Features of The Great Indian Desert
Important features of The Great Indian Desert are as follows:
- The Great Indian Desert stretches out from the Aravalli Hills in the upper east to Punjab and Haryana in the north, the Rann of Kutch along the western coast, and the Indus River alluvial fields in the northwest.
- The dirt of the Great Indian Desert stays dry the entire year and is inclined to wind disintegration.
- Fast breezes shoot strong sand from the desert, storing some of it on useful fields. The desert’s sand hills shift because of the solid breezes.
- Because of the way that not very many neighborhood tree species can endure the serious desert environment, non-local tree species are planted.
- Jojoba has demonstrated to be the most encouraging of these, as well as the most monetarily practical for establishing in these spots.
- It has a dry environment with little vegetation. Due to these distinctive qualities, this is otherwise called Marusthali.
- This region was believed to be submerged during the Mesozoic period. This is upheld by information from the Akal Wood Fossil Park and ocean stores.
- The Luni River is the main enormous stream around here.
- It is a water-focused locale because of little precipitation and unreasonable vanishing. A few streams stop after a specific distance and address a regular event of inland waste by joining a lake or playa.
- The lakes and playas have saline water, which is the essential wellspring of salt.
Write short note on The Indian Desert
The Great Indian Desert, notable as the Thar Desert, is a huge and parched district in the northwestern piece of the Indian subcontinent. Covering around 200,000 km2 as far as the region it frames a characteristic limit between India and Pakistan. The Thar Desert is a huge dry region covering more than 200,000 square kilometers. It fills in as a characteristic obstruction among India and Pakistan. The surface is comprised of aeolian (wind-saved) sand that has aggregated over 1.8 million years.