Western ghat and eastern meet at a point

Eastern and Western Ghats of India UPSC; Eastern and Western Ghats Facts

western ghat and eastern meet at a point

India&#;s Western Ghats and Eastern Ghats meet at the: Cardamom Hills Annamala Hills Secondary School · Social sciences; 13 points They meet at nilgiri omarcafini.info it helps plz mark my answer brainlist answer. The Eastern Ghats are a discontinuous range of mountains along India's eastern coast. The Deccan Plateau lies to the west of the range, between the Eastern Ghats and Western Ghats. The coastal . The Eastern Ghats are the source points for many small and medium rivers along the east coastal plains of South India. Eastern and Western Ghats of India UPSC; Eastern and Western Ghats Facts; difference Eastern Ghats and Western Ghats meeting point.

Situated between Narmada and Tapi River. Starting from Rajpipla hills in the west through Mahadeo hill to Maikal range. Extending in east west direction, are all spurs of Western Ghats forming local watersheds.

Kalsubai 1,m the highest peak of Western Ghat forming local watersheds. Kalsubai m Runs along the western coastal plain from the south of valley of Tapi to Kanya Kumari, the southernmost point of mainland India.

Region which receives maximum rainfall and is covered with evergreen forest The Western Ghats meet with Eastern Ghats in the Nilgiri hills. Acts as a main watershed of Peninsular Rivers. Doda Betta 2,m is the highest peak of Nilgiri Hills.

western ghat and eastern meet at a point

Formed of gneisses and schists. Runs along the eastern coast of India from northern Orissa to the Nilgiri Hills. Characterised by unbroken hills between Mahanadi and Godavari. Mahendragiri is the highest peak of Eastern Ghats. Nallamalli Hills is situated between Krishna and Penneru Rivers. Western Ghats runs parallel to the western coast in a north-south direction from the Tapi River to Kanayakumari.

But Eastern Ghats runs in a north-east to south-west direction parallel to the eastern coast from Orissa to the Nilgiri hills.

western ghat and eastern meet at a point

Western Ghats is source of many large rivers which flow in the Peninsular India. But no big river originates from the Eastern Ghats.

Prelims Answer Key with Explanations

Western Ghats is almost perpendicular to the south-west monsoons coming from the Arabian Sea and causes heavy rainfall in the west coastal plain.

But Eastern Ghats is almost parallel to the monsoons coming from the Bay of Bengal and does not cause much rainfall.

western ghat and eastern meet at a point

Western Ghats continuous and can be crossed through passes only. But Eastern Ghats has been divided into several parts by large rivers. Western Ghats average elevation is to 1, meters above sea-level.

The Eastern and Western Ghats meet in the -

But the average elevation of Eastern Ghats is about metres above sea level. Eastern coastal plains lie along India's east coast and is washed by the Bay of Bengal. Western Coastal Plains, on the other hand, are washed by the Arabian Sea.

WCP are sometimes so narrow that Western Ghats touch the sea water. There are waterfalls in remote areas, such as the Kiliyur Falls. Its northern boundaries are marked by the flat Palnadu basin, while in the south it merges with the Tirupati hills.

An extremely old system, the hills have been extensively weathered and eroded over the years. The Palar River cuts through the ranges. The Velikonda Range eventually descends to the coastal plain in northern Nellore districtwhile the Nallamalla Range in Kurnool continues to the River Krishna.

The Kondapalli Hills are a range of low hills which lie between the Krishna and the Godavari rivers. The Krishna River bisects these hills of the Eastern Ghats. The main hill range starts from Nandigrama to Vijayawada known as Kondapalli. Madhurawada Dome in the Eastern Ghats mobile belt is formed by a tectonic arrangement with the khondalite suite and quartz Archean rocks along the Eastern Ghats north of Visakhapatnam. The region covers about three-fourths of the entire Odisha state.

Geologically it is a part of the Indian Peninsula which was a part of the ancient land mass of Gondwanaland. The major rivers of Odisha with their tributaries have cut deep and narrow valleys.

The Garhjat Range is a northeastern prolongation of the eastern Ghats which rises abruptly and steeply in the east and slopes gently to a dissected plateau in the west running from north-west Mayurbhanj to south-west Malkangiri.