Duar Formation
Question 1: What is duar formation?
Answer:
Duar formations are typically formed by a combination of erosion and tectonic activity. The movement of tectonic plates can create uplift in the earth’s crust, which is then worn away by erosion.
Question 2: What is the main characteristic of a duar formation?
Answer:
The main characteristic of a duar formation is a series of parallel ridges and valleys.
Question 3: What are some examples of duar formations?
Answer:
Some examples of duar formations are the Himalayan Duars in India and Bhutan, and the Great Dividing Range in Australia.
What is Duar Formation?
Duar formations are geological structures that occur in certain mountainous regions around the world. They are characterized by a series of parallel ridges and valleys that have been formed by erosion and tectonic activity.
In the Indian context, duars refer to the floodplains situated around the Himalayas, in the state of Assam in the North-East and in the north of West Bengal. The altitude of duars varies from a minimum of 90 m to a maximum of 1750 m. It is also referred to as silts, in case of river overflow, floods occur and leave behind sediments classified mostly as duars.
Duar Formation in Assam
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