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• Alluvial Valfev Floor /nvesiigmiort ... .......... ` ::::..::.::::::'::::::: :::':.:..: ;.:.::::::.:. f:QRENCl'I'Q: G:4NYON 3VIIN)~: ::: ' .:: '.:.:'- . 1996-ItIJAGH.MAPEING:IN:hORENGITt3 ;AND:G~t~ CANYbNS:: ...':: 7/15/96 - Location 3/30/96 4/24/96 5/23/96 7/17/96 8/l9/96 9/l7/96 10/9/96 Lorencito Canyon between LC~4 and SPACE X X X X X X X SPACE and LC-3 X X X X LC-3 to Pl/P2 X X X X X X Bozcu[ P1/P2 Bozcutto X X X X X Little Pine Puerteci[o and Leff X X X X Jeff and the X X X X Purgatoire River Alamosa Canyon X Cow Canyon Cow near Windmill X X WMCWC-2 Cow below CWC-I X X X X X LC-1 has exhibited flow more than any other site, but was dry in March and June. Flows ranged from an unmeasurable seep to 2.25 cubic feet per second (cfs). LC-2 and LC-3 were dry from January through April and again in June. Flows ranged from an unmeasurable seep to 0.75 cfs at LC-2 and from an unmeasurable seep to 0.06 cfs at LC-3. LCD was dry m January, February, April, May and June. Flows ranged from an unmeasurable seep to 0.35 cfs. There are no stock ponds in Lorencito Canyon itself, but there aze several within many of the side canyons, as noted below. The reach mapping suggests that flow in Lorencito appears to be intermittent, with water recharging the channel substrate during periods of low saturation and discharging to shallower areas of unconsolidated materials. However, the stream appears to constantly recharge the unconsolidated deposits at the specific monitoring sites established in Lorencito Canyon. AC-1 is located on Alamosa Canyon approximately a half a mile above the confluence with Lorencito Canyon. There are no stock ponds within the permit area in Alamosa Canyon. It was • dry from January through May and again in July and October. Flows ranged from an unmeasurable seep to 0.46 cfs. Flow in Alamosa Canyon appears to be intermittent, with water Avf.d75\Decemlxr l3, 1996 g