Development of Road Rail Water and Air routes in India Upsc

This is Tnpsc notes for Geography. For the topic “Transport”. The notes compiled from Samacheer Kalvi books.

Development of road, rail, water and air routes

The transport system is considered the lifeline of the country, and it is the primary goal of both the state and the centre.

There are three major means of transport

  • Land (Roadways, Pipelines, Railways),
  • Water (Inland, Waterways, Ocean Routes),
  • Air (Domestic, International).

This article discusses transport in India and the development of roads, rail, water, and air routes.

Development of transport in India

India has good transport Infrastructure such as roads, railways, airways, and waterways.

Road Infrastructure in India

An important mode of transport for goods and passengers for short, medium, and long distances. The road is easy, and cheap to construct, build and maintain.

Asia’s largest tunnel is Patnitop Tunnel. It is also India’s longest road tunnel with a length of 9.28 km (5.8 mi), and the country’s first tunnel with a fully integrated tunnel control system.

India has the second-longest road network with a total length of 56,03,293 Km as of 2016. About 85% of passengers and 70% of freight traffic are carried out every year.

Road Network of India

The road network in India is classified based on the purpose of construction, maintenance, etc., into National Highways (NH), State Highways (SH), District Roads, Rural Roads (Village Roads), Border Roads, and International Highways.

1. National Highways (NH)

  • These highways connect the capitals of states, major ports, rail junctions, and industrial and tourist centres.
  • The Ministry of Road Transport and Highways of India is responsible for the development and maintenance of the National Highways in India. The total length is 1,01,011 km, which is 1.8% of the total road network in 2016.
  • The longest National Highway is NH-7, which runs from Varanasi in UP to Kanniyakumari in TN, covering a distance of 2369 km.
  • The shortest National Highway in India is NH-47A, which runs from Ernakulum to Kochi Port (Willington Island) covering a distance of 6km. The total number of national highways in India is 200.

2. State Highways (SH)

  • SH are roads that connect important cities, towns, and district headquarters within the state and connect them with the National highways or Highways of neighbouring states.
  • These roads are financed and administered by the State government. State Highway runs to a length of 1,76,166 km as of 2016.

3. District Road

  • District roads connect the district and taluk headquarters with the state highway and national highways.
  • District roads are constructed and maintained by the Public Works Department of the state and the Zila Parishad. The total length of the district road is 5,61,940 km (16.81%) in 2016.

4. Rural Road

  • This connects different villages with neighbouring towns. Maintained by Village Panchayats. The total length is 39,35,337 Km as of 2016.
  • Rural roads consist of Panchayat roads ( Zilla Parishad, Panchayat Samiti, Gram Panchayat); roads of the Pradhan Mantri Gram Sadak Yojana (PMGSY), and those constructed by the state PWDs.

5. Border Roads

  • These roads are of strategic importance and are constructed and maintained by Border Road Organisation (BRO).
  • BRO was established in 1960, for the development of roads of strategic importance in the Northern and Northeastern Border areas.
  • BRO has constructed the world’s highest road joining Chandigarh and Leh in Ladakh. Border road runs at an average altitude of 4270 meters.

6. Expressways

  • Expressways are multi-lane, good-quality highways for high-speed traffic.
  • Important expressways are Mumbai-Pune Road, Kolkata-Dumdum Airport Road, Durgapur-Kolkata Road, and Yamuna Expressway between Delhi and Agra.

7. International Highway

  • It links India with neighbouring countries for the promotion of harmonious relationships with them.
  • These highways are constructed with aid from the World Bank under an agreement with the Economic and Social Commission for Asia-Pacific (ESCAP).
  • These highways connect India with Pakistan, Nepal, Bhutan, Bangladesh, and Myanmar.
  • In India, the densest road network is found in the northern plains, where it is relatively easy to construct roads. In the mountainous areas, it is difficult to construct roads. Road density is highest in Kerala and lowest in Jammu & Kashmir.
  • The total number of national highways in India is 6, they run from Moreh in Manipur, India, to Maesot in Thailand via Myanmar’s Tamu, Mandalay, and Myawaddy. 
  • Shershah suri built the Shahi (Royal) road, from the Indus Valley to Sonar Valley in Bengal. This road from Kolkata to Peshawar was renamed the Grand Trunk(GT) road during the British era. At present, it extends from Amritsar to Kolkata, and it is bifurcated into two segments: NH-1 from Delhi to Amritsar and NH-2 from Delhi to Kolkata.

National Highway Authority of India (NHAI), established in 1995. It is an autonomous body under the Ministry of Surface Transport

Tamil State board books

Golden Quadrilateral: Also referred to as the golden highway of India, that extends about 5,846 km long road of 4/6 lanes connecting India’s four metropolitan cities: Delhi, Kolkata, Chennai, and Mumbai, was launched in 1999.

North-South and East-West Corridors: The North-South corridor aims at connecting Srinagar in Jammu and Kashmir with Kanyakumari in Tamil Nadu (including Kochi-Salem Spur) with a 4,076 km long road.

The East-West corridor has been planned to connect Silchar in Assam with the port town of Porbandar in Gujarat, with 3,640km of road length. The two corridors intersect at Jhansi.

Railway Infrastructure in India (Railway infrastructure upsc)

Railways are considered the backbone of the surface transportation system of India. Indian Railways network is the largest in Asia and the second-largest in the world.

Length is 67,368 km with 7349 railway stations as of 2017. The history of rail transport in India started 160 years ago, when the first passenger train ran between Bori Bunder (Bombay) and Thane, a distance of 34 km.

The highest-speed train in India is the Gatimaan Express.

The light rail system in India is a type of city train public transportation that generally has a lower seating capacity and lower speed than heavy rail. It is called MRTS or Metro Trains in India, or Urban Rail Transit in India. An example is Chennai Metro, Chennai MRTS, etc.

Importance of rail transport in India

It is considered the cheapest and fastest means of Public Transport for the general public, and it is a lifeline for a country like India, where the Land is huge, with tough terrains.

Generally, rail transport is considered the safest means of transport.

The development of rail transport in India is done by the Indian Railways. For ease of operation and management, the Indian Railways is organised into 16 zones (railway zones in India UPSC).

  1. Northern Railway – Delhi,
  2. North-Western Railway – Jaipur,
  3. North-Central Railway- Allahabad,
  4. North-Eastern Railway – Gorakhpur,
  5. North-East Frontier Railway – Guwahati,
  6. Eastern Railway – Kolkata,
  7. East Coast Railway – Bhubaneswar,
  8. East-Central Railway – Hazipur
  9. West-Central Railway – Jabalpur
  10. Central Railway – Mumbai (VT)
  11. Western Railway-Mumbai (Churchgate)
  12. Southern Railway – Chennai
  13. South-Central Railway – Secunderabad
  14. South-Eastern Railway – Kolkata
  15. South-Western Railway – Hubball
  16. South East Central Railway – Bilaspur

The Northern Railway accounts for the longest route length, followed by the Western Railway.

On the basis of the track, the Indian railway’s categories are Broad Gauge with a width of 1.676 meters, Meter Gauge with a width of 1 meter, Narrow gauge with a width of 0.762 meters, and light gauge with 0.610 meters.

The arrival of Konkan Railways Corporation (KRC), Mass Rapid Transit System (MRTS), Metro, and Sub-Urban railways give easy means of transport.

a) Konkan Railway

The construction of Konkan Railways was completed in 1998. It connects Roha in Maharashtra to Mangaluru in Karnataka over a length of 760km.

On its routes, the railway crosses 146 rivers and streams, nearly 2000 bridges, and 73 tunnels. Asia’s longest tunnel is nearly 6.44 km long on this route.

The states of Maharashtra, Goa, and Karnataka are partners in this undertaking. The rail link between Banihal in the Jammu region and Qazigund in the Kashmir valley was opened in 2013; this rail passes under the Pir Panjal Range through an 11.2 km long tunnel.

b) Metro Railway in India
  • 8 cities with Metro rail in India.
  • Kolkata, Chennai, Delhi, Bengaluru, Gurgaon, Mumbai, Jaipur, and Kochi.
  • Kolkata is the first city in India to have a metro rail, also called the Mass Rapid Transit System (MRTS).
  • As of September 2018, India has 507 km of operational metro lines and 381 stations.

“The state of Meghalaya has no railway network“

The first train in India was from Mumbai to Thane in 1853, covering a distance of 34 km. In 1951, the railway was nationalised as one unit “

“The Indian Railways is headquartered in New Delhi.”

“The first suburban railway started in 1925 in Mumbai.”

“Chennai becomes the 6th Indian city with the metro railway.”

“Gatiman Express is the fastest operational train in India, which connects New Delhi and Agra and touches 160 km/h. This train takes a travel time of 105 minutes to cover a 200 km journey.”

Pipeline Transport in India

The pipeline is a convenient mode of transport for oil and natural gas fields, refineries, and markets. Also used to transport water.

The initial cost of laying the pipeline is high, but the maintenance cost is less. Its advantages are a steady supply of goods and reduced transhipment losses and delays.

Important networks of pipeline transportation in India are:

Oil field in upper Assam to Kanpur, from Salaya in Gujarat to Jalandhar in Punjab, and a gas pipeline from Hazira in Gujarat to Jagadispur in Uttar Pradesh

Water Transport System in India

It is a fuel-efficient and eco-friendly mode of transport. The oldest and cheapest mode of transport.

Two types of waterways are Inland Waterways and Ocean Waterways (see routes)

History of water transport in India

Although India has been using water transport for thousands of years, officially, the Inland Waterways Authority of India (IWAI) came into existence on 27 October 1986 to improve and develop Inland water transport.

Inland Waterways in India

India has an extensive network of inland waterways in the form of rivers, canals, lakes, and backwaters.

The total navigable length in India is 14,500 km, out of which 5200 km of rivers and 4000 km length of canals are used by mechanised crafts.

The total cargo carried by inland waterways is just about 0.1% of the total inland traffic in India. The Inland Waterways Authority was set up in 1986.

The Major national waterways are :

National Waterway 1: Between Haldia and Allahabad measures 1620 km and includes stretches of the Ganga-Bhagirathi- Hooghly river system. It is the longest national waterway in India.

National Waterway 2: a stretch of the Brahmaputra River between Dhubri and Sadiya, a distance of 891 km.

National Waterway 3: extends between Kollam and Kottapuram in Kerala, it is the first national waterway in the country with 24-hour navigation facilities along its entire stretch of 205 km.

Oceanic Routes

About 95% of India’s foreign trade by volume and 70% by value moves by ocean routes. There are 13 major and 200 minor or intermediate ports in India.

The major ports are administered by the central government, and minor ports are managed by various state governments.

The major ports on the east coast are Kolkata (including Haldia Dock), Paradip, Visakhapatnam, Chennai, Ennore, and Tuticorin.

The major ports on the west coast are Kandla, Mumbai, Nhava Seva (Jawaharlal Nehru Port), New Mangalore, Marmagao, and Kochi.

India has four major shipyards: the Hindustan Shipyard in Vishakhapatnam, the Garden Reach workshop in Kolkatta, Mazagaon Dock in Mumbai, and Kochi Shipyard in Kochi.

India is the second-largest ship-owning country in Asia and 16th in the world.

