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Essay On Peninsular Malaysia

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Peninsular Malaysia is a part of the Eurasian Plate, the South-East Asian part which is known as Sundaland (Hutchison, 1973). The Bentong-Raub line (Bentong Suture line) was proposed as the major tectonic boundary between the western and central belt of Peninsula Malaysia (Tjia & Syed, 1996). Since its initial recognition, researchers have interpreted the suture as a subduction plate-margin mainly due to the basis of serpentinite and other metabasic bodies occurring within the zone (Tjia & Syed, 1996).
During Early Permian, the rifted Sibumasu oceanic and East Malaya-Indochina continent from Gondwanaland collided. Sibumasu was subsided at the Palaeo-Tethys Ocean. This subduction continued till Middle to Late Permian until the whole oceanic crust was melted into the mantle. The collision was then continued by continent-continent collision during Middle to Late Triassic, resulting Main Range development in Peninsula and Bentong-Raub suture zone.
The Peninsula is subdivided into three belts characterized by different stratigraphy, specifically …show more content…
There are the geometric factor, geological factor, hydrological factor and geomechanical factor. In Tropical areas such as Malaysia, slope failure is either initiated by natural processes or by human activities (Jasmi and Azlikamil, 2000). A landslide takes place when slope materials are no longer able to resist the force of gravity. This decrease in shear resistance resulting in mass movements is due either to internal or external causes. Internal causes involve some change in either the physical or the chemical properties of the rock or soil or its water content. External causes which lead to an increase in shear stress on the slope usually involve a form of disturbance that may be either natural or induced by man (Majeed et. al.). Slope failure or landslides are classified based on the type of movement and type of material (Figure

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