Geomorphology of the upper Mkhomazi River basin, KwaZulu-Natal, South Africa, with emphasis on late Pleistocene colluvial deposits

We present a 1:50 000 scale geomorphological map of the upper Mkhomazi River basin, located in the foothills of the Drakensberg mountains in KwaZulu-Natal Province, South Africa. The sub-horizontal strata of the Permo-Triassic Beaufort Group forms plateau interfluves with a concave valley slope morp...

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Main Authors: Alberto Bosino, Alice Bernini, Greg A. Botha, Greta Bonacina, Luisa Pellegrini, Adel Omran, Volker Hochschild, Christian Sommer, Michael Maerker
Format: Article
Language:English
Published: Taylor & Francis Group 2021-06-01
Series:Journal of Maps
Subjects:
Online Access:http://dx.doi.org/10.1080/17445647.2020.1790435
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spelling doaj-131c3cfa86754e429952fe5ab07001bd2021-07-15T13:10:34ZengTaylor & Francis GroupJournal of Maps1744-56472021-06-0117351610.1080/17445647.2020.17904351790435Geomorphology of the upper Mkhomazi River basin, KwaZulu-Natal, South Africa, with emphasis on late Pleistocene colluvial depositsAlberto Bosino0Alice Bernini1Greg A. Botha2Greta Bonacina3Luisa Pellegrini4Adel Omran5Volker Hochschild6Christian Sommer7Michael Maerker8Department of Earth and Environmental Sciences, Pavia UniversityDepartment of Earth and Environmental Sciences, Pavia UniversityCouncil for GeoscienceDepartment of Earth and Environmental Sciences, Pavia UniversityDepartment of Earth and Environmental Sciences, Pavia UniversityDepartment of Geography, Tübingen UniversityDepartment of Geography, Tübingen UniversityDepartment of Geography, Tübingen UniversityDepartment of Earth and Environmental Sciences, Pavia UniversityWe present a 1:50 000 scale geomorphological map of the upper Mkhomazi River basin, located in the foothills of the Drakensberg mountains in KwaZulu-Natal Province, South Africa. The sub-horizontal strata of the Permo-Triassic Beaufort Group forms plateau interfluves with a concave valley slope morphology. Locally, thick sequences of late Pleistocene colluvial deposits and associated buried paleosols (Masotcheni Formation) infill first-order tributary stream valleys and extend across the adjacent lower slopes. Surface runoff processes preferentially incise into the poorly consolidated, highly erodible sediments causing severe gully erosion that is responsible for widespread land degradation and desertification phenomena. The main purpose of this work is to derive a geomorphological map of the study area focussing on the erosional landforms to understand their spatial distribution and their relation to the colluvial deposits. Finally, a local and regional stratigraphic correlation of colluvial deposits and associated buried palaeosol profiles is proposed.http://dx.doi.org/10.1080/17445647.2020.1790435geomorphological mapkwazulu-natal (rsa)gully erosionrill-interrill erosionriver terracesmasotcheni formation
collection DOAJ
language English
format Article
sources DOAJ
author Alberto Bosino
Alice Bernini
Greg A. Botha
Greta Bonacina
Luisa Pellegrini
Adel Omran
Volker Hochschild
Christian Sommer
Michael Maerker
spellingShingle Alberto Bosino
Alice Bernini
Greg A. Botha
Greta Bonacina
Luisa Pellegrini
Adel Omran
Volker Hochschild
Christian Sommer
Michael Maerker
Geomorphology of the upper Mkhomazi River basin, KwaZulu-Natal, South Africa, with emphasis on late Pleistocene colluvial deposits
Journal of Maps
geomorphological map
kwazulu-natal (rsa)
gully erosion
rill-interrill erosion
river terraces
masotcheni formation
author_facet Alberto Bosino
Alice Bernini
Greg A. Botha
Greta Bonacina
Luisa Pellegrini
Adel Omran
Volker Hochschild
Christian Sommer
Michael Maerker
author_sort Alberto Bosino
title Geomorphology of the upper Mkhomazi River basin, KwaZulu-Natal, South Africa, with emphasis on late Pleistocene colluvial deposits
title_short Geomorphology of the upper Mkhomazi River basin, KwaZulu-Natal, South Africa, with emphasis on late Pleistocene colluvial deposits
title_full Geomorphology of the upper Mkhomazi River basin, KwaZulu-Natal, South Africa, with emphasis on late Pleistocene colluvial deposits
title_fullStr Geomorphology of the upper Mkhomazi River basin, KwaZulu-Natal, South Africa, with emphasis on late Pleistocene colluvial deposits
title_full_unstemmed Geomorphology of the upper Mkhomazi River basin, KwaZulu-Natal, South Africa, with emphasis on late Pleistocene colluvial deposits
title_sort geomorphology of the upper mkhomazi river basin, kwazulu-natal, south africa, with emphasis on late pleistocene colluvial deposits
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2021-06-01
description We present a 1:50 000 scale geomorphological map of the upper Mkhomazi River basin, located in the foothills of the Drakensberg mountains in KwaZulu-Natal Province, South Africa. The sub-horizontal strata of the Permo-Triassic Beaufort Group forms plateau interfluves with a concave valley slope morphology. Locally, thick sequences of late Pleistocene colluvial deposits and associated buried paleosols (Masotcheni Formation) infill first-order tributary stream valleys and extend across the adjacent lower slopes. Surface runoff processes preferentially incise into the poorly consolidated, highly erodible sediments causing severe gully erosion that is responsible for widespread land degradation and desertification phenomena. The main purpose of this work is to derive a geomorphological map of the study area focussing on the erosional landforms to understand their spatial distribution and their relation to the colluvial deposits. Finally, a local and regional stratigraphic correlation of colluvial deposits and associated buried palaeosol profiles is proposed.
topic geomorphological map
kwazulu-natal (rsa)
gully erosion
rill-interrill erosion
river terraces
masotcheni formation
url http://dx.doi.org/10.1080/17445647.2020.1790435
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