El paisaje eólico de la llanura aluvial de San Juan (Llanura Manchega Central)
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1983
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Seminario de Estudos Galegos. Area de Xeoloxía e Minería ; Instituto Universitario de Xeoloxía "Isidro Parga Pondal"
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Abstract
El campo dunar de la Llanura aluvial de San Juan, esta caracterizado por la presencia de dunas arcillosas, limosas o limo-arcillosas. Morfológicamente, son dunas de tipo parabólico y otras con aspecto "cónico", "transverso" o "longitudinal", construidas por paleovientos efectivos que provenían del W y SI-J.. Finalmente, se discute la edad y origen de estos complejos dunares.
The dunes of the San Juan alluvial p1ain consists most characteristically of c1ayey, silty, and c1ayey si1ty dunes, which morphologically are most common1y of parabolic type , but dome-shaped, transverse and linear dunes are present as well. These were built up by effective winds coming from the W and SW. Finally, both the age and genesis of these dunes is discussed.
The dunes of the San Juan alluvial p1ain consists most characteristically of c1ayey, silty, and c1ayey si1ty dunes, which morphologically are most common1y of parabolic type , but dome-shaped, transverse and linear dunes are present as well. These were built up by effective winds coming from the W and SW. Finally, both the age and genesis of these dunes is discussed.