Use this link to cite:
http://hdl.handle.net/2183/5832 Dinámica geomorfológica de los Llanos de Apure (Venezuela)
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Clemente, L.
Pascual, J.
Siljestrom, P.
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Cadernos do Laboratorio Xeolóxico de Laxe, 1983, 5: 255-281 ISBN: 84-7492-198-8
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Abstract
[Resumen] Dentro de la zona de estudio se definen una serie de unidades geomorfológicas (Banco,Bajío y Estero) que están íntimamente relacionadas con los suelos que en ellas se desarrollan. Las características edáficas, el análisis granulométrico de las fracciones gruesas (arenas) y finas (limos) de los horizontes más representativos, y la mineralogía de la fracción arcilla, permiten conocer la dinámica geomorfológica del área.
[Abstract] In the studied area, three main geomorphological units have been defined: (Banco, Bajío and Estero), very closely related to the soils developed in them. The edaphic features, particle-size distribution of coarse and fine fractions (sand and silt) from the most representative horizons and the clayfraction mineralogy, allow us to know the geomorphological dynamics of the area.
[Abstract] In the studied area, three main geomorphological units have been defined: (Banco, Bajío and Estero), very closely related to the soils developed in them. The edaphic features, particle-size distribution of coarse and fine fractions (sand and silt) from the most representative horizons and the clayfraction mineralogy, allow us to know the geomorphological dynamics of the area.