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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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134:Indian peninsular plateau
66:"Karbi-Meghalaya Plateau"
348:Karbi-Meghalaya plateau
130:Karbi-Meghalaya plateau
18:Karbi-Meghalaya plateau
415:Bijawar-Panna Plateau
353:Karbi Anglong Plateau
217:North East India Info
198:North East India Info
138:Karbi Anglong Plateau
343:Chota Nagpur Plateau
51:improve this article
194:"Meghalaya Plateau"
451:Landforms of Assam
338:Changthang plateau
446:Plateaus of India
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284:Plateaus of India
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49:Please help
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379:Mangi-Tungi
440:Categories
179:References
107:April 2007
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160:Meghalaya
403:Central
166:Details
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