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LESSON -2 Physical Features of India


India is a vast country with varied landforms. Our country has practically all major physical features of the earth i.e. mountains, plains, deserts, plateaus and islands. India is a large landmass formed during different geological periods which has influenced her relief. Besides geological formations, a number of processes such as weathering, erosion and deposition have created and modified the relief its present form. INTRODUCTION


. CAUSES OF PLATE MOVEMENT The movement of the plates results in the building up of stresses within the plates and the continental rocks above, leading to folding, faulting and volcanic activity

Broadly, these plate movements are classified into three types. :

. Broadly, these plate movements are classified into three types. While some plates come towards each other and form convergent boundary.


DIVERGENT BOUNDARY . Some plates move away from each other and form divergent boundary


TRANSFORM BOUNDARY In the event of two plates coming together they may either collide and crumble, or one may slide under the other. At times, they may also move horizontally past each other and form transform boundary.


The movement of these plates have changed the position and size of the continents over millions of years. Such movements have also influenced the evolution of the present landform features relief of India PLATE MOVEMENT

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The oldest landmass, (the Peninsula part), was a part of the Gondwana land. The Gondwanaland included India, Australia, South Africa and South America as one single land mass. The convectional currents split the crust into a number of pieces, thus leading to the drifting of the Indo-Australian plate after being separated from the Gondwana land, towards north. The northward drift resulted in the collision of the plate with the much larger Eurasian Plate. Due to this collision, the sedimentary rocks which were accumulated in the geosynclines known as the Tethys were folded to form the mountain system of western Asia and Himalaya. The Himalayan uplift out of the Tethys sea and subsidence of the northern flank of the peninsular plateau resulted in the formation of a large basin. In due course of time this depression, gradually got filled with deposition of sediments by the rivers flowing from the mountains in the north and the peninsular plateau in the south


A flat land of extensive alluvial deposits led to the formation of the northern plains of India. The land of India displays great physical variation. Geologically, the Peninsular Plateau constitutes one of the ancient landmasses on the earth’s surface. It was supposed to be one of the most stable land blocks. The Himalayas and the Northern Plains are the most recent landforms. From the view point of geology, Himalayan mountains form an unstable zone. The whole mountain system of Himalaya represents a very youthful topography with high peaks, deep valleys and fast flowing rivers. The northern plains are formed of alluvial deposits. The peninsular plateau is composed of igneous and metamorphic rocks with gently rising hills and wide valleys. CONCLUSION

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The physical features of India can be grouped under the following physiographic divisions :- (i) The Himalayan Mountains (ii) The Northern Plains (iii) The Peninsular Plateau (iv) The Indian Desert (v) The Coastal Plains (vi) The Islands

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The Himalayas, geologically young and structurally fold mountains stretch over the northern borders of India. These mountain ranges run in a west-east direction from the Indus to the Brahmaputra. The Himalayas represent the loftiest and one of the most rugged mountain barriers of the world. They form an arc, which covers a distance of about 2,400 Km . Their width varies from 400 Km in Kashmir to 150 Km in Arunachal Pradesh. The altitudinal variations are greater in the eastern half than those in the western half. The Himalayan Mountains

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The Himalaya consists of three parallel ranges in its longitudinal extent.

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THE GREATER OR INNER HIMALAYA It is the most continuous range consisting of the loftiest peaks with an average height of 6,000 metres . It contains all the prominent Himalayan peaks like – Mt. Everest (8,848m) in Nepal and Kanchenjunga(8,598) Sikkim in India. The folds of Great Himalayas are asymmetrical in nature. The core of this part of Himalayas is composed of granite. It is perennially snow bound , and a number of glaciers descend from this range.

Himachal or lesser Himalaya:

Himachal or lesser Himalaya The ranges are mainly composed of highly compressed and altered rocks. The altitude varies between 3,700 and 4,500 metres and the average width is of 50 Km. While the Pir Panjal range forms the longest and the most important range, the Dhaula Dhar and the Mahabharat ranges are also prominent ones. This range consists of the famous valley of Kashmir , the Kangra and Kullu Valley in Himachal Pradesh. This region is well known for its hill stations


THE SHIWALIKS They extend over a width of 10-50 Km and have an altitude varying between 900 and 1100 metres. These ranges are composed of unconsolidated material such as mud, silt and soft rocks and is prone to earthquakes and Landslides. Some narrow valleys are found between Shiwaliks and Himachal. They are called duns. For example Dehradun

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The part of Himalayas lying between Indus and Satluj has been traditionally known as Punjab Himalaya but it is also known regionally as Kashmir and Himachal Himalaya from west to east respectively The part of the Himalayas lying between Satluj and Kali rivers is known as Kumaon Himalayas . The Kali and Tista rivers demarcate the Nepal Himalayas and The part lying between Tista and Dihang rivers is known as Assam Himalayas .The are made up of Patkai, Naga and Mizo hills. The Himalayas have been divided on the basis of regions from west to east. These divisions have been demarcated by river valleys.

