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and non-alluvial material. This headcutting is expected to initiate some natural <br />gullying on the aide slopes adjacent to the channels as the base level of the elopes <br />is lowered. The cuts probably move head ward in the spring during snowmelt runoff. <br />The scars left by the advancement are naturally revegetated as the year progresses. <br />Therefore, as concluded earlier, the erosion is not excessive enough to be causing <br />management problems. <br /> <br /> <br />2-454j <br />f~fISED FEB 13 '87 <br />