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Alta resolución de cambios ambientales del holoceno en el desierto de Thar, noroeste de la India

Enzel1, Ely, Mishra

  • 1Institute of Earth Sciences and Department of Geography, The Hebrew University of Jerusalem, Jerusalem 91904, Israel. Department of Geology, Central Washington University, Ellensburg, WA 98926, USA. Deccan College, Deccan College Road, Pune 4110.

Science (New York, N.Y.)
|April 2, 1999
PubMed
Resumen

El clima del Holoceno en la India vio cambios en el nivel del lago impulsados por las lluvias monzónicas. La civilización Harappan prosperó durante condiciones áridas, no sincronizadas con el lago.

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