In hilly regions, land slides associated with earthquakes are common and many times, it blocks the flow, forcing river to carve another path or small deviation. At the same time, there can be a major alteration in the path even in plain areas and that changes the course drastically.
Rivers change in kinetic energy, water flow rates, velocity, discharge, and more as they go from start to finish. ... In order to achieve this balance rivers erode their banks, change their paths, and transport and deposit sediment along their way. Rock shelter formation by river erosion.
The rivers were rerouted 5 million years ago, probably as the ongoing collision of the Indian and Eurasian tectonic plates bulldozed the terrain, tilting it westward or lifting up river-diverting mountains.
Rivers in the upper course erode down vertically which often creates a steep channel profile in what becomes the river valley. The middle course sees a river at a slightly lower altitude than the upper course, but is still maintains a sense of trying to acquire equilibrium in flow and shape.
Initially, when a slight curve is already present in the river, water travels around the outer edge of the curve faster than the inner edge, because it's covering a greater distance in the same amount of time. As water moves faster, more of the sediment in it stays suspended, instead of settling to the bottom.
Over a period of time, rivers tend to change their course due to the rocks present at the shores. It is quite simple to understand that in plain areas, rivers will take the easiest and least resistant route. The pathway that is easier to erode and cut through will be the path for the river.
The Indus, which used to flow by Kutch's Lakhpat port, changed its course due to the tectonic movements and inched closer to Pakistan, around 125 km southeast of Karachi, flowing downwards to meet the Arabian Sea while it moved 150km northwest from the Lakhpat port.
EXPLANATION: Due to constant deposition of river sediments on the slower side and the vast amount of erosion that takes place on the faster side. This process keeps on continuing till the curves get sharpened, so that river cuts through the curve and forms another path and thus river changes its course.
0:062:56Why Do Rivers Curve? - YouTubeYouTubeStart of suggested clipEnd of suggested clipWater rushes into the newly formed hollow sweeping away loose dirt. And making the hollow evenMoreWater rushes into the newly formed hollow sweeping away loose dirt. And making the hollow even hollow er which lets the water rush a little faster. And sweep away a little more dirt.
There is also evidence of a steady shift in the course of the river since prehistoric times – it deviated westwards from flowing into the Rann of Kutch and adjoining Banni grasslands after the 1816 earthquake. Presently, Indus water flows in to the Rann of Kutch during its floods breaching flood banks.
MississippiNamed by Algonkian-speaking Indians, Mississippi can be translated as "Father of Waters." The river, the largest in North America, drains 31 states and 2 Canadian provinces, and runs 2,350 miles from its source to the Gulf of Mexico.
What geographic factors do you think encouraged the growth of civilization in the Indus River Valley? The geographic factors that helped was that there was lots of water so they could grow crops. They could also take baths, and make the land fertile.
The scientists concluded that the rivers were once Ganges tributaries that were “captured” by the Indus River. “This is the first time such a major sediment capture event has been dated,” Blusztajn said. It shows the potential “to use ancient sediments to reconstruct what mountains looked like in the past.”.
The Sutlej, Ravi, Chennab, and Jellum Rivers flow westward to join the Indus River and drain into the Arabian Sea, west of Pakistan. But the rivers once flowed eastward into the Ganges River and drained into the Bay of Bengal, east of India, the scientists say.
The fan is 6 miles (10 kilometers) thick and extends about 900 miles (1,500 kilometers) into the Arabian Sea. The scientists analyzed seismic surveys of the fan’s sedimentary layers.
Punjab means “five rivers.”. The region in northern Pakistan is named for the great rivers that branch through the landscape, creating an ancient cradle of civilization and a modern agricultural breadbasket.
Before then, the relatively high ratios of neodymium-143 to neodymium-144 in the sediments indicated that they came from the Karakoram Mountains, far north of Punjab, and were eroded from the old southern edge of the Eurasian Plate.