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WSPC06489
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Last modified
1/26/2010 12:06:14 PM
Creation date
10/9/2006 5:54:47 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
7630.125
Description
Wild and Scenic - Colorado Wilderness Act - 1991
State
CO
Basin
Statewide
Date
12/19/1991
Author
Unknown
Title
Instream Flow Needs Assessment and Recommended Instream Flow Claim for the Proposed Piedra Wilderness - Final Draft
Water Supply Pro - Doc Type
Report/Study
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<br />,10i18 /1 <br /> <br />DRAFT <br /> <br />FINAL DRAFT - 1:!/20l9t <br /> <br />Streamflow is lowest during me wimer and C.lrly spring. It begins to increase due to snow <br />melt runoff sometime between the end of ~Iarch and the middle of ~1ay. The higher flo.....s <br />associated with snow melt persist for one and a half to two and a half months and there are <br />typically several peaks during this period. See Figure C. This is due to combinations of one <br />or more factors. such as precipitation events, shan-term changes in temperature, or the <br />individual characteristics of the suh-watersheds. such as slope. aspect. and elevation. There <br />Me aLsu 100t~ summer ;md lall p~k5 ~su..:jat..:J \101m fronul .illl.1lhunJer ~tufms. Allhuubh tho: <br />IT!.1:;::nit1ldl" nflh~"e ]~I" ~l":~<:"" ["t':A<: v",ri,..:. ;,nd j" "<:IJ311~'lm~-'..~ lh",n Ih..",.. "(;<;P:;'I~,i \\;I!, <br />snow mdt. the)' do occur every year. <br /> <br />AnnualllydrOltf".pb .1938 <br />Pitdr. Riv~ .t UpfM"f" lAild~~ Boundary <br />Sum orPit"dra Riv~. Wrlllinu(ht and \\illi.m.~ Crr-t"-' <br /> <br />:: I <br />'''''' <br />3' I <br />~ 12w ~ <br />~ I <br />j 1~)] r <br />f ~! <br /> <br />, ~ <br />'" - ~ - s. - ~ - ~ ~ % - " <br />" ;; ;;; ;;; ;;; ;;; '" ~ <br />~ ~ <br /> <br /> <br />~ ~ ~ ~ ~ ~ - ~ ~ - <br />S:;-~::7S~S%~~~~ <br /> <br />Figure C <br /> <br />A typical riparian site along the river corridor contains mountain alder, red-osier, several <br />species of willow, and horsetail. Coyote and Bebb are the most common species of willow. <br />The narrow valley bottom and steep canyon sideslopes prevent the riparian vegetation from <br />occurring too far from the stream channel edges. Therefore, the riparian lone is typically <br />lhree to ten feet wide. Alder, red"sier, and willow occupy a broad band adjacent to the active <br />channel. lndividual uees and small stands of narrowleaf cottonwood are scattered along the <br />mainstem of the Piedra and along the uibutaries near the mainstem; most are located on low <br />terraces. Cottonwood is not considered a major component of the plant community at these <br />sites, Riparian species, especially willow, will colonize deposition areas behind debris dams <br />and gravel bars. Although the location of these areas will shift over a several year period, <br />their acreage within the wilderness is probably relatively constant. There are two sites within <br />the wilderness near the upper boundary where narrowleaf cottonwood is a major component of <br />the plant community. At these sites, the valley bottom is wider and has both floodplains and <br />low terraces which are occupied by cottonwood. <br /> <br />Page 6 <br />
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