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Geography of India

Geography of India
250px
Continent Asia
Region South Asia
Indian subcontinent
Coordinates

21°N 78°E / 21°N 78°E / 21; 78{{#coordinates:21|N|78|E|type:country|||| | |name=

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Area Ranked 7th
 • Total Script error: No such module "convert".
 • Land 90.08%
 • Water 9.92%
Coastline Script error: No such module "convert".
Borders Total land borders:[1]
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Bangladesh:
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China (PRC):
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Pakistan:
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Nepal:
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Burma:
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Bhutan:
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Highest point Kangchenjunga
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Lowest point Kuttanad
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Longest river Ganges Brahmaputra[citation needed]
Largest lake Chilka Lake
File:Western Europe to Central India.ogv
This video was taken by the crew of Expedition 29 on board the ISS on a pass from western Europe to Central India.

The Geography of India describes the geographic features of India, a country in South Asia. India lies largely on the Indian Plate, the northern portion of the Indo-Australian Plate, whose continental crust forms the Indian subcontinent. The country is situated north of the equator between 8°4' and 37°6' north latitude and 68°7' and 97°25' east longitude.[2] It is the seventh-largest country in the world, with a total area of Script error: No such module "convert"..[3] India measures Script error: No such module "convert". from north to south and Script error: No such module "convert". from east to west. It has a land frontier of Script error: No such module "convert". and a coastline of Script error: No such module "convert"..[4]

On the south, India projects into and is bounded by the Indian Ocean – in particular, by the Arabian Sea on the southwest, the Laccadive Sea to the south, and the Bay of Bengal on the southeast. The Palk Strait and Gulf of Mannar separate India from Sri Lanka to its immediate southeast, and the Maldives are some Script error: No such module "convert". to the southwest. India's Andaman and Nicobar Islands, some Script error: No such module "convert". southeast of the mainland, share maritime borders with Burma, Thailand and Indonesia. Kanyakumari at 8°4′41″N and 77°32′28″E is the southernmost tip of the Indian mainland, while the southernmost point in India is Indira Point on Great Nicobar Island.[4] India's territorial waters extend into the sea to a distance of Script error: No such module "convert". from the coast baseline.[5]

The northern frontiers of India are defined largely by the Himalayan mountain range, where the country borders China, Bhutan, and Nepal. Its western border with Pakistan lies in the Punjab Plain and the Thar Desert. In the far northeast, the Chin Hills and Kachin Hills, deeply forested mountainous regions, separate India from Burma. On the east, its border with Bangladesh is largely defined by the Khasi Hills and Mizo Hills, and the watershed region of the Indo-Gangetic Plain.[clarification needed]

The Ganges is the longest river originating in India. The Ganges–Brahmaputra system occupies most of northern, central, and eastern India, while the Deccan Plateau occupies most of southern India. Kangchenjunga, on the border between Nepal and the Indian state of Sikkim, is the highest point in India at Script error: No such module "convert". and the world's 3rd highest peak. Climate across India ranges from equatorial in the far south, to alpine and tundra in the upper reaches of the Himalayas.

Geological development

Main article: Geology of India

India is entirely contained on the Indian Plate, a major tectonic plate that was formed when it split off from the ancient continent Gondwanaland (ancient landmass, consisting of the southern part of the supercontinent of Pangea). The Indo-Australian is subdivided into the Indian and Australian plates. About 90 million years ago, during the late Cretaceous Period, the Indian Plate began moving north at about 15 cm/year (6 in/yr).[6] About 50 to 55 million years ago, in the Eocene Epoch of the Cenozoic Era, the plate collided with Asia after covering a distance of Script error: No such module "convert"., having moved faster than any other known plate. In 2007, German geologists determined that the Indian Plate was able to move so quickly because it is only half as thick as the other plates which formerly constituted Gondwanaland.[7] The collision with the Eurasian Plate along the modern border between India and Nepal formed the orogenic belt that created the Tibetan Plateau and the Himalayas. As of 2009, the Indian Plate is moving northeast at 5 cm/yr (2 in/yr), while the Eurasian Plate is moving north at only 2 cm/yr (0.8 in/yr). India is thus referred to as the "fastest continent".[7] This is causing the Eurasian Plate to deform, and the Indian Plate to compress at a rate of 4 mm/yr (0.15 in/yr).

