Pasword is anaskirk
they kill them self by cuting thair poo
i dont knowwho caresshut upSince this post has such an idiotic answer, I'll explain it. During flooding the force of the current cuts across narrow bends, making the river shift to the new channel. Sometimes obstructions in a river will cause the current to divert and cut a new channel in a different direction around the obstruction. Rivers have also been know to change course because of earthquakes, as did the Mississippi River in 1811 (New Madrid earthquake).
Of course not. It is a physical change. A chemical change occurs when the identity of a substance changes.
Energy is lost along a river's course through friction with the riverbed and banks, as well as through turbulence and drag caused by obstacles like rocks and vegetation. Energy can also be lost through heat transfer to the surrounding environment. Overall, these factors contribute to the gradual decrease in the river's flow velocity and energy as it travels downstream.
Sedimentary rocks are typically found in layers along the sides of rivers and at the mouth of rivers. One very famous place where sedimentary rocks are most prevalent, more than metamorphic and igneous rocks the two other types of rocks, the Grand Canyon in Arizona. These rocks are associated with the vivid red rock layers seen throughout the canyon and took millions of years to form.
In geography, traction refers to the process of large rocks and boulders being rolled along the riverbed by flowing water. This action occurs in rivers where the water flow is strong enough to move and transport these larger particles. Traction is one of the processes involved in the transportation of sediment in rivers.
Having rocks scattered along a valley floor typically indicates past geological processes such as erosion, glaciation, or rock falls. These rocks may have been transported by glaciers or rivers and left behind as the landscape evolved. The distribution of rocks can provide insights into the history and formation of the valley.
Mechanical weathering, like wind, water, and other forms of erosion. Now, rain and some rivers contain diluted rocks and can change rocks.
Other rocks or minerals can also abrade rocks. For example, the movement of glaciers can cause rocks to scrape against each other, leading to abrasion. Additionally, the force of flowing water in rivers or waves along coastlines can help to abrade rocks.
The two primary sources of sediment for beaches are rivers and coastal erosion. Rivers transport sediments from the land and deposit them along the coast, while coastal erosion breaks down rocks and cliffs along the shoreline, contributing sediment to the beach.
The load of rocks and soil picked up by rivers is transported downstream through erosion and sedimentation. Along the way, the rocks and soil can be deposited as sediment, contributing to the formation of riverbanks, deltas, and floodplains. This process plays a critical role in shaping the landscape and maintaining the health of river ecosystems.
From rocks in rivers and lakes and when the rocks break up over time the sediments inside the rocks go into the rivers and lakes and overtime into the water supply.