Geology and slope assessment along Jalan Tun Sardon, Penang Siti Nur Laila Jamaludin.
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TextPublisher: 2010 Description: viii, 42 p. col. ill. , maps 30 cmSubject(s): Dissertations, Academic -- Malaysia | Geology -- Pulau Pinang -- survey | Landslides -- Pulau Pinang | Jalan Tun Sardon (Pulau Pinang)Dissertation note: Thesis (B.Sc) Pure Geology - Universiti Malaya, 2010 Summary: The study area is located at central part of Penang Island, speciically at Jalan Tun Sardon. The study area is chosen due to lot of damages in Penang Island was carried out by landslides. Landslides are closely related to instability of the slope. Generally, the area is the underlain by granitic fromation, which is medium to course grained biotite muscovite granite and quaternary sediments. The study is focusing on the slope stability and slope assessment where both are useful in characterizing the slope in several ranges of hazard rating from very low to very high hazardous.
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JMG IBUPEJABAT Thesis | Thesis | 551.09595113 SNL (Browse shelf) | Available | 00002841 |
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Thesis (B.Sc) Pure Geology - Universiti Malaya, 2010
The study area is located at central part of Penang Island, speciically at Jalan Tun Sardon. The study area is chosen due to lot of damages in Penang Island was carried out by landslides. Landslides are closely related to instability of the slope. Generally, the area is the underlain by granitic fromation, which is medium to course grained biotite muscovite granite and quaternary sediments. The study is focusing on the slope stability and slope assessment where both are useful in characterizing the slope in several ranges of hazard rating from very low to very high hazardous.
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