Political geography

India is divided into 29 states (further subdivided into districts) and 7 union territories.

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Indian Kashmir, LoC and LAC

India's borders run a total length of Script error: No such module "convert"..[1] Its borders with Pakistan and Bangladesh were delineated according to the Radcliffe Line, which was created in 1947 during Partition of India. Its western border with Pakistan extends up to Script error: No such module "convert"., dividing the Punjab region and running along the boundaries of the Thar Desert and the Rann of Kutch.[1] This border runs along the Indian states of Jammu & Kashmir, Rajasthan, Gujarat, and Punjab.[8] Both nations delineated a Line of Control (LoC) to serve as the informal boundary between the Indian and Pakistan-administered areas of Kashmir. According to India's claim, it also shares a Script error: No such module "convert". border with Afghanistan in northwestern Kashmir, which is under Pakistani control.[1]

India's border with Bangladesh runs Script error: No such module "convert"..[1] West Bengal, Assam, Meghalaya, Tripura and Mizoram are the States which share the border with Bangladesh.[9] There are 92 enclaves of Bangladesh on Indian soil and 106 enclaves of India are on Bangladeshi soil.[10] The Teen Bigha Corridor is a strip of land formerly belonging to India on the West Bengal–Bangladesh border which has been leased indefinitely to Bangladesh so that it can access its Dehgram–Angalpota enclaves.[citation needed]

The Line of Actual Control (LAC) is the effective border between India and the People's Republic of China. It traverses 4,057 km along the Indian states of Jammu and Kashmir, Uttarakhand, Himachal Pradesh, Sikkim and Arunachal Pradesh.[11] The border with Burma (Myanmar) extends up to Script error: No such module "convert". along the southern borders of India's northeastern states viz. Arunachal Pradesh, Nagaland, Manipur and Mizoram.[12] Located amidst the Himalayan range, India's border with Bhutan runs Script error: No such module "convert"..[1] Sikkim, West Bengal, Assam and Arunachal Pradesh are the States, which share the border with Bhutan.[13] The border with Nepal runs Script error: No such module "convert". along the foothills of the Himalayas in northern India.[1] Uttarakhand, Uttar Pradesh, Bihar, West Bengal and Sikkim are the States, which share the border with Nepal.[14] The Siliguri Corridor, narrowed sharply by the borders of Bhutan, Nepal and Bangladesh, connects peninsular India with the northeastern states.

Physiographic regions

India can be divided into five physiographic regions. They are

  1. The Northern Mountains
  2. Indo Gangetic Plains
  3. The Peninsular Plateau
  4. The Island
  5. The Coastal Plains

The Northern Mountains

File:Indiahills.png
Map of the hilly regions in India.

A great arc of mountains, consisting of the Himalayas, Hindu Kush, and Patkai ranges define the northern Indian subcontinent. 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 Indo–Gangetic 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 Script error: No such module "convert".

