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History of landslide susceptibility and a chorology of landslide-prone areas in the Western Ghats of Kerala, India
Kerala is the third most densely populated state in India. It is a narrow strip of land, of which 47 is occupied by the most prominent orographic feature of peninsular India, The Western Ghats mountain chain. The highlands of Kerala experience several types of landslides, of which debris flows are t...
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| Format: | Printed Book |
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Environ Geol (2009) 57:1553-1568
2009
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| Online Access: | http://10.26.1.76/ks/003352.pdf |
| LEADER | 024820000a22001450004500 | ||
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| 100 | |a Sekhar L. Kuriakose G. Sankar C. Muraleedharan | ||
| 245 | |a History of landslide susceptibility and a chorology of landslide-prone areas in the Western Ghats of Kerala, India | ||
| 260 | |c 2009 | ||
| 260 | |b Environ Geol (2009) 57:1553-1568 | ||
| 520 | |a Kerala is the third most densely populated state in India. It is a narrow strip of land, of which 47 is occupied by the most prominent orographic feature of peninsular India, The Western Ghats mountain chain. The highlands of Kerala experience several types of landslides, of which debris flows are the most common. They are called ``Urul Pottal'' in the local vernacular. The westfacing Western Ghats scarps that runs the entire extent of the mountain system is the most prone physiographic unit for landslides. The highlands of the region experience an annual average rainfall as high as 500 cm through the South-West, North-East and Pre-Monsoon showers. A survey of ancient documents and early news papers indicates a reduced rate of slope instability in the past. The processes leading to landslides were accelerated by anthropogenic disturbances such as deforestation since the early 18th century, terracing and obstruction of ephemeral streams and cultivation of crops lacking capability to add root cohesion in steep slopes. The events have become more destructive given the increasing vulnerability of population and property. Majority of mass movements have occurred in hill slopes [20 along the Western Ghats scarps, the only exception being the coastal cliffs. Studies conducted in the state indicates that prolonged and intense rainfall or more particularly a combination of the two and the resultant pore pressure variations are the most important trigger of landslides. The initiation zone of most of the landslides was typical hollows generally having degraded natural vegetation. A survey of post-landslide investigation and news paper reports enabled the identification of 29 major landslide events in the state. All except one of the 14 districts in the state are prone to landslides. Wayanad and Kozhikode districts are prone to deep seated landslides, while Idukki and Kottayam are prone to shallow landslides | ||
| 650 | |a LAND USE RAINFALL INTENSITY PORE PRESSURE | ||
| 856 | |u http://10.26.1.76/ks/003352.pdf | ||
| 942 | |c KS | ||
| 999 | |c 72740 |d 72740 | ||
| 952 | |0 0 |1 0 |4 0 |7 0 |9 64704 |a MGUL |b MGUL |d 2015-08-01 |l 0 |r 2015-08-01 |w 2015-08-01 |y KS | ||