Well, honey, as you travel downstream, the bedload size decreases because the heavier, larger particles settle out first closer to the source. And as for the roundness increase, well, that's just nature's way of giving those rocks a nice little spa treatment as they bump and grind their way downstream, getting smoother and rounder with each mile. So, in a nutshell, it's all about physics and erosion doing their thang as the river does its own version of a rock makeover.
The river stage characterized by slow-flowing water, very shallow depths, and banks with low gentle slopes is known as the "bedload" or "meandering" stage. In this stage, sediment is often deposited, leading to the formation of sandbars and islands. The gentle gradient allows for the river to meander, creating wide curves and bends. This stage is typically found in the lower reaches of a river or in floodplains.
V-shaped valleys The river channel - vertical erosion, shallow but a very fast flow Waterfalls Gorges(which are formed by waterfalls) Bedload is also very big and angular.
Banks of coarse river load and other material that has been transported down river, that are made when the river floods and bedload is carried out wider then before and desposited. It is left with the river recedes creating a higher banks
winky
The size of the pebble will decrease down stream because the further downstream you go the quicker the river velocity. This means there will be more abrasion against the sides and bed of the river and the friction will be greater, this wears away the river load making it decrease in size. Increase velocity means that bigger material will be picked up by the river and carried as river load. More load in the river and increased size of load will mean more attrition and the river load will keep colliding into each other smoothening and rounding their shape. Brap brap !!
As bedload sediment moves downstream, its size typically decreases due to abrasion and weathering, leading to smaller particles being transported. Additionally, the shape of the sediment tends to become more rounded as angular particles collide with each other and the riverbed, smoothing their surfaces. This process results in a gradual sorting of sediment, with coarser material often found upstream and finer material downstream. Overall, the downstream transport leads to a more uniform sediment composition.
Faster river velocities are capable of carrying greater amounts of bedload and transporting them farther and faster. The shape of the sediments of the bedload would therefore be exposed to more physical weathering which would progressively round the sediments and also decrease their size.
waste transported from the river!
You cannot:)
bedload
a bedload
Angular bedload consists of coarse sediment particles, such as gravel and cobbles, that are transported along a riverbed by rolling or sliding. These particles have angular shapes due to their solid and hard composition, which makes them more resistant to abrasion compared to more rounded particles. Angular bedload contributes to the erosion and sediment transport processes in rivers.
The bedload becomes smaller when the river is flowing downstream, and the rocks also become smaller, smoother and rounder due to attrition and abrasion. (The reason the flow slows down is because the energy of the flow decreases.)
River efficiency is how easily a river can move water, sediment and bedload.
M. A. Carson has written: 'Bedload transport in gravel channels'