
The mountain range which stretches from Gujarat in west to Delhi in the north is the _____________.
(A) Aravallis
(B) Vindhyas
(C) Satpuras
(D) Kaimur range
Answer
535.2k+ views
Hint: The mountain range which stretches from Gujarat in the west to Delhi in the north is a scope of mountains running around 692 km a southwest way. Beginning in North India, it goes through southern Haryana, through to Western India over the conditions of Rajasthan and finishing off with Gujarat.
Complete step-by-step solution:
The Aravalli Range is a mountain range in Northwestern India, running roughly 692 km in a south-west bearing, beginning close to Delhi, going through southern Haryana and Rajasthan, and finishing off with Gujarat. The most noteworthy pinnacle is Guru Shikhar at 1,722 meters.
The Aravalli Range, a dissolved stub of antiquated mountains, is the most seasoned scope of Crease Mountains in India. The common history of the Aravalli Range goes back to times when the Indian Plate was isolated from the Eurasian Plate by a sea. The Proterozoic Aravalli-Delhi orogenic belt in northwest India is like the more youthful Himalayan-type orogenic belts of the Mesozoic-Cenozoic time (of the Phanerozoic) as far as segment parts and seems to have gone through a close efficient Wilson supercontinental pattern of occasions. The reach rose in a Precambrian occasion called the Aravalli-Delhi Orogen. The Aravalli Range is an upper east southwest moving orogenic belt that is situated in the northwestern piece of Indian Peninsula. It is essential for the Indian Shield that was framed from a progression of cratonic collisions. In antiquated occasions, Aravalli was very high yet has worn out totally by a great many long stretches of enduring, while the Himalayas being youthful overlay mountains are still consistently rising.
Thus, option (A) is correct.
Note: Aravalli, being the old crease mountains, have quit becoming higher because of the end of upward push brought about by the halting of development of the structural plates in the Earth's outside underneath them. The Aravalli Range joins two of the antiquated earth outside portions that make up the more noteworthy Indian craton, the Aravalli Craton which is the Marwar section of the earth's covering toward the northwest of the Aravalli Range, and the Bundelkhand Craton fragment of earth's hull toward the southeast of the Aravalli Range.
Complete step-by-step solution:
The Aravalli Range is a mountain range in Northwestern India, running roughly 692 km in a south-west bearing, beginning close to Delhi, going through southern Haryana and Rajasthan, and finishing off with Gujarat. The most noteworthy pinnacle is Guru Shikhar at 1,722 meters.
The Aravalli Range, a dissolved stub of antiquated mountains, is the most seasoned scope of Crease Mountains in India. The common history of the Aravalli Range goes back to times when the Indian Plate was isolated from the Eurasian Plate by a sea. The Proterozoic Aravalli-Delhi orogenic belt in northwest India is like the more youthful Himalayan-type orogenic belts of the Mesozoic-Cenozoic time (of the Phanerozoic) as far as segment parts and seems to have gone through a close efficient Wilson supercontinental pattern of occasions. The reach rose in a Precambrian occasion called the Aravalli-Delhi Orogen. The Aravalli Range is an upper east southwest moving orogenic belt that is situated in the northwestern piece of Indian Peninsula. It is essential for the Indian Shield that was framed from a progression of cratonic collisions. In antiquated occasions, Aravalli was very high yet has worn out totally by a great many long stretches of enduring, while the Himalayas being youthful overlay mountains are still consistently rising.
Thus, option (A) is correct.
Note: Aravalli, being the old crease mountains, have quit becoming higher because of the end of upward push brought about by the halting of development of the structural plates in the Earth's outside underneath them. The Aravalli Range joins two of the antiquated earth outside portions that make up the more noteworthy Indian craton, the Aravalli Craton which is the Marwar section of the earth's covering toward the northwest of the Aravalli Range, and the Bundelkhand Craton fragment of earth's hull toward the southeast of the Aravalli Range.
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