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Some Highest Peaks of the Himalayas

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The Northern Plain The northern plain has been formed by the interplay of the three major river systems, namely– the Indus, the Ganga and the Brahmaputra along with their tributaries. This plain is formed of alluvial soil . The deposition of alluvium in a vast basin lying at the foothills of the Himalaya over millions of years, formed this fertile plain. It spreads over an area of 7 lakh sq. km . The plain being about 2400 Km long and 240 to 320 Km broad , is a densely populated physiographic division. With a rich soil cover combined with adequate water supply and favourable climate it is agriculturally a very productive part of India


Punjab Plains. Formed by the Indus and its tributaries, the larger part of this plain lies in Pakistan. The Indus and its tributaries–the Jhelum, the Chenab, the Ravi, the Beas and the Satluj originate in the Himalaya. This section of the plain is dominated by the doabs. The Ganga plain The extends between Ghaggar and Teesta rivers. It is spread over the states of North India, Haryana, Delhi, U.P., Bihar, partly Jharkhand and West Bengal to its East, particularly in Assam lies the Brahmaputra plain. THE NORTHERN PLAIN

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. The rivers, after descending from the mountains deposit pebbles in a narrow belt of about 8 to 16 km in width lying parallel to the slopes of the Shiwaliks. It is known as bhabar. All the streams disappear in this bhabar belt. South of this belt, the streams and rivers re-emerge and create a wet, swampy and marshy region known as terai The largest part of the northern plain is formed of older alluvium. They lie above the flood plains of the rivers and present a terrace like feature. This part is known as bhangar . The soil in this region The soil in this region contains calcareous deposites locally known as kankar. The newer, younger deposits of the flood plains are called khadar . They are renewed almost every year and so are fertile, thus, ideal for intensive agriculture. According to the variations in relief features

The Peninsular plateau:

The Peninsular plateau The Peninsular plateau is a tableland composed of the old crystalline, igneous and metamorphic rocks. It was formed due to the breaking and drifting of the Gondwana land. The plateau has broad and shallow valleys and rounded hills .

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Central Highlands Deccan Plateau Deccan Plateau Deccan Plateau The Central Highlands The Deccan Plateau

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The Central Highlands The Deccan Plateau The part of the Peninsular plateau lying to the north of the Narmada river covering a major area of the Malwa plateau is known as the Central Highlands. The Vindhyan range is bounded by the Central Highlands on the south and the Aravalis on the northwest. The further westward extension gradually merges with the sandy and rocky desert of Rajasthan. The flow of the rivers draining this region, namely the Chambal , the Sind, the Betwa and Ken is from southwest to northeast. The Deccan Plateau is a triangular landmass that lies to the south of the river Narmada . The Satpura range flanks its broad base in the north while the Mahadev, the Kaimur hills and the Maikal range form its eastern extensions. The Deccan Plateau is higher in the west and slopes gently eastwards. An extension of the Plateau is also visible in the northeast– locally known as the Meghalaya and Karbi-Anglong Plateau . It is separated by a fault from the Chotanagpur Plateau. Three Prominent hill ranges from the west to east are the Garo, the Khasi and the Jaintia Hills.

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The Western Ghats T he Eastern Ghats Western Ghats lie parallel to the western coast. They are continuous and can be crossed through passes only. The Western Ghats are higher than the Eastern Ghats. Their average elevation is 900– 1600 metres The Eastern Ghats stretch from the Mahanadi Valley to the Nigiris in the south. The Eastern Ghats are discontinuous and irregular and dissected by rivers draining into he Bay of Bengal. Their average elevation is 600 metres

The Indian Desert :

The Indian Desert The Indian desert lies towards the western margins of the Aravali Hills. It is an undulating sandy plain covered with sand dunes. This region receives very low rainfall below 150 mm per year. It has arid climate with low vegetation cover . Streams appear during the rainy season.

The Coastal Plains :

The Coastal Plains The northern part of the coast is called the Konkan (Mumbai – Goa), the central stretch is called the Kannad Plain while the southern stretch is referred to as the Malabar coast The plain along the Bay of Bengal are wide and level In the northern part, it is referred to as the Northern Circar , while the southern part is known as the Coromandal Coast . Large rivers such as the Mahanadi, the Godavari, the Krishna and the Kaveri have formed extensive delta on this coast. Lake Chilika is an important feature along the eastern coast

Lakshadweep Islands:

Lakshadweep Islands Lakshadweep Islands group are lying close to the Malabar coast of Kerala. This group of islands is composed of small coral islands. Earlier they were known as Laccadive, Minicoy and Amindive. In 1973 these were named as Lakshadweep. It covers small area of 32 sq km . Kavaratti island is the administrative headquarters of Lakshadweep. This island group has great diversity of flora and fauna. The Pitli island , which is uninhabited, has a bird sanctuary.

Andaman and Nicobar Islands :

Andaman and Nicobar Islands They are bigger in size and are more numerous and scattered. The entire group of islands is divided into two broad categories – The Andaman in the north and the Nicobar in the south . It is believed that these islands are an elevated portion of submarine mountains . These island groups are of great strategic importance for the country.


The northern mountains are the major sources of water and forest wealth . The northern plains are the granaries of the country. They provide the base for early civilisations. The plateau is a storehouse of minerals , which has played a crucial role in the industrialisation of the country. The coastal region and island groups provide sites for fishing and port activities. Thus, the diverse physical features of the land have immense future possibilities of development . CONCLUSION



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