Stream beds are slowest inside the bend due to the phenomenon of centrifugal force, which causes water to flow faster along the outer edge of the bend. As the water moves around the curve, it erodes the outer bank and deposits sediment on the inner bank, where the flow velocity is lower. This reduced velocity inside the bend allows sediment to accumulate, creating a point bar. Consequently, the inner bend experiences slower water flow compared to the outer bend.
on the inside of the bend
stream channel
slowest,causes the ground to twist and bend.
A point bar is formed on the inside of a meandering stream because the water flow slows down on the inside of the bend, causing the water to deposit sediment. This deposition of sediment builds up over time, creating a point bar.
The water usually flows fastest on the outside of the bend (meander) and flows the slowest on th einside of the bend.
The part of a stream that will experience a buildup of sand and gravel is typically the inside bend of a meander, known as a point bar. As water flows around the bend, it slows down, leading to decreased energy and allowing sediment to settle and accumulate. This contrasts with the outside bend, where the current is faster and erosion occurs. Additionally, areas where the stream widens or slows down, such as floodplains, can also experience sediment deposition.
A comb can bend a stream of water through the process of electrostatics. When the comb is rubbed against a material, it acquires a static electric charge. This charge can then attract or repel the polar molecules in the water, causing the stream to bend toward the charged comb. The effect is most noticeable when the comb is brought close to the stream without touching it.
Meander.
A stream will be tend to be eroded most where the water current is the swiftest and the surrounding ground the softest. Materials carried by the water will also affect erosion. Such materials include ice, sand, and pebbles The current is swifter on the outside of a river bend. On the inside of a river bend the current may slow and erosion materials may be left in the river bed.
A curve in a stream channel is called a meander. Meanders are caused by the flow of water eroding the outside of a bend and depositing sediment on the inside, leading to a winding pattern in the channel. Meanders are a natural feature of rivers and streams and play a vital role in shaping the landscape.
lakes &rivers
a meander