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Boha 3 forms a cluster of lines oriented towards the NE, immediately at the apex of the giant spiral. Boha 4 , on the other hand, is located about 50 meters away, SW of the boustrophedon . We experienced more difficulty achieving a precise mapping because many of these lines are heavily eroded .
This is an accepted version of this page This is the latest accepted revision, reviewed on 10 January 2025. Arid region in India and Pakistan Thar Desert Great Indian Desert Thar Desert in Rajasthan, India Map of the Thar Desert ecoregion Ecology Realm Indomalayan Biome Deserts and xeric shrublands Borders Northwestern thorn scrub forests Rann of Kutch seasonal salt marsh Geography Area ...
The Dune Free Tract spans across several districts including Bikaner, Jaisalmer, Phalodi, and Pokhran, covering an area of approximately 65 square kilometers. Notably, this region is distinguished by its rocky terrain with exposures of limestone and sandstone rocks belonging to the Jurassic and Eocene formations.
The Thar Desert of Sindh is divided into Nara, Achro, and Thar, all situated in the southern part of Sindh. [3] Historical records indicate that the normal monsoon is around 127.5 mm, but it reached a maximum of 443.9 mm in 2011 due to sudden climatic changes. Water scarcity is prevalent in many areas, leading to limitations in agriculture.
Nara is the northeastern part of the Thar Desert in Sindh. It primarily occupies the Khairpur district and a few parts of Sanghar District . [ 1 ] It covers an area of approximately 23,000 km 2 and is composed of sandy hills, steep slopes, and extensive low-lying regions, referred to locally as " Patt (پَٽ)".
The Thar Desert, also known as the Great Indian Desert, is a large, arid region in the northwestern part of the Indian subcontinent that forms a natural boundary between India and Pakistan. It is the world's 16th largest desert, and the world's 9th largest subtropical desert. 85% of the Thar Desert is in India, and the remaining 15% is in ...
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The distribution coefficient K d is the ratio of the soil's radioactivity (Bq g −1) to that of the soil water (Bq ml −1). If the radioactivity is tightly bonded to by the minerals in the soil then less radioactivity can be absorbed by crops and grass growing in the soil. Cs-137 K d = 1000; Pu-239 K d = 10000 to 100000; Sr-90 K d = 80 to 150 ...