Slow forms of mass wasting such as creep and solifluction are considered slow because they are restricted to gentle slopes and cannot achieve a high velocity.

Name: Slow forms of mass wasting such as creep and solifluction are considered slow because they are restricted to gentle slopes and cannot achieve a high velocity.
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Creep and solifluction are slow forms of mass wasting that occur on gentle slopes and have low velocities compared to faster types of mass wasting like rockfall or debris flow.

Slow Forms of Mass Wasting Such as Creep and Solifluction