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Doli Gutta is a peak in the northern part of the Deccan Plateau. ... At 965 m Doli Gutta is the highest peak in the state of Telangana since the Chintoor and ...
The Deccan is a plateau region extending over an area of 422,000 km 2 (163,000 sq mi) and occupies the majority of the Indian peninsula. It is shaped like an inverted triangle with its upper boundary at the Narmada River basin near the Vindhya-Satpura ranges and the lower boundary at the northern fringes of Tamil Nadu in the south.
2nd highest peak in Ahmednagar. 15: Brahmagiri: 1,295: Trimbakeshwar Range: Nasik: Site of origin of the sacred Godavari River is near Trimbak. 16: Anjaneri: 1,280: Trimbakeshwar Range: Nasik: According to Hindu scriptures, it is the birthplace of Lord Hanuman and thus is named after his mother. 17: Pratapgad: 1,080: Satara Range: Satara
Parasnath is the highest peak in the Chota Nagpur Plateau. [19] Madhya Pradesh: Dhupgarh: Satpura Range: 1,352 4,435 Dhupgarh is the highest peak in the Satpura Range. [20] Chhattisgarh: Nandiraj Bailadila Range section of the Deccan Plateau: 1,276 4,186
At the northern part of the Western Ghats, the height may vary from 900 to 1,200 m (3,000 to 3,900 ft), but in the south they reach a height of 2,637 m (8,652 ft) at Doda Beta, their highest peak. The region between the Eastern and Western Ghats is referred to as the Deccan Plateau. The east-sloping plateau is protected from the heavier rains ...
The range is located in the northeastern area of the Deccan Plateau. It extends in a roughly SW - NE direction for a length of about 70 km south of the Indravati River. [3] Rising to a height of 1,276 m, one of the hills of the Bailadila Range is the highest point in the state of Chhattisgarh.
Kapadia, Harish (2001), Across Peaks & Passes in Darjeeling & Sikkim, Indus Publishing, ISBN 978-81-7387-126-9 World 7200-meter Peaks , peakbagger.com , retrieved 15 February 2015 Weare, Gary (2009), Trekking in the Indian Himalaya , Lonely Planet , ISBN 978-1-74059-768-5 , archived from the original on 2015-08-17 , retrieved 2015-02-14
After the break-up, the Deccan plateau was formed by basalt rocks, which caused the western side to rise at an elevation. [5] Geophysical evidence indicates that the mountains came along the west coast of India somewhere in the late Jurassic and early Cretaceous periods when India separated from the African continent. [6]