Soil creep occurs on almost every soil-covered slope.

Name: Soil creep occurs on almost every soil-covered slope.
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Soil creep is a common form of slow mass wasting that occurs on slopes composed of soil or weathered rock fragments. It is typically driven by gravity and results in the gradual downhill movement of soil particles, often causing visible soil displacement and formation of terracettes. Therefore, it can be observed on almost every soil-covered slope.

Soil Creep Occurs on Almost Every Soil-Covered Slope