Geomorphology of the Kenyan Coast: Not as a Result of Sea-Level Change Alone
The coastal setting and the geology control the geomorphology on the Kenyan coast. The evolution of the physical environment has also been influenced by climate, wave and tidal regime, sedimentation and river discharge. The shore terraces of Kenyan coast correspond to eustatic movements of sea level. There seems to be evidence of a high water level during the late Pleistocene. For the lower terraces a Holocene age is suggested. During the Pleistocene, sea level fluctuations associated with glacial / interglacial phases left well developed raised platforms and beaches. The Kenyan coast has a strong tectonic influence and it is difficult to describe the coast in terms of emergence or submergence only. It can therefore be concluded that the geomorphology of the Kenyan coast is not only as a result of sea level changes but also due to isostatic readjustments and tectonic movements. This paper examines the previous works done on the Kenyan coast in relation to the developments that have led to its geomorphology.
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Format: | Report biblioteca |
Language: | English |
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1993
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Subjects: | Geomorphology, Sea level, |
Online Access: | http://hdl.handle.net/1834/407 |
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dig-aquadocs-1834-4072021-05-19T06:21:47Z Geomorphology of the Kenyan Coast: Not as a Result of Sea-Level Change Alone Abuodha, P.A.W. Geomorphology Sea level The coastal setting and the geology control the geomorphology on the Kenyan coast. The evolution of the physical environment has also been influenced by climate, wave and tidal regime, sedimentation and river discharge. The shore terraces of Kenyan coast correspond to eustatic movements of sea level. There seems to be evidence of a high water level during the late Pleistocene. For the lower terraces a Holocene age is suggested. During the Pleistocene, sea level fluctuations associated with glacial / interglacial phases left well developed raised platforms and beaches. The Kenyan coast has a strong tectonic influence and it is difficult to describe the coast in terms of emergence or submergence only. It can therefore be concluded that the geomorphology of the Kenyan coast is not only as a result of sea level changes but also due to isostatic readjustments and tectonic movements. This paper examines the previous works done on the Kenyan coast in relation to the developments that have led to its geomorphology. Kenya Marine and Fisheries research Institute (KMFRI) International Union for Quaternary Research (INQUA) Published 2005-07-18T07:35:50Z 2005-07-18T07:35:50Z 1993 Report Non-Refereed http://hdl.handle.net/1834/407 en 288062 bytes application/pdf Kenyan Coast |
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Geomorphology Sea level Geomorphology Sea level Abuodha, P.A.W. Geomorphology of the Kenyan Coast: Not as a Result of Sea-Level Change Alone |
description |
The coastal setting and the geology control the geomorphology on the Kenyan coast.
The evolution of the physical environment has also been influenced by climate, wave
and tidal regime, sedimentation and river discharge. The shore terraces of Kenyan
coast correspond to eustatic movements of sea level. There seems to be evidence of a
high water level during the late Pleistocene. For the lower terraces a Holocene age is
suggested. During the Pleistocene, sea level fluctuations associated with glacial /
interglacial phases left well developed raised platforms and beaches. The Kenyan
coast has a strong tectonic influence and it is difficult to describe the coast in terms of
emergence or submergence only. It can therefore be concluded that the
geomorphology of the Kenyan coast is not only as a result of sea level changes but
also due to isostatic readjustments and tectonic movements. This paper examines the
previous works done on the Kenyan coast in relation to the developments that have
led to its geomorphology. |
format |
Report |
topic_facet |
Geomorphology Sea level |
author |
Abuodha, P.A.W. |
author_facet |
Abuodha, P.A.W. |
author_sort |
Abuodha, P.A.W. |
title |
Geomorphology of the Kenyan Coast: Not as a Result of Sea-Level Change Alone |
title_short |
Geomorphology of the Kenyan Coast: Not as a Result of Sea-Level Change Alone |
title_full |
Geomorphology of the Kenyan Coast: Not as a Result of Sea-Level Change Alone |
title_fullStr |
Geomorphology of the Kenyan Coast: Not as a Result of Sea-Level Change Alone |
title_full_unstemmed |
Geomorphology of the Kenyan Coast: Not as a Result of Sea-Level Change Alone |
title_sort |
geomorphology of the kenyan coast: not as a result of sea-level change alone |
publishDate |
1993 |
url |
http://hdl.handle.net/1834/407 |
work_keys_str_mv |
AT abuodhapaw geomorphologyofthekenyancoastnotasaresultofsealevelchangealone |
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1756075332010508288 |