Laserfiche WebLink
<br />I <br /> <br />ooo's:Si <br /> <br />I <br /> <br />I <br /> <br />with the Gunnison River at Delta. <br /> <br />West of the Uncompahgre <br /> <br />RivEtr a series of nearly level stream terraces separated by <br /> <br />I <br /> <br />small valleys 50 to 100 feet deep have been carved by Uncom- <br /> <br />I <br /> <br />pahgre <br /> <br />River <br /> <br />tributaries <br /> <br />as they traverse the area in a <br /> <br />northeasterly <br /> <br />direction. <br /> <br />These terraces or mesas are pre- <br /> <br />I <br /> <br />dominantly stream deposits of varying ages and are remnants <br /> <br />of a once large outwash plain. <br /> <br />Three distinct terrace levels <br /> <br />I <br /> <br />are <br /> <br />evident including the present flood plain or lower <br /> <br />ter- <br /> <br />races <br /> <br />about 5 to 10 feet above the river. <br /> <br />The higher <br /> <br />ter- <br /> <br />I <br /> <br />races <br /> <br />are, <br /> <br />for the most part, <br /> <br />west of and about 300 <br /> <br />feet <br /> <br />!I <br /> <br />above <br /> <br />the river while the middle terraces are only about <br /> <br />50 <br /> <br />feet above the stream. <br /> <br />The area east of the river is undula- <br /> <br />I <br /> <br />ting to rolling and is formed by the irregular erosion sur- <br />1 <br />face of the underlying Mancos Formation. <br /> <br />I <br /> <br />I <br /> <br />The <br /> <br />surface formations <br /> <br />in the San Juan Mountains and <br /> <br />Uncompahgre Valley are composed of both igneous and sedimen- <br /> <br />I <br /> <br />tary rock, <br /> <br />with the igneous material predominating in the <br /> <br />I <br /> <br />mountains and the sedimentary in the valley. <br /> <br />In the Uncom- <br /> <br />I <br /> <br />pahgre Valley there are significant volumes of gravelly <br />2 <br />material which were deposited by glacial melt-waters. <br /> <br />II <br /> <br />I <br /> <br />E-5 <br /> <br />I <br /> <br />I I <br />