Air Transport in India

Air transport in India started on 18th February 1918, when Henry Piquet carried mail from Allahabad to Naini. In 1953, eight different airlines operating in India were nationalised.

Domestic airways fly within the country, and international airways connect major cities of the world. Indian Airlines and Air India are the two airline services run by the Indian Government.

Indian Airlines provides domestic air services, and Air India provides international air services. At present, there are 19 designated international airports.

These airports are managed by the Airport Authority of India,

Examples: Netaji Subhash Chandra Bose International Airport, Kolkata, Chennai International Airport, Chennai, Indira Gandhi International Airport, Delhi, Chhatrapati Shivaji International Airport, Mumbai, etc

There are 80 domestic airports and 25 civil enclaves at defence airfields.

Pavan-Hans Helicopter Ltd

Pavan-Hans Helicopter Ltd provides Helicopter support to the petroleum sector, such as ONGC and Oil India Ltd.

It is a public sector company based in New Delhi. Its operation is based at the Juhu Aerodrome in Vile Parle (West), Mumbai.

Pavan-Hans is a Mini Ratna-I category public sector undertaking. It also provides services to state governments in India, particularly North East India, Inter-Island Ferry Services in Andaman & Nicobar Islands, services to Lakshadweep Island, etc.

Airport Authority of India (AAI)

Constituted in 1995

It provides security to Indian Airports.

AAI, under the Ministry of Civil Aviation, is responsible for creating, upgrading, maintaining, and managing civil aviation infrastructure in India.

Transport in India geography project pdf

Transport in India in the latest news

2025

  • PM Modi inaugurated the Vizhinjam International Seaport (VIS) in Kerala. It is India’s first deep-water transhipment port. It handles containers and multi-purpose cargo. This port is developed under a Public-Private Partnership.
  • PM Modi inaugurated the Chenab Bridge and Anji Bridge on the USBRL Project in Jammu and Kashmir. The Chenab Raid Bridge is the World’s highest railway arch bridge, standing 359 metres above the riverbed. Whereas Anji Khad Bridge is India’s first cable-stayed railway bridge, built over the Anji River, a tributary of the Chenab.
  • AIZAWL joins the rail network. Mizoram’s capital, Aizawl, is now connected to the national railway network via the Bairabi-Sairang line, making it the fourth North-East state capital with rail connectivity after Guwahati, Agartala and Itanagar.
  • Indian Railways has successfully tested its first hydrogen-powered coach at the Integral Coach Factory (ICF) in Chennai.
  • Sagarmala Finance Corporation Limited – The Ministry of Ports, Shipping & Waterways (MoPSW) inaugurated SMFCL, India’s first NBFC dedicated to the maritime sector.
  • Rudrastra (India’s longest Freight Train) – On August 7, Indian Railways successfully operated “Rudrastra”, a long freight train created by combining six empty BOXN rakes, from Ganjkhwaja station under the Pandit Deen Dayal Upadhyay (DDU) division. The train measures approximately 4.5 km with 345 wagons, and it is the longest freight train ever operated by Indian Railways. It uses seven engines.
  • The Ministry of Ports, Shipping and Waterways has inducted India’s third Very Large Gas Carrier (VLGC), Shivalik, under the Indian flag at Visakhapatnam Port.
  • On December 7 2025, Shyok Tunnel was inaugurated, which is a project of Border Roads Organisation (BRO). Shyok tunnel is a 920-metre cut-and-cover tunnel on the 255 km-long Durbuk-Shyok-Daulat Beg Oldie (DS-DBO) Road, which runs along the Line of Actual Control (LAC) in eastern Ladakh.

Unveiling the Mysteries of Iraver Formations in Brazil: A Geological Marvel

Iraver Formations in Brazil

Brazil, known for its diverse landscapes and rich biodiversity, is home to some of the most fascinating geological formations on the planet. One such marvel that has captivated the attention of scientists and enthusiasts alike is the Iraver Formations. In this blog post, we will embark on a journey to explore the intricate details of these formations, delving into their geological history, unique features, and the scientific significance they hold.

Understanding the Iraver Formations

The Iraver Formations are a series of geological structures located in Brazil, primarily in the central-western region of the country. Comprising a vast and intricate network of rock formations, these structures have puzzled geologists for years, sparking curiosity about their origin and formation processes.

Geological History

To comprehend the Iraver Formations, it is essential to delve into the geological history of the region. These formations date back millions of years, with their origins rooted in complex geological processes. The region underwent a series of tectonic movements, volcanic activities, and erosion, contributing to the creation of the unique landscape we see today.

Formation Processes

One of the distinctive features of the Iraver Formations is the way they were shaped over time. Erosion played a significant role in sculpting the rocks into intricate patterns and designs. Wind and water erosion, coupled with the region’s climatic conditions, have contributed to the distinctive appearance of these formations. The intricate interplay of geological processes has resulted in a mesmerizing display of natural artistry.

Breathtaking Landscapes

The Iraver Formations offer a breathtaking visual spectacle, with towering rock formations, deep canyons, and unique geological structures that defy the imagination. Exploring these landscapes is like stepping into a surreal world where time seems to have stood still. The vibrant colors of the rocks, shaped by mineral deposits, add to the allure of the Iraver Formations.

Ecological Importance

Beyond their aesthetic appeal, the Iraver Formations play a crucial role in the local ecosystem. The unique geological composition of the rocks creates microenvironments that support diverse flora and fauna. Scientists have identified several rare and endemic species that have adapted to the specific conditions offered by these formations. Preserving the Iraver Formations is not only essential for geological research but also for the conservation of the region’s biodiversity.

Scientific Significance

Geologists and researchers flock to the Iraver Formations to unravel the mysteries hidden within the rocks. The unique geological features provide valuable insights into Earth’s history, helping scientists understand past climatic conditions, tectonic movements, and evolutionary processes. The rocks serve as a geological archive, offering a glimpse into the dynamic forces that have shaped our planet over millions of years.

Challenges and Conservation Efforts

While the Iraver Formations are a source of wonder and scientific discovery, they face various challenges, including anthropogenic activities, climate change, and tourism impact. Conservation efforts are underway to protect these geological wonders and ensure their preservation for future generations. Balancing the need for scientific exploration with sustainable tourism practices is crucial to safeguard the Iraver Formations.

Visiting the Iraver Formations

For those eager to witness the marvels of the Iraver Formations firsthand, several access points and guided tours are available. However, it’s essential to adhere to responsible tourism practices to minimize environmental impact and preserve the integrity of this unique geological landscape.

Conclusion

The Iraver Formations of Brazil stand as a testament to the Earth’s geological complexity and the wonders that nature can create over millennia. As scientists continue to unravel the secrets hidden within these rocks, the Iraver Formations remain a source of inspiration, inviting us to appreciate the beauty of our planet’s natural wonders and to contribute to their conservation for future generations to cherish. Whether you’re a geology enthusiast, a nature lover, or simply someone seeking awe-inspiring landscapes, the Iraver Formations are a must-see destination that promises an unforgettable journey into the heart of Brazil’s geological heritage.

Forest and wildlife in India Upsc

Forest and wildlife in India

India is one of the world’s richest in biological diversity. Also, several numbers of species are yet to be discovered. Some estimate that 10% of wild flora and 20% of its mammals are on the threatened list.

Natural Vegetation and Planted Vegetation

Natural vegetation is something that certain plant species left undisturbed over some time. For example, in a forest or mountain terrain, these plant communities start to adapt themselves to the conditions, might be soil or climate, etc.

On the other hand, Planted vegetation, is growing a specific plant from the forest or some source and planting it in the farm/garden under some human supervision.

India’s land is huge and it is so large that it is called the Indian subcontinent, which has a large variety of natural vegetation. Also, India has got so many types of vegetation that differ from one place to another. Due to this, there are great variations in climate and soil in India.

For example, the Himalayas has temperate vegetation. This is in the North part of India. On the other hand in places such as Andaman and Nicobar, Western Ghat, etc. These two places are separated by hundreds of miles of sea but still, these two has similarity in vegetation. These two are Tropical Rain Forest.

To completely contrast the above two vegetation we find yet another type of vegetation that is desert and semi-deserts of Rajasthan. It is known as Cactii, it is a kind of busy or thorny vegetation.

You will find tropical forests and mangroves in the deltaic regions.

 Types of Forest in the India

  1. Tropical Evergreen and Semi-Evergreen Forest
  2. Tropical Deciduous Forest
  3. Tropical Thorn Forest
  4. Montane Forest
  5. Littoral and Swamp Forest

Tropical Evergreen and Semi-Evergreen Forest

Forest and wildlife Types of Forest-Evergreen Forest
Photo by Brady Knoll on Pexels.com

Ok, these Woods are found in Andaman Nicobar Is, Northeastern regions, and Western Ghats slopes.

As far as climate is concerned these are generally in warm and humid places, where there are rainfall of excess of 200 cm and an annual mean temperature of almost 22 degrees Celcius.

The tropical evergreen forest is well arranged with a layer that is nearer to land and is well sheltered with creepers, and shrubs. A unique pattern is found, a short tree along with a variety of tall trees in this vegetation.

These trees of evergreen forests reach up to 60 meters and above. You know another exciting fact about this vegetation, there is a definite period these trees for fruition, flowering, or shedding their leaves.

It appears green throughout the year. Examples of Evergreens are ebony, aini, mahogany, rosewood, etc. Next, the other one is found in the less rainy area which has an amalgamation of moist deciduous trees and evergreen that is known as a semi-evergreen forest.

Another characteristic feature is the presence of Climbers.

The main examples of semi-evergreen forests are white cedar, kail, and hollock.

Someone might have known the value of these forests, Yes that someone is the British, who knows the commercial value of the woods, they replace Oak forest with Pine in Kumaon and Garhwal.

Oakwood was used to lay rails and for constructions as woods were insulators. Also, Brits cleared forests for the plantations of rubber, tea, coffee.

Tropical Deciduous Forest in India

Types of Forest-Tropical Deciduous Forest
Photo by Pixabay on Pexels.com

These are like viruses, like everywhere in India, it’s widespread and also called monsoon forests. They found where the precipitation was around 70-200 cm.

Based on the amount of water and moist presence, these are further divided into moist and dry deciduous.

Moist Deciduous found in heavy precipitated areas with 100-200 cm, found in the Himalayan foothill in the northeastern Indian states.

Also found in eastern ranges of the western ghats and parts of Odisha. Some of the tree species are Teak, Sandalwood, sal, Kusum, etc. Dry Deciduous found in margins of wetter areas where there is the transition, moist to drier to thorns. The precipitated areas with 70-100 cm.

Cover vast regions of the country. Found in the Indian peninsula, UP plains, and Bihar and also in higher Peninsular plateau and north Indian plains.

These have striking characteristics such as patches of grass in common, with trees scatter between other things and mixed with teak. Another common feature is, these trees shed their leaves and become leafless in dry seasons

Some of the tree species are Axlewood, tendu, palas, etc. Due to low rainfall and perhaps overgrazing to some extent, this vegetation is found very low in the western Rajasthan and southern Rajasthan.

