Geography of India

Geography of India
Continent Asia
Region South Asia
Indian subcontinent
Coordinates 21°N 78°E / 21°N 78°E / 21; 78
Area Ranked 7th
 • Total 3,287,263 km2 (1,269,219 sq mi)
 • Land 90.08%
 • Water 9.92%
Coastline 7,516.6 km (4,670.6 mi)
Borders Total land borders:[1]
15,106.70 km (9,386.87 mi)
Bangladesh:
4,096.70 km (2,545.57 mi)
China (PRC):
3,488 km (2,167 mi)
Pakistan:
2,910 km (1,808 mi)
Nepal:
1,751 km (1,088 mi)
Myanmar:
1,643 km (1,021 mi)
Bhutan:
699 km (434 mi)
Highest point Kanchenjunga
8,598 m (28,209 ft)
Lowest point Kuttanad
−2.2 m (−7.2 ft)
Longest river Ganges
2,525 km (8,284,121 ft)
Largest lake Wular Lake
30 to 260 km² (12 to 100 sq mi}

India lies 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' to 37°6' north latitude and 68°7' to 97°25' east longitude.[2] It is the seventh-largest country in the world, with a total area of 3,287,263 square kilometres (1,269,219 sq mi).[3] India measures 3,214 km (1,997 mi) from north to south and 2,933 km (1,822 mi) from east to west. It has a land frontier of 15,200 km (9,445 mi) and a coastline of 7,516.6 km (4,671 mi).[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 400 kilometres (250 mi) to the southwest. India's Andaman and Nicobar Islands, some 1,200 kilometres (750 mi) southeast of the mainland, share maritime borders with Myanmar, 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. Northernmost point which is under Indian administration is Indira Col, Siachen Glacier.[4] India's territorial waters extend into the sea to a distance of 12 nautical miles (13.8 mi; 22.2 km) 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.

The Ganga is the longest river originating in India. The Ganga–Brahmaputra system occupies most of northern, central, and eastern India, while the Deccan Plateau occupies most of southern India. Kanchenjunga, on the border between Nepal and the Indian state of Sikkim, is the highest point in India at 8,598 m (28,209 ft) 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

The Indian Plate
Main article: Geology of India

India is situated entirely 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 plate 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 2,000 to 3,000 km (1,243 to 1,864 mi), 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 cm/yr (1.6 in/yr).

Political geography

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

Indian Kashmir, LoC and LAC

India's borders run a total length of 15,106.70 km (9,386.87 mi).[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 3,323 km (2,065 mi), 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 106 km (66 mi) border with Afghanistan in northwestern Kashmir, which is under Pakistani control.[1]

India's border with Bangladesh runs 4,096.70 km (2,545.57 mi).[1] West Bengal, Assam, Meghalaya, Tripura and Mizoram are the States which share the border with Bangladesh.[9] Before 2015, there were 92 enclaves of Bangladesh on Indian soil and 106 enclaves of India were on Bangladeshi soil.[10] These enclaves were eventually exchanged in order to simplify the border.[11] After the exchange, India lost roughly 40 km² (10,000 acres) to Bangladesh.[12]

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.[13] The border with Burma (Myanmar) extends up to 1,643 km (1,021 mi) along the southern borders of India's northeastern states viz. Arunachal Pradesh, Nagaland, Manipur and Mizoram.[14] Located amidst the Himalayan range, India's border with Bhutan runs 699 km (434 mi).[1] Sikkim, West Bengal, Assam and Arunachal Pradesh are the States, which share the border with Bhutan.[15] The border with Nepal runs 1,751 km (1,088 mi) 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.[16] The Siliguri Corridor, narrowed sharply by the borders of Bhutan, Nepal and Bangladesh, connects peninsular India with the northeastern states.

Physiographic regions

topography map

India can be divided into six physiographic regions. They are

  1. The Northern Mountains
  2. The Peninsular Plateaus
  3. Indo Gangetic Plains
  4. Thar Desert
  5. The Coastal Plains
  6. The Islands

The Northern Mountains

Snow leopard at Hemis National Park, Jammu and Kashmir.

A great arc of mountains, consisting of the Himalayas of Nepal, 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.

The Himalayan range is the world's highest mountain range, with its tallest peak Mt. Everest (8,848 metres (29,029 ft)) on the Nepal–China border.[17] 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 2,500 km (1,600 mi), covering an area of 500,000 km2 (190,000 sq mi).[17] 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 7,000 m (23,000 ft) and the snow line ranges between 6,000 m (20,000 ft) in Sikkim to around 3,000 m (9,800 ft) in Kashmir. Kanchenjunga—on the Sikkim–Nepal 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.

