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Abstract
Four Xerofluvents from the Linares map (1 :50.000), sampled in the newst terraces of Guadalquivir, Guadalimar, Guadiel and Rumblar rivers, were studied: Soil classification in diferent systems (C.P.C.S., FAO-UNESCO, SOIL TAXONOMY, REFERENTlEL PEDOLOGIQUE) are similar an all cases Xerofluvents, Fluvisols, or aluvial soils. Other important characteristic are: variable
mineralogy of sand; illitic clay; a little pedogenetic evolution in coleur and structure inherited from parent material; commonly lithological discontinuites; in two cases reddish and yellowish spots, owing to oxiduced deep free water.
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