Tropical Thorn Forests in India

Types of Forest-Tropical Thorn Forest
Photo by Tomas Anunziata on Pexels.com

From the word thorn, you might have concluded this kind of vegetation is found in dry areas. Thorn forests are found in areas where there is very low precipitation of about less than that of 50 cm.

Thorn vegetation, yes it consists of a variety of Shrubs, grasses, thorns, etc. In India, as you know it is found Northwestern part of the country, where the land is semi-arid.

Prominent areas of Tropical Thorn are southwestern Punjab that borders Punjab and Rajasthan, and of course Rajasthan, Gujarat, MP, and UP. In thorn vegetation, the plants are leafless throughout or most of the year.

Examples of Thorn vegetation are Babool, Ber, Wild Date, Palas, etc. A kind of grass grows up to 2m called Tussocky grass.

Montane Forest in India

These forests are classified based on altitude and amount of rainfall. Accordingly two different types of forest namely the Eastern Himalayas Forest and the Western Himalayas forest.

Eastern Himalayas

Found on the slopes of the mountains in northeast states. These forests receive rainfall of more than 200 cm. The vegetation of the eastern Himalayan forest is evergreen type.

The altitude is between 1200- 2400 m found in this type of forest Sal, Oak, Laurel, Amura, Chestnut, Cinnamon are the main trees. At the altitude of 2400 to 3600m, oak, birch, silver, fir, fine, spruce and juniper are found.

Western Himalayas

In this region rainfall is moderate. Western Himalayas forest is found in the states of Jammu and Kashmir, Himachal Pradesh, and Uttarakhand.

Up to 900m altitude semi-desert vegetation is found. This region is known for bushes and small trees. At an altitude of 900 to1800m, chir tree is most common. Other important trees of this region are sal, semal, dhak, Jammun, and jujube.

At the altitude of 1800 to 3000m, is covered with semi temperate coniferous forest, Chir, Deodar, Blue pine, poplar, birch, and elder.

Alpine

Alpine is found all along the Himalayas with above 2400m altitude. They purely have coniferous trees. Oak, Silver fir, pine, and Juniper are the main trees of the Alpine forest.

The eastern parts of the Himalayas have a large extent of these forests.

Tidal Forest

Tidal forests are found in and around the deltas, estuaries, and creeks prone to tidal influences. The tidal forest is also called Delta Forest or Swamp Forest.

The delta of Ganga – Brahmaputra has the largest tidal forest. The deltas of Mahanadi, Godavari and Krishna rivers are also known for Tidal forests. These are also known as Mangrove Forest.

Coastal Forest

These are littoral forests. Coastal Forest is found in coastal areas. Casurina, palm, and coconut are the dominant trees. Both the eastern and western coasts have this kind of forest.

The coast of Goa and Kerala is known for its coastal forest.

Riverine Forest

Riverine forests are found along the rivers in Khadar Area. These are known for Tamarisk and Tamarind Trees. The rivers of great plains are more prominent for this type of natural vegetation.

Wildlife

Wildlife includes Animals of any habitat in nature. The non-domesticated animals are wild animals. The wild animals include vertebrates such as fish, amphibians, reptiles, birds, and mammals and invertebrates such as bees, butterflies, moths, etc.

Flaura means plants and Fauna means animals. India has a fauna of about 81,251 species out of 1.5 million species in the world.

India has 6500 species of invertebrates, 5000 species of mollusks, 2546 species of fishes, 1228 species of birds, 458 species of mammals, 446 species of reptiles, 204 species of amphibians, 4 species of panthers, and 6000 species of insects.

India is home to tigers, lions, leopards, snow leopards, pythons, wolves, foxes, bears, crocodiles, rhinoceroses, camels, wild dogs, monkeys, snakes, antelope species, deer species, bison, and the mighty Asian elephant.

Various human activities caused troubles to various species that led them to decrease in population and even cause extinction.

A conversation of biodiversity is necessary to maintain ecological balance. IBWL (Indian board for wildlife) was created in 1952 to suggest ways of protection, conservation, and management of wildlife to the government.

In 1972, the union government passed the Wildlife (Protection) Act. The objective of the Wildlife (Protection) Act 1972 is to effectively protect the wildlife and control poaching, smuggling, and illegal trade of wildlife.

UN Convention on Biological Diversity (CBD) in 1992 recognizes the sovereign rights of states to use their Biological Resources. India developed 102 National Park and 515 Wildlife Sanctuaries to preserve the wildlife.

Biosphere Reserves

Biosphere Reserves are protected areas of the land, coastal environment, where the people are also part of the system. There are 18 Biosphere reserves established by the Indian government.

Biosphere reserves protect a large area of natural habitat and usually include one or more National parks along with buffer zones. Buffer zones are open to some economic uses.

Eleven of the Eighteen biosphere reserves in India are under the list of Man and Biosphere programme of UNESCO. They are Gulf of Mannar, Nandadevi, Nilgiris, Nokrek, Pachmarhi, Simlipal, Sundarbans, Agasthiyamalai, Great Nicobar, Kanjanjunga and Amarkantak.

Biosphere ReservesState
Achanakmar-AmarkantakChattisgarh, Madya Pradesh
AgasthyamalaiKerala
Dibru SaikhowaAssam
Dihand DibangArunachal Pradesh
Great NicobarAndaman and Nicobar Islands
Gulf of MannarTamil Nadu
KachchGujarat
KanchenjungaSikkim
ManasAssam
Nanda DeviUttarakhand
NilgirisTamil Nadu
NokrekMeghalaya
PachmarhiMadya Pradesh
SimlipalOdisha
SundarbansWest Bengal
Cold DesertHimachal Pradesh
Sesahachalam HillsAndra Pradesh
PannaMadya Pradesh

Project Tiger launched in April 1973. Its object is to conserve the tiger population, especially in Tiger Reserves in India. The project increased over 60% population of Tiger from 1979 consensus put the population at 3015.

Other species like barasingha (swamp deer), rhino, and elephants population also increased parallel due to this project.

forest and wildlife resources in india

forest and wildlife sanctuaries in india

forest and wildlife laws in india

forest conservation laws in india

Bibliography

  1. Samacheer Kalvi Geography Class X, 2019 Edition.

6 natural Regions: India’s geographical position and Physical features Upsc Ncert Notes

India’s geographical position

  • India is the seventh-largest country in the world and forms part of the continent of Asia.
  • Together with its neighbours—Pakistan, Bangladesh, Nepal, Bhutan, Sri Lanka, and Myanmar—it constitutes the region known as the Indian Subcontinent.
  • The country is enclosed by natural boundaries: the Himalayan Mountain range serves as a natural barrier in the north; the Thar Desert and the Arabian Sea mark the western limits; the Bay of Bengal borders it to the east; and the Indian Ocean lies to the south.
  • In 1984, Rakesh Sharma, the first Indian astronaut in space, described India to Prime Minister Indira Gandhi as “Sāre jahān se achchha” (better than the whole world).
  • For regional discussion, India is grouped into five broad divisions: the great mountain zone, the plains of the Ganga and the Indus, the desert region, the southern peninsula, and the islands.

Geological Evolution and Plate Tectonics

  • The earth is approximately 4600 million years old and has evolved through changes brought about by endogenic and exogenic forces.
  • These forces played a significant role in shaping the surface and subsurface features of the earth.
  • Millions of years ago, the Indian plate was located to the south of the equator, was much larger in size, and included the Australian plate.
  • The plate broke into multiple parts; the Australian plate moved towards the southeast, while the Indian plate moved to the north.
  • The northward movement of the Indian plate continues to this day, bringing significant consequences to the physical environment of the Indian subcontinent.
  • The present geological structure and geomorphologic processes in the Indian subcontinent result from the interplay of endogenic and exogenic forces, as well as the lateral movements of tectonic plates.

Geological Divisions of India

  • India can be divided into three geological divisions that broadly follow its physical features: The Peninsular Block, The Himalayas and other Peninsular Mountains, and the Indo-Ganga-Brahmaputra Plain.
  • The Peninsular Block:
    • The northern boundary is an irregular line running from Kachchh along the western flank of the Aravali Range near Delhi, roughly parallel to the Yamuna and the Ganga, up to the Rajmahal Hills and the Ganga delta.
    • Extensions of this block include the Karbi Anglong and the Meghalaya Plateau in the northeast, and Rajasthan in the west.
    • The northeastern parts are separated from the Chotanagpur plateau by the Malda fault in West Bengal.
    • The block is mainly formed by a great complex of very ancient gneisses and granites.
    • Since the Cambrian period, it has stood as a rigid block, with exceptions on the western coast which is submerged beneath the sea and some areas changed by tectonic activity without affecting the original basement.
    • As part of the Indo-Australian Plate, it experienced vertical movements and block faulting, resulting in the rift valleys of the Narmada, Tapi, and Mahanadi, and the Satpura block mountains.
    • It consists of relict and residual mountains like the Aravali, Nallamala, Javadi, Veliconda, Palkonda, and Mahendragiri hills.
    • River valleys are shallow with low gradients, and most east-flowing rivers (Mahanadi, Krishna, Kaveri, Godavari) form deltas before entering the Bay of Bengal.
  • The Himalayas and other Peninsular Mountains:
    • In contrast to the rigid Peninsular block, these are young, weak, and flexible in geological structure.
    • They are subjected to the interplay of exogenic and endogenic forces, resulting in faults, folds, and thrust plains.
    • Tectonic in origin, they are dissected by fast-flowing, youthful rivers and feature landforms like gorges, V-shaped valleys, rapids, and waterfalls.
  • Indo-Ganga-Brahmaputra Plain:
    • Formed by the rivers Indus, Ganga, and Brahmaputra.
    • Originally a geo-synclinal depression that attained maximum development during the third phase of Himalayan mountain formation about 64 million years ago.
    • It has been gradually filled by sediments from Himalayan and Peninsular rivers, with alluvial deposits averaging 1,000 to 2,000 meters in depth.

6 natural regions of India

  • Based on macro variations, India is divided into six physiographic divisions: The Northern and North-eastern Mountains, The Northern Plain, The Peninsular Plateau, The Indian Desert, The Coastal Plains, and The Islands.

1. The Northern and North-eastern Mountains

  • Consists of the Himalayas and the Northeastern hills.
  • The Himalayas consist of parallel ranges, including the Greater Himalayan range (Great Himalayas and the Shiwalik).
  • Orientation: Runs from northwest to southeast in northwestern India, east-west in the Darjiling and Sikkim regions, southwest to northwest in Arunachal Pradesh, and north-south in Nagaland, Manipur, and Mizoram.
  • The Great Himalayan range (central axial range) has a length of approximately 2,500 km from east to west and a width of 160-400 km from north to south.
  • It acts as a strong wall between the Indian subcontinent and Central and East Asian countries, serving as a physical barrier and a climatic, drainage, and cultural divide.

