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Médanos (geology) : ウィキペディア英語版 | Médanos (geology)
__NOTOC__ In South America, the word médanos refers to continental dunes whereas dunas refers to dunes of coastal origin. Médanos may be vegetated or unvegetated. For example, the médanos of La Pampa Province in Argentina are mostly vegetated dunes with occasional blowouts. On the other hand, the dunes of Médanos de Coro National Park in Venezuela are mostly unvegetated. An early description of unvegetated médanos in Peru is provided by the Swiss naturalist and explorer Johann Jakob von Tschudi (1847):〔Tschudi, J.J. von. 1847. Travels in Peru during the years 1838-1842. New York: Wiley & Putnam, 354 pp. (Translated from the German by Thomasina Ross)〕
"The médanos are hillock-like elevations of sand, some having a firm, others a loose base. The former, which are always crescent-shaped, are from ten to twenty feet high, and have an acute crest. The inner side is perpendicular, and the outer or bow side forms an angle with a steep inclination downward. When driven by violent winds, the médanos pass rapidly over the plains. The smaller and lighter ones move quickly forwards before the larger ones; but the latter soon overtake and crush them, whilst they are themselves shivered by the collision. These medanos assume all sorts of extraordinary figures, and sometimes move along the plain in rows forming most intricate labyrinths, whereby what might otherwise be visible in the distance is withdrawn from the view of the traveller. A plain often appears to be covered with a row of médanos, and some days afterwards it is again restored to its level and uniform aspect. Persons who have the greatest experience of the coast are apt to mistake their way, when they encounter these sandhills."
==See also==
*Aeolian processes *Barchan *Blowout (geology)
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