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horizon was mined at the Hawk's Nest Mine and at the Blue Ribbon Mine. It may be mined at the West Elk Mine and at the Bear No. 3 Mine in the future. The F horizon contains two coal seams and presently is only mined at the West Elk Mine. Coal seams of the F horizon do not exist to the north of the North Fork in thicknesses sufficient for mining. The Barren (Undifferentiated) member of the Mesaverde Formation consists of up to 1,500 feet of terrestrial sedimentary rocks. This unit consists of fine-grained, buff-colored, lenticular sandstones, gray shales and thin lenticular coal beds. The sandstones predominate and are highly lenticular, discontinuous and of limited lateral extent in outcrop (Johnson, 1948). The Mesaverde Formation is unconformably overlain by the Tertiary Age Rudy or Wasatch Formation. This formation consists of red- to buff-colored shales, red sandstones, and red to gray conglomerates. The sediments of this formation are weathered volcanic rocks. The Ohio Creek conglomerate is the basal unit within the formation and is 100 to Z00 feet thick. Tertiary igneous intrusive rocks exist within the North Fork Drainage Basin. A diorite plug about 1,000 feet in diameter outcrops along Hubbard Creek in the SE 1/4 of Section 7, T13S, R91W of the 6th P.M. This may represent the erosional remnants of a volcanic flow feeder. Sills have infected the lower Coal-Bearing member, particularly the B and C seams. These sills consist of diorite and appear to have their source to the northwest of Terror Creek. The alluvium of the North fork of the Gunnison River consists of Quaternary Age deposits of mixed coarse sand, cobbles and boulders. These coarse sediments are composed primarily of igneous and metamorphic rock types and have their source area in the headwaters and upper reaches of the North Fork