2. The Northern Plain

  • Formed by alluvial deposits of the Indus, Ganga, and Brahmaputra rivers.
  • Extends approximately 3,200 km from east to west, with an average width of 150-300 km and a maximum depth of alluvium ranging from 1,000 to 2,000 meters.
  • Divided into three major zones from north to south: the Bhabar, the Tarai, and the alluvial plains (further divided into Khadar and Bhangar).
  • Bhabar: An 8-10 km narrow belt parallel to the Shiwalik foothills at the break-up of the slope where streams deposit heavy rocks and boulders, sometimes disappearing into the zone.
  • Tarai: A 10-20 km wide belt south of the Bhabar where streams re-emerge without demarcated channels, creating marshy and swampy conditions. It has luxurious natural vegetation and varied wildlife.
  • Bhangar and Khadar: A belt south of the Tarai containing old and new alluvial deposits respectively. These feature mature-stage fluvial erosional and depositional landforms like sand bars, meanders, ox-bow lakes, and braided channels.
  • The Brahmaputra plains are known for riverine islands, sand bars, periodic floods, and shifting river courses that form braided streams.
  • River mouths form some of the world’s largest deltas, such as the Sunderbans delta.
  • Mostly a featureless plain with a general elevation of 50-150 meters above mean sea level.
  • The states of Haryana and Delhi form a water divide between the Indus and Ganga river systems.
  • The Brahmaputra flows from northeast to southwest before taking an almost 90° southward turn at Dhubri into Bangladesh.
  • Possesses fertile alluvial soil supporting crops like wheat, rice, sugarcane, and jute, sustaining a large population.

3. The Peninsular Plateau

  • An irregular triangle rising from 150 meters above the river plains to an elevation of 600-900 meters.
  • The outer extent is marked by the Delhi ridge (northwest), the Rajmahal hills (east), the Gir range (west), and the Cardamom hills (south), with an extension in the northeast including the Shillong and Karbi-Anglong plateau.
  • Composed of a series of patland plateaus like Hazaribagh, Palamu, Ranchi, Malwa, Coimbatore, and Karnataka.
  • It is one of the oldest and most stable landmasses of India, with a general elevation sloping from west to east (as proved by the pattern of river flow).
  • Features include tors, block mountains, rift valleys, spurs, bare rocky structures, hummocky hills, wall-like quartzite dykes, and an emphatic presence of black soil in the west and northwest.
  • The northwestern part features a complex relief of ravines and gorges (e.g., Chambal, Bhind, and Morena).
  • Divided into three broad groups: The Deccan Plateau, The Central Highlands, and The Northeastern Plateau.
  • The Deccan Plateau:
    • Bordered by the Western Ghats (west), Eastern Ghats (east), and the Satpura, Maikal range, and Mahadeo hills (north).
    • Western Ghats (known locally as Sahyadri, Nilgiri hills, Anaimalai hills, and Cardamom hills) are higher (average 1,500 m) and more continuous than Eastern Ghats, with height increasing from north to south.
    • Highest peak: Anaimudi (2,695 m) on the Anaimalai hills, followed by Dodabetta (2,637 m) on the Nilgiri hills.
    • The discontinuous Eastern Ghats (Javadi hills, Palconda range, Nallamala hills, Mahendragiri hills) are highly eroded by rivers like the Mahanadi, Godavari, Krishna, and Kaveri.
    • The Eastern and Western Ghats meet at the Nilgiri hills.
  • The Central Highlands:
    • Bounded to the west by the Aravali range.
    • The southern boundary is formed by the Satpura range, consisting of scarped plateaus (600-900 m) which form the northernmost boundary of the Deccan plateau.
    • An extension reaches Jaisalmer in the west, covered by longitudinal sand ridges and crescent-shaped sand dunes called barchans.
    • It has undergone metamorphic processes, evidenced by rocks like marble, slate, and gneiss.
    • General elevation is 700-1,000 meters, sloping north and northeast.
    • Most Yamuna tributaries originate in the Vindhyan and Kaimur ranges; Banas is the only significant Chambal tributary originating from the Aravalli.
    • The eastern extension is formed by the Rajmahal hills, with the mineral-rich Chotanagpur plateau to its south.
  • The Northeastern Plateau:
    • An extension of the main Peninsular plateau, detached due to a huge fault created between the Rajmahal hills and the Meghalaya plateau during the Himalayan origin.
    • Divided into the Garo, Khasi, and Jaintia Hills, with an extension in the Karbi Anglong hills of Assam.
    • Rich in mineral resources like coal, iron ore, sillimanite, limestone, and uranium.
    • Receives maximum rainfall from the southwest monsoon, resulting in a highly eroded surface (e.g., Cherrapunji’s bare rocky surface).

4. The Indian Desert

  • Lies to the northwest of the Aravali hills.
  • Topography is undulating and dotted with longitudinal dunes and barchans.
  • Has an arid climate, low rainfall (below 150 mm per year), and low vegetation cover, earning the name “Marusthali”.
  • Evidence like ~180 million-year-old wood fossils at Aakal and marine deposits around Brahmsar suggests it was under the sea during the Mesozoic era.
  • Surface features carved by physical weathering and wind include mushroom rocks, shifting dunes, and oases.
  • Slopes towards Sindh in the north and towards the Rann of Kachchh in the south.
  • Rivers are mostly ephemeral (Luni river is significant in the south), presenting inland drainage where streams disappear or join a lake/playa.
  • Lakes and playas contain brackish water, serving as the main source of salt.

5. The Coastal Plains

  • Divided into the western coastal plains and the eastern coastal plains.
  • The Western Coastal Plains:
    • An example of a submerged coastal plain (evidenced by the submerged city of Dwaraka).
    • Forms a narrow belt providing natural conditions for ports and harbours (e.g., Kandla, Mazagaon, JLN port Navha Sheva, Marmagao, Mangalore, Cochin).
    • Extends from Gujarat to Kerala, divided into the Kachchh and Kathiawar coast, Konkan coast, Goan coast, and Malabar coast.
    • Narrow in the middle, broadening towards the north and south, and its rivers do not form any deltas.
    • The Malabar coast features ‘Kayals’ (backwaters) used for fishing, inland navigation, and tourism (like the Nehru Trophy Vallamkali boat race in Punnamada Kayal).
  • The Eastern Coastal Plains:
    • Broader than the western plains and serves as an example of an emergent coast.
    • Features well-developed deltas formed by eastward-flowing rivers like the Mahanadi, Godavari, Krishna, and Kaveri.
    • Has fewer ports and harbours due to its emergent nature, and the continental shelf extends up to 500 km into the sea, hindering port development.

6. The Islands

  • Two major groups located in the Bay of Bengal and the Arabian Sea.
  • Bay of Bengal Islands:
    • Consists of about 572 islands/islets located roughly between 6°N-14°N and 92°E-94°E.
    • Divided into two broad categories separated by the Ten degree channel: Andaman (north) and Nicobar (south).
    • Two principal groups of islets include the Ritchie’s archipelago and the Labrynth island.
    • Believed to be elevated portions of submarine mountains, with some smaller islands being volcanic in origin.
    • Features Barren island, the only active volcano in India.
    • Important peaks include Saddle peak (North Andaman, 738 m), Mount Diavolo (Middle Andaman, 515 m), Mount Koyob (South Andaman, 460 m), and Mount Thuiller (Great Nicobar, 642 m).
    • The coastal line features coral deposits and beautiful beaches, experiencing convectional rainfall and supporting equatorial vegetation.
  • Arabian Sea Islands:
    • Includes Lakshadweep and Minicoy, scattered between 8°N-12°N and 71°E-74°E longitude, located 220-440 km off the Kerala coast.
    • Entire group is built of coral deposits, containing approximately 36 islands of which 11 are inhabited.
    • Minicoy is the largest island with an area of 453 sq. km.
    • The group is broadly divided by the Nine degree channel (Amini Island to the north, Canannore Island to the south).
    • Features storm beaches with unconsolidated pebbles, shingles, cobbles, and boulders on the eastern seaboard.

Location physical features Tnpsc Samacheer notes

The geographical features of India consist of the peninsula which is surrounded by water on three sides, the world’s highest mountain ranges in the north, the desert in Rajasthan, etc.

Coast and Land Boundary of India

India shares a 15,200 Km land frontier in the west with Pakistan, northwest with Afghanistan, Nepal-China-Bhutan in the north, and Bangladesh-Myanmar in the east and also shares the longest border with Bangladesh with 4156 km and shares the shortest border with Afghanistan at 106 km.

The country has a coastline of 6100 km with three sides, namely the Indian Ocean, and its two arms lie on the Arabian Sea in the west, and in the east, it is the Bay of Bengal. The total length of India’s coastline including the islands is 7516.6 km.

The Palk Strait, a narrow and shallow sea, separates India and Sri Lanka.

India’s Geographic Location in the World

India’s landmass is centrally located between East and West Asia. India has a southward extension to the Asian continent and the Indian Ocean. India has a strategic location as it is located in the trans-Indian Ocean route that connects Europe and East Asia.

This helps in establishing contact with West Asia, Africa, and Europe

India: A Subcontinent

India, along with Myanmar, Bangladesh, Pakistan, Nepal, Bhutan, and Sri Lanka, forms the Indian Subcontinent. A chain of mountains in the northwest, north, and northeast separates this area from Asia. Also separated by Sea in the South.

This region’s unique continental characteristics in physiography, climate, natural vegetation, minerals, etc., define it as a subcontinent. Therefore, people call India a subcontinent.

The physical features of India

  • Geographically India’s physical features are divided into five physiographic divisions:
    • Himalayas
    • Great Northern Plains
    • Peninsular Plateau
    • Great India Desert
    • Coastal Plains
    • Islands

1. The Himalayan mountains

The Himalayan mountains (northern mountains) are the youngest and the loftiest mountain chains in the world. Tectonic activity folded the earth’s crust, forming the Himalayas only a few million years ago.

Himalaya stretches for a distance of about 2,500 Km from the Indus Gorge in the west to the Brahmaputra Gorge in the east. The width of the Himalayas varies from 500 km in Kashmir to 200 Km in Arunachal Pradesh.

People famously refer to the Pamir Knot as the “Roof of the World,” which connects the Himalayas and the high ranges of Central Asia. From the Pamir Knot, the Himalayas extend eastwards in an arc.


Pamir Knot in India Map

The term Himalaya means “Abode of Snow” in the Sanskrit language. The Himalayas act as a great wall and are classified into three divisions:

  • Trans Himalayas
  • Himalayas
  • Eastern or Purvanchal Hills

The Aravalli range is the oldest fold mountain range in India.

1.1 The Trans-Himalayas

The western Himalayas also known as the Trans-Himalayas lie to the north of the great Himalayan Range. It lies in the Tibetian plateau and Jammu-Kashmir. The western Himalayas are about 40km wide in the eastern and western extremities.

It is about 225 km wide in its central part. The trans-Himalayas contain the Tethys sediments. This region’s rock contains fossil-bearing marine sediments which underlie ‘Tertiary granite. It also has partly metamorphosed sediments and constitutes the core of the Himalayas axis.

The prominent ranges of Trans-Himalayas are Zaskar, Ladakh, Kailash, and the Karakoram.

1.2 The Himalayas

The Himalayas constitute the core part of the northern mountains and are young-fold mountains. The movement of the Angara landmass in the north and the Gondwana landmass in the south formed it.

The compression uplifted the Tethys sea found between these two landmasses, resulting in the formation of the Himalayas. The Himalayas consist of many ranges.

