A gully is a
landform created by running water, eroding sharply into soil, typically on a
hillside. Gullies resemble large ditches or small valleys, but are metres to
tens of metres in depth and width.
When the
gully formation is in process, the water flow rate can be substantial, causing
a significant deep cutting action into soil.
Hillsides
are more prone to gullying when they are cleared of vegetation, through
deforestation, over-grazing or other means.
A rill is a
shallow channel (no more than a few tens of centimetres deep) cut into soil by
the erosive action of flowing water. Similar but smaller incised channels are
known as microrills; larger incised channels are known as gullies.
Artificial
rills are channels constructed to carry a water supply from a distant water
source. In landscape or garden design, constructed rills are an aesthetic water
feature.