Streambank erosion
Streambank erosion is the removal of material from the bank usually during high flows. Bed and bank scouring removes support and leads to the toppling in of the bank. This normally occurs when flood waters are receding, and the bank material is saturated, heavy and loses the support of the river. Water velocity along the streambank can also shear off large blocks.
Rill erosion
Rills are closely spaced channels resulting from the uneven removal of surface soil by running water. Rills are <60cm deep and <30cm wide and commonly occur on cultivated slopes where they normally erode down to the base of the cultivated layer. They are occasionally observed on slopes with established pasture cover. In general, the potential for rill erosion increases with slope angle.
Gully erosion
Gullies are formed by the removal of soil, subsoil or rock by water. They are large, permanent features >60cm deep and >30cm wide that initially form when water is channelled and the sides and head of the channel begin to erode. The channel normally only carries water during rainstorms.
Tunnel gully erosion
Tunnel gully erosion is initiated by the subsurface concentration and flow of water resulting in scouring and the formation of narrow conduits, tunnels or pipes underground. As softer material is eroded away the tunnel collapses and can be visible as either holes in the ground or continuous open channel.