  • Greater Himalayas
  • Lesser Himalayas
  • Siwaliks
PeakCountryHeight in metres
Mt. EverestNepal8848
Mt.K2 or Godwin AustenIndia8611
KanchenjungaIndia8598
MakaluNepal8481
DhaulagiriNepal8172
Nanga ParbatIndia8126
AnnapurnaNepal8078
Nanda DeviIndia7817
KametIndia7756
Namcha BarwaIndia7756
Gurla MandhataNepal7728
Peaks of Himalayas with height

Himalayan Mountain Ranges with its Height and country

The Himalaya is the home of several high peaks. However, it holds the record of having the maximum number of highest peaks among any mountain range in the world. Out of the 14 highest peaks in this world, the Himalayas hold 9.

1.2.1 The Greater Himalayas or the Himadri

The Himadri rises abruptly like a wall north of the lesser Himalayas. It is 25 km wide and the average height is about 6000m. The Greater Himalayas receive lesser rainfall compared to the lesser Himalayas and the Siwaliks. Physical weathering is less effective over the Greater Himalayas (Himadri) compared to the other ranges.

Almost all the lofty peaks of the Himalayas are located in this range. The famous ones are Mt.Everest (8,848m) and Kanchenjunga (8,586m). Mt.Everest is located in Nepal and Kanchenjunga is located between Nepal and Sikkim.

This range is the most continuous of all ranges. It is a region of permanent snow cover. It has many glaciers, Gangotri, Yamunotri, and Siachen are famous ones.

1.2.2 The Lesser Himalayas or The Himachal

The Himachal (Lesser Himalayas) is in the middle range of the Himalayas. The height of this range varies from 3,700 to 4,500m. Its width varies up to 80 km. The major rocks of the Himachal ranges are slate, limestone, and quartzite.

Heavy rainfall, deforestation, and urbanization expose this region to extensive erosion. The Pir Panjal, Dhauladhar, and Mahabharat are the mountain ranges found here. Major hill stations of the Himalayas are located in the Lesser Himalayas (Himachal). Shimla, Mussourie, Nainital, Almora, Ranikhet, and Darjeeling are the famous ones.

Major Passes in the Himalayan
  • Karakoram Pass in Jammu Kashmir.
  • Zojila Pass, Shipkila Pass in Himachal Pradesh
  • Bomdila Pass in Arunachal Pradesh
  • Nathala Pass and Jhelepla Pass in Sikkim
  • Khyber Pass which connects Pakistan and Afghanistan
  • Bolan Pass in Pakistan is an important pass of the Indian Subcontinent.
1.2.3 The Siwaliks or Outer Himalayas

The Siwaliks extend from Jammu and Kashmir to Assam. It is partly made by the debris brought by the Himalayas rivers. The altitude varying between 900-1100 meters elevation of this range is 1300m. The width of Siwaliks varies from 10km in the east to 50km in the west.

It is the most discontinuous range.

Duars and Duns

The longitudinal valleys found between the Siwaliks and the Lesser Himalayas are Duns in the west. In the east it is Duars. These are the ideal sites for settlements in this region.

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1.3 Purvanchal Hills

Purvanchal Hills are the eastern offshoot of the Himalayas. These ranges extend to the northeastern states of India. The states lying in the Purvanchal hill ranges are Arunachal Pradesh, Nagaland, Manipur, Mizoram, Tripura, and eastern Assam.

Most of the Purvanchal hills are located along the border of India and Myanmar and some are inside India.

Purvanchal Hills or Purvanchal Ranges are collection of hill such as Dafla Hills, Abor Hills, Mishmi Hills, Patkai Bum Hills, Naga Hills, Manipur Hills, Mizo Hills, Tripura Hills, Mikir Hills, Garo Hills, Khasi Hills, and Jaintia Hills.

Longitudinal Divisions of Himalayas

Longitudinal division of Himalayas

  1. The Kashmir Punjab Himachal Himalayas are located between the rivers of Indus and Sutlej.
  2. The Kumaun Himalayas are located between the rivers of Sutlej and Kali.
  3. The Central-Nepal Himalayas are located between the rivers of Kali and Tista.
  4. The Assam Eastern Himalayas are located between the rivers of Tista and Dihang.

The Great Northern Plains

The fertile land extending across seven north Indian states forms the great northern plains. These extensive plains lie to the south of the northern mountains. This plain is one of the most extensive stretches of alluvium in the world and is deposited by the river Indus, Ganga, Brahmaputra, and its tributaries.

The length of the plain is about 2400 km and the width varies from 240 to 320 km. Its width increases from east to west. It covers an area of over 7 lakh sq. km. The great plains of India are formed mostly by the depositional process of the Himalayan and Vindhyan rivers.

These rivers deposit sediments along the foothills and flood plains. The important characteristics and features of sediment deposition in the plains areas are as follows.

1. The Bhabar Plain

This plain is made of unassorted sediments and gravel deposited by the rivers of the Himalayas. Small stream flow disappears in this region due to the high porosity of this plain. Bhabar Plain lies to the south of the Siwalik from west to east (Jammu Division to Assam).

The width of the Bhabar Plain varies from 8 to 15km. It is wider in the western plains (Jammu Division) than in the east (Assam). This plan is not suitable for cultivation, and only big trees with large roots thrive in this region.

2. The Tarai Tract or Teraje Region of India

The Tarai Tract is a zone of excessive dampness with thick forests and rich wildlife and is located in the south of Nepal and northern India which is parallel to the lower Himalayas. It is stretched from the Brahmaputra in the east and Yamuna in the west.

It lies south of the Bhabar plains. The width of the Tarai Tract is 15 to 30 Km and is wider in the eastern of the Great Plains especially in the Brahmaputra Valley because of the heavy rainfall.

The Tarai forest is cleared for farming in many states. The Tarai region is important as it provides connectivity to Eastern Himalayas across Nepal. The ecological importance of the Tarai region has Tiger, Elephant, Asian Rhino, etc.

In Nepal, the Tarai region is referred to as the “Granary of Nepal”, as the soil in this region is very fertile and receives good rainfall and a suitable climate for agriculture.

3. The Bhangar Plains

The Bhangar represents the upland alluvial tracts of the Great Plains of India. It is formed by the older alluvium. The Bhangar land lies above the flood limits of the rivers. This soil is dark in colour, rich in humus content, well-drained, and useful for agriculture.

4. The Khadar Plains

The new alluvium tracts along the courses of the rivers are known as Khadar or Bet lands. The Khadar tracts are enriched by fresh deposits of silt every year during rainy seasons. The Khadar land consists of sand, silt, clay, and mud. It is highly fertile soil.

5. Delta Plains

The deltaic plain is an extension of the Khadar land. It covers 1.9 Lakh sq. km in the lower reaches of the Ganga River. It is an area of deposition as the river flows in this tract sluggishly.

Chars and Bils

The deltaic plains consist of old mud, new mud, and marsh. In the delta region, the uplands are called ‘Chars‘. And the marshy areas are called ‘Bils’.

The Peninsular Plateaus

It lies to the south of the Great Northern Plains. This is the largest Physiographic division in India. Peninsular Plateaus cover about 16 lakh sq. km (about half of the total area). It is an old rocky plateau region. The topography has a series of plateaus and hill ranges interspersed with rivers.

Aravalli hills mark the north-western boundary of the plateau region. Its northern and northeastern boundaries are marked by the Bundelkhand upland, Kaimur, and Rajmahal hills. The Western Ghats and the Eastern Ghats mark the western and eastern boundaries respectively.

The altitude of a large portion of the plateau is more than 600m from the mean sea level. The peak of Anaimudi is the highest point in the plateau, its height is 2695m, and is located in Anaimalai. The general slope of this plateau is towards the east.

The Great Plateau is a part of the Gondwana landmass. Due to old age, rivers in this region attained their base level and developed broad and shallow valleys. The river Narmada divides the plateau region of India broadly into two parts.

The region lying to the north of Narmada is called the Central Highlands, and the region lying to the south of Narmad is called the Deccan Plateau. All the major rivers such as Mahanadi, Godavari, Krishna, Kaveri, etc. lie to the south of the Vindhyas that flow eastwards and fall into the Bay of Bengal. Narmada and Tapti are the two rivers situated to the south of the Vindhyas flow westward.

Their movement towards the west is due to the presence of a rift valley in the region.

1. Central Highlands

The Central Highlands lies between the Narmada River and the Northern Great Plains. The Aravallis form the west and northwestern edge of the Central Highlands. These hills extend from Gujarat, through Rajasthan to Delhi in the Northwesterly direction for a distance of about 700km.

The height of these hills is about 1500m in the southwest while near Delhi the height is hardly 400m. Guru Shikhar with 1722m is the highest peak of this range. The western part of the central highland is known as the Malwa Plateau. It lies to the southeast of Aravallis and to the north of the Vindhyachal range.

The rivers Chambal, Betwa, and Ken drain the Malwa plateau before they join the river, Yamuna.

  • The part of the Central Highlands that extends to the east of Malwa Plateau is known as Bundelkhand and its further extension is known as Bagelkhand.
  • The eastern part of the central Highlands which lies in the north-eastern part of the Indian plateau is known as Chhota-Nagpur Plateau.
  • It covers much of Jharkhand, and adjacent parts of Odisha, West Bengal, Bihar, and Chhattisgarh.
  • This region is very rich in mineral resources, particularly iron ore and coal.

2. Deccan Plateau

It is the largest part of the plateau region of India. The shape of this plateau is almost triangular. On the sides of the triangle is marked by a line joining Kanyakumari with Rajmahal Hills and this line passes through the Eastern Ghats.

The second arm is marked by Satpura Range, Mahadeo Hills, Maikal Range, and the Rajmahal Hills. The third arm is marked by the Western Ghats. The total area is about 7 lakh square km and the height ranges from 500 to 1000m above sea level.

The Western Ghats form the western edge of the Peninsular Plateau and run parallel to the Arabian Sea Coast. The northern part of this range is called Sahyadris. The height of the Sahyadris increases from north to south. Anaimudi is a sort of tri-junction of the Anaimalai range, the cardamom hills, and the Palani hills.

Kodaikanal is a hill resort situated on the Palani Hills. The Eastern Ghats run from southwest to northeast from the eastern edge of this plateau. This range is also called Poorvadri. The Eastern ghats join the western ghats at the Nilgiri hills, bordering Karnataka and Tamil Nadu.

The Eastern ghats are not continuous like the Western ghats. The rivers of Mahanadi, Godavari, Krishna, Pennar, and Kaveri have dissected this range in many places.

The Indian Desert

The Thar desert, also known as the Great Indian Desert is a large arid region in the northwestern part of the Indian subcontinent that covers an area of 2,00,000 sq. km and forms a natural boundary between India and Pakistan. It is the world’s 7th largest desert and the world’s 9th largest subtropical desert located in the western part of India.

The desert lies in the western part of the Aravali range and covers 2/3 of Rajasthan state. There are two major divisions in the Thar desert and they are the Actual desert region called Marusthali and the semi-desert region called Bhangar. And different types of sand dunes and salt lakes called Dhands are seen here.

The Coastal Plains

The Peninsular Plateau of India is flanked by narrow coastal plains of varied width from north to south known as the Western Coastal Plains and the Eastern Coastal Plains. They were formed by the depositional action of the river and the erosional and depositional actions of the sea waves.

The Indian coastal plains are divided into Western and Eastern Coastal Plains.

