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<br />. i'': <br /> <br />1.0 INTRODUCTION--Continued <br />1. 2 study Area <br /> <br />AREA HAS EXTENSIVE ENERGY RESOURCES <br /> <br />The White River basin, located in northwestern Colorado and northeastern <br />Utah, contains extensive reserves of oil shale, coal, oil, <br />and natural gas. <br /> <br />Energy developments are taking place or are being planned in Colorado and <br />Utah. Particular attention is focused on the White River basin because of <br />extens i ve exi st i ng and planned energy-resource deve 1 opment that may affect <br />surface-water quantity and qual i ty. The Whi te Ri ver bas in is located in <br />northwestern Colorado and northeastern Utah (fig. 1.2-1). The surface area of <br />the bas in is 5,120 square mil es, 74 percent of whi ch is in Colorado and 26 <br />percent in Utah. The White River flows to the east and drains into the Green <br />River in Utah. Most of the tributaries, such as the South Fork White River, <br />Piceance Creek, and Yellow Creek, drain from the south into the White River. <br /> <br />Exi st i ng energy production from the area cons i sts pri marily of oil and <br />natura 1 gas, wi th some coal (fi g. 1. 2-2). Ri 0 Bl anco County, Co 10., con- <br />taining the Rangely oil and natural gas fields, ranks first in Colorado for <br />product i on of these two resources. Two major coa 1fi e 1 ds of the area are the <br />Dansforth Hills coalfield near Meeker, Colo., and the lower White River coal- <br />field near Rangely, Colo. The coal from these areas primarily consists of a <br />highly volatile bituminous type. <br /> <br />The most extens i ve underdeve loped natural resource in the bas in is the <br />extensive oil-shale deposits in the Green River Formation of Tertiary age. <br />The Green River Formation is. within the Piceance basin in Colorado, the Uinta <br />bas i n in Utah, and the Green Ri ver and Washaki e bas ins in Wyomi ng. Oil <br />resources in these areas are about 2 trillion barrels (Donnell, 1965). <br /> <br />6 <br />