Mt. Kanchenjunga from Sikkim.
The Vindhyas in central India

The Peninsular Plateau

Dry deciduous and thorny forests of plateau regions in India

Kutch Kathiawar plateau is located in Gujarat state.

Western Ghats near Matheran
Kolli Hills of the Eastern Ghats, Tamil Nadu
Dry Evergreen Forests along the Eastern Ghats, Andhra Pradesh

Indo-Gangetic plain

Extent of the Indo-Gangetic plain across South Asia.
Many areas remain flooded during the heavy rains brought by monsoon in the Indian state of West Bengal.
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 700,000 km2 (270,000 sq mi). 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.

The great plains are sometimes classified into four divisions:

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.

Thar Desert

Thar desert, Rajasthan India
Main article: Thar Desert

The Thar Desert (also known as the deserts) is by some calculations the world's seventh largest desert, by some others the tenth.[29] It forms a significant portion of western India and covers an area of 200,000 to 238,700 km2 (77,200 to 92,200 sq mi).[30] 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 0 °C (32 °F) in the winter to over 50 °C (122 °F) during the summer. Most of the rainfall received in this region is associated with the short July–September southwest monsoon that brings 100 to 500 mm (3.9 to 19.7 in) of precipitation. Water is scarce and occurs at great depths, ranging from 30 to 120 metres (98 to 394 ft) below the ground level.[31] Rainfall is precarious and erratic, ranging from below 120 mm (4.7 in) in the extreme west to 375 mm (14.8 in) 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.

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

Visakhapatnam Beach View, Bay of Bengal, Andhra Pradesh

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 30 °C (86 °F), 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 1,000 and 3,000 mm (39 and 118 in). The width of the plains varies between 100 and 130 km (62 and 81 mi).[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.

The Western Coastal Plain is a narrow strip of land sandwiched between the Western Ghats and the Arabian Sea, ranging from 50 to 100 km (31 to 62 mi) 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.

Varkala beach on Kerala's coast, Arabian Sea

Islands

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 200 to 300 km (120 to 190 mi) off the coast of Kerala in the Arabian sea with an area of 32 km2 (12 sq mi). 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 1,255 km (780 mi) from Kolkata (Calcutta) and 193 km (120 mi) 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 352 km (219 mi). India's only active volcano, Barren Island is situated here. It last erupted in 2008. 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 189 km (117 mi) from the Indonesian island of Sumatra, to the southeast. The highest point is Mount Thullier at 642 m (2,106 ft).

Other significant islands in India include Diu, a former Portuguese colony; Majuli,[37] 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

Main article: Rivers of India

India has around 14,500 km of inland navigable waterways.[38] There are twelve rivers which are classified as major rivers, with the total catchment area exceeding 2,528,000 km2 (976,000 sq mi).[22] All major rivers of India originate from one of the three main watersheds:[22]

  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.[39]

Bhagirathi River at Gangotri, source river of the Ganges .
National Highway 31A winds along the banks of the Teesta River near Kalimpong (West Bengal), in the Darjeeling Himalayan hill region.

The Ganges-Brahmaputra-Meghana system has the largest catchment area of about 1,600,000 km2 (620,000 sq mi).[40] The Ganges Basin alone has a catchment of about 1,100,000 km2 (420,000 sq mi).[22] The Ganges originates from the Gangotri Glacier in Uttarakhand.[39] It flows southeast, draining into the Bay of Bengal.[22] The Yamuna and Gomti rivers also arise in the western Himalayas and join the Ganges in the plains.[22] 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.[22][41]

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.

The Godavari River at Papi Hills

The Western Ghats are the source of all Deccan rivers, which include the through Godavari River, Krishna River and Kaveri River, all draining into the Bay of Bengal. These rivers constitute 20% of India's total outflow.[39]

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.[42] 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

A map of the Indian Sunderbans in West Bengal.
Pichavaram Mangroves, Tamil Nadu

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.[43] 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 4,461 km2 (1,722 sq mi),[44] 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.[42]

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 27,900 km2 (10,800 sq mi).[45] 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

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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)'.[39]

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.

Temperature averages in India; units are in degree Celsius.

Summer lasts between March and June in most parts of India. Temperatures can exceed 40 °C (104 °F) during the day. The coastal regions exceed 30 °C (86 °F) coupled with high levels of humidity. In the Thar desert area temperatures can exceed 45 °C (113 °F). 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 51 °C (124 °F) in Phalodi, Rajasthan. The lowest was −45 °C (−49 °F) in Kashmir.

Geology

Main article: Geology of India
Eparchaean Unconformity of Detrital rocks of Tirumala Hills, Eastern Ghats

India's geological features are classified based on their era of formation.[46] 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.[46] The Paleozoic formations from the Cambrian, Ordovician, Silurian and Devonian system are found in the Western Himalaya region in Kashmir and Himachal Pradesh.[46] 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.[46] 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.

