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The soils are generally kaolinitic latosols, meaning a highly leached soil with kaolinite as its principal clay component.The predominance of iron and aluminum oxides in the soil give it a distinctive bright red to orange-yellow color.

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Schematic Elevation - THE ISLAND OF GRENADA Reconstructing Grenada's geologic history poses a formidable task for the geologist." In Grenada the answer to that question involves analysis of several variables: parent material (geology), climate, relief, and time, among others.Grenada has basically two physiographic regions: the rugged, high-relief interior, and the relatively low-relief coastal periphery.In contrast to the volcanic centers of the interior, the coastal deposits are dominated by "reworked" volcanic rocks, including fluviatile (stream) and mudslide deposits.Originally, the topography of the coast may have been quite rugged.Since water is the principle erosive agent on the Island, the high elevations are eroding at a greater rate than the lowlands.Over time, this disparity in erosion will serve to reduce the relief between the interior and the coastal periphery.In Grenada, the small variation in temperature between sea level and the higher elevations is not of great geomorphological importance, but the great difference in rainfall is very significant.An analysis of rainfall indicates that annual rainfall varies directly with elevation.Most significantly, the geology of Grenada is complex and presents many rock types of different ages.Several geologic studies have been conducted in Grenada, dealing with the chemical composition of particular rock types.An important manifestation of the weathering process is the formation of soils.Soils form from the same interplay of factors which influence topography, with vegetation becoming a significant variable.The western coast displays a more rugged landscape, owing to the asymmetric eruption to the west, which is a pattern throughout the Windward Islands.Climate is an important factor in the formation of topography.

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