  • The Himalayan range is the world's highest mountain range, with its tallest peak Mt. Everest (Script error: No such module "convert".) on the Nepal–China border.[15] They form India's northeastern border, separating it from northeastern Asia. They are one of the world's youngest mountain ranges and extend almost uninterrupted for Script error: No such module "convert"., covering an area of Script error: No such module "convert"..[15] The Himalayas extend from Jammu and Kashmir in the north to Arunachal Pradesh in the east. These states along with Himachal Pradesh, Uttarakhand, and Sikkim lie mostly in the Himalayan region. Numerous Himalayan peaks rise over Script error: No such module "convert". and the snow line ranges between Script error: No such module "convert". in Sikkim to around Script error: No such module "convert". in Kashmir. Kanchenjunga—on the SikkimNepal border—is 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 Script error: No such module "convert"., including K2, the second highest peak in the world Script error: No such module "convert".. K2 is just Script error: No such module "convert". smaller than the Script error: No such module "convert". Mount Everest. The range is about Script error: No such module "convert". in length and the most heavily glaciated part of the world outside of the polar regions. The Siachen Glacier at Script error: No such module "convert". and the Biafo Glacier at Script error: No such module "convert". rank as the world's second and third-longest glaciers outside the polar regions.[16] Just to the west of the northwest end of the Karakoram, lies the Hindu Raj range, beyond which is the Hindu Kush range. 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 Patkai–Bum, the GaroKhasiJaintia and the Lushai hills. The Garo–Khasi 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.[17]
  • The Vindhya range runs across most of central India, extending Script error: No such module "convert"..[15] The average elevation of these hills is from Script error: No such module "convert". and rarely goes above Script error: No such module "convert"..[15] They are believed to have been formed by the wastes created by the weathering of the ancient Aravali mountains.[18] Geographically, it separates northern India from southern India. 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.
  • The Satpura Range begins in eastern Gujarat near the Arabian Sea coast and runs east across Maharashtra, Madhya Pradesh and Chhattisgarh. It extends Script error: No such module "convert". with many peaks rising above Script error: No such module "convert"..[15] It is triangular in shape, with its apex at Ratnapuri and the two sides being parallel to the Tapti and Narmada rivers.[19] It runs parallel to the Vindhya Range, which lies to the north, and these two east-west ranges divide the Indo–Gangetic plain from the Deccan Plateau located north of River Narmada.
  • The Aravali Range is the oldest mountain range in India, running across Rajasthan from northeast to southwest direction, extending approximately Script error: No such module "convert"..[20] The northern end of the range continues as isolated hills and rocky ridges into Haryana, ending near Delhi. The highest peak in this range is Guru Shikhar at Mount Abu, rising to Script error: No such module "convert"., lying near the border with Gujarat.[21] The Aravali Range is the eroded stub of an ancient fold mountain system.[22] The range rose in a Precambrian event called the Aravali–Delhi orogen. 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 Script error: No such module "convert".[19] from south of the Tapti River near the Gujarat–Maharashtra border and across Maharashtra, Goa, Karnataka, Kerala and Tamil Nadu to the southern tip of the Deccan peninsula. The average elevation is around Script error: No such module "convert"..[19] Anai Mudi in the Anaimalai Hills Script error: No such module "convert". in Kerala is the highest peak in the Western Ghats.[23]
  • The Eastern Ghats are a discontinuous range of mountains, which have been eroded and vivisected by the four major rivers of southern India, the Godavari, Mahanadi, Krishna, and Kaveri.[24] These mountains extend from West Bengal to Orissa, Andhra Pradesh and Tamil Nadu, along the coast and parallel to the Bay of Bengal. Though not as tall as the Western Ghats, some of its peaks are over Script error: No such module "convert". in height.[19] The Nilgiri hills in Tamil Nadu lies at the junction of the Eastern and Western Ghats. Arma Konda (Script error: No such module "convert".) in Andhra Pradesh is the tallest peak in Eastern Ghats.[25]

Indo-Gangetic plain

Main article: Indo-Gangetic plain

The Indo-Gangetic plains, also known as the Great Plains are large alluvial plains dominated by three main rivers, the Indus, Ganges, and Brahmaputra. 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 encompass an area of Script error: No such module "convert".. The major rivers in this region are the Ganges, Indus, and Brahmaputra along with their main tributaries–Yamuna, Chambal, Gomti, Ghaghara, Kosi, Sutlej, Ravi, Beas, Chenab, and Tista—as well as the rivers of the Ganges Delta, such as the Meghna.

File:IndoGangeticPlain Map.png
Extent of the Indo-Gangetic plain across South Asia.

