Search results
Results From The WOW.Com Content Network
The Deccan Plateau is one of the oldest and most stable land formations in the Indian subcontinent. [28] The plateau is marked by rocky terrain with an average of about 600 m (2,000 ft). [9] The Deccan Traps consist of multiple layers of igneous rocks, which are more than 2 km (1.2 mi) in thickness.
"South India" is also known as "Peninsular India" indicating its location in a peninsula surrounded by water on three sides. [4] The term "Deccan", referring to the area covered by the Deccan Plateau that covers most of peninsular India excluding the coastal areas, is an anglicised form of the Prakrit word dakkhiṇa derived from the Sanskrit word dakshiṇa meaning south. [5]
The Indian plate (or India plate) is a minor tectonic plate straddling the equator in the Eastern Hemisphere. Originally a part of the ancient continent of Gondwana , the Indian plate broke away from the other fragments of Gondwana 100 million years ago and began moving north, carrying Insular India with it. [ 2 ]
The highlands of the plateau are covered with different types of forests, which provide a large variety of forest products. The Deccan plateau includes the region lying south of the Satpura range.it extends up to the southern tip of peninsular India. Anai mudi is the highest peak of this region. The Deccan plateau is surrounded by the western ...
Karbi Anglong plateau is an extension of the Indian Peninsular Plateau (Deccan Plateau) in Assam, a North Eastern state of India. This area receives maximum rainfall from the Southwest summer Monsoon from June through September.
Over time, however, "India" evolved to refer to a distinct political entity that eventually became a nation-state (today the Republic of India). [ 10 ] According to the Oxford English Dictionary , the term subcontinent signifies a "subdivision of a continent which has a distinct geographical, political, or cultural identity" and also a "large ...
Due to continental drift, the India Plate split from Madagascar and collided with the Eurasian Plate resulting in the formation of the Himalayas.. The earliest phase of tectonic evolution was marked by the cooling and solidification of the upper crust of the earth's surface in the Archaean Era (prior to 2.5 billion years) which is represented by the exposure of gneisses and granites especially ...
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 northeastern plateau of India. [3]