Anai Mudi, the highest peak, is 2, m above sea level. The highest point of Eastern Ghats is Mahendragiri m. Deccan Plateau is a triangle-shaped plateau that encompasses the majority of areas of peninsular India. This is an example of extrusive igneous rock.
The general horizontality of the strata shows that this area has not undergone any major disturbance. Deccan Traps The northwestern part of the plateau is made up of lava flows or igneous rocks known as the Deccan Traps.
This plateau has isolated hills. The region is uneven with general elevation varying from m to 1, m.
Its western extremity is known as the Rajpipla Hills and the easternmost part as the Amarkantak Plateau and in between as the Mahadev Hills. Narmada-Tapti are the exceptions which flow from east to west in a rift rift is caused by divergent boundary Go back to Interaction of plates.
The Anaimalai throws off two branches viz. The Deccan is rich in minerals. Major mineral ores seen in this area are iron ore and mica in the Chhota Nagpur plateau and gold, diamond, and other precious metals in the Golconda area in Andhra Pradesh.
This gap was formed by down-faulting normal fault: A large portion of Deccan Plateau consists of volcanic rocks basalt. Chhattisgarh Plain The Chhattisgarh plain is the only plain worth the name in the Peninsular plateau. The Urdu dialect spoken in this region is also known as Dakhini or as Deccani, named after the region itself.
Rivers have further subdivided this plateau into a number of smaller plateaus. The entire plateau is divided into Ghats and the Peneplains a vast featureless, undulating plain which the last stage of deposition process.
The horizontal lava sheets have led to the formation of typical Deccan Trap topography [step like]. The southern tributaries of the Ganga River and Yamuna River drain the plateau.
Towards the north-west it is lined by the Aravallis. This composition is continental in origin meaning it is the primary composition of the continental crust.
It rises to m in the south but dips to m in the north. Its general slope is from west to east which is indicated by the flow of its major rivers. Geography of Great Indian Peninsular Plateau Malwa Plateau is drained to the north and is formed by horizontally bedded sandstones and limestones that were laid down during the earlier Gondwana period.
Meghalaya Plateau The peninsular plateau extends further east beyond the Rajmahal hills to from Meghalaya or the Shillong plateau.
The Malnad in Kannada means hill country. As the volcanoes became dormant, they left over an area of tablelands with characteristically huge expanses of plains similar to a table. It is triangular in shape and is bounded by the Satpura and the Vindhya in the north-west, the Mahadev and the Maikal in the north, the Western Ghats in the west and the Eastern Ghats in the east.
During the Gondwana period, when drainage of the neighbouring area flowed into these basins, deposited clays and sandstones and turned them into swamps.
At places it is interruped by monadnocks an isolated hill or ridge of erosion-resistant rock rising above a peneplain. In its southern part the Abu Hills contain its highest peak, the Guru Sikhar m.
It also includes the upper courses of the Sindh, the Ken and the Betwa. Several layers of volcanic eruptions that occurred for thousands of years resulted in the formation of Deccan Trap.
Basalt is similar in composition to mantle rocksindicating that it came from the mantle and did not mix with continental rocks. The principal language of the northwestern segment of the Deccan Plateau in the Maharashtra state is Marathi, which is a type of an Indo-Aryan language.
Northeastern parts of the Deccan are in the state of Odisha. This is named as the Malwa Plateau.
The Deccan Plateau is dissevered from the Gangetic Basin towards the north by the Vindhya and Satpura Mountain Ranges, which create its northern border. Here are found the Gondwana coal fields which provide bulk of coal in India.
Shillong 1, m is the highest point of the plateau. Rain falls during the monsoon season from about June to October.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.
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 ultimedescente.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.
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. 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.Download