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 Script error: No such module "convert"..
  • The Terai belt lies south of the adjacent Bhabar region and is composed of newer alluvium. The underground streams reappear in this region. The region is excessively moist and thickly forested. It also receives heavy rainfall throughout the year and is populated with a variety of wildlife.
  • 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 Indo-Gangetic plains rank among the world's most densely populated areas.[citation needed]

Thar Desert

Main article: Thar Desert

The Thar Desert (also known as the deserts) is by some calculations the world's seventh largest desert,[26] by others the tenth.[27] It forms a significant portion of western India and covers an area of Script error: No such module "convert"..[26][28] The desert continues into Pakistan as the Cholistan Desert. Most of the Thar Desert is situated in Rajasthan, covering 61% of its geographic area.

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 Script error: No such module "convert". in the winter to over Script error: No such module "convert". during the summer. Most of the rainfall received in this region is associated with the short July–September southwest monsoon that brings Script error: No such module "convert". of precipitation. Water is scarce and occurs at great depths, ranging from Script error: No such module "convert". below the ground level.[29] Rainfall is precarious and erratic, ranging from below Script error: No such module "convert". in the extreme west to Script error: No such module "convert". eastward.The only river in this region is Luni. The soils of the arid region are generally sandy to sandy-loam in texture. The consistency and depth vary as per the topographical features. The low-lying loams are heavier may have a hard pan of clay, calcium carbonate or gypsum.[30]

Highlands

The Central Highlands consists 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.

File:Dry deciduous Jungles at Ramatheertham 03.jpg
Dry deciduous and thorny forests of plateau regions in India

The Malwa Plateau is spread across Rajasthan, Madhya Pradesh and Gujarat. The average elevation of the Malwa plateau is 500 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.

The Deccan Plateau is a large triangular plateau, bounded by the Vindhyas to the north and flanked by the Eastern and Western Ghats. The Deccan covers a total area of 1.9 million km² (735,000 mile²). It is mostly flat, with elevations ranging from Script error: No such module "convert".. The average elevation of the plateau is Script error: No such module "convert". above sea level. The surface slopes from Script error: No such module "convert". in the west to Script error: No such module "convert". in the east.[31] It slopes gently from west to east and gives rise to several peninsular rivers such as the Godavari, the Krishna, the Kaveri and the Mahanadi which drain into the Bay of Bengal. This region is mostly semi-arid as it lies on the leeward side of both Ghats. Much of the Deccan is covered by thorn scrub forest scattered with small regions of deciduous broadleaf forest. Climate in the Deccan ranges from hot summers to mild winters.

The Chota Nagpur Plateau is situated in eastern India, covering much of Jharkhand and adjacent parts of Orissa, Bihar and Chhattisgarh. Its total area is approximately Script error: No such module "convert". and is made up of three smaller plateaus — the Ranchi, Hazaribagh, and Kodarma plateaus. The Ranchi plateau is the largest, with an average elevation of Script error: No such module "convert".. Much of the plateau is forested, covered by the Chota Nagpur dry deciduous forests. Vast reserves of metal ores and coal have been found in the Chota Nagpur plateau. The Kathiawar peninsula in western Gujarat is bounded by the Gulf of Kutch and the Gulf of Khambat. The natural vegetation in most of the peninsula is xeric scrub, part of the Northwestern thorn scrub forests ecoregion.

In western India, the Kutch region in Gujarat and Koyna in Maharashtra are classified as a Zone IV region (high risk) for earthquakes. The Kutch city of Bhuj was the epicentre of the 2001 Gujarat earthquake, which claimed the lives of more than 1,337 people and injured 166,836 while destroying or damaging near a million homes.[32] The 1993 Latur earthquake in Maharashtra killed 7,928 people and injured 30,000.[33] Other areas have a moderate to low risk of an earthquake occurring.[34]

