Which feature forms on the inside of a meander as a result of slow moving water and deposition?

Which feature forms on the inside of a meander as a result of slow moving water and deposition?

• A. Alluvium
• B. Air Pressure
• C. Source
• D. Slip Off Slope

Answer: (D)

When a river meanders, the flow is faster on the outside of each bend and slower on the inside. That slowdown means the river loses enough energy to carry sediments, so material settles out along the inner bank. Over time this deposited sediment builds up a gentle slope—the slip-off slope—on the inside of the bend. It marks where the inner-bank deposits accumulate as the river migrates. The other options aren’t named landforms created by this specific inside-bend deposition: alluvium is the sediment itself rather than a particular feature, air pressure isn’t involved in shaping river meanders, and a source isn’t relevant to this coastal or fluvial process.

When a river meanders, the flow is faster on the outside of each bend and slower on the inside. That slowdown means the river loses enough energy to carry sediments, so material settles out along the inner bank. Over time this deposited sediment builds up a gentle slope—the slip-off slope—on the inside of the bend. It marks where the inner-bank deposits accumulate as the river migrates. The other options aren’t named landforms created by this specific inside-bend deposition: alluvium is the sediment itself rather than a particular feature, air pressure isn’t involved in shaping river meanders, and a source isn’t relevant to this coastal or fluvial process.