The alluvial geology of the lower Orange river and adjacent coastal deposits, South West Africa select="/dri:document/dri:meta/dri:pageMeta/dri:metadata[@element='title']/node()"/>

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dc.contributor.advisor Bishop WW en_US
dc.contributor.author Fowler Jonathan Anthony en_US
dc.date.accessioned 2013-07-02T14:12:40Z
dc.date.available 2013-07-02T14:12:40Z
dc.date.issued 19760101 en_US
dc.identifier.uri http://hdl.handle.net/11070.1/5416
dc.description.abstract Abstract provided by author: en_US
dc.description.abstract Both the marine and riverine deposits lie unconformably on the rocks of the Precambrian Gariep Group. The succession of the latter within the area studied is briefly described en_US
dc.description.abstract The adjacent marine deposits, which form a raised beach complex on the coast, are described and the relationship between these marine and riverine deposits is examined en_US
dc.description.abstract It is concluded that the marine deposits are considerably younger than the riverine deposits, which had previously been considered virtually contemporaneous. It is thought that the marine beaches range from Mid- to Late-Pleistocene, while the riverine deposits are possibly? Plio- Pleistocene to Early Pleistocene in age en_US
dc.format.extent 285 p. [vol 1] en_US
dc.format.extent maps in vol 2 en_US
dc.language.iso eng en_US
dc.subject Sedimentology en_US
dc.subject Coastal regions en_US
dc.subject Regional geology en_US
dc.subject Orange river en_US
dc.subject Alluvium en_US
dc.title The alluvial geology of the lower Orange river and adjacent coastal deposits, South West Africa en_US
dc.type thesis en_US
dc.identifier.isis F099-199502130000442 en_US
dc.description.degree London en_US
dc.description.degree United Kingdom en_US
dc.description.degree University of London en_US
dc.description.degree Ph M en_US
dc.masterFileNumber 441 en_US


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