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The mountain range is formed by a complex of tectonic faults resulting from the collision of the
Caribbean and Atlantic plates, rising and leaving the sea. This means that we can find rocks at more than 2000 meters high that at first glance can be seen remains of ancient corals that were in the sea.
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The mountain range is a massif of volcanic origin from the
Cretaceous period (from 145 to 66 million years ago) and later covered by a layer of calcareous sediment of marine origin, this means that the entire mountain range was once submerged under the sea and in mostly inhabited by corals that left
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Its name is mentioned for the first time by
Bartolomé de las Casas in his "Brief History of the Indies", who takes it from the phonetic sound used by the Taino Indians to describe that region.
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It is rich in deposits of salt and gypsum, and also has a lagoon in the southern part (Oviedo lagoon) and between this mountain range and the Neiba mountain range is
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Larimar is the
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The Sierra de
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167:, which formed in the range's volcanic vesicles.
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199:. Tuscaloosa, AL: University of Alabama Press.
137:'within the jungle' in the purportedly related
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
