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The northern mountains Northern Plains The Peninsular Plateau Thar desert Another method divides India into five physiographic regions: The Himalayas, northern plains the Indo-Gangetic plain , peninsular region, coastal plains, and islands.
These were formed by the ongoing tectonic collision of the Indian and Eurasian plates. The mountains in these ranges include some of the world's tallest mountains which act as a natural barrier to cold polar winds.
They also facilitate the monsoon winds which in turn influence the climate in India. Rivers originating in these mountains, flow through the fertile IndoGangetic plains. These mountains are recognised by biogeographers as the boundary between two of the Earth's great ecozones: the temperate Palearctic that covers most of Eurasia and the tropical and subtropical Indomalaya ecozone which includes the Indian subcontinent, Southeast Asia and Indonesia. India has eight major mountain ranges having peaks of over 1, m 3, ft Map of the hilly regions in India.
The Himalayan range is considered as the world's highest mountain range, with its tallest peak Mt. Everest on the NepalChina border.
They are one of the world's youngest mountain ranges and extend almost uninterrupted for 2, km 1, mi , covering an area of , km2 , sq mi.
These states along with Himachal Pradesh, Uttarakhand, and Sikkim lie mostly in the Himalayan region. Numerous Himalayan peaks rise over 7, m 22, ft and the snow line ranges between 6, m 19, ft in Sikkim to around 3, m 9, ft in Kashmir.
Kanchenjungaon the SikkimNepal borderis the highest point in the area administered by India. Most peaks in the Himalayas remain snowbound throughout the year. The Himalayas act as a barrier to the frigid katabatic winds flowing down from Central Asia.
Thus, North India is kept warm or only mildly cooled during winter; in summer, the same phenomenon makes India relatively hot. The Karakoram is situated in the disputed state of Jammu and Kashmir. It has more than sixty peaks above 7, m 22, ft , including K2, the second highest peak in the world 8, m 28, ft. K2 is just m ft smaller than the 8, m 29, ft Mount Everest.
The range is about km mi in length and the most heavily glaciated part of the world outside of the polar regions. The Siachen Glacier at 70 km 43 mi and the Biafo Glacier at 63 km 39 mi rank as the world's second and third-longest glaciers outside the polar regions. Kanchenjunga in Sikkim. The southern boundary of the Karakoram is formed by the Gilgit, Indus and Shyok rivers, which separate the range from the northwestern end of the Himalayas.
The Patkai, or Purvanchal, are situated near India's eastern border with Burma. They were created by the same tectonic processes which led to the formation of the Himalayas.
The physical features of the Patkai mountains are conical peaks, steep slopes and deep valleys. The Patkai ranges are not as rugged or tall as the Himalayas. There are three hill ranges that come under the Patkai: the PatkaiBum, the en.
The GaroKhasi range lies in Meghalaya. Mawsynram, a village near Cherrapunji lying on the windward side of these hills, has the distinction of being the wettest place in the world, receiving the highest annual rainfall. The western end of the range lies in eastern Gujarat, near its border with Madhya Pradesh, and runs east and north, almost meeting the Ganges at Mirzapur. It extends km mi with many peaks rising above 1, m 3, ft.
The Aravali Range is the oldest mountain range in India, running across Rajasthan from northeast to southwest direction, extending approximately km mi. The highest peak in this range is Guru Shikhar at Mount Abu, rising to 1, m 5, ft , lying near the border with Gujarat. The range joins two of the ancient segments that make up the Indian craton, the Marwar segment to the northwest of the range, and the Bundelkhand segment to the southeast.
The Western Ghats or Sahyadri mountains run along the western edge of India's Deccan Plateau and separate it from a narrow coastal plain along the Arabian Sea. The range runs approximately 1, km mi  from south of the Tapti River near the GujaratMaharashtra border and across Maharashtra, Goa, Karnataka, Kerala and Tamil Nadu to the southern tip of the Deccan peninsula.
The average elevation is around 1, m 3, ft. Though not as tall as the Western Ghats, some of its peaks are over 1, m 3, ft in height. They run parallel to the Himalayas, from Jammu and Kashmir in the west to Assam in the east, and drain most of northern and eastern India. The plains Eastern Ghats Javadi Hills in encompass an area of , km2 , sq mi.
The great plains are sometimes classified into four divisions: The Bhabar belt is adjacent to the foothills of the Himalayas and consists of boulders and pebbles which have been carried down by streams.
As the porosity of this belt is very high, the streams flow underground. The Bhabar is generally narrow with its width varying between 7 to 15 km. The Terai belt lies south of the adjacent Bhabar region and is composed of newer alluvium.
The underground streams reappear in this Extent of the Indo-Gangetic plain region. The region is excessively moist and thickly forested. It also across South Asia. The Bangar belt consists of older alluvium and forms the alluvial terrace of the flood plains.
In the Gangetic plains, it has a low upland covered by laterite deposits. The Khadar belt lies in lowland areas after the Bangar belt. It is made up of fresh newer alluvium which is deposited by the rivers flowing down the plain.
The Indo-Gangetic belt is the world's most extensive expanse of uninterrupted alluvium formed by the deposition of silt by the numerous rivers. The plains are flat making it conducive for irrigation through canals. The area is also rich in ground water sources. The plains are one of the world's most intensely farmed areas.
The main crops grown are rice and wheat, which are grown in rotation. Other important crops grown in the region include maize, sugarcane and cotton. The IndoGangetic plains rank among the world's most densely populated areas.
Thar Desert Main article: Thar Desert The Thar Desert also known as the deserts is the world's seventh largest desert, by others the tenth. About 10 percent of this region comprises sand dunes, and the remaining 90 percent consist of craggy rock forms, compacted salt-lake bottoms, and interdunal and fixed dune areas.
Annual temperatures can range from 0C in the winter to over 50C during the summer. Most of the rainfall received in this region is associated with the short JulySeptember southwest monsoon that brings around mm of precipitation.
Water is scarce and occurs at great depths, ranging from 30 to m below the ground level. The soils of the arid region are generally sandy to sandy-loam in texture.
The consistency and depth vary as Desert tribes living in the Thar Desert near per the topographical features. The low-lying loams are heavier and Jaisalmer, India. Highlands The Central Highlands comprise of three main plateaus the Malwa Plateau in the west, the Deccan Plateau in the south covering most of the Indian peninsula and the Chota Nagpur Plateau in the east.
The average elevation of the Malwa plateau is metres, and the landscape generally slopes towards the north.
Most of the region is drained by the Chambal River and its tributaries; the western part is drained by the upper reaches of the Mahi River. Availability — Out of Stock; Shipping. Alert on more product reviews. Insights Insights, Account, Orders. Books are not only written to educate, they are written for leisure and even for manorzma metamorphosis of the soul.
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