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History of sediments at Khommabes, central Namib Desert / James T. Teller; N. Lancaster

By: Contributor(s): Material type: TextTextLanguage: English Series: Madoqua, Vol. 14, No. 3, (1985) ; p. 267 - 278Publication details: Windhoek : Nature Conservation and Tourism Division, 1985, : John Meinert PrintingDescription: 12 pages : plates, fig.; 28 cmSubject(s): DDC classification:
  • PER 154 Madoqua
Summary: Sediments of the Khommabes depression provide evidence for a varied history of deposition and secondary alteration during the Quaternary and contains deposits representing a long and varied history of sedimentation and secondary alteration. During a period of a wetter climate, fluvial sediments, probably deposited on a former flood-plain of the Kuiseb River, were cemented by calcite to form calcrete
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Sediments of the Khommabes depression provide evidence for a varied history of deposition and secondary alteration during the Quaternary and contains deposits representing a long and varied history of sedimentation and secondary alteration. During a period of a wetter climate, fluvial sediments, probably deposited on a former flood-plain of the Kuiseb River, were cemented by calcite to form calcrete

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