Geographical Features
A series of low hills surround the basin which has an oval shape (almost round) with circumference at top of about 8 km (five miles). The sides of the basin rises abruptly at an angle of about 75°. At the base, the lake has a circumference of about 4.8 km (three miles). The slopes are covered with jungle interspersed with teak trees. A belt of large trees about a mile broad runs all round the basin; this belt is formed of concentric rings of different species of trees. A ring of date-palms followed by a ring of tamarind trees (nearly 1.6 km or a mile broad) leads to a ring of babul trees, bounded on the inside by a belt of bare muddy space. This space is several hundred metres/yards broad, devoid of all vegetation (due to the soda content of the water) and covered with a whitish slimy soil. During the rainy season, the drainage into the lake covers this muddy space. The water of the lake contains various salts or sodas, and during dry weather when evaporation reduces the water level, large quantities of soda are collected. Two small streams drain into the lake, and a well of sweet water is located on the southern side, close to the water's edge.
The historical document called the Ain-i-Akbari (written about C.E. 1600) states: These mountains produce all the requisites for making glass and soap. And here are saltpetre works which yield a considerable revenue to the State, from the duties collected. On these mountains is a spring of salt water, but the water from the centre and the edges is perfectly fresh.
Read more about this topic: Lonar Crater Lake
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