No: That is where deposition occurs. Erosion is where the river is flowing at its fastest, the mountain torrent stage.
Lateral or horizontal erosion means erosion taken place on the sides of a footpath or river bank. The opposite if lateral/horizontal erosion is vertical erosion, where erosion is taken place under the river bed or the bottom of a footpath.
The sides of the canyon would always be crumbling into it, but as that would mean it was getting wider, it wouldn't fill up, just get more level. But presumably there's a stream/river at the bottom which caused the canyon in the first place and this is likely to continue the erosion.
Rejuvenation in a stream involves the deepening of the stream channel by erosion of the stream bed. This erosion can occur due to changes in tectonic uplift, climate, or land use that increase the stream's energy and ability to erode its bed and banks.
the site is where you place your settlement. for example, it could be at the bottom of a hill with a forest and a stream nearby
Erosion is formed when wind, water, or ice gradually wears away the surface of rocks and soil. This process occurs over a long period of time, as the movement of these elements breaks down and transports particles from one place to another, shaping the landscape. Human activities like deforestation or construction can also contribute to erosion by disrupting natural processes.
That's something you'll have to ask your piercer. Enamel erosion usually occurs behind your bottom front teeth so maybe if those are really out of place, you could be at higher risk of enamel erosion.
Because erosion only takes place on land
Erosion causes them to be moved from one place to another place.
The crust is the only place erosion takes place, primarily on the land surfaces.
i thinkflow of data from one place to other place is called a stream...
Erosion is the wearing away of landscape by different agents such as water,wind etc.So erosion takes place rapidly in a place where these agents act actively on material.
Jet streams are fast-flowing, narrow, meandering air currents found in the upper atmosphere, typically around 9-12 km above the Earth's surface, near the tropopause. They are predominantly located in the mid-latitude regions of the Northern and Southern Hemispheres.