THE HOLOCENE-TO-RECENT GEOMORPHOLOGICAL, SEDIMENTOLOGICAL AND STRATIGRAPHIC DEVELOPMENT OF THE LOWER PERAK RIVER AND ITS COASTAL-DELTAIC PLAIN
This study focuses on the geomorphology, sedimentology and stratigraphy of lower Perak coastal deltaic-plain in relation to Holocene sea level change. The Perak River is located on the west flank of Peninsular Malaysia and can be divided into four geographic regions; lower and upper parts for bot...
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| Format: | Thesis |
| Language: | English |
| Published: |
2016
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| Subjects: | |
| Online Access: | http://utpedia.utp.edu.my/id/eprint/19980/1/2015-GEOSCEINCE%20AND%20PETROLEUM-THE%20HOLOCENE-TO-RECENT%20GEOMORPHOLOGICAL%2CSEDIMENTOLOGICAL%20AND%20STRATIGRAPHIC%20DEVELOPMENT%20OF%20THE%20LOWER%20PERAK%20RIVER%20AND%20ITS%20COASTAL-DELTAIC%20PLAIN.pdf http://utpedia.utp.edu.my/id/eprint/19980/ |
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| Summary: | This study focuses on the geomorphology, sedimentology and stratigraphy of lower
Perak coastal deltaic-plain in relation to Holocene sea level change. The Perak River
is located on the west flank of Peninsular Malaysia and can be divided into four
geographic regions; lower and upper parts for both of the upstream and coastal areas.
The channel pattern occurred in this area includes the straight-braided and
meandering. The river flow changes it direction from north to south before drifted
easterly to the west at Teluk Intan. |
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