Use this link to cite:
http://hdl.handle.net/2183/5855 El paisaje eólico de la llanura aluvial de San Juan (Llanura Manchega Central)
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Authors
Pérez-González, Alfredo
Aleixandre, T.
Pinilla, Ascensión
Gallardo, J. F.
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Cadernos do Laboratorio Xeolóxico de Laxe, 1983, 5: 631-656 ISBN: 84-7492-198-8
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Abstract
[Resumen] El campo dunar de la Llanura aluvial de San Juan, esta caracterizado por la presencia dedunas arcillosas, limosas o limo-arcillosas. Morfologicamente, son dunas de tipo parabólico y otras con aspecto "cónico", "transverso" o "longitudinal", construidas por paleovientos efectivos que provenían del W y SW. Finalmente, se discute la edad y origen de estos complejos dunares.
[Abstract] The dunes of the San Juan alluvial plain consists most characteristically of clayey, silty, and clayeysilty dunes, which morphologically are most commonly of parabolic type , but dome-shaped, transverse and linear dunes are present as well. These were built up by effective winds coming from the Wand SW. Finally, both the age and genesis of these dunes is discússed.
[Abstract] The dunes of the San Juan alluvial plain consists most characteristically of clayey, silty, and clayeysilty dunes, which morphologically are most commonly of parabolic type , but dome-shaped, transverse and linear dunes are present as well. These were built up by effective winds coming from the Wand SW. Finally, both the age and genesis of these dunes is discússed.