Geological investigations of proposed bridge sites at Jerantut and Kampung Kuala Lepar, Pahang Ang Num Kiat.

By: Ang, Num KiatMaterial type: TextTextPublisher: 1973Description: 7 p. ill 33 cmSubject(s): Engineering geology -- Pahang -- Kampung Kuala Lepar | Kampung Kuala Lepar (Jerantut, Pahang)Summary: The general area around the bridge site is underlain by rocks of sedimentary origin, consisting mainly of shale, sandstone, conglomerate and minor amount of limestone. Alluvium, predominantly of clay and sand, is largely confined to the banks of Sungei Pahang.
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Reports JMG IBUPEJABAT
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Open Shelf 551.09595123 ANG (Browse shelf) Available 00003759
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The general area around the bridge site is underlain by rocks of sedimentary origin, consisting mainly of shale, sandstone, conglomerate and minor amount of limestone. Alluvium, predominantly of clay and sand, is largely confined to the banks of Sungei Pahang.

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