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• 2.04.7 <br />They are characterized by steep to nearly vertical canyon walls. All four <br />gulches have well developed colluvial deposits within their streambeds. <br />From south to north the gulches are known as 1) Freeman Gulch; 2) Sheep <br />Corral Gulch; 3) Dove Gulch; and 4) Iron Point Gulch. Freeman Gulch is <br />typically dry with only one flow event noted in monitoring results from June <br />1995 through November 1997 and that was in June 1997 during a significant <br />precipitation event. <br />Lower Sheep Corral Gulch and Lower Dove Gulch are also expected to be <br />typically dry with flow occurring during spring snowmelt and after significant <br />precipitation events. They were noted as dry during the late 1997 field <br />reconnaissance and during all 1998 monitoring events. <br />Iron point gulch is an intermittent stream. Following are flow measurements <br />taken through March 1999. <br />• <br />Downstream Iron Point Gulch <br />Date 10/97 6/98 7/98 9/98 11 /98 3/99 <br />Flow cfs 1.0 2.4 0.2 D D D <br />Terror Creek is a perennial stream which drains approximately 29 square <br />miles (18,560 acres). The dendritic drainage pattern of tributary streams <br />may be modified in part by geologic structures fracture zones or faults. <br />Peak stream flows for the East and West Forics of Terror Creek occur during <br />spring snowmelt and heavy rainstorm events. Discharges from Terror Creek <br />Reservoir enhance continued stream flow from May-June through <br />September-October. <br />Diversions for agricultural uses are withdrawn through Terror Creek Ditch <br />from Terror Creek from May through October. <br />There are four unnamed, generally east to west flowing, ephemeral gulches <br />which are tributary to Terror Creek within the permit and adjacent area. <br />These gulches are expected to be typically dry with flow occurring during <br />spring snowmelt and after significant precipitation events. On the <br />PR-03 2.04 - 33 - 5/99 <br />