03.40 This group corresponds to stream plains on the western littoral, such as the one along Arroyo Negro, within the Fray Bentos Formation regions, and is therefore found in the departments of Paysandú, Río Negro, Soriano, and Colonia. Some stream plains with similar characteristics in the department of Durazno, such as the one along Aº Villasboas, have also been included in this group. The geological material consists of silty clay sediments and alluvial sediments of variable, stratified textures associated with waterways. The plains have mesorelief. On the higher flats there is an association of Luvic Eutric Brunisols (maximum and planosolic Brown Grasslands), dark brown in color, with silty loam texture, high fertility, and imperfect drainage, and Ochric Solonetz, light grayish brown in color, with silty loam texture, very low fertility, and imperfect drainage. In depressed areas there are Typical Melanic Gleysols (humic Gleys) and, near waterways, Fluvisols (Alluvial Soils), usually with tree vegetation of the riverine forest type. The land is used for grazing, with parkland vegetation and trees of variable density. For scale reasons, this group is included in the Fray Bentos, San Manuel, and Young units on the 1:1.000.000 map (D.S.F.). Productivity Index 96.
Reference code: GCH7250991
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Our office is at Zorrilla de San Martín 447, corner of Roosevelt, Carmelo, Uruguay.
