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Paleosols as indicators of paleoclimatic conditions in the quaternary deposits of New Mexico

โœ Scribed by H.Curtis Monger; David R. Cole


Book ID
117699043
Publisher
Elsevier Science
Year
1998
Tongue
English
Weight
104 KB
Volume
51-52
Category
Article
ISSN
1040-6182

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Late Quaternary playa (stand-water) deposits are present in river channels upstream from dune fields in the northwestern Negev and represent a drainage disordering caused by dune migration during periods of aridity. These deposits are associated with modifications in the drainage system, including c