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Was (wer) ist gully erosion - definition
![Gullied landscape in [[Somalia]].](https://commons.wikimedia.org/wiki/Special:FilePath/SomaliaLuftaufnahme1993.jpg?width=200 "Gullied landscape in [[Somalia]].")
![A gully in [[Saratov Oblast]], [[Russia]].](https://commons.wikimedia.org/wiki/Special:FilePath/A gully (Budanova Gora) 1.jpg?width=200 "A gully in [[Saratov Oblast]], [[Russia]].")
 3.jpg?width=200 "Inside the gully (to the left) in Saratov Oblast, Russia.")
![''Voçoroca'' (Portuguese for gully) in [[Avaré]], [[Brasil]]](https://commons.wikimedia.org/wiki/Special:FilePath/Voçoroca (23 12 24S - 48 47 59W) - REFON 3.JPG?width=200 "''Voçoroca'' (Portuguese for gully) in [[Avaré]], [[Brasil]]")
![Gully formed from volcanic sedimentation in [[West Java]], [[Indonesia]]](https://commons.wikimedia.org/wiki/Special:FilePath/Montane Savannah Landscape in West Java.png?width=200 "Gully formed from volcanic sedimentation in [[West Java]], [[Indonesia]]")
Wikipedia
A gully is a landform created by running water, mass movement, or commonly a combination of both eroding sharply into soil or other relatively erodible material, typically on a hillside or in river floodplains or terraces. Gullies resemble large ditches or small valleys, but are metres to tens of metres in depth and width and are characterised by a distinct 'headscarp' or 'headwall' and progress by headward (i.e. upstream) erosion. Gullies are commonly related to intermittent or ephemeral water flow usually associated with localised intense or protracted rainfall events, or snowmelt. Gullies can be formed and accelerated by cultivation practices on hillslopes (often gentle gradient) in farmland, and they can develop rapidly in rangelands from existing natural erosion forms subject to vegetative cover removal and livestock activity.
