There are three main types of soils in the Bahamas: sandy, organic, and lateritic soils. Sandy soils occur on unconsolidated carbonate sands and consist of unaltered carbonate minerals plus organic matter. Organic soils contain abundant organic material and lack mineral matter. They are most common on flat, rocky lands of the larger Bahamian islands. Lateritic soils are thin and discontinuous, and occur on lithified Pleistocene eolian and beach ridges. They have low SiO 2 /Al 2 O 3 ratios and contain calcite, aragonite, hematite, goethite, hydroxy-interlayered clay (HIC), boehmite, and quartz. The following petrographic features were observed in pedogenically altered Pleistocene grainstones: rhizoliths, pedotubules, alveolar textures, calcified root hairs, Microcodium, laminated micrite, clotted micrite, soil pisoids, circumgranular cracking, horizontal fractures, microbial borings, and iron-rich clay accumulations. The characteristics of Bahamian soils result from a complex interaction of the five major soil-forming factors: climate, topography, vegetation, parent material and time.