Reference soil Cuba 12: Ferralsol
Ferralsols occur in tropical and subtropical regions of the world, mainly on old and stable land surfaces.
Characteristics
Soils having a ferralic horizon (strongly weathered horizon with low-activity clays and very low amounts of weatherable minerals) between 25 and 200 cm from the soil surface. They lack a nitic horizon (a horizon with strongly developed, nut-shaped structure) and do not have a layer which fulfils the requirements of an argic horizon and which has, in the upper 30 cm, 10 percent or more water-dispersible clay.
Reference soil CU012: Ferralsols
Short field description: Very deep, well drained, strong brown, clay loam. Well structured, with diffuse boundaries, porous ferromanganese concretions. Geology: Jurasic higher, oxfordiano and tithoniano: limestones, marbles. Geomorphology: tectonic-lithological low mountain. The monolith was taken in a small area (40 cm x 40 cm), surrounded by coffee and degraded forest.