Coasts

The Eastern Coastal Plain is a wide stretch of land lying between the Eastern Ghats and the oceanic boundary of india. It stretches from Tamil Nadu in the south to West Bengal in the east. The Mahanadi, Godavari, Kaveri, and Krishna rivers drain these plains. The temperature in the coastal regions often exceeds Script error: No such module "convert"., and is coupled with high levels of humidity. The region receives both the northeast monsoon and southwest monsoon rains. The southwest monsoon splits into two branches, the Bay of Bengal branch and the Arabian Sea branch. The Bay of Bengal branch moves northwards crossing northeast India in early June. The Arabian Sea branch moves northwards and discharges much of its rain on the windward side of Western Ghats. Annual rainfall in this region averages between Script error: No such module "convert".. The width of the plains varies between Script error: No such module "convert"..[35] The plains are divided into six regions—the Mahanadi delta, the southern Andhra Pradesh plain, the Krishna-Godavari deltas, the Kanyakumari coast, the Coromandel Coast, and sandy coastal.[citation needed]

The Western Coastal Plain is a narrow strip of land sandwiched between the Western Ghats and the Arabian Sea, ranging from Script error: No such module "convert". in width. It extends from Gujarat in the north and extends through Maharashtra, Goa, Karnataka, and Kerala. Numerous rivers and backwaters inundate the region. Mostly originating in the Western Ghats, the rivers are fast-flowing, usually perennial, and empty into estuaries. Major rivers flowing into the sea are the Tapi, Narmada, Mandovi and Zuari. Vegetation is mostly deciduous, but the Malabar Coast moist forests constitute a unique ecoregion. The Western Coastal Plain can be divided into two parts, the Konkan and the Malabar Coast.

Islands

File:Andaman.jpg
Aerial view of the Andaman Islands

The Lakshadweep and the Andaman and Nicobar Islands are India's two major island formations and are classified as union territories. The Lakshadweep Islands lie Script error: No such module "convert". off the coast of Kerala in the Arabian sea with an area of Script error: No such module "convert".. They consist of twelve atolls, three reefs, and five submerged banks, with a total of about 35 islands and islets.

The Andaman and Nicobar Islands are located between 6° and 14° north latitude and 92° and 94° east longitude.[36] They consist of 572 isles, lying in the Bay of Bengal near the Burmese coast. They are located Script error: No such module "convert". from Kolkata (Calcutta) and Script error: No such module "convert". from Cape Negrais in Burma.[36] The territory consists of two island groups, the Andaman Islands and the Nicobar Islands. The Andaman Islands consists of 204 small islands across a total length of Script error: No such module "convert".. India's only active volcano, Barren Island is situated here. It last erupted in May 2005. The Narcondum is a dormant volcano and there is a mud volcano at Baratang. Indira Point, India's southernmost land point, is situated in the Nicobar islands at 6°45’10″N and 93°49’36″E, and lies just Script error: No such module "convert". from the Indonesian island of Sumatra, to the southeast. The highest point is Mount Thullier at Script error: No such module "convert"..

Other significant islands in India include Diu daman, a former Portuguese enclave; Majuli, a river island of the Brahmaputra; Elephanta in Bombay Harbour; and Sriharikota, a barrier island in Andhra Pradesh. Salsette Island is India's most populous island on which the city of Mumbai (Bombay) is located. Forty-two islands in the Gulf of Kutch constitute the Marine National Park.

Water bodies

File:Indiarivers.png
Rivers in India.
Main article: Rivers of India

India has around 14,500 km of inland navigable waterways.[37] There are twelve rivers which are classified as major rivers, with the total catchment area exceeding Script error: No such module "convert"..[19] All major rivers of India originate from one of the three main watersheds:[19]

  1. The Himalaya and the Karakoram ranges
  2. Vindhya and Satpura range in central India
  3. Sahyadri or Western Ghats in western India

The Himalayan river networks are snow-fed and have a perennial supply throughout the year. The other two river systems are dependent on the monsoons and shrink into rivulets during the dry season. The Himalayan rivers that flow westward into Pakistan are the Indus, Jhelum, Chenab, Ravi, Beas, and Sutlej.[38]

