Give brief account on Aaravali range.
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The Aravalli Range is one of the most popular mountain ranges in the western part of India. Stretching about 300 miles from the northeast to the southwest, the Aravallis intercept the state of Rajasthan on its stretch. The highest point in the Aravalli Range is called as Guru Shikhar, which is located in Mount Abu. At this point, the peak rises to about 5653 feet.
The northern end of the Aravalli Range is a stretch of isolated and rocky hills and ridges that starts in Haryana and ends in Delhi. The southwestern range of the Aravalli passes through Gujarat and Rajasthan. Ajmer in Rajasthan is located on the southern slopes of the Aravallis. Situated near a narrow gorge, the city of Bundi in Rajasthan is surrounded by the Aravalli Range on its three sides.
The Aravallis are some of the oldest fold mountains in the world. Beginning from the Rajasthan in western India, the mountain range extends to Delhi. The peaks of the Aravalli range are not pointed as young fold mountains. They have been eroded by the forces of nature like rain, wind and sunshine.
The Aravalli Range(Devanagari: आरवल्लि ) is a range of mountains running approximately 692 km (430 mi) in a southwest direction, starting in North India from Delhi and passing through southern Haryana,[1] through to Western India across the states of Rajasthan and ending in Gujarat
The Aravalli Range, an eroded stub of ancient mountains, is the oldest range of fold mountains in India.[6] The natural history of the Aravalli Range dates back to times when the Indian Plate was separated from the Eurasian Plate by an ocean. The Proterozoic Aravalli-Delhi orogenic belt in north west India is similar to the younger Himalayan-type orogenic belts of the Mesozoic-Cenozoic era (of the Phanerozoic) in terms of component parts and appears to have passed through a near-orderly Wilson supercontinental cycle of events. The range rose in a Precambrian event called the Aravalli-Delhi Orogen. The Aravalli Range is a northeast-southwest trending orogenic belt that is located in the northwestern part of Indian Peninsula. It is part of the Indian Shield that was formed from a series of cratonic collisions.[7] In ancient times, Aravalli were extremely high but since have worn down almost completely by millions of years of weathering, where as the Himalayas being young fold mountains are still continuously rising. Aravalli, being the old fold mountains, have stopped growing higher due to the cessation of upward thrust caused by the stopping of movement of the tectonic plates in the Earth's crust below them. The Aravalli Range joins two of the ancient earth's crust segments that make up the greater Indian craton, the Aravalli Craton which is the Marwar segment of earth's crust to the northwest of the Aravalli Range, and the Bundelkand Craton segment of earth's crust to the southeast of the Aravalli Range. Cratons, generally found in the interiors of tectonic plates, are old and stable parts of the continental lithosphere that has remained relatively undeformed during the cycles of merging and rifting of continents.
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