1. The Western Coastal Plain

The western coastal plain lies between the Western Ghats and the Arabian Sea. It extends from Rann of Kutch in the North to Kanyakumari in the south and its width varies from 10 to 80 km. It is mainly characterized by Sandy beaches, coastal sand dunes, mudflats, lagoons, estuary, laterite platforms, and residual hills.

The northern part of the west coastal plain is known as the Konkan plain. The middle part of this plain is known as Kanara. The southern part of the plain is known as the Malabar coast which is about 550km long and 20-100 km wide.

This part of the coast is characterized by sand dunes. Along the coast, there are numerous shallow lagoons and backwaters called Kayals and Teris. Vembanad is a famous backwater lake found in this region.

2. The Eastern Coastal Plain

It lies between the eastern ghats and the Bay of Bengal and it stretches along with the states of West Bengal, Odisha, Andhra Pradesh, and Tamil Nadu. These plains are formed by the alluvial fillings of the littoral zone by the east-flowing rivers of India. The coastal plain consists mainly of the recent alluvial deposits.

This coastal plain has a regular shoreline with well-defined beaches.

  • The coastal plain between the Mahanadi and Krishna Rivers is known as the Northern Circars and the southern part lies between the Krishna and Kaveri Rivers is called the Coromandel Coast.
  • The Marina Beach on this coast in Chennai is the second-longest beach in the world.

Important Lakes in the Eastern Coastal Plain

Among the backwater lakes of this coast, lake Chilka (Odisha) is the largest lake in India located to the southwest of the Mahanadi delta, the Kolleru Lake lies between the deltas of Godavari and Krishna, and the Pulicat Lake lies on the border of Andhra Pradesh and Tamil Nadu are the well-known lakes in the eastern coastal plain.

The Islands of India

There are two major island groups namely Andaman-Nicobar and Lakshadweep. Andaman and Nicobar Islands consist of 572 islands and are located in the Bay of Bengal. Lakshadweep Islands are located in the Arabian Sea and have 27 islands that are mainly of coral origin.

The Andaman and Nicobar Islands are of largely tectonic and volcanic origin. India’s only active volcano is found on Barren Island in Andaman and Nicobar Islands.

1.Andaman and Nicobar Islands

Andaman and Nicobar Islands are located in an elevated portion of the submarine mountains. It lies close to the equator, as a result, it remains hot and wet throughout the year and has a dense forest. The area of the island group is about 8249 sq km.

The entire group of islands is divided into two, which are Andaman in the North and Nicobar in the South. Andaman and Nicobar Islands are of great strategic importance for the country. Port Blair is the capital of Andaman and Nicobar Islands.

The Ten Degree Channel separates Andaman from the Nicobar group. The southernmost tip, Indira Point is a part of Nicobar Island

The southernmost tip of India, which is Indira Point is located at the latitude of 6°45’N or 6-1/2 N which is part of Nicobar Island.

2. Lakshadweep Islands

Lakshadweep archipelago is a group of coral islands situated off the west coast of the Indian Subcontinent. The administrative capital of Lakshadweep is Kavaratti. The Eight Degree Channel separates the Lakshadweep from the Maldives Islands.

Their uninhabited Island is known as Pitt Island, which has a bird sanctuary. Lakshadweep has three divisions earlier namely Laccadive, Minicoy, and Amindivi. It was named Lakshadweep in 1973.

3. Offshore Islands

Besides Andaman-Nicobar and Lakshadweep islands, India has a number of Islands along the Western Coast, Eastern Coast, in the delta region of Ganga, and in the Gulf of Mannar. Many of these islands are uninhabited and are administered by the adjacent states.

India Location

The latitude and longitude extent of India

India extends from  8°4 ‘N to 37°6 ‘N latitude and 68°7 ‘E to 97°25 ‘E longitudes. India is located in the North-Eastern Hemisphere. The Southernmost part of India is Indira Point or 6-1/2 N latitude is 6°45’N latitude and is located in the Andaman and Nicobar Islands.

The southernmost point of the mainland is Cape Comorin or Kanyakumari. The north-south extent of India is 3214 km, it extends from Indira Col in Jammu and Kashmir to Kanyakumari in Tamil Nadu. The east-west extension is 2933 km, it extends from Rann of Kutch in Gujarat in the west to Arunachal Pradesh in the east.

The tropic of Cancer at 23°30′ N passes through the center of the country and divides the country into two halves. One half is northern temperate and the other half is southern tropical lands. India is politically divided into 28 states and 8 union territories as of 16-11-2020.

The newly formed union territories are Jammu and Kashmir, and Ladakh after the removal of Article 370. Total union territories along the west coast are Diu Daman-Dadra Nagar Haveli, Mahe (Pondicherry), and Lakshadweep. Totally three.

The number of union territories on the eastern coast is Puducherry and Andaman Nicobar Islands. Totally two. The smallest state in India is Goa. The largest state in India is Rajasthan.

The smallest union territory in India is Lakshadweep. The largest union territory is the Andaman & Nicobar Islands. The largest district in India is Kachchh (Gujarat). The smallest district in India is Mahe (Pondicherry).

The states that do not have an international border or lie in the largest state Rajasthan are Haryana, Uttar Pradesh, and Madya Pradesh. The states that do not have an international border or lie on international coastal boundaries are Haryana, Jharkhand, Madhya Pradesh, Chhattisgarh, and Telangana.

Conclusion

This post is for the topic ‘Location – Physical Features of India‘ for the Tnpsc exam. These notes are taken from Samacheer Kalvi’s book 10th Standard. It is also useful for Upsc and other state service exams.

References

  1. https://ncert.nic.in/textbook/pdf/iess102.pdf

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Rivers in India Tnpsc notes

This article discusses the Indian rivers and their tributaries. It also covers west and east flowing rivers in India and types of rivers in India.

Rivers in India

Rivers in India is an important topic in Civil services, often a number of questions asked from its topic. There are seven major rivers namely Indus, Brahmaputra, Narmada, Tapi, Godavari, Krishna, and Mahanadi. Along with its tributaries, it makes the river system of India.

It is important to know the river as about most as India is an agriculture-dependent country, and most of the politics, interstate disputes happen because of it. Also, it is important to know about climate-related to the river, which helps in Agriculture and also disaster management.

A river system or drainage system is an integrated system of tributaries and a trunk stream that collects and drains surface water into the sea, lake, or some other water bodies. The total area drained by a river and its tributaries is known as the drainage basin. The drainage pattern of an area is the result of the geological structure of the respective areas.

It provides irrigation, drinking water, navigation, and helps in power generation to the people.

Types of rivers in India

The Indian drainage system is classified into Himalayan, and Peninsular rivers based on their location. Let us see what are Himalayan and peninsular drainage systems?

Himalayan Rivers

Himalayan rivers are found in North India. These rivers originate from the Himalayas. Thereby they are called Himalayan rivers. Himalayan rivers are perennial rivers, that is there is constant water flow throughout the year. Examples of Himalayan rivers are Indus, Ganga, Brahmaputra, etc.

Types of Rivers in India
Types of rivers in India

The Indus River System

Indus river is one of the largest rivers in the world. Indus river originates from a northern slope of the Kailash range in Tibet near Manasarovar Lake at a height of 5150 metres above sea level. The length of the Indus is about 2880km but it flows only 709 km in India. The Indus river has a total drainage area extending 11,65,500 sq km in which 321,289 sq km areas are drained in India.

Its flows through the Indian state Ladakh. It flows through Zaskar ranges and creates deep gorges. The river runs through formerly called Jammu and Kashmir, turns south near Chillar, and enters Pakistan.

Indus major tributaries are Jhelum, Chenab (Largest tributary of Indus), Ravi, Beas, and Sutlej. It enters the Arabian Sea.

Indus River Tributaries: East to West Order

TributaryOriginKey Characteristics
SatlujRakas lake near MansarovarAntecedent river cutting through Himalayas at Shipki La
BeasBeas kund near Rohtang PassJoins Satluj at Harike in Punjab
RaviRohtang Pass, Kullu hillsFlows between Dhauladhar and Pir Panjal ranges
ChenabChandra and Bhaga rivers meet at TandiLargest tributary of Indus
JhelumSheshnag lake near Verinag, KashmirFlows through Wular lake
ShyokRimo Glacier, Karakoram RangeFlows through Northern Ladakh
GilgitNorthern Areas of PakistanRight bank tributary
HunzaKarakoram RangeJoins Indus in Kashmir region
KabulAfghanistanMajor right bank tributary

Important Note: According to the Indus Water Treaty of 1960, Indus, Jhelum, and Chenab are under Pakistan’s control, while Ravi, Beas, and Satluj are under India’s control.


The Ganga River System

The Ganga river has the largest drainage system in India. It extends over an area of 8,61,404 sq km in India. The Ganga plain is the densely populated plain in India. The Ganga River originates as Bhagirathi from the Gangotri Glacier in Uttar Khasi District of Uttarkhand, at an elevation of 7010 metres.

The length of the Ganga river is 2525 km. The major tributaries of Ganga from the north are Gomti, Gandak, Kosi, and Ghaghra and from the south, the Yamuna which is the largest tributary of Ganga, Son, Chambal, etc.

The Ganga river is called the Padma in Bangladesh. The Ganga and Brahmaputra together create the world’s largest delta known as Sundarbans in Bangladesh before joining the Bay of Bengal.

Ganga River Tributaries: East to West Order

TributaryTypeOriginKey Characteristics
MahanandaLeft BankDarjeeling hillsLast left bank tributary of Ganga
KosiLeft BankNepal, TibetFamous for changing river courses
GandakLeft BankNepal HimalayasMajor left bank tributary
GhagharaLeft BankMapcha Chung Glacier, TibetKnown as Karnali in Nepal
GomatiLeft BankPilibhit districtPasses through Lucknow
RamgangaLeft BankDudhatoli Hill, UttarakhandFlows through Corbett National Park
YamunaRight BankYamunotri GlacierLongest tributary, joins at Prayagraj
SonRight BankAmarkantak PlateauKnown as ‘Swarna Nadi’
KarmanasaRight BankKaimur District, BiharForms boundary between Bihar and UP
PunpunRight BankPalamu District, JharkhandJoins Ganga near Patna

Unique Features:

  • Originates from Himalayan and Plateau regions
  • Supports extensive agricultural landscapes
  • Critical for North Indian ecological systems

Brahmaputra River System

Brahmaputra river originates from the Chemayungdung Glacier of the Kailash range to the east of Lake Manasarovar in Tibet at a height of 5150 metres about sea level. The Brahmaputra is also known as Tsangpo (Purifier) in Tibet. The total drainage area of the Brahmaputra river is about 5,80,000 sq. km.

Its total drainage area in India is 1,94,413 sq. km. The total length of the Brahmaputra rivers is about 2900 km. The total length of the Brahmaputra river in India is 900 km. Brahmaputra river enters India through a gorge in Arunachal Pradesh namely Dihang. The tributaries of Brahmaputra river are Tista, Manas, Barak, Subansiri etc. Brahmaputra river is called Jamuna in Bangladesh.

Brahmaputra river joins with Ganga river in Bangladesh. The resultant river is called Meghna.