The Ganges-Brahmaputra-Meghana system has the largest catchment area of about Script error: No such module "convert"..[39] The Ganges Basin alone has a catchment of about Script error: No such module "convert"..[19] The Ganges originates from the Gangotri Glacier in Uttarakhand.[38] It flows southeast, draining into the Bay of Bengal.[19] The Yamuna and Gomti rivers also arise in the western Himalayas and join the Ganges in the plains.[19] The Brahmaputra originates in Tibet, China, where it is known as the Yarlung Tsangpo River (or "Tsangpo"). It enters India in the far-eastern state of Arunachal Pradesh, then flows west through Assam. The Brahmaputra merges with the Ganges in Bangladesh, where it is known as the Jamuna River.[19][40]

The Chambal, another tributary of the Ganges, via the Yamuna, originates from the Vindhya-Satpura watershed. The river flows eastward. Westward-flowing rivers from this watershed are the Narmada and Tapti, which drain into the Arabian Sea in Gujarat. The river network that flows from east to west constitutes 10% of the total outflow.[clarification needed]

The Western Ghats are the source of all Deccan rivers, which include the Mahanadi River through the Mahanadi River Delta, Godavari River, Krishna River and Kaveri River, all draining into the Bay of Bengal. These rivers constitute 20% of India's total outflow.[38]

The heavy southwest monsoon rains cause the Brahmaputra and other rivers to distend their banks, often flooding surrounding areas. Though they provide rice paddy farmers with a largely dependable source of natural irrigation and fertilisation, such floods have killed thousands of people and tend to cause displacements of people in such areas.

Major gulfs include the Gulf of Cambay, Gulf of Kutch, and the Gulf of Mannar. Straits include the Palk Strait, which separates India from Sri Lanka; the Ten Degree Channel, which separates the Andamans from the Nicobar Islands; 'and the Eight Degree Channel, which separates the Laccadive and Amindivi Islands from the Minicoy Island to the south. Important capes include the Kanyakumari (formerly called Cape Comorin), the southern tip of mainland India; Indira Point, the southernmost point in India (on Great Nicobar Island); Rama's Bridge, and Point Calimere. The Arabian Sea lies to the west of India, the Bay of Bengal and the Indian Ocean lie to the east and south, respectively. Smaller seas include the Laccadive Sea and the Andaman Sea. There are four coral reefs in India, located in the Andaman and Nicobar Islands, the Gulf of Mannar, Lakshadweep, and the Gulf of Kutch.[34] Important lakes include Sambhar Lake, the country's largest saltwater lake in Rajasthan, Vembanad Lake in Kerala, Kolleru Lake in Andhra Pradesh, Loktak Lake in Manipur, Dal Lake in Kashmir, Chilka Lake(lagoon lake) in Orrisa, and Sasthamkotta Lake in Kerala.

Wetlands

India's wetland ecosystem is widely distributed from the cold and arid located in the Ladakh region of Jammu and Kashmir, and those with the wet and humid climate of peninsular India. Most of the wetlands are directly or indirectly linked to river networks. The Indian government has identified a total of 71 wetlands for conservation and are part of sanctuaries and national parks.[41] Mangrove forests are present all along the Indian coastline in sheltered estuaries, creeks, backwaters, salt marshes and mudflats. The mangrove area covers a total of Script error: No such module "convert".,[42] which comprises 7% of the world's total mangrove cover. Prominent mangrove covers are located in the Andaman and Nicobar Islands, the Sundarbans delta, the Gulf of Kutch and the deltas of the Mahanadi, Godavari and Krishna rivers. Parts of Maharashtra, Karnataka and Kerala also have large mangrove covers.[34]

The Sundarbans delta is home to the largest mangrove forest in the world. It lies at the mouth of the Ganges and spreads across areas of Bangladesh and West Bengal. The Sundarbans is a UNESCO World Heritage Site, but is identified separately as the Sundarbans (Bangladesh) and the Sundarbans National Park (India). The Sundarbans are intersected by a complex network of tidal waterways, mudflats and small islands of salt-tolerant mangrove forests. The area is known for its diverse fauna, being home to a large variety of species of birds, spotted deer, crocodiles and snakes. Its most famous inhabitant is the Bengal tiger. It is estimated that there are now 400 Bengal tigers and about 30,000 spotted deer in the area.

The Rann of Kutch is a marshy region located in northwestern Gujarat and the bordering Sindh province of Pakistan. It occupies a total area of Script error: No such module "convert"..[43] The region was originally a part of the Arabian Sea. Geologic forces such as earthquakes resulted in the damming up of the region, turning it into a large saltwater lagoon. This area gradually filled with silt thus turning it into a seasonal salt marsh. During the monsoons, the area turn into a shallow marsh, often flooding to knee-depth. After the monsoons, the region turns dry and becomes parched.

Climate

File:Kalinagar Floods B.JPG
Many areas remain flooded during the heavy rains brought by monsoon in the Indian state of West Bengal.
File:Teestavalley.jpg
National Highway 31A winds along the banks of the Teesta River near Kalimpong (West Bengal), in the Darjeeling Himalayan hill region.

Based on the Köppen system, India hosts six major climatic subtypes, ranging from arid desert in the west, alpine tundra and glaciers in the north, and humid tropical regions supporting rainforests in the southwest and the island territories. The nation has four seasons: winter (January–February), summer (March–May), a monsoon (rainy) season (June–September) and a post-monsoon period (October–December)'.[38]

File:Indiatemperaturetemp.png
Temperature averages in India; units are in degree Celsius.

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. Although the Tropic of Cancer—the boundary between the tropics and subtropics—passes through the middle of India, the whole country is considered to be tropical.[citation needed]

Summer lasts between March and June in most parts of India. Temperatures can exceed Script error: No such module "convert". during the day. The coastal regions exceed Script error: No such module "convert". coupled with high levels of humidity. In the Thar desert area temperatures can exceed Script error: No such module "convert".. The rain-bearing monsoon clouds are attracted to the low-pressure system created by the Thar Desert. The southwest monsoon splits into two arms, the Bay of Bengal arm and the Arabian Sea arm. The Bay of Bengal arm moves northwards crossing northeast India in early June. The Arabian Sea arm moves northwards and deposits much of its rain on the windward side of Western Ghats. Winters in peninsula India see mild to warm days and cool nights. Further north the temperature is cooler. Temperatures in some parts of the Indian plains sometimes fall below freezing. Most of northern India is plagued by fog during this season. The highest temperature recorded in India was Script error: No such module "convert". in Alwar, Rajasthan. The lowest was Script error: No such module "convert". in Kashmir.

Geology

Main article: Geology of India

India's geological features are classified based on their era of formation.[44] The Precambrian formations of Cudappah and Vindhyan systems are spread out over the eastern and southern states. A small part of this period is spread over western and central India.[44] The Paleozoic formations from the Cambrian, Ordovician, Silurian and Devonian system are found in the Western Himalaya region in Kashmir and Himachal Pradesh.[44] The Mesozoic Deccan Traps formation is seen over most of the northern Deccan; they are believed to be the result of sub-aerial volcanic activity.[44] The Trap soil is black in colour and conducive to agriculture. The Carboniferous system, Permian System and Triassic systems are seen in the western Himalayas. The Jurassic system is seen in the western Himalayas and Rajasthan.

File:India-geology-map.png
Geological regions of India

Tertiary imprints are seen in parts of Manipur, Nagaland, Arunachal Pradesh and along the Himalayan belt. The Cretaceous system is seen in central India in the Vindhyas and part of the Indo-Gangetic plains.[44] The Gondowana system is seen in the Narmada River area in the Vindhyas and Satpuras. The Eocene system is seen in the western Himalayas and Assam. Oligocene formations are seen in Kutch and Assam.[44] The Pleistocene system is found over central India. The Andaman and Nicobar Island are thought to have been formed in this era by volcanoes.[44] The Himalayas were formed by the convergence and deformation of the Indo-Australian and Eurasian Plates. Their continued convergence raises the height of the Himalayas by 1 cm each year.

Soils in India can be classified into 8 categories: alluvial, black, red, laterite, forest, arid & desert, saline & alkaline and peaty & organic soils.[45][46] Alluvial soil constitute the largest soil group in India, constituting 80% of the total land surface.[46] It is derived from the deposition of silt carried by rivers and are found in the Great Northern plains from Punjab to the Assam valley.[46] Alluvial soil are generally fertile but they lack nitrogen and tend to be phosphoric.[46]

Black soil are well developed in the Deccan lava region of Maharashtra, Gujarat, and Madhya Pradesh.[47] These contain high percentage of clay and are moisture retentive.[46] Red soil are found in Tamil Nadu, Karnataka plateau, Andhra plateau, Chota Nagpur plateau and the Aravallis.[47] These are deficient in nitrogen, phosphorus and humus.[46][47] Laterite soils are formed in tropical regions with heavy rainfall. Heavy rainfall results in leaching out all soluble material of top layer of soil. These are generally found in Western ghats, Eastern ghats and hilly areas of northeastern states that receive heavy rainfall. Forest soils occur on the slopes of mountains and hills in Himalayas, Western Ghats and Eastern Ghats. These generally consist of large amounts of dead leaves and other organic matter called humus.

Natural resources

File:Coal mine in Dhanbad, India.jpg
Indian coal production is the 3rd highest in the world according to the 2008 Indian Ministry of Mines estimates. Shown above is a coal mine in Jharkhand.

India's total renewable water resources are estimated at 1,907.8 km3/year.[48] Its annual supply of usable and replenshable groundwater amounts to 350 billion cubic metres.[49] Only 35% of groundwater resources are being utilized.[49] About 44 million tonnes of cargo is moved annually through the country's major rivers and waterways.[37] Groundwater supplies 40% of water in India's irrigation canals. 56% of the land is arable and used for agriculture. Black soils are moisture-retentive and are preferred for dry farming and growing cotton, linseed, etc. Forest soils are used for tea and coffee plantations. Red soil have a wide diffusion of iron content.[47]

Most of India's estimated Script error: No such module "convert". in oil reserves are located in the Mumbai High, upper Assam, Cambay, the Krishna-Godavari and Cauvery basins.[50] India possesses about seventeen trillion cubic feet of natural gas in Andhra Pradesh, Gujarat and Orissa.[50] Uranium is mined in Andhra Pradesh. India has 400 medium-to-high enthalpy thermal springs for producing geothermal energy in seven "provinces" — the Himalayas, Sohana, Cambay, the Narmada-Tapti delta, the Godavari delta and the Andaman and Nicobar Islands (specifically the volcanic Barren Island.)[51]

India is the world's biggest producer of mica blocks and mica splittings.[52] India ranks second amongst the world's largest producers of barites and chromites.[52] The Pleistocene system is rich in minerals. India is the third-largest coal producer in the world and ranks fourth in the production of iron ore.[50][52] It is the fifth-largest producer of bauxite and crude steel, the seventh-largest of manganese ore and the eighth-largest of aluminium.[52] India has significant sources of titanium ore, diamonds and limestone.[53] India possesses 24% of the world's known and economically viable thorium, which is mined along shores of Kerala.[54] Gold had been mined in the now-defunct Kolar Gold Fields in Karnataka.[55]

Antipodes

The only land area antipodal to India is Easter Island, which is antipodal to the western corner of Rajasthan. The triangular island closely reflects the triangle between the cities of Mokal, Kuchchri, and Habur. Habur corresponds to Hanga Roa, and Mokal to the eastern cape.

Further reading

  • "The Incredible History of India's Geography", Author: Sanjeev Sanyal, Publisher: Penguin Books Ltd
  • Allaby, M (1998). "Floods". Facts on File. ISBN 0-8160-3520-2. .
  • Balfour, E (1976). Encyclopaedia Asiatica: Comprising Indian Subcontinent, Eastern and Southern Asia. Cosmo Publications. ISBN 81-7020-325-2. .
  • Nash, JM (2002). "El Niño: Unlocking the Secrets of the Master Weather Maker". Warner. ISBN 0-446-52481-6. .
  • "Land and Natural Resources". Terrain. Retrieved 6 June 2005. 
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