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The underlying Cayman Ridge is proposed as an uplifted fault block. The oldest rocks are believed to be granodiorite , followed by a cap of basalt . [ 1 ] Situated near the Oriente Transform Fault and the Mid-Cayman Rise, the islands are tectonically active. [ 2 ]
Map of Grand Cayman Sunset from North Side beach, Grand Cayman. Natural resources include fish and a climate and beaches that foster tourism, which is the islands' major industry. A 2012 estimate of land use determined that the Cayman Islands' had 0.83 percent arable land and 2.08 percent permanent crops.
Mastic Reserve is an 834 ha tract of mainly forested land. It is bounded on the south and west by the Central Mangrove Wetland, and on the north by farmland.It encompasses the largest tract of contiguous native dry forest in the Cayman Islands, as well as the highest part of the low-lying island, with an elevation of 18 m.
The Cayman Trough (also known as the Cayman Trench, Bartlett Deep and Bartlett Trough) is a complex transform fault zone pull-apart basin which contains a small spreading ridge, the Mid-Cayman Rise, on the floor of the western Caribbean Sea between Jamaica and the Cayman Islands. [1]
The location of the Cayman Islands An enlargeable map of the Cayman Islands. The following outline is provided as an overview of and topical guide to the Cayman Islands: Cayman Islands – British overseas territory located in the western Caribbean Sea, comprising the islands of Grand Cayman, Cayman Brac, and Little Cayman. [1]
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The formation of the Cayman Trough produced the last significant tectonic feature on the islands after 39 million years ago, with sinistral strike-slip faults. A structural block produced as a result creates a 5.7 kilometer sinistrally offset contact between the Water Island and Louisenhoj formations. [1]
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