2 The area where gravel and pebble sediments deposited at foot hills of Himalayas is
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bhabar
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The Himalayan foreland is the area where gravel and Pebble sediment deposited at the foot of Himalaya.
Explanation:
- After descending from the mountains, the rivers deposit pebbles in a narrow belt. This belt is about 8 to 16 km wide and runs parallel to the Shiwaliks. This region is known as Bhabar.
- All streams disappear in this region. The Himalayan foreland basin is an active collisional foreland basin system in South Asia.The uplift and loading of the Eurasian Plate on the Indian Plate led to bending (bending) of the Indian Plate and the creation of a depression adjacent to the Himalayan mountain belt.
- The Himalayan Foreland Basin has been studied in the Himalayas (where the foreland basin sequence has been uplifted and exposed in the Sub-Himalayas and Lesser Himalayas) and underground.
- The backfilling of the foreland basin dates back to the beginning of the development of the foreland basin, which began around 45 to 50 Ma during the Paleogene period. The foreland basin deposition appears to be diachronic; there is a time lag between parts of the pelvis.
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