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<br />N'1 OONTENTS <br /> PagF <br />FIGURE 6. Contributions to mean annual run-off of the Green River at <br /> Little Valley ----------------------------------------- 8 <br />7. Typical regimen of the Price and San Rafael Rivers--------- 91 <br />8. Green River Lakes reservoir site-------------------------- 102 <br />9. New Fork Lake reservoir site---------------------------- 103 <br />10. Willow Lake reservoir site-------------------------------- 104 <br />11. Fremont Lake reservoir site------------------------------ 105 <br />12. Half Moon Lake reservoir site---------------------------- 106 <br />13. Burnt Lake reservoir site--------------------------------- 107 <br />14. Boulder Lake reservoir site------------------------------- 103 <br />15. Upper Bear reservoir site-------------------------------- 118 <br />16. Upper Bear dam site------------------------------------ 119 <br />17. Starvation dam site------------------------------------- 140 <br />18. Superior Lake reservoir site------------------------------ 142 <br />19. Five Point Lake reservoir site---------------------------- 143 <br />20. Scanner reservoir site ------------------------------------ <br />-------------- <br />------------------- - - <br />146 <br />21. Whiterocks Lake reservoir site---------------------------- 149 <br />22. Paradise Park reservoir site------------------------------ 150 <br />23. Lower Joes Valley reservoir site--------------------------- 157 <br />24. Map of Green River Basin in Wyoming showing principal <br /> irrigation projects------------------------------------- 174 <br />25. Red Canyon dam site---------------------------------- 238 <br />26. Swallow Canyon dam site------------------------- ---- 239 <br />27. Echo Park dam site------------------------------------- 242 <br />28. Rock Creek dam site------------------------------------ 244 <br />29. Rattlesnake dam site ------------------------------------ 246 <br />- -- - Y <br /> <br />PREFACE <br />By NATHAN C. GROVER ' <br />The Green River and its drainage basin are interesting economically, <br />historically, and scenically. The river constitutes one of the great <br />natural resources of Wyoming, Colorado, and Utah. It has had an <br />influence on the exploration, settlement, and development of the <br />Vest and is woven into the history of the white man's progress <br />throughout a broad region. Its canyons are grand and beautiful <br />but unfortunately are so difficult to traverse that tbev have been <br />seen by relatively few people. <br />The Green River is the largest tributary of the Colorado and brings <br />to that river nearly one-half of the water flowing in the stretch just be- <br />low the junction. The mean annual run-off of the Green from a drain- <br />age area of nearly 45,000 square miles is about 5,700,000 acre-feet; the <br />mean annual run-off from a drainage area of 26,500 square miles of the <br />Colorado above the Green is about 6,800,000 acre-feet. Although <br />its drainage basin is more than 70 per cent greater than that of -the <br />Colorado above the junction, the run-off of the Green is somewhat <br />smaller because of the relatively low precipitation on much of the <br />basin. It is far larger,than any other tributary of the Colorado, the <br />next in size being the San Juan, which has a mean annual run-off of <br />somewhat more than 2,500,000 acre-feet. <br />The drainage basin of the Green, situated in Wyoming, Colorado, <br />and Utah, ranges in altitude from more than 15,000 feet in the summits <br />of the mountains to about 3,900 feet in the valley at its mouth: - The <br />average annual precipitation on the basin ranges from perhaps 50 <br />inches or more near the summits of the high mountains to 6 inches or <br />less in -the southernLvalleys.- The -run-off from -tributaries-ranges <br />from perhaps 30 inches or more in depth in the high mountain areas <br />to a small fraction of an inch in the driest valleys. <br />Within the basin of the Green are mountain valleys that have <br />excefent stands of timber, broad fertile valleys that are irrigated in <br />part, excellent range lands for :stock and vast areas of mountains <br />and valleys that are essenti .v of desert character..:Within i't.,also <br />are large deposits of phosphate rock, extensive coal fields which yield <br />valuable-bitumunovs coals add yi.st.azeas-of oil $hat? Qil ede <br />that may have eonsiderAle fut i? j portance may yet-be d'iseovered <br />? Chie(hyd.B?s erb?,:n?r, U. S Oeclegfml 9tmeY, ., _.