The sediments removed from the outer bank are carried forward by the flow of the water to the inner bank and deposited.
•Deposition occurs because the friction between the inner bank and the water is greater than at the outer bank, thus reducing its velocity.
•With successive deposition, the water at the inner bank gets shallower, resulting in a slip-off slope.
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thalweg >>> depositon >> inner bend
Rock that piles up at the foot of a cliff is a formed regolith slope.
Rock that forms at the foot of a cliff forms regolith slope.
A bumpy, rough surface so you don't slip.
Talus slopes are broken rocks formed by gravity and the convergent boundary. Ex: Devils Lake Gorge.