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.[46] 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.[46] The Pleistocene system is found over central India. The Andaman and Nicobar Island are thought to have been formed in this era by volcanoes.[46] 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.[47][48] Alluvial soil constitute the largest soil group in India, constituting 80% of the total land surface.[48] 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.[48] Alluvial soil are generally fertile but they lack nitrogen and tend to be phosphoric.[48] National Disaster Management Authority says that 60% of Indian landmass is prone to earthquake and 8% susceptible to cyclone risks.

Black soil are well developed in the Deccan lava region of Maharashtra, Gujarat, and Madhya Pradesh.[49] These contain high percentage of clay and are moisture retentive.[48] Red soil are found in Tamil Nadu, Karnataka plateau, Andhra plateau, Chota Nagpur plateau and the Aravallis.[49] These are deficient in nitrogen, phosphorus and humus.[48][49] 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

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.[50] Its annual supply of usable and replenshable groundwater amounts to 350 billion cubic metres.[51] Only 35% of groundwater resources are being utilised.[51] About 44 million tonnes of cargo is moved annually through the country's major rivers and waterways.[38] 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.[49]

Most of India's estimated 5.4 billion barrels (860,000,000 m3) in oil reserves are located in the Mumbai High, upper Assam, Cambay, the Krishna-Godavari and Cauvery basins.[52] India possesses about seventeen trillion cubic feet of natural gas in Andhra Pradesh, Gujarat and Odisha.[52] 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.)[53]

India is the world's biggest producer of mica blocks and mica splittings.[54] India ranks second amongst the world's largest producers of barites and chromites.[54] 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.[52][54] It is the fifth-largest producer of bauxite and crude steel, the seventh-largest of manganese ore and the eighth-largest of aluminium.[54] India has significant sources of titanium ore, diamonds and limestone.[55] India possesses 24% of the world's known and economically viable thorium, which is mined along shores of Kerala.[56] Gold had been mined in the now-defunct Kolar Gold Fields in Karnataka.[57]

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.

