology | |
| Mountain type | Seamount |
| Volcanic arc/ belt | Cayman Trough |
The Cayman Ridge is an undersea mountain range on the northern margin of the Cayman Trough in the Caribbean Sea. It extends from the Sierra Maestra in the east to the Misteriosa Bank and Rosario Bank in the west, a distance of about 1,500 km (930 mi). The Cayman Ridge also includes the Cayman Islands. [1]
The ridge formed as an island arc when the Cayman Trough was the site of a subduction zone during the Paleocene and Eocene epochs. As the dynamics of the area changed, the subduction zone became a transform fault zone with a pull-apart basin during which time volcanism had dwindled along the entire length of the arc. The Cayman Ridge is now an inactive volcanic zone. [1]
References
- ^ a b "The Cayman Islands: A Geological View". 2008-05-01. Archived from the original on 2015-05-09. Retrieved 2018-02-12.
19°31′22.8″N 80°43′13.8″W / 19.523000°N 80.720500°W
 | This Cayman Islands-related article is a stub. You can help Wikipedia by expanding it. |
 | This Caribbean location article is a stub. You can help Wikipedia by expanding it. |
- Underwater ridges of the Atlantic Ocean
- Borders of Cuba
- Geography of the Cayman Islands
- Geography of Cuba
- Geography of Honduras
- Island arcs
- Paleocene volcanism
- Eocene volcanism
- Mountains of Honduras
- Landforms of Honduras
- Mountains of Central America
- Landforms of Central America
- Caribbean islands of Honduras
- Undersea banks of the Caribbean Sea
- Cayman Islands stubs
- Caribbean geography stubs
| Cayman Ridge | |
|---|---|
|
Cayman Ridge and
Cayman Trough. | |
| Highest point | |
| Coordinates |
86°30′N 17°30′W / 86.500°N 17.500°W 77°45′N 20°00′W / 77.750°N 20.000°W |
| Geography | |
Cayman Ridge Location of Cayman Ridge in Caribbean Sea | |
| Location |
Caribbean Sea
Cuba
Cayman Islands
Honduras |
| Parent range |
Sierra Maestra Cayman Islands Misteriosa Bank Rosario Bank |
| Geology | |
| Mountain type | Seamount |
| Volcanic arc/ belt | Cayman Trough |
The Cayman Ridge is an undersea mountain range on the northern margin of the Cayman Trough in the Caribbean Sea. It extends from the Sierra Maestra in the east to the Misteriosa Bank and Rosario Bank in the west, a distance of about 1,500 km (930 mi). The Cayman Ridge also includes the Cayman Islands. [1]
The ridge formed as an island arc when the Cayman Trough was the site of a subduction zone during the Paleocene and Eocene epochs. As the dynamics of the area changed, the subduction zone became a transform fault zone with a pull-apart basin during which time volcanism had dwindled along the entire length of the arc. The Cayman Ridge is now an inactive volcanic zone. [1]
References
- ^ a b "The Cayman Islands: A Geological View". 2008-05-01. Archived from the original on 2015-05-09. Retrieved 2018-02-12.
19°31′22.8″N 80°43′13.8″W / 19.523000°N 80.720500°W
|
| This Cayman Islands-related article is a stub. You can help Wikipedia by expanding it. |
|
| This Caribbean location article is a stub. You can help Wikipedia by expanding it. |
- Underwater ridges of the Atlantic Ocean
- Borders of Cuba
- Geography of the Cayman Islands
- Geography of Cuba
- Geography of Honduras
- Island arcs
- Paleocene volcanism
- Eocene volcanism
- Mountains of Honduras
- Landforms of Honduras
- Mountains of Central America
- Landforms of Central America
- Caribbean islands of Honduras
- Undersea banks of the Caribbean Sea
- Cayman Islands stubs
- Caribbean geography stubs