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The name Western Ghats derives from the word ghat and the cardinal direction in which it is located with respect to the Indian mainland. Ghat, a term used in the Indian subcontinent, depending on the context, could either refer to a range of stepped hills such as the Eastern Ghats and Western Ghats, or a series of steps leading down to a body of water or wharf.
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 ...
Anamudi, on the right, is the highest peak of the Western Ghats at 2,695 m (8,842 ft) Nilgiris, a part of Western Ghats at Masinangudi, Tamil Nadu Nilambur Mukurthi Peak Indian top cool peak Kerala, Nilagiri Tamil Nadu Vagamon Hills with shola vegetation Kodachadri Hills Chembra Peak covered with mist Banasura Hill with cloud covered Illikkal Kallu Malleswaran in a distant vision Varayadumotta ...
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The Western Ghats lie between coastal plains adjoining the Arabian Sea and the Deccan Plateau. There are many Ghat Roads which connect Karavali districts with the Malenadu and Bayaluseemae regions. Most of these ghats are very scenic during monsoon season in the months of June, July, and August. Landslides can occur in a few of these ghats ...
They are broadly divided into the Western Coastal Plains and the Eastern Coastal Plains. The two coastal plains meet at Kanyakumari, the southernmost tip of the Indian mainland. The eastern coastal plain is located between The Bay of Bengal and the eastern Ghats and the western coastal plain is located between the Arabian Sea and the western ...
The geography of Texas is diverse and large. Occupying about 7% of the total water and land area of the U.S., [1] it is the second largest state after Alaska, and is the southernmost part of the Great Plains, which end in the south against the folded Sierra Madre Oriental of Mexico.
Shaded relief map of the Llano Estacado. Texas contains a wide variety of geologic settings. The state's stratigraphy has been largely influenced by marine transgressive-regressive cycles during the Phanerozoic, with a lesser but still significant contribution from late Cenozoic tectonic activity, as well as the remnants of a Paleozoic mountain range.