Cenozoic climates in deserts

dc.contributor.authorWilliams, M.
dc.contributor.editorParsons, A.
dc.contributor.editorAbrahams, A.
dc.date.issued2009
dc.description.abstractDeserts are superb repositories of geological, geomorphic and archaeological evidence. The very aridity to which they owe their existence has enabled them to preserve a remarkably good record of past depositional and erosional events. The fossil river valleys of the Sahara, the great salt lakes of Australia, China, and Patagonia, the dissected volcanic mountains of the Arabian peninsula and the Afar Desert - all are legacies of former tectonic, volcanic, and climatic episodes which ultimately gave rise to the deserts we see today. Each desert reflects its own individual geological inheritance and geomorphic history; each is unique in its assemblage of landforms; each ideally deserves detailed and separate study in its own right (Pesce 1968, McKee 1978, Rognon 1989). © 2009 Springer Netherlands.
dc.description.statementofresponsibilityM.A.J. Williams
dc.identifier.citationGeomorphology of Desert Environments, 2009 / Parsons, A., Abrahams, A. (ed./s), pp.799-824
dc.identifier.doi10.1007/978-1-4020-5719-9_28
dc.identifier.isbn9781402057182
dc.identifier.orcidWilliams, M. [0000-0003-3114-9337]
dc.identifier.urihttp://hdl.handle.net/2440/58481
dc.language.isoen
dc.publisherSpringer
dc.publisher.placeDordrecht, Netherlands
dc.rights(c) Springer Science+Business Media B.V. 2009
dc.source.urihttp://dx.doi.org/10.1007/978-1-4020-5719-9_28
dc.titleCenozoic climates in deserts
dc.typeBook chapter
pubs.publication-statusPublished

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