How was the Ganges basin formed?

Question

Need Detailed answers. Plz give the actual history of the formation ,not just the features.

Answer 1

Ganges, most important river of the Indian subcontinent. The Ganges flows 2,510 km (1,560 mi) from the Himalayas of north central India southeast through Bangladesh and into the Bay of Bengal. Named for the Hindu goddess Ganga, the river draws from a basin of 1 million sq km (400,000 sq mi), one of the world’s most fertile and densely populated regions.

II Course of the River

Print this section
The Ganges is formed by the junction of two headstreams, the Bhagirathi and the Alaknanda, in the Himalayas of India’s Uttaranchal state. The commonly acknowledged source of the Ganges is the Bhagirathi, which originates in an ice cave at an elevation of 4,000 m (13,000 ft) and is the smaller of the two headstreams. The Alaknanda rises below the peak Nanda Devi (7,817 m/25,646 ft) near the Tibetan border. Fed by melting snow and ice from glaciers such as Gangotri and from peaks such as Nanda Devi and Kāmet (7,756 m/25,446 ft), the two streams flow southward through the Middle Himalayas toward their point of convergence.

After traveling more than 200 km (125 mi), the Ganges reaches the city of Haridwār (altitude 310 m/1,020 ft), where it breaks through the low Siwālik Range and begins its generally southeasterly flow across the Gangetic Plain. At Haridwār a dam diverts water to the Upper Ganges Canal. Between Haridwār and Allahābād, a distance of nearly 800 km (500 mi), the river follows a winding course made unnavigable by shoals and rapids. At Allahābād, the Ganges is joined by the Yamuna River from the southwest, then flows east past the cities of Mirzāpur, Vārānasi, Patna, and Bhāgalpur near the Bangladesh border. In this portion of the river, the Ganges also receives the Son River from the south and the Gumti, Ghāghra, Gandak, and Kosi rivers from the north.

Past Bhāgalpur, the river skirts the Rājmahal Hills on the border of Bangladesh. Here, bending south, lies the head of the Ganges delta, roughly 900 km (560 mi) downstream from Allahābād and about 450 km (280 mi) short of the Bay of Bengal. Near Pākaur, India, the river branches. The subsidiary branch, the Bhagirathi, winds south to form the Hugli River (Hooghly), the westernmost branch of the delta as well as its principal channel of navigation. Oceangoing vessels may navigate the Hugli from its mouth on the Bay of Bengal to the port city of Kolkata, about 130 km (80 mi) upstream. Since the mid-1970s India has diverted water into the silted Hugli, aiding transportation to Kolkata but creating disputes over water rights with Bangladesh.

Answer 2

Heh, guess some people don't read the whole question before launching in on trivia about the river...

First, here is a good reference to look up:

Holocene and modern sediment budgets for the Ganges-Brahmaputra river system; evidence...
Goodbred and Kuehl Geology.1999; 27: 559-562


The Ganges basin began its history with the formation of the Himalaya. Here is the short version answer to your question:

According to the most accepted geological theories, India once belonged to an Island continent called Gondwanaland and was separated from the Eurasian continent by the primordial Tethyan ocean. One billion years ago, the Aravallis, whose eroded remnants are visible around Delhi, formed a chain higher than the Himalayas today. Over millions of years these mountains suffered the forces of erosion and their sediments were deposited in the Tethyan ocean. Then 140 million years ago, India began it's northward movement, on a collision course with the Eurasian continent.

The point where the two continents were joined is known, appropriately, as the Indus- Yarlung Suture zone, marked by the courses of these two greatest rivers of the Kailash. After 60 million years, the Indian and Asian plates became closely welded along this suture zone. The northward movement of India continued but at a slower rate - 2-3 centimeters per year.

And what birth pangs.... as a result of the collision itself, and the related contraction of the Tethyan ocean, all the rocks of this area, from the mountains of then northern India to the oceanic crust, and the deep sea sediments of the Jurassic and Cretaceous ages, joined in the formation of the Himalayas.

This then is the result of those ancient events ..... each layer tells the story of the play of millions of years of brute force by nature.

The Himalayas as we see them today went through some distinct epochs of uplift. First came the Trans. Himalaya. South of this is the high Himalayan region, where the range reaches it's highest points. Here we find old crystalline rock, the oldest core material in the entire Himalayas, almost 2 billion years old, the bottom layers of the compacted Tethyan sediments. This is known as the main central thrust.

As the Himalayas rose the forces of erosion kept pace, leading to the formation of a contiguous lower range of hills known as the Shivaliks. Made of erosion material from the still rising Himalayas, their sediments reflect the history of the up thrust of the emergent Himalayas. Numerous fossil finds allow the Shivaliks to be dated with accuracy and provide evidence of the comparative youth of the Himalayas.

