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Geology and slope assessment along Jalan Tun Sardon, Penang Siti Nur Laila Jamaludin.

By: Siti Nur Laila JamaludinMaterial type: Text

TextPublisher: 2010Description: vii, 43 p. col. ill 30 cmSubject(s): Dissertations, Academic -- Malaysia | Geology -- Pulau Pinang -- Survey | Topography -- Pulau Pinang -- Survey | Slopes (Physical geography) | 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, specifically 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 underlain by granitic formation, which is medium to coarsegrained biotite muscovite granite and quarternary 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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Item type	Current location	Collection	Call number	Status	Date due	Barcode	Item holds
Books	JMG IBUPEJABAT Thesis	Thesis	551.09595113 SNL (Browse shelf)	Available		00002934

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Thesis (B.Sc) Pure Geology - Universiti Malaya, 2010

The study area is located at central part of Penang Island, specifically 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 underlain by granitic formation, which is medium to coarsegrained biotite muscovite granite and quarternary 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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