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Alfisols
developed under forest regime
Andisols
volcanoes; nutrient rich
Aridisols
dry; very little horizon development
Entisols
just beginning to form; no horizons
Gelisols
cold temps; permafrost
Histosols
seasonal wetness; non-fully decomposed organic matter; almost all O layer
Inceptisols
little bit more developed than entisol
Mollisols
prairie soils; large A horizon organic matter
Oxisols
very weathered, organics have been moved out, wet warm tropical, iron oxides
Spodosols
often found in acidic (pine) forests, slight organic A horizon, well developed E horizon
Ultisols
humid areas, older
Vertisols
inverted profile, shrinking and swelling clays