In the second phase of upheaval, further uplift of the central axis took place. It was now that the great peaks of the Garhwal himalaya..Nanda devi etc achieved their present eminences. In this period, intrusions of young granites, known as leucogranites because of their whitish colour, took place in the highest peaks.. such as the Bhagirathi sisters and Shivling.

The last up thrust affected not only the Himalayas, Transhimalaya and the Karakorum, but also the whole of the Tibetan region. With an area of 2.5 million square kilometers, this region is the highest land mass on earth and in the last 1 million years it has risen by nearly 5,000 meters, an average of 4-5 millimeters per year.

The uplift continues even today at a measurable 10 meters every hundred years. Mount Everest has itself risen 8.2 meters in the last 100 years.

Very little is known about the start, duration and extent of the Ice ages in the Himalayas. Geologists have however determined that the second last was the most severe. The period after this major ice age saw a marked retreat of the glaciers and this was also the period that most Himalayan lakes came into being, amidst the ice polished rock landscape. The Pangong and the Chandratal are classic examples of such glacial remnants.

Large lakes were also formed as rising rivers were blocked by the emergent ranges. As the rising Pir panjal blocked the Jhelum it turned, what we know as The Vale of Kashmir, into a lake. This primeaval lake, called the Karewa, drained, and from it's sediments, pieces of primitive tools have been recovered - our only evidence of a pre ice- age culture in the Himalayas.

All the major rivers of the Himalayas have their source in the holy Kailash region. The Indus to the north, the Yarlung -Brahmaputra in the east, the Sutluj in the west and the Ganga, Karnali streams to the south and southwest. This amazing situation, making Mt. Kailash the literal lynchpin of the Himalaya, is the result of a 30 million year old upthrust of the Kailash range at a time when the Himalayas were in the slow, initial phase of their formation.

Two of these great rivers, the Indus and the Yarlung-Brahmaputra, were forced to flow along the lines of the suture zone in an east west direction, only penetrating the range at it's eastern and western extremities.

To further confound matters, this penetration takes place at points of highest uplift, Nanga Parbat in the west and Namche Barwa in the east. The cutting action of the other rivers kept pace with the rising Himalaya and they come right through the range at some of the highest points.

In the East, the Yarlung Tsangpo parallels the Himalaya till it comes to the great axial bend at Namche Barwa. Then, cutting one of the deepest gorges on earth, three times as deep as the Grand canyon, it enters the plains of Assam.

The sources of all major Himalayan rivers lie, therefore, on the north side of the great range and besides the Kailash group, include most larger Himalayan rivers.

These rivers are the principal architects of the Himalayan landscape and each river system has created it's own unique geomorphology. The Indus and it's tributaries like the Zanskar and the Suru in the transhimalaya. It's major Himalayan tributaries which are river systems in their own right ... the Chenab, Ravi, Beas and the Sutlej. Further east the Garwhal himalaya is the domain of the Ganga and it's feeder streams while the Teesta drains the Sikkimese himalaya. Beyond, in Arunachal is the true lower catchement of the great Brahmaputra river system.

The gradual rise of the Himalaya took place in a series of long, curvilinear, parallel folds, and in this stupendous upthrust of the earth's crust, was created a mountain range that contains all the worlds mountains over 7,000 meters in height, and constitutes the line of demarcation between two of the world's great faunal realms - the Oriental to the south and the Palearctic to the north. Here we find compressed into a few tens of kilometers, the most abrupt environmental changes in the terrestrial world.

Geographically the range has been traditionally divided into :-
The Punjab Himalaya....... consisting of the catchement basins of the Indus, Jhelum, Chenab, Ravi, Beas and Sutluj.

The Garhwal Himalaya ...... consisting of the catchement basins of the the Yamuna and the Ganga.

Quaternary (began about 2 million years ago and extends to the present) sediments, deposited mainly by the ganges, brahmaputra (jamuna) and meghna rivers and their numerous distributaries, cover about three-quarters of Bangladesh. The physiography and the drainage pattern of the vast alluvial plains in the central, northern and western regions have gone under considerable alterations in recent times. The deposition of Quaternary sediments was influenced and controlled by structural activities. The eastward shift of the Ganges and tista as well as the significant westward shift of the Brahmaputra during the last 200 years gives evidence of epeirogenic movements even in recent days. Hillocks and hills are confined to a narrow strip along the southern spur of the shillong plateau, to the eastern and southern portions of the Sylhet district, and to the chittagong hill tracts (CHT) in the southeast of the country bordering upon the Indian states of Tripura and Mizoram and Myanmar.

Okay...that's it in a nutshell...there is soooooooo much more to know about this topic...combine this with the information above andyou have a more complete picture.

Good luck