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This is an accepted version of this page This is the latest accepted revision, reviewed on 20 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.
It is situated in the Thar Desert region. Surrounded by rocks, sand and five salt ranges, the word "Pokaran" (पोकरण) means "place surrounded by five salt-ranges" in Rajasthani. The site for India's first and second underground nuclear weapon test is near Pokhran.
The Boha geoglyphs or Great Indian Desert geoglyph are a group of large geoglyphs made in the soil in the Thar Desert of Rajasthan, India. Several sites were found located around the city of Jaisalmer , marked by geometrical lines resembling geoglyphs.
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 ...
The Thar Desert — located within Rajasthan in northwestern India, and Sindh and Punjab provinces of eastern Pakistan. An Indomalayan ecoregion of the Deserts and xeric shrublands Biome . Subcategories
Jiří Hála's textbook states that soils vary greatly in their ability to bind radioisotopes, the clay particles and humic acids can alter the distribution of the isotopes between the soil water and the soil. 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).