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The Aravalli Range (also spelled Aravali) is a mountain range in Northern-Western India, running approximately 670 km (420 mi) in a south-west direction, starting near Delhi, passing through southern Haryana, [1] Rajasthan, and ending in Ahmedabad Gujarat.
The Khathiar–Gir dry deciduous forests include the Aravalli Range, the high point of which is Mount Abu with an elevation of 1,721 m (5,646 feet), and a small part of the Northwestern thorn scrub forests in the west. In the west is the Kathiawar Peninsula and the strip of western Rajasthan between the Aravalli Range and Thar Desert.
Nag Pahad (also known as Naga Pahar; English: Snake Mountain) is a mountain in the Aravalli mountain range located between the towns of Pushkar and Ajmer in the Indian state of Rajasthan. This mountain holds cultural and mythological importance, intertwined with legends and beliefs that have been passed down through generations. [1]
The Aravalli range extends from Delhi south-west to near Ahmedabad for a distance of about 800 km. To the east of the Aravalli range lies the East Rajasthan Upland that ranges in height from 250 to 500 m. The Chambal river enters the State of Rajasthan near the northern end of the Gandhi Sagar Reservoir and flows for 360 km in Rajasthan. The ...
"Kumbhal fort"), also known as the Great Wall of India, [2] is a fortress on the westerly range of Aravalli Hills in Kumbhalgarh in the Rajsamand district of the Rajasthan state in India. Situated approximately 48 km (30 mi) from Rajsamand city, 84 km (52 mi) from Udaipur, it was built during the 15th century by Rana Kumbha. [3]
The Arvari River, which originates in Aravalli range, is a small river flowing through the Alwar District of Rajasthan, India. It has a total length of 45 km (28 mi) and a total basin area of 492 km 2 (190 sq mi). [1] Downstream of the Sainthal Sagar dam on Arvari, the Arvari river meets Sarsa River to become the Sanwan River.
The Aravalli Mountain Range is a northeast-southwest trending orogenic belt in the northwest part of India and is part of the Indian Shield that was formed from a series of cratonic collisions. [1] The Aravalli Mountains consist of the Aravalli and Delhi fold belts, and are collectively known as the Aravalli-Delhi orogenic belt.
Malani Igneous Suite Contact below Mehrangarh Fort in Jodhpur. Jodhpur Group-Malani Igneous Suite Contact of Aravalli range is a geological feature representing the last phase of igneous activity of Precambrian age in the Indian Subcontinent at the foot of the picturesque Mehrangarh Fort in Jodhpur city, the second largest city in Rajasthan after Jaipur.