Geological history and diversity in phyiogegarphical aspects of our nation has resulted in the arise of diverse riverine systems in our subcontinent.
The source of water and their draining area has been the chief factor for diverse characteristc the riverse sysytems.
Himalayan rivers are perenial rivers as they drain through out the year by getting water from rainfall in rain season and melting of glaciers in summer.The catchment area of the northern river systems are extensive.They form wide ,large fertile plains along their course.Their swift movement and velocity enabling them to erode large quantities of sediments and forming plains by their depositional.Steep gorges formed by their erosional activities has been harnessing to generate Hydo power.The ever growing feature of the Himalayas has making them youth ful and active.In lower course they are useful for water transport.Due to existemce level palins inceasent ,intensive rain fall often results in floods.
The Deccan Plateau is located between the Western Ghats and the Eastern Ghats mountain ranges in India.
The Himalayan mountain range acts as a physical barrier that separates the Deccan Plateau and Tibet. Its rugged terrain and high altitude make it difficult for people to easily cross over, limiting contact and interactions between these two regions.
The other name for the southern plateau is the Deccan Plateau.
The Deccan Plateau is located in the continent of Asia. It covers a large area in southern India.
The Northern Plain is a low-lying region formed by the depositional activity of rivers like the Ganges and Indus, characterized by fertile alluvial soil. The Peninsular Plateau is an elevated region made up of hard igneous and metamorphic rocks, with plateaus and hills like the Deccan Plateau. The Northern Plain is flatter and more agriculturally productive, while the Peninsular Plateau is older, more rugged, and mineral-rich.
Rivers which rise from Himalayas contain water throughout the year due to melting snow of Himalayas, whereas rivers of Deccan plateau contain water only during rainy season.
Deccan Plateau, the Himalayan Mountain System and the Northern Plains.
the plateau in southern India is called the Deccan Plateau. It is located between the Eastern and Western Ghats, surrounded bye the Bay of Bengal and the Arabian Sea.
Deccan plateau is a plateau formed very early in terms of history of Indian geography in volcanic movement while Malabar coast lies along side west of Deccan plateau. Also Deccan plateau is a triangle formed by western ghat, eastern ghat and Satpura range. while Malabar is just coastal area lying west of western ghat.
The Deccan Plateau is located between the Western Ghats and the Eastern Ghats mountain ranges in India.
The Deccan Plateau
The Himalayan mountain range acts as a physical barrier that separates the Deccan Plateau and Tibet. Its rugged terrain and high altitude make it difficult for people to easily cross over, limiting contact and interactions between these two regions.
The other name for the southern plateau is the Deccan Plateau.
The Deccan Plateau is a triangular in shape.
Deccan Plateau
No. The Deccan Plateau is a large flat plateau region located in central India.
deccan plateau is located in soutern India