Laserfiche WebLink
<br />", l <br /> <br />fl <br />t- i <br />II <br /> <br /> <br />s <br /> <br />f1 <br />[I <br />1:(,j <br /> <br />Q) <br />c: <br />.....J <br />Q) <br />- <br />as <br />(j) <br />o <br />"tJ <br />as <br />.... <br />o <br />o <br />() <br /> <br /> <br />N <br /> <br />W*E <br /> <br />r~~l <br />: 1 <br /> <br />Lorna <br /> <br />~< <br /> <br />o <br /> <br />0010 <br />'~Ii <br />~e,. <br /> <br />~. <br /> <br />, <br /> <br /> <br /> <br />Brid9~" <br /> <br />r.1 <br /> <br />lJ <br /> <br />10 <br /> <br />, <br /> <br />o <br /> <br />10 <br /> <br />20 Miles <br />. <br /> <br />if] <br />~ <br /> <br />Figure 4. Location of study area in the IS-Mile Reach, Colorado River. <br /> <br />~ <br /> <br />It appears that low flows are not a factor during the non-irrigation season in the .IS- <br /> <br />mile reach. Winter (November to March) flows recorded at the Cameo gage (RM 199~9) and <br /> <br />[1 <br />l ' <br />r-, <br /> <br />in the IS-Mile Reach appear to be native Of higher due to the senior water right at the <br /> <br />Shoshone power Plant in Glenwood Canyon. Also there are some releases for power <br /> <br />L., <br /> <br />generation from Green Mountain (per comm, Karen Flogequest USBR).Flows recorded at <br /> <br />r , <br />,~ <br />U <br /> <br />Palisade are usually higher than at Cameo between November and April due to Plateau Creek <br /> <br />f1 <br />l ,j <br />I' - ~ <br />I:' '.::I <br /> <br />which joins the river at RM 193.3 (Appendix Figure 1.3). <br /> <br />9 <br />