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and the Karbi-Meghalaya plateau. Later, this depression was filled up by the depositional activity of numerous rivers. Today the
Maghalaya and Karbi Anglong plateau remains detached from the main Peninsular block. This area receives maximum rainfall from the South-West monsoon. It is located in the
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is traditionally divided into Garo, Khasi and
Jaintia Hills. The region from the river Dhansiri in the east to the Singimari River on the west is about 400 km long with an average width of about 40 km, covering about 35, 291 km2.
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It is believed that due to the force exerted by the northeastward movement of the Indian plate at the time of the
Himalayan origin, a huge fault was created between the
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plateau proper is towards the south through a patch of highly denuded and subdued senile terrain.
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is pear-shaped and has an area of about 7000 km2. Its link with the
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Vasudevan, Hari; et al. (2006). "Structure and
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121:is, in fact, an extension of the main
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164:north eastern plateau of India.
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221:India:Physical Environment
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123:Indian peninsular plateau
55:"Karbi-Meghalaya Plateau"
337:Karbi-Meghalaya plateau
119:Karbi-Meghalaya plateau
404:Bijawar-Panna Plateau
342:Karbi Anglong Plateau
206:North East India Info
187:North East India Info
127:Karbi Anglong Plateau
332:Chota Nagpur Plateau
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183:"Meghalaya Plateau"
440:Landforms of Assam
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373:Kaas plateau
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38:Please help
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368:Mangi-Tungi
429:Categories
168:References
96:April 2007
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149:Meghalaya
392:Central
155:Details
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