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Bukit Antarabangsa is a hillside township located in Ulu Klang, Ampang District, Selangor, Malaysia. The area is well known for being an affluent residential suburb occupied by occasional celebrities and political figures alike.
The disastrous landslide of a hill side in 1993 which caused the 12-story Highland Tower to collapse, the 1999 landslide and the 6 December 2008 landslide indicate that this area has a high risk potential for landslide. This can be attributed to the convergence of 3 factors: rainfall, steep hill sides, and soil type/geological foundation.
In a tropical country high rainfall through the year is common, and very high intensity rain during south west and north east monsoons in December and May can be as high as 350 mm a month. Due to the spillover of the East Coast Monsoon rainfall, critical holding capacity can be overwhelmed. This results in highly saturated soils.
In addition to the rain, the steep slopes and soil type are other factors contributing to a high risk of landslides. Geologically, these areas often consist of shale or schist which easily weathers to deep clay-like material of oxic or ferralictic nature, which absorbs water through its deep profile instead of allowing a surface runoff. This may lead to a critical point which results in mass movement of soil.
According to the reconnaissance soil map from the Department of Agriculture, the soil type of the Mountain Area can be of granitic materials (Rengam-Jerangau soil series) while the lower hilly area of Bukit Antarabangsa most probably consist of shale or sandstone materials, which give risk.
Erosion is the action of surface processes that removes soil, rock, or dissolved material from one location on the Earth's crust and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as physical or mechanical erosion; this contrasts with chemical erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres.
Landslides, also known as landslips, or rockslides, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, mudflows, shallow or deep-seated slope failures and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides.
A slump is a form of mass wasting that occurs when a coherent mass of loosely consolidated materials or a rock layer moves a short distance down a slope. Movement is characterized by sliding along a concave-upward or planar surface. Causes of slumping include earthquake shocks, thorough wetting, freezing and thawing, undercutting, and loading of a slope.
Mud is loam, silt or clay mixed with water. It is usually formed after rainfall or near water sources. Ancient mud deposits hardened over geological time to form sedimentary rock such as shale or mudstone. When geological deposits of mud are formed in estuaries, the resultant layers are termed bay muds. Mud has also been used for centuries as a construction resource for mostly houses and also used as a binder.
A gully is a landform created by running water, mass movement, or commonly a combination of both eroding sharply into soil or other relatively erodible material, typically on a hillside or in river floodplains or terraces.
A mudflow, also known as mudslide or mud flow, is a form of mass wasting involving fast-moving flow of debris and dirt that has become liquified by the addition of water. Such flows can move at speeds ranging from 3 meters/minute to 5 meters/second. Mudflows contain a significant proportion of clay, which makes them more fluid than debris flows, allowing them to travel farther and across lower slope angles. Both types of flow are generally mixtures of particles with a wide range of sizes, which typically become sorted by size upon deposition.
Kerala is situated between the Lakshadweep Sea to the west and the Western Ghats to the east. Kerala's coast runs some 590 km in length, while the state itself varies between 35–120 km in width. Geologically, pre-Cambrian and Pleistocene formations comprise the bulk of Kerala's terrain. The topography consists of a hot and wet coastal plain gradually rising in elevation to the high hills and mountains of the Western Ghats. Kerala lies between northern latitude of 8°.17'.30" N and 12°. 47'.40" N and east longitudes 74°.27'.47" E and 77°.37'.12" E. Kerala's climate is mainly wet and maritime tropical, heavily influenced by the seasonal heavy rains brought up by the monsoon Weather.
The Highland Towers collapse occurred on 11 December 1993 in Taman Hillview, Ulu Klang, Selangor, Malaysia. Tower Block 1 collapsed from a major landslide caused by heavy rains that burst diversion pipes. The Highland Towers consisted of three 12-storey buildings or "blocks". The collapse of Block 1 resulted in 48 deaths. Residents of the other two blocks and neighbouring establishments were evacuated due to safety concerns.
Setiawangsa is an eastern suburb in Kuala Lumpur, Malaysia, located less than 4 kilometres from the city centre and located right next to Ampang. There are 4 main residentials within this area;
Ulu Kelang, is a mukim and a state constituency in Gombak District, Selangor, Malaysia. It is one of five state constituencies administered by Majlis Perbandaran Ampang Jaya (MPAJ).
Taman Hillview is a township in Ulu Klang, Gombak District, Selangor, Malaysia. The township lies in a landslide-prone area. It is located next the Kuala Lumpur Middle Ring Road 2.
Landslides in Malaysia are regular natural disasters in Malaysia which occur along hillsides and steep slopes.
There have been known various classifications of landslides. Broad definitions include forms of mass movement that narrower definitions exclude. For example, the McGraw-Hill Encyclopedia of Science and Technology distinguishes the following types of landslides:
The Selangor State Park is a park located in Gombak District, Selangor, Malaysia. The 914.41 square kilometre park was gazetted by the state on January 25, 2007. Upon its establishment, it became the second largest park in Peninsular Malaysia with the largest being the Taman Negara.
An earthflow is a downslope viscous flow of fine-grained materials that have been saturated with water and moves under the pull of gravity. It is an intermediate type of mass wasting that is between downhill creep and mudflow. The types of materials that are susceptible to earthflows are clay, fine sand and silt, and fine-grained pyroclastic material.
Sungai Lalang is a small town in Kuala Muda District, Kedah, Malaysia. It is located 5 kilometer north from Sungai Petani. Sg. Lalang River situated in this town flows into the Merbok River.
The 2008 Bukit Antarabangsa landslide was a landslide that occurred on the early morning of 6 December 2008, at the town of Bukit Antarabangsa of Selangor, Malaysia. 4 people were killed while 15 others were injured from the incident. 14 houses were destroyed during the process. The landslide was colloquially referred with the Highland Towers collapse of 1993, due to its close proximity and similar circumstances.
The Lower Greensand Group is a geological unit present across large areas of Southern England. It was deposited during the Aptian and Albian ages of the Early Cretaceous. It predominantly consists of sandstone and unconsolidated sand that were deposited in shallow marine conditions.
The 2011 Hulu Langat landslide was a landslide attributed to heavy rain that occurred on the afternoon of 21 May 2011, at Kampung Gahal in the district of Hulu Langat at Selangor, Malaysia. The landslide struck an orphanage nearby, killing 16 people, including 13 children.
The Chinese Loess Plateau, or simply the Loess Plateau, is a plateau in north-central China formed of loess, a clastic silt-like sediment formed by the accumulation of wind-blown dust. It is located southeast of the Gobi Desert and is surrounded by the Yellow River. It includes parts of the Chinese provinces of Qinghai, Gansu, Shaanxi and Shanxi. The depositional setting of the Chinese Loess Plateau was shaped by the tectonic movement in the Neogene period, after which strong southeast winds caused by the East Asian Monsoon transported sediment to the plateau during the Quaternary period. The three main morphological types in the Loess Plateau are loess platforms, ridges and hills, formed by the deposition and erosion of loess. Most of the loess comes from the Gobi Desert and other nearby deserts. The sediments were transported to the Loess Plateau during interglacial periods by southeasterly prevailing winds and winter monsoon winds. After the deposition of sediments on the plateau, they were gradually compacted to form loess under the arid climate.