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The geologic history and the geomorfologic
evolution of the archipelago present quite defined features. The carried out studies have
revealed that the well-known formation as Complex Granitic of the The Great one Asleep
he/she had their origin during the Superior Cretácico in rocks igneous metamorphose that
today appears in the hills of The Great Roque and the successive variations in its
morphology they have its origin in a movement geoanticlinal that embraced the whole area
of the Antilles. These barriers
protectors are located between Barlovento of the winds and the oceanic currents, that are
separated from the keys located to the north of the archipelago by a great central lagoon
of still waters with a greenish bottom that is sometimes interrupted by smudgy coral riefs
or prairies of marine grasses. This great central lagoon of the archipelago has been
denominated bay or under of "The Corrals". Its approximate surface is of 400
square kilometers.To the south of the archipelago a narrow and abrupt submarine platform
appears where the depths of the sea oscillate between the 500 and the 1.000 meters. To the
north, the platform is but wide and the depths are inferior to the 10 meters. 1. - Sandy keys without vegetable covering and with little stability known as "Pelones", are the most numerous in the archipelago. 2. - Sandy keys covered with low vegetation, bushes and gramineous that are more stable than the previous class due to the presence of the vegetable covering that fixes the sand and it avoids the erosion. 3. - Sandy keys where there is vegetation of gramineous, bushes and cringing plants; with these it can have beach rocks originated by the segmentation of the sand or of the coral gravel, which forms "Storm Terraces." 4. - Sandy keys of a lot of extension covered with gramineous and that in certain places form a surrounded bay of mangrove; there are big accumulations of coral gravel and fragments of mollusks, result of the erosion caused by the sea. 5. - Keys of great size that have a lagoon open of flat waters, where the depth is smaller than 3 meters; the vegetation is of gramineous and swamp formations that skirt the lagoon; there are also storm terraces and beach rock 6. - Keys of bigger size of the archipelago where there are lagoons open of flat waters, internal and saline lagoons; the sandy plains are very extensive and they are covered for gramineous; there there are four mangrove species; "storm terraces and beach rock can appear on the side of windward.
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