Brahmaputra River Tributaries: East to West Order

TributaryBankOriginKey Characteristics
Lohit RiverLeftEastern TibetOriginates in Zayal Chu range, flows through Mishmi Hills
Dibang RiverLeftArunachal PradeshPart of left bank tributaries
Dhansiri RiverLeftLaisang Peak, NagalandRuns through Dimapur and Golaghat districts
Kopili RiverLeftAssamSouth bank tributary
Manas RiverRightBhutan376 km long, flows through Assam and southern Bhutan
Kameng RiverRightTawang districtOriginates near Gori Chen Mountain
Subansiri RiverRightChina/Tibet442 km long, enters Brahmaputra in Lakhimpur district
Teesta RiverRightCholomo Lake, SikkimFlows through Himalayan Mountains
Sankosh RiverRightBhutanKnown as Puna Tsang in Bhutan

Unique Features:

  • Originates as Tsangpo in Tibet
  • Enters India as Siang/Dihang
  • Becomes Brahmaputra after joining Dibang and Lohit rivers

Characteristics of Himalayan Rivers

a.Originate from the Himalayas
b.Long and wide
c.Perennial in nature
d.Unsuitable for hydropower generation
e.Middle and lower courses are navigable

Peninsular Rivers of India

The south Indian rivers are called the Peninsular rivers. Most of the Peninsular rivers originate from the Western Ghats. Peninsular rivers are non-perennial rivers. The peninsular rivers are non-perennial rivers because of large seasonal fluctuation in the volume of water as they are solely fed by rain.

These rivers flow in the valley with steep gradients. Based on the direction of flow, the peninsular rivers are divided into West flowing and East flowing rivers.

East Flowing Rivers

Mahanadi

Mahanadi river originates near Sihawa in the Raipur district of Chattisgarh. It flows through Odisha and its length is 851 km. Seonath, Telen, Sandur, and Ib are its major tributaries. The mainstream of Mahanadi is divided into several distributaries such as Paika, Birupa, Chitartala, Genguti and Nun.

All these distributaries form the Delta of Mahanadi which is one of the largest deltas in India. The Mahanadi empties its water in the Bay of Bengal.

Godavari

The Godavari is the longest among the Peninsular rivers and its length is 1465km. Its drainage area is 3.13 lakh sq. km. The Godavari river is also called Vridha Ganga. This river originates in the Nasik district of Maharashtra, a portion of Western Ghats. Godavari river flows through Telangana and Andra Pradesh before joining the Bay of Bengal.

The Major Tributaries of the Godavari river are Purna, Penganga, Pranitha, Indravati, Tal, and Salami. The Godavari river gets divided into two channels called Vasistha and Gautami near Rajahmundry. Then it forms one of the largest deltas in India. Kolleru, a freshwater lake is located in the deltaic region of the Godavari.

Krishna

The Krishna river originates from a spring at Mahabaleshwar in the Western Ghats of Maharashtra. The length of the Krishna River is 1400 km. Its drainage area is 2.58 lakh sq. km. Krishna is the second-longest Peninsular river.

The major tributaries of the Krishna river are Bhima, Peddavagu, Musi, Koyna, and Tungabhadra. Krishna river flows through Andra Pradesh and joins the Bay of Bengal at Hamasaladeevi.

Kaveri

The Kaveri river originates at Talakaveri, from Kudagu hills of Karnataka. Its length is 800km.Kaveri river is called Dhaksin Ganga or Ganga of South Harangi. The major tributaries of the Kaveri river are Hemavati, Kabini, Bhavani, Arkavathy, Noyyal, Amaravathi, etc.

In Karnataka, the river bifurcates twice, forming the sacred islands of Srirangapatnam and sivasamudram. While entering Tamil Nadu, Kaveri continues through a series of twisted wild gorges until it reaches Hogenakkal Falls and flows through a straight, narrow gorge near Salem.

The Kaveri breaks at Srirangam Island with two channels, river Coleroon and Kaveri. At last, it empties into the Bay of Bengal at Poompuhar.

 

rivers in india
rivers in india map

West Flowing Rivers

Narmada

Narmada river rises in Amarkantak Plateau in Madhya Pradesh at an elevation of 1057 metres. It flows for a distance of about 1312 km. Narmada drainage area is about 98796 sq. km. It forms a 27 km long estuary before entering the Arabian Sea through the Gulf of Cambay.

Narmada is the largest among the west-flowing rivers of Peninsular rivers. The major tributaries of Narmada are Burhner, Halon, Heran, Banjar, Dudhi, Shakkar, Tawa, Barna and Kolar.

Tapti

The Tapti is one of the major rivers of Peninsular India with a length of about 724 km. It covers an area of 65,145 sq km. Tapti river rises near Multai in the Betul district of Madhya Pradesh at an elevation of about 752 m.

It is one of only the three rivers in Peninsular India that run from east to west – the others being the Narmada and the Mahi. The major tributaries are Vaki, Gomai, Arunavati, Aner, Nesu, Buray, Panjhra, and Bori.

It outfalls into the Arabian Sea through the Gulf of Cambay.

east and west flowing rivers in india map
east and west flowing rivers in India map

Rivers of India: East and West Flowing Classification

East Flowing RiversWest Flowing Rivers
GodavariNarmada
KrishnaTapti
MahanadiMahi
KaveriSabarmati
BrahmaputraLuni
Subarnarekha–
Pennar–
Damodar–
Brahmani–
Ponnaiyar–
Vaigai–

Key Characteristics:

  • East Flowing Rivers: Drain into the Bay of Bengal
  • West Flowing Rivers: Drain into the Arabian Sea

Notable Points:

  • Godavari is the longest river in South India, covering 10% of India’s area
  • Most east-flowing rivers originate from Western Ghats, Eastern Ghats, and central highlands
  • These rivers are crucial for agriculture, irrigation, and supporting biodiversity

Characteristics of South Indian Rivers

• Originate from the Western Ghats
• Short and narrow
• Non-perennial in nature
• Suitable for hydropower generation
• Not useful for navigation

In which river the Gerosappa (jog) fall is found?

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Monsoon rainfall weather and climate in India Tnpsc

Climate of India primarily categorised as Winter during January to february, Pre-Monsoon or Summer during March to May, Southwest monsoon during June to September and Northeast Monsoon during October to December

This post for the Tnpsc exam in geography from the topic ‘Monsoon, rainfall, weather, and climate’. It is referenced from the Samacheer Kalvi book.

It covers Monsoon winds in India such as Southwest monsoon, north-west monsoon, the direction of retreating monsoon in India, and weather and climate.

Weather and Climate in India

The word Monsoon is derived from the word Mausim, an Arabic word. It is used by Arabic navigators to describe the seasons of the shores of the Indian Ocean. The winds blow from southwest to northeast during summer. Similarly, the wind blows from northeast to southwest during winter. Different concepts by Meteorologists surrounding this complex phenomenon.

By Dynamic concept, Monsoon wind originates due to seasonal migration of planetary winds and pressure belts following the position of the sun. During summer solstice ‘June 21’, the sun rays fall vertically over the tropic of cancer.

Thereby all the pressure and wind belts of the globe shift northwards. At this time, Inter-Tropical Convergence Zone (ITCZ) also moves northwards and a major part of the Indian landmass comes under the influence of southeast trade winds.

While crossing the equator this wind gets deflected and takes the direction of south-west and becomes south-west monsoon. During winter, the pressure and wind belts shift southward, thereby establishing the northeast monsoon(trade winds) over this region. This phenomenon of systematic change in the direction of the planetary winds is known as the monsoon.

Types of monsoon in India or Seasons of India

According to the experts, there are four main Monsoon seasons in India namely:

  1. Winter or Cold weather season (January – February)
  2. Pre-Monsoon or summer or hot weather season (March-May)
  3. Southwest Monsoon or rainy season (June – September)
  4. Northeast monsoon season (October – December)

Winter or cold-weather season or Winter Season in India

During this season, Sun’s vertical rays fall over the tropic of Capricorns which is far away from India. As a result, India receives slanting sun rays that result in low temperatures.The cold season is characterized by clear skies, fine weather, low humidity, light northerly winds, and large daytime variations of temperature.

High pressure develops in North India and a north-westerly wind blows down the Indus and Ganges valleys.In South India, the general direction of the wind is from east to west.The mean temperature increases from North to south, the decrease is sharp as moving towards northwards in the north-western part of the country.

The minimum temperature in the south is 22 degrees Celsius and 10 degrees Celsius in the Northern plains, 6 degrees Celsius in Punjab.The rain generally falls in the Western Himalayas, Tamil Nadu, and Kerala in this season.

Western disturbances and associated troughs in the west are the main precipitation systems in the northern part of the country.The jet stream plays a dominant role in bringing these disturbances in India. These disturbances cause rain precipitation in Himachal Pradesh Punjab, Haryana and snowfall in the hills of Jammu and Kashmir. This rainfall is used for the cultivation of Winter Wheat.

Pre Monsoon or hot weather season (March-May) or Summer Season in India

In this season the vertical rays of the sun fall over peninsular India and there is a steady increase in temperature from South to North.It is almost hot and dry in most of the country in the initial part of the season.

The weather over the land areas of the country is influenced by thunderstorms associated with rain and sometimes with hail mostly in the middle and later part. During this season, the temperature increases in all parts of the country, and in April the interior part of the southern part of India, the temperature daily mean will be 30 to 35 degrees Celsius.

In the central part of India, the mean temperature would reach up to 40 degrees in most parts. Some parts of India, such as Gujarat, North Maharashtra, Rajasthan, and North Madhya Pradesh experience high day temperatures and low night temperatures.

Because of the atmospheric pressure, the wind blows from the southwest to the northeast direction in the Arabian Sea and Bay of Bengal. This brings pre-monsoon showers to the west coast during May month called summer monsoon in India.

There are showers also called ‘Mango Showers’ that helps in the quick ripening of mangoes along the Kerala and Karnataka coast. Northwesters or Kalbaisakhis are local severe storms associated with strong thunderstorms, winds, and short-duration rains.

Kalbaisakhis occurs over the eastern and northeastern parts of Bihar, West Bengal, and Assam during April and May and approaches from the Northwesterly directions.

Southwest Monsoon Or Rainy Season

direction of south west monsoon in india
Direction of the southwest monsoon over India

South west monsoon in India

The southwest monsoon is the most important feature of the Indian climate. It takes place in the Southern Tip of India Peninsula normally by the first week of June. South-West monsoon advances along the Konkan coast during starting of June and it covers the whole country by July 15.

The global phenomenon El Nino influences the South West Monsoon. In North India, the temperature reaches almost 46-degree Celsius before the southwest monsoon or rainy season. There occurs a “Burst of Monsoon”, which is termed as Break, which is a sudden approach of monsoon wind over southern India with Thunder Showers. This show reduces the temperature of the country.

South West Monsoon Winds

The monsoon wind that is the southern tip of India’s landmass gets separated into two branches. One branch starts from the Arabian Sea and Another Branch starts from the Bay of Bengal. The one from the Arabian sea provides heavy showers to the west coast of India and is located on the west ghats windward side.

The other part towards the north hits the Himalayan Mountains and brings heavy rainfall in the North. Rajasthan and western parts get rain from these winds as the direction of the wind is parallel to the Aravali mountains and there is nothing to hold or intrude the wind.

