The geology of the Kalahari Gemsbok National Park

The floor rocks of the Kalahari Group are only known from boreholes. It consists of rocks of the Karoo Sequence with its associated intrusions of dolerite. The pre-Kalahari topography was dissected by rivers which drained in the direction of the present Botswana. The distribution of the oldest forma...

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Main Author: S. J Malherbe
Format: Article
Language:English
Published: AOSIS 1984-12-01
Series:Koedoe: African Protected Area Conservation and Science
Online Access:http://www.koedoe.co.za/index.php/koedoe/article/view/567
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author S. J Malherbe
author_facet S. J Malherbe
author_sort S. J Malherbe
collection DOAJ
description The floor rocks of the Kalahari Group are only known from boreholes. It consists of rocks of the Karoo Sequence with its associated intrusions of dolerite. The pre-Kalahari topography was dissected by rivers which drained in the direction of the present Botswana. The distribution of the oldest formation of the Kalahari Group, the Wessels Formation (clayey gravel), and the overlying Budin Formation (clay) was also determined from borehole records. The Karoo Sequence was probably the source of these rocks. The overlying Eden Formation (sandstone, grit and conglomerate) had a source which could yield much sand. All these formations were deposited under fluviatile conditions. The Mokalanen Formation (calcrete) and the Gordonia Formation (sand) indicate a change from a humid to an arid environment. The Lonely Formation (clayey diatomaceous limestone) was deposited in a lacustrine environment. It also indicates a higher rainfall in an otherwise arid period. The Goeboe Goeboe Formation consists of clay and sand in the pans and rivers.
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spelling doaj.art-179a982748d543659d8845d32523aad32022-12-22T02:01:03ZengAOSISKoedoe: African Protected Area Conservation and Science0075-64582071-07711984-12-012723344516The geology of the Kalahari Gemsbok National ParkS. J Malherbe0Geological SurveyThe floor rocks of the Kalahari Group are only known from boreholes. It consists of rocks of the Karoo Sequence with its associated intrusions of dolerite. The pre-Kalahari topography was dissected by rivers which drained in the direction of the present Botswana. The distribution of the oldest formation of the Kalahari Group, the Wessels Formation (clayey gravel), and the overlying Budin Formation (clay) was also determined from borehole records. The Karoo Sequence was probably the source of these rocks. The overlying Eden Formation (sandstone, grit and conglomerate) had a source which could yield much sand. All these formations were deposited under fluviatile conditions. The Mokalanen Formation (calcrete) and the Gordonia Formation (sand) indicate a change from a humid to an arid environment. The Lonely Formation (clayey diatomaceous limestone) was deposited in a lacustrine environment. It also indicates a higher rainfall in an otherwise arid period. The Goeboe Goeboe Formation consists of clay and sand in the pans and rivers.http://www.koedoe.co.za/index.php/koedoe/article/view/567
spellingShingle S. J Malherbe
The geology of the Kalahari Gemsbok National Park
Koedoe: African Protected Area Conservation and Science
title The geology of the Kalahari Gemsbok National Park
title_full The geology of the Kalahari Gemsbok National Park
title_fullStr The geology of the Kalahari Gemsbok National Park
title_full_unstemmed The geology of the Kalahari Gemsbok National Park
title_short The geology of the Kalahari Gemsbok National Park
title_sort geology of the kalahari gemsbok national park
url http://www.koedoe.co.za/index.php/koedoe/article/view/567
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