A geographical overview of the indo gangetic plain

The Great Himalayas lie mostly above the line of perpetual snow and thus contain most of the Himalayan glaciers. Its eastern boundary is rather obscure and has become a controversial topic among geographers.

Inan agreement between the British Government and the State of Jind was signed to regulate the supply of water for irrigation from the Western Jumna Canal.

Indo-Gangetic Plain

It is worth mentioning here that right from the Vedic age the people of this region patronized creative and progressive art, and literature. To a limited extent, farmers have started to irrigate horticultural crops, including orchards, using hose pipes and surface irrigation methods.

As a result, the mountains are still rising, and earthquakes —often accompanied by landslides —are common. The area constitutes the land between the river Brahmaputra and Aravli mountain ranges.

Of those, the two main headstreams are the Alaknanda the longer of the twowhich rises about 30 miles 50 km north of the Himalayan peak of Nanda Devi, and the Bhagirathi, which originates at about 10, feet 3, metres above sea level in a subglacial meltwater cave at the base of the Himalayan glacier known as Gangotri.

People who came from different castes could not eat together. Stamp and later adopted by O. Please update this article to reflect recent events or newly available information.

The Southern Peninsula The Vindhya and the Satpura mountains along with Narmada and Tapti rivers form the great dividing line between northern and southern India. That deltaic area is characterized by annual flooding attributed to intense monsoon rainfall, an exceedingly gentle gradient, and an enormous discharge that the alluvium-choked rivers cannot contain within their channels.

Geographical Features of India

India constructed the dam to ameliorate the condition of Kolkata by flushing away the seawater and raising the water level. This resulted in building many cities, flourishing civilizations and powerful kingdoms to exhibit the courage and gallantry of the Indian Community.

It is composed of repeated alternations of clays, sands, and marls, with recurring layers of peat, lignite, and beds of what were once forests. With a further doubling of capacity envisaged by the end of the Eleventh Five-Year Planthe energy sector will probably contribute close to half of GDP.

Among those are the confluence of the Ganges and the Yamuna near Allahabad, where a bathing festival, or mela, is held in January and February; during the ceremony hundreds of thousands of pilgrims immerse themselves in the river.

The delta region experiences strong cyclonic storms both before the commencement of the monsoon season, from March to May, and at the end of it, from September to October.

Some rivers join the Ganga from the south also, the Son being the most important. Between those extremes the mountains fall across India, southern Tibet, Nepal, and Bhutan.

Persia controlled this region for about years until Alexander the Great invaded South Asia. About 7 percent of the total area of Bangladesh is covered with rivers and inland water bodies and the surrounding areas are routinely flooded during the monsoon. Climate The GBM river basin is unique in the world in terms of diversified climate.

This means that they have been terraced for basin irrigation. Only in the Sundarbans area of the delta are some Bengal tigers, crocodiles, and marsh deer still found.

Most of the central portion of the country experiences a cool, temperate climate year-round. The insurmountable height of the Himalayas well fortified by thick snow and impossibility to establish any land route has made the Himalayas a formidable barrier.

Seasonal canals accounted for 58 percent of the area irrigated by surface water, permanent canals for 39 percent, and ponds for 3 percent.Sep 04,  · Smoke from the fires appears to have blown all the way across North America and more than half way across the Atlantic Note: I’ve updated this.

Indo-gangetic plain is a name given to the great plain that lies to the south of the shuwalik and north of the Himalayas in the Indian peninsular. It is an Aggradational plain formed by the Alluvial deposits of Indus river, Ganges river and as well Brahmaputra river together with their tributaries.

Indo-Aryan migration models discuss scenarios around the theory of an origin from outside the Indian subcontinent of Indo-Aryan peoples, an ascribed ethnolinguistic group that spoke Indo-Aryan languages, the predominant languages of North agronumericus.coments of Indo-Aryan origin outside of the Indian subcontinent generally consider migrations into the region and Anatolia (ancient Mitanni) from.

Thus the Indo-Gangetic plain contributed a maximum share in the process of cultural awakening of India. (iii) The great Deccan Plateau: The Deccan Plateau lies in the south of Indo-Gangetic plain.

The Indo-Gangetic Plain The second great structural component of India, the Indo-Gangetic Plain (also called the North Indian Plain), lies between the Himalayas and the Deccan.

The plain occupies the Himalayan foredeep, formerly a seabed but now filled with river-borne alluvium to depths of up to 6, feet (1, metres). Ancient India is often called the Harappan Civilization because one of the ancient cities was called Harappa.

Ganges River

Harappa was just one of cities in the Indus River Valley. Another well-known city is called Mohenjo-Daro.

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A geographical overview of the indo gangetic plain
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