Which form of erosion results from rain splash?

Splash erosion specifically refers to the detachment and movement of soil particles caused by the impact of falling raindrops. When raindrops strike the soil surface, they create a force that can dislodge small particles of soil, which then gets scattered or transported a short distance. This process is particularly prevalent in areas where the surface is bare and unprotected by vegetation.

Other forms of erosion, such as rill, sheet, and gully erosion, involve different mechanisms of soil movement. Rill erosion occurs when water gathers in small channels and flows, increasing the water's eroding power. Sheet erosion refers to the uniform removal of thin layers of soil over a larger area, often due to the flowing water across a slope. Gully erosion occurs in larger, more established channels where significant water flow can lead to deeper, more extensive erosion.

Therefore, understanding the mechanics and contexts of each type of erosion highlights why splash erosion is distinctly characterized by the immediate impact of raindrops on the soil.