“…The third hypothesis would be related to a predominantly clay to sandy clay loam thick sediment pack deposited in the continental environment of an old closed basin, possibly associated with karst cavities, which could also have been developed when the regional base level of the Samaná Peninsula was well-below the current level. The fourth (karst marble and schist) (Ertunç, 1999) in Turkey, Tianhuanping (andesite) (Wang and Liu, 2005) in China, Porthimund (charnockites) (Ramana and Gogte, 1982) and Uri and Nathpa Jhakri (schist rocks) (Behrestaghi et al, 1996) in India, Hickory Log Creek (mica-schist) (Rogers et al, 2006) in the United States, Scott (shales) (Goodman and Ahlgren, 2000) and Clyde (schist) (Macfarlane, 2009) in New Zealand, and Mujib (limestone) (Wiesner and Ewert, 2013) in Jordan, with few publications for schist materials as foundations developed in tropical climate, mainly for projects of concrete gravity dams.…”