Intro to Geology
Rill erosion is a type of soil erosion that occurs when small channels, or rills, form on the surface of the soil due to the concentrated flow of water. This process typically happens during heavy rainfall or rapid snowmelt when water accumulates and begins to flow over the land, cutting into the soil and creating these small, narrow grooves. Rill erosion plays a significant role in the overall erosion processes and landscape evolution by altering the topography and contributing to sediment transport.
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