Soil Creep is the term used to describe the very slow downhill movement of soil and regolith.

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Soil creep is indeed the term used to describe the very slow downhill movement of soil and regolith, which is typically caused by gravity and repeated expansion and contraction due to freeze-thaw cycles. This process can lead to the gradual tilting of trees and buildings, as well as the formation of terracettes and other landforms.

Soil Creep Is the Term Used to Describe the Very