The region is uneven with general elevation varying from m to 1, m. Situated amidst the Western Ghatswhich constitutes its western frontier, and the Eastern Ghats forming its eastern frontier, the Deccan Plateau stretches from the Vindhyas to the southern tip of the peninsula.
Eastern Ghats are not as continuous as Western Ghats and are much fragmented by river valleys. Climate[ edit ] The climate of the region varies from semi-arid in the north to tropical in most of the region with distinct wet and dry seasons. Its average elevation is m. This triangular plateau is at its broadest in the north.
The average elevation of the plateau is m above sea level. Also in certain sections of the region, we can find granitewhich is an intrusive igneous rock. It has been a stable shield which has gone through little structural changes since its formation.
The southernmost section of the plateau is irrigated by the Kaveri River, which has its source in the Western Ghats Mountain Range in Karnataka and twists to the south to penetrate the Nilgiri Mountains at Hogenakal Waterfalls into Tamil Nadu, subsequently creating the Sivasamudram Falls at the island township of Shivanasamudra, which is the second largest waterfall in India and also the 16th biggest in the world, prior to pouring into the Stanley Reservoir and the Mettur Dam that formed the reservoir.
The general trend of the hills is either parallel to the Western Ghats or across it. The Deccan Plateau is affluent with minerals.
The Western Ghats Mountain Range is quite high and stops the humidity from the southwestern monsoon from arriving at the plateau. The difference between these two rock types is: Anai Mudi, the highest peak, is 2, m above sea level.
The jungles are also comparatively arid but function to preserve the rainwaters to create torrents that supply rivers that move into valleys and subsequently into the Bay of Bengal. The Krishna River, Tungabhadra River, and the tributaries of the Krishna River, which include the Bhima River, which also flows from the west to east, irrigate the middle segment of the plateau.
It was formed from hard metamorphic and igneous rocks. Here are found the Gondwana coal fields which provide bulk of coal in India.
The Peninsular Plateau is a one of the oldest landforms of earth. The east coast is wide with deltas formed by the rivers Godavari, Mahanadi and Kaveri. The southern tributaries of the Yamuna River and Ganga River irrigate the plateau. This is named as the Malwa Plateau.
It forms the northern part of the Deccan Plateau. Basalt is produced in locations that are stretching while granite is produced primarily in locations that are having a collision.
A large portion of Deccan Plateau consists of volcanic rocks basalt. Since few hundred million years, Peninsular block has been a land area and has never been submerged beneath the sea except in a few places.
On the western edge of the plateau lie the Sahyadrithe Nilgirithe Anaimalai and the Elamalai Hills, commonly known as Western Ghats. The Deccan Plateau is densely inhabited.
Primary mineral ores found in this region are mica and iron ore in the Chhota Nagpur region, and diamondsgold and other metals in the Golconda region. Interestingly, the Hazaribagh Plateau lies to the north of the Ranchi Plateau. It is to the east of the Marwar or Mewar Upland. The Bhanrer and Kaimur are located close to the trough-axis.
Spreads over five districts of Uttar Pradesh and four districts of Madhya Pradesh. It was later filled by sediments deposited by the Ganga and Brahmaputa. Each of the two mountain ranges ascends from their particular adjacent seaward plains and almost joins at the southernmost point of India.
April Learn how and when to remove this template message The Deccan is home to many languages and people.
This plateau has been separated from the main block of the Indian Plateau by a wide stretch of alluvial lowland called the Garo-Rajmahal Gap. Average elevation of m above sea level, this area slopes down from the Vindhyan Scarp toward the Yamuna River. As it lost heat in a comparatively gradual manner, it features big observable crystals.
The plateau slopes down to Brahmaputra valley in the north and the Surma and Meghna valleys in the south.Indian Peninsular Plateau or the Deccan Plateau is a raised flat landscape that stretches to the south of the alluvial plains of the Northern India The Great Indian Peninsular Plateau, alternatively known as the Plateau of the Peninsular India, is a vast plateau, comprising most of the southern part of the country.
Aug 03, · A peninsula is a piece of land which is surrounded by water on three sides. The fourth side is attached to a larger body of mi-centre.com is a peninsula as it is surrounded by the Bay of Bengal in the East,Arabian sea in the west and the Indian Ocean in the South.
India Physiography – The Indian Peninsular Plateaus The Peninsular Plateaus Largest of India’s physical divisions – Comprises of broad & shallow valleys with rounded hills Triangular in shape; composed of the oldest rocks & Surrounded by hills Narmada – Tapi divides it into 2 parts viz.
Central highland & Deccan plateau Division of Peninsular Plateau. Peninsular Plateau of India The triangular shaped Peninsular Plateau of India extends from the south of Indo-Ganga Plain to the Cape Comorin (now Kanyakumari). This plateau is one of the oldest surfaces of the Earth and represents a.
The Peninsular Plateau The Peninsular plateau is a tableland. It is composed of the old crystalline, igneous and metamorphic rocks.
The Peninsular plateau is considered the oldest land mass as it was formed due to the drifting of the Gondwana land. The plateau consists of broad and shallow valleys and rounded hills.
The Peninsular Plateau can be broadly categorized into the Central Highlands and the Deccan Plateau. To the south of the Satpura Mountain Range, the Indian peninsula is known as the Deccan Plateau.Download