- Location
- The Himalayan Mountains
- The Northern Plains
- The Peninsular Plateau
- The Indian Desert
- The Coastal Plains
- The Islands
Location
India has all major physical features of the Earth, i.e., mountains, plains, deserts, plateaus, and islands.
In India, the soil colour varies from place to place as it is formed from different types of rocks.
India has varied physical features whose formation can be explained on the basis of the ‘Theory of Plate Tectonics’.
According to the theory of Plate Tectonics, the seven major and minor plates that form the Earth’s crust keep moving, causing stress and thus leading to folding, faulting and volcanic activity.
The physical features of India can be grouped under the following physiographic divisions:
- The Himalayan Mountains or the Northern Mountains
- The Northern Plains or the Indo-Gangetic Plains
- The Peninsular Plateau
- The Great Indian Desert
- The Coastal Plains
- The Islands
The Himalayan Mountains
The Himalayas are young-fold mountains which are the loftiest and one of the most rugged mountain barriers of the world.
The Himalayas are 2400 km long, 400 km to 150 km wide from Kashmir to Arunachal Pradesh respectively.
Himalayan mountains are stretched over the northern borders of India. These mountain ranges run in a west-east direction from the Indus to the Brahmaputra. The Himalaya consists of 3 parallel ranges in its longitudinal extent.
- The northern-most range is known as the Great or Inner Himalayas or the Himadri. It is the most continuous range consisting of the loftiest peaks with an average height of 6,000 metres.
- The folds of the Great Himalayas are asymmetrical in nature. The core of this part of Himalayas is composed of granite.
- The range lying to the south of the Himadri forms the most rugged mountain system and is known as Himachal or lesser Himalaya.
- Pir Panjal range forms the longest and the most important range.
- The outermost range of the Himalayas is called the Shiwaliks. These ranges are composed of unconsolidated sediments.
- The longitudinal valley lying between lesser Himalaya and the Shiwaliks are known as Duns. DehraDun, Kotli Dun and Patli Dun are some of the well-known Duns.
The Himalayas have also been divided on the basis of regions from west to east.
- 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 Teesta rivers divide the Nepal Himalayas and the part lying between Teesta and Dihang rivers is known as Assam Himalayas.
- The Brahmaputra marks the eastern-most boundary of the Himalayas.
- Beyond the Dihang gorge, the Himalayas bend sharply to the south and spread along the eastern boundary of India, which is known as the Purvachal or the Eastern hills and mountains. The Purvachal comprises the Patkai hills, the Naga hills, the Manipur hills and the Mizo hills.
The Himalayas have three parallel ranges in the longitudinal extent namely :
- Great or Inner Himalayas also called Himadri.
- Middle Himalayas or Himachal.
- Outer Himalayas or Shiwaliks.
The Himalayas can be divided into four sections :
- Punjab Himalayas – between Indus and Satluj.
- Kumaon Himalayas – between Satluj and Kali.
- Nepal Himalayas – between Kali and the Tista.
- Assam Himalayas (Eastern Himalayas) – Between Tista and the Dibang (Tsangpo).
The Northern Plains
The Northern Plains spread over an area of 7 lakh sq. km, 240 km long and 240 km to 320 km broad.
The rivers that flow to the plains from the mountains are involved in depositional work.
The difference in relief causes the Northern Plains to have four regions.
- Bhabar – Adjacent to the foothills of Shiwaliks, a narrow 8 to 16 km wide belt of pebbles and boulders.
- Bangar – Older alluvial plain which rises above the level of the flood plains.
- Khadar – Newer and younger alluvial of the flood plains deposited by the rivers flowing down the plain.
- Tarai – Lies adjacent to Bhabar region, composed of newer alluvium and is thickly forested.
The Peninsular Plateau
The Peninsular Plateau is the tableland formed due to the breaking and drifting of the Gondwanaland.
The plateau consists of two broad divisions, namely, the Central Highlands and the Deccan Plateau.
The eastward extensions of Peninsular Plateau are locally known as Bundelkhand and Baghelkhand. The Chhota Nagpur Plateau marks the further eastward extension drained by the Damodar river.
The Deccan Plateau, a triangular mass, lies to the south of the river Narmada.
The western and eastern edges of the Deccan Plateau are marked by the Western Ghats and the Eastern Ghats respectively.
The Western Ghats are higher than the Eastern Ghats.
The Malwa Plateau is spread across Rajasthan, Madhya Pradesh and Gujarat and slopes towards the
north.
A distinct feature of the peninsular plateau is the black soil area known as Deccan Trap.
The Indian Desert
The undulating sandy plain covered with sand dunes towards the western margins of the Aravalli Hills is the Indian Desert.
Crescent-shaped dunes called barchans cover large parts of the Indian Desert.
Luni is the only large river that flouts in this region.
The Coastal Plains
The narrow’ coastal strips flank the Peninsular Plateau.
On the west, the coastal strips are divided into Konkan (Mumbai-Goa), Kannada Plain and the Malabar Coast from northern to the southern part.
On the east the coastal strip is divided into Northern Circar and the Coromandel Coast from northern to southern part.
The Islands
The Lakshadweep Islands group in the Arabian Sea is close to Kerala.
The Andaman and Nicobar Islands are the two island groups. Andaman Island consists of 204 small islands. India’s only active volcano, Barren Island is situated here.