Direction of South West monsoon in India

The Bay of Bengal wind moves to northeast India, Myanmar and this wind is trapped by mountain groups such as Khasi, Garo, and Jaintia. This results in the heaviest rainfall in the world, that is Mawsynram located in Meghalaya. Then it moves to the west, which results in a rainfall decrease from east to west.

The southwest monsoon winds in India are responsible for 75% of the Indian rainfall. Tamil Nadu that is located on the leeward side receives less rainfall from this wind.

Post Monsoon or Retreating or Northeast Monsoon in India

north east monsoon winds
North East Monsoon in India

The southwest monsoon starts in North India by the end of the second half of September because of the southward shifting of pressure belts. This wind gets backs from the Indian peninsula and blows towards the Bay of Bengal.

The Coriolis forces deflect this wind and make this wind blow from the Northeast and it is known as North-East Monsoon or Post Monsoon season. The Northeast Monsoon in India is connected with the formation of the North-Easterly wind system over the Indian subcontinent.

From this season, the states such as Tamil Nadu, Andhra Pradesh, Kerala, and south interior Karnataka get good rainfall that almost 35% of its annual rainfall. The Retreating monsoon creates a large-scale loss of life during the storms that occur frequently in Tamil Nadu, Andra Pradesh, and some parts of Karnataka.

During these seasons, strong winds and storms hit the coastal regions, and the daytime temperature falls rapidly all over the country. The average temperature over North-west India shows a decreasing trend from 38 and falling to 28-degree celsius in November.

Distribution of Rainfall

About 118 cm is the average rainfall of India. The spatial distribution of the rainfall in the country is uneven. About 11% area receives over 200 cm,21% area receives 125 to 200 cm, 37 % area receives 75 to 125, 24 % area gets 35 to 75 cm and 7% area gets less than 35 cm of rainfall annually.

Rajasthan, Punjab, Haryana, west and south-west Uttar Pradesh, Western Madhya Pradesh, and the entire Deccan Trap or Plateau region east of Western Ghats except for a narrow strip along Tamil Nadu coast receive less than 100 cm rainfall annually.

The rest of the country receives 100 to 200 cm of rainfall.

Areas of High Rainfall

The west coast has the highest rainfall. The western Ghats, Himalayan areas in the northeast, and hills of Meghalaya. In these areas, the rainfall exceeds 200 cm. In parts of Khasi and Jaintia Hills, the rainfall exceeds 1000 cm. But in the Brahmaputra valley and its adjoining hills receives less than 200 cm.

Areas of Medium Rainfall

The southern parts of Gujarat, east Tamil Nadu, Northeastern Peninsula covering Odisha, Jharkhand, Bihar, eastern Madhya Pradesh, Northern Ganga Plain along the sub-Himalayas and Cachar valley and Manipur receives rainfall between 100-200 cm.

Area of Low Rainfall

Western Uttar Pradesh, Delhi, Haryana, Punjab, Jammu and Kashmir, eastern Rajasthan, Gujarat, and Deccan Plateau receives rainfall around 50-100 cm.

Areas of Inadequate Rainfall

Some parts of the Peninsula, especially in Andra Pradesh, Karnataka and Maharashtra, Ladakh, and most of western Rajasthan receive less than 50cm of rainfall.

Snowfall occurs only in Himalayan regions.

Conclusion

This article takes about the Monsoon and four primary seasons of the country concerning the precipitation and temperature change as drafted by the India Meteorological Department. Also provided with data of the distribution of rainfall in the Indian subcontinent.

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Agricultural pattern and cropping seasons in India Tnpsc

The agricultural pattern in India or cropping seasons in India refers to three different agricultural seasons, namely Kharif, Rabi, and Zaid. The Kharif season is started by the Southwest Monsoon, which helps produce tropical crops such as rice, cotton, bajra, jowar, etc.

Similarly, the Rabi season starts in October. The agriculture and allied sectors include dairy, sheep, goat, poultry, piggery, fisheries, horticulture, sericulture, etc.

India has three cropping Seasons namely:

  • Rabi
  • Kharif
  • Zaid

Cropping seasons in India

Rabi

The Rabi season is one of the main cropping seasons in India, corresponding to the winter months. It follows the Kharif season and precedes the Zaid season. The Rabi season typically spans from October to March, and crops cultivated during this period are known as Rabi crops. Here are some key features of the Rabi season:

Rabi crop in India includes wheat, barley etc
Rabi crops or rabi harvest, also known as winter crops, are crops that are sown in winter and harvested in the spring in India, Pakistan, and Bangladesh.

Timing: The Rabi season starts with the onset of winter and continues until early spring. It is characterized by relatively cool temperatures, making it suitable for the cultivation of certain crops.

Crops: Rabi crops are predominantly winter crops that include cereals, pulses, and oilseeds. Some of the major Rabi crops include wheat, barley, mustard, gram (chickpea), linseed, and various fruits and vegetables such as carrots, peas, and tomatoes.

Water Availability: Rabi crops are often grown in areas where irrigation facilities are available. In regions with dependable water sources, farmers can cultivate Rabi crops even in the absence of significant rainfall.

Crop Rotation: The Rabi season is an important period for crop rotation and diversification. It allows farmers to vary the types of crops they cultivate, helping in soil fertility management and pest control.

Geographic Distribution: Rabi crops are cultivated in different parts of India, with their distribution influenced by climatic conditions and water availability. Wheat, for example, is a major Rabi crop in states like Punjab, Haryana, and Uttar Pradesh.

Importance: Rabi crops contribute significantly to India’s food grain production. Wheat, in particular, is a staple food for a large portion of the population. The cultivation of pulses and oilseeds during the Rabi season helps meet the demand for protein and cooking oil.

Government Initiatives: Various government policies and initiatives are implemented to support Rabi crop cultivation, including providing subsidies, credit facilities, and promoting better agricultural practices.

Harvesting Time: Harvesting of Rabi crops usually occurs in late winter or early spring, depending on the specific crop. The harvested crops are important for both domestic consumption and as a source of income for farmers.

The Rabi season is a crucial component of India’s agricultural calendar, contributing significantly to the country’s overall food production and economic well-being. It complements the Kharif season by providing a diverse range of crops and maintaining a continuous agricultural cycle throughout the year.

Kharif

The Kharif season is one of the two main cropping seasons in India, the other being Rabi. Kharif crops are sown in the monsoon season and harvested in the autumn. The Kharif season typically starts with the onset of the southwest monsoon, which generally occurs from June to September. Here are some key features of the Kharif season:

Kharif crop in India includes rice, cotton , sugarcane
Kharif crops, also known as monsoon crops or autumn crops, are domesticated plants that are cultivated and harvested in India, Pakistan and Bangladesh during the Indian subcontinent’s monsoon season.

Timing: The Kharif season corresponds to the monsoon period in India, starting with the arrival of the southwest monsoon winds around June and extending until September. The exact timing varies across different regions of the country.

Crops: Kharif crops are predominantly summer crops, and they include a variety of cereals, pulses, oilseeds, and cash crops. Some major Kharif crops include rice, maize, millets (jowar, bajra), pulses (moong, urad), oilseeds (soybeans, groundnuts), cotton, sugarcane, and various fruits and vegetables.

Rainfall Dependence: Kharif crops are heavily dependent on adequate rainfall, as the monsoon provides the primary source of water for cultivation during this season. Regions with good monsoon rains are more suitable for Kharif crop cultivation.

Geographic Distribution: Kharif crops are cultivated across different agro-climatic zones in India. Rice, for example, is a major Kharif crop in states like West Bengal, Odisha, and Andhra Pradesh, where conditions are conducive to its growth.

Importance: Kharif crops play a vital role in India’s food security and agricultural economy. They contribute significantly to the country’s overall food grain production and provide livelihoods to a large number of farmers.

Crop Diversity: The Kharif season allows for the cultivation of a diverse range of crops, reflecting the varied agro-climatic conditions in different parts of the country. The choice of crops depends on factors such as soil type, water availability, and local climate.

Sowing Period: Sowing of Kharif crops typically begins with the onset of the monsoon, and the timing varies based on the specific crop and regional conditions. For example, rice is often sown early in the Kharif season.

Harvesting Time: Harvesting of Kharif crops usually occurs in the autumn months, depending on the specific crop. The timing of harvesting is crucial to ensure optimal yield and quality of the produce.

The success of Kharif crops is closely linked to the monsoon rains, and variations in rainfall patterns can impact agricultural productivity. Government policies and initiatives, such as providing irrigation facilities, crop insurance, and subsidies, aim to support farmers during the Kharif season and enhance overall agricultural resilience.

Zaid Season

Zaid is a term used in Indian agriculture to describe a short-duration cropping season that typically occurs during the summer months, from March to June. This season falls between the Rabi (winter) and Kharif (monsoon) seasons. The Zaid crops are generally grown in regions where there is adequate water availability for summer cultivation, often with the help of irrigation.

Zaid season
Bitter Gourd flower, the bitter Gourd is cultivated and Harvested in Zaid season

Key features of the Zaid season include:

Timing: Zaid crops are planted during the summer months when temperatures are relatively high. The season begins after the Rabi crops have been harvested.

Crops: Zaid crops primarily consist of quick-growing and short-duration crops, especially vegetables. Common Zaid crops include cucumber, watermelon, muskmelon, pumpkin, bitter gourd, and other vegetables. Some fodder crops may also be cultivated during this season.

Water Management: Irrigation plays a crucial role in Zaid farming because the summer months in India are often characterized by high temperatures and lower rainfall. Farmers rely on irrigation systems, including wells, tube wells, and canals, to provide the necessary water for crop growth.

Geographic Distribution: Zaid crops are grown in regions where the climate and water availability are suitable for summer cultivation. These areas may include parts of North India, Western India, and other regions with access to water sources.

Crop Rotation: Zaid crops are often part of a crop rotation strategy, allowing farmers to make the most of the available growing seasons and diversify their agricultural activities.

Importance: Zaid crops contribute to the overall agricultural productivity and income of farmers. They provide an opportunity for additional income during the summer months when certain crops can be cultivated successfully.

While Zaid crops are not as predominant as Kharif and Rabi crops in terms of overall agricultural production, they play a vital role in the agricultural calendar by allowing farmers to make productive use of the summer season. Additionally, the cultivation of Zaid crops can help meet the demand for specific vegetables and fruits during this period.

Agriculture

Agriculture is a method of production of food, fodder, cash crops such as Fiber, and raising plants and animals (Livestock). Agriculture employs more than 50% of the national population directly or indirectly.

Agriculture provides 25% of the national income.

Factors Influencing Agriculture

Relief, Climate, and Soil, Institutional factors such as the size of farms, land tenure, and land reforms, Technological factors such as HYV (High Yielding a Variety of seeds), artificial or chemical insecticides, pesticides, and fertilizers and Infrastructure factors such as Irrigation, credit, market insurance, storage facilities, Power, and Transport.

References

  • https://ncert.nic.in/ncerts/l/jess104.pdf

Downloads

1. Agricultural pattern in india Pdf

* * All the Notes in this blog, are referred from Tamil Nadu State Board Books and Samacheer Kalvi Books. Kindly check with the original Tamil Nadu state board books and Ncert Books.