A river's slope, volume of flow, and the shape of its streambed all affect how fast the river flows and how much sediment it can erode.
How deep it is and how fast it is going downhill that can also affect it
Factors that affect a river's ability to erode and carry sediment include velocity of the water flow, volume of water, slope of the riverbed, geology of the surrounding area, and the presence of vegetation or obstructions along the river's path. High velocity and volume of water, steep slopes, soft rock formations, and minimal vegetation can increase erosion and sediment transport capacity.
In a meander, a river erodes sediment on the outer bank of the bend, where the water flows faster and exerts greater force on the bank. Conversely, sediment is deposited on the inner bank of the bend, where the water flows more slowly, allowing particles to settle. This process creates a distinctive pattern of erosion and deposition that shapes the river's channel over time.
A delta.
A "Delta".
As the slope of a river decreases, its ability to erode the land beneath it also diminishes. This is because a gentler slope results in lower water velocity, reducing the river's energy and capacity to transport sediment and erode the riverbed. Consequently, sediment deposition may increase, leading to a more stable river channel. Overall, lower slopes tend to promote sediment accumulation rather than erosion.
The river flows into a lake
water erodes a canyon by carrying sediment from the rock walls down the river
True. When a river flows over a flat surface like a plateau, the water may carry sediment and erode the land, shaping the terrain over time. This erosion is a natural process that can create valleys and canyons.
The water flows over a water fall
When a river flows into a lake or ocean, the sediments that the river carries settle to the bottom. Layers of sediment may covor the dead organism.
the three factors that affect how fast a river flows is the steep ,width and depth and how it is curved