Deposition in depressions formed by random roughness and in furrows between ridges is local deposition.
	The deposition occurs very near to the location where the detachment occurred.
	The area of deposition is comparable to the area of detachment.
	The deposition is widespread over the entire slope rather than being concentrated in relatively small downslope areas.
	The detachment computed by RUSLE2 is actually the net of local detachment and local deposition.  That is, RUSLE2 does not explicitly compute local deposition, but RUSLE2 explicitly computes remote deposition.
	Oriented roughness, such as ridging, may also cause local deposition.