Thar Desert, the huge unending expanse of burning hot
sand is spread over four states in India, namely Punjab, Haryana, Rajasthan,
and Gujarat, and two states in Pakistan covering an area of about 446,000
square kilometres. Deriving its name from 'thul' denoting the sand ridges of
the region, Thar stands divided between Sindh region in Pakistan and
Rajasthan in India.

A tract of rolling sand hills, the Thar Desert is bordered by the irrigated
Indus plains to the west, the Aravalli Range to the southeast, the Rann of
Kachchh to the south, and the Punjab plain to the north and northeast.
Yielding salt and gypsum, the thardesert is formed due to the scant rainfall
received by the region as a result of the dryness of the prevailing monsoon
winds.
Receiving an annual average rainfall of less than 10 inches, the desert is
a largely a sun-scorched region of shifting sand dunes, broken rocks, and
scrub vegetation. The sparsely populated region has a pastoral economy. In
May 1974, India exploded its first nuclear device at Pokhran in the deserts
of Rajasthan.
The Legend - Thar Desert
It is believed that aeons ago, Shri Ram drew an arrow in his bow,
targetting Lanka, the island capital where his wife was held captive by the
demon king, Ravana. However, such were its destructive powers that the gods
pleaded with the Lord to desist from his intended purpose. But the arrow
once drawn could not be pulled back and thus Rama pointed the arrow to a
far-flung sea. The heat generated by the arrow dried the sea and and in its
place arose a dry, arid and hot desert.
Archaeological Evidence - Thar Desert
The many excavations of the fossils in the desert have led to the belief
that the area was teeming with marine life once upon a time. It is believed
that centuries ago, the earliest inhabitants who were a part of an urban
civilization that arose 4500 years ago, belonged to this region. Recent
excavations of the Indus Valley Civilization reveal that the settlements
penetrated deep into the heart of the desert. Archaeologists have found a
remarkable resemblance between the citadels and the manner of building along
narrow lanes that dissect each other at right angles and more recent
settlements.
Vegetation of The Thar Desert
Providing nutritive and delectable pasturage, grasses form the main natural
vegetation of the desert. These also have medicinal value and hence
alkaloids, used for making medicine, and oils for making soap, are also
extracted therefrom. There is a great paucity of water and hence, the desert
vegetation is mostly herbaceous; with the trees very rarely dotting the
landscape. On the hills, Gum Arabic Acacia and Euphorbia may be found. The
Khajri (Prosopis Cineraria) tree grows throughout the plains. Water is very
scarce.
The Wild In The Arid Land
Stretches of sand in the desert are interspersed by hillocks and sandy and
gravel plains. About 23 species of lizards and 25 species of snakes are
found here and several of them are endemic to the region. The thinly
populated grasslands support the endangered Great Indian Bustard, the Black
Buck, the Chikara (gazelle), and some feathered game, notably the Francolin
and Quail. Among the migratory birds, Sand Grouse, Ducks and Geese are
common.
Climate of Thar Desert

The
area receives very scant rainfall, with the average annual rainfall varying
from 100 to 500 mm. With around 90% of the rainfall attributable to
southwest monsoon during the months of July and September, there are wide
fluctuations in the amount of rainfall from year to year. May and June are
the hottest months of the year while January is the coldest month. The mean
average temperature varies from a minimum of 24 to 26 degrees C in summer to
4 to 10 degrees C in winter. Dust storms and dust raising winds blowing at
very high velocity are very rampant.
General Information - Thar Desert in India
Location
Punjab, Haryana, Rajasthan, Gujarat.
Area
446,000 square kilometres.
Unique Features
Rolling Sand Hills, Scant Rainfall.
Origin
The ancient desert is believed to have been a witness to one of the
earliest human civilizations. The origin of this desert is a matter of much
controversy. Some consider it to be only 4000 to 10,000 years old. Many
others believe that the region started becoming arid much earlier.