Laserfiche WebLink
<br />A"A <br />~",;t. <br />(\~l' <br /> <br />L") <br />L'- <br />C\J <br />CJ <br />,~ <br />C:' <br /> <br />" <br /> <br />~: <br /> <br />~ <br />~ <br />f <br /> <br />2~ <br />h. <br /> <br />" <br /> <br />, <br /> <br />in the valley, accompanied the Committee and rendered invaluablo <br /> <br />assistance through his intimate kncwledge of the irrigation and <br /> <br />drainage systems. <br /> <br />On the night of Feb~~ary 15, the Committee returned to <br /> <br />Denver ,\here it has since continued a study of the proj ect. <br /> <br />GENEIU\.L DESCPJ:PTION <br /> <br />A clear comprehension of topographic, irrigation and drain- <br /> <br />age conditions in San Luis Valley and the functions of the proposed <br /> <br />San Luis Valley Drain is essential in the following discussion in <br /> <br />which every effort has been made to concentrate only on those natur- <br /> <br />al features bearing directly on the project. <br /> <br />San Luis Valley is located in south-central Colorado and <br /> <br />north-central New Gexico. The valley extends almost due north <br /> <br />ffild south 150 miles and is 50 miles wide at its vddest point. The <br /> <br />lower end of the vall6'J narrows down arcd extends about 15 miles into <br /> <br />Nev. Mexico. North of the Colorado-New Mexico state line the valley <br /> <br />is divided diagonally by the San Luis hills extending from Antonito <br /> <br />to Fort Garland. <br /> <br />The northern part of the valley, with \'hi ch this report is <br /> <br />chiefly concerned, is a remarkably large, broad-bottomed basin lying <br /> <br />west of the Sangre de Cristo Range and north of the tovm of Alamosa. <br /> <br />On casual inspection, the entire valley seems to slope very <br /> <br />gently and drain into the Rio Grande, which enters the basin almost <br /> <br />due west of Alamosa and turns south at the city toward the New Mexico <br /> <br />line. However, as a matter of fact, an imperceptible low divide <br /> <br />in the valley floor parallels the north side of the Rio Grande, at a <br /> <br />2 <br /> <br /> <br />