Photo Gallery

See also

References

  1. 1 2 3 4 5 6 7 "Ministry of Home Affairs (Department of Border Management)" (DOC). Retrieved 9 January 2008.
  2. ↑ India Yearbook, p. 1
  3. ↑ "India". Encyclopædia Britannica. Retrieved 17 July 2012. Total area excludes disputed territories not under Indian control.
  4. 1 2 Manorama Yearbook 2006 (India – The Country). Malayala Manorama. 2006. p. 515. ISSN 0542-5778.
  5. ↑ "Territorial extent of India's waters". The International Law of the Sea and Indian MaritimeLegislation. 30 April 2005. Retrieved 16 May 2006.
  6. ↑ Zhu, Bin; et al. Age of Initiation of the India-Asia Collision in the East-Central Himalaya (PDF). Department of Earth and Atmospheric Sciences, University at Albany. p. 281. Retrieved 19 November 2008.
  7. 1 2 Kind, Rainer (September 2007). "The Fastest Continent: India's truncated lithospheric roots". Helmholtz Association of German Research Centres.
  8. ↑ http://mha.nic.in/sites/upload_files/mha/files/BM_MAN-IN-PAKS-060513.pdf
  9. ↑ http://mha.nic.in/sites/upload_files/mha/files/BM_MAN-IN-BANG-270813.pdf
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  13. ↑ "Another Chinese intrusion in Sikkim". Oneindia.in. 19 June 2008. Retrieved 19 November 2008.
  14. ↑ http://mha.nic.in/sites/upload_files/mha/files/Indo-Myanmar-1011.pdf
  15. ↑ http://mha.nic.in/sites/upload_files/mha/files/Indo-Bhutan-1011.pdf
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  17. 1 2 3 4 5 Manorama Yearbook 2006 (India – The Country). Malayala Manorama. 2006. p. 516. ISSN 0542-5778.
  18. ↑ Measurements are from recent imagery, generally supplemented with Russian 1:200,000 scale topographic mapping as well as Jerzy Wala, Orographical Sketch Map: Karakoram: Sheets 1 & 2, Swiss Foundation for Alpine Research, Zurich, 1990.
  19. ↑ "Physical divisions" (PDF). Archived from the original (PDF) on 12 December 2004.
  20. ↑ The Indian geographical journal. 46. Indian Geographical Society. 1971. p. 52.
  21. ↑ "The Deccan Plateau". How Stuff Works. Retrieved 14 November 2008.
  22. 1 2 3 4 5 6 7 8 9 10 Manorama Yearbook 2006 (India – The Country). p. 517.
  23. ↑ Aravali Range Students' Britannica India, by Dale Hoiberg, Indu Ramchandani. Published by Popular Prakashan, 2000. ISBN 0-85229-760-2. Page 92-93.
  24. ↑ Gupta, Harsh K; Aloka Parasher-Sen; Dorairajan Balasubramanian (2000). Deccan Heritage. Orient Blackswan. p. 28. ISBN 81-7371-285-9.
  25. ↑ Sharma, Hari Shanker (1987). Tropical geomorphology: a morphogenetic study of Rajasthan. Concept. p. 295. ISBN 81-7022-041-6.
  26. ↑ Clayton, Pamela (November 2006). "Introduction" (PDF). Literacy in Kerala. University of Glasgow. ISBN 0-86389-068-7. Retrieved 8 September 2009.
  27. ↑ Pullaiah, Thammineni; D.Muralidhara Rao (2002). "Preface". Flora of Eastern Ghats: Hill ranges of south east India. 1. Daya Books. p. 1. ISBN 81-87498-49-8.
  28. ↑ Kenneth Pletcher (August 2010). The Geography of India: Sacred and Historic Places. The Rosen Publishing Group, 2010. p. 28. ISBN 978-16-1530-142-3. Retrieved 27 March 2014.
  29. ↑ "The World's Largest Desert". geology.com. Retrieved 14 May 2011.
  30. ↑ "Thar Desert". Encyclopaedia Britannica. Retrieved 14 May 2011.
  31. ↑ Kaul, R.N. (1970). Afforestation in Arid zones. N.V. Publishers, The Hague.
  32. ↑ "Preliminary Earthquake Report". USGS Earthquake Hazards Program. Retrieved 21 November 2007.
  33. ↑ Brijesh Gulati (January 2006). "Earthquake Risk Assessment of Buildings: Applicability of HAZUS in Dehradun, India" (PDF). Indian Institute of Remote Sensing, National Remote Sensing Agency. Archived from the original (PDF) on 28 May 2008. Retrieved 19 November 2008.
  34. ↑ Manorama Yearbook 2006 (India – The Country). p. 519.
  35. ↑ "The Eastern Coastal Plain". Rainwaterharvesting.org. Retrieved 19 November 2008.
  36. 1 2 "National Portal of India: Know India: State of UTs". Government of India. Archived from the original on 19 June 2010. Retrieved 19 November 2008.
  37. ↑ Majuli, River Island. "Largest river island". Guinness World Records. Retrieved 6 September 2016.
  38. 1 2 "Introduction to Inland Water Transport". Government of India. Retrieved 19 November 2008.
  39. 1 2 3 4 Manorama Yearbook 2006 (India – The Country). p. 518.
  40. ↑ Elhance, Arun P. (1999). Hydropolitics in the Third World: conflict and cooperation in international river basins. US Institute of Peace Press. pp. 156–158. ISBN 978-1-878379-91-7. Retrieved 24 April 2011.
  41. ↑ Brahmaputra River, Encyclopædia Britannica
  42. 1 2 Manorama Yearbook 2006 (India – Environment). p. 580.
  43. ↑ India Yearbook, p. 306
  44. ↑ India Yearbook, p. 309
  45. ↑ World Wildlife Fund (2001). "Rann of Kutch". WildWorld Ecoregion Profile. National Geographic Society. Archived from the original on 2010-03-08. Retrieved 19 November 2008.
  46. 1 2 3 4 5 6 7 Manorama Yearbook 2006 (India – Geology). p. 521.
  47. ↑ "India Agronet – Soil Management". Indiagronet.com. Retrieved 18 July 2007.
  48. 1 2 3 4 5 6 "Fertilizer use by crop in India". U.S. Food and Agriculture Organization. Retrieved 2 August 2007.
  49. 1 2 3 4 "Krishi World website". Krishiworld.com. Retrieved 18 July 2007.
  50. ↑ "Water profile of India". Encyclopedia of Earth. Retrieved 20 November 2008.
  51. 1 2 Jain, J.K.; Farmer, B. H.; Rush, H.; West, H. W.; Allan, J. A.; Dasgupta, B.; Boon, W. H. (May 1977). "India's Underground Water Resources". Philosophical Transactions of the Royal Society of London. 278 (962): 507–22. doi:10.1098/rstb.1977.0058.
  52. 1 2 3 "Energy profile of India". Encyclopedia of Earth. Retrieved 20 November 2008.
  53. ↑ Chandrasekharam, D. "Geothermal Energy Resources of India". Indian Institute of Technology Bombay. Retrieved 2 November 2008.
  54. 1 2 3 4 "India's Contribution to the World's Mineral Production". Ministry of Mines, Government of India. Retrieved 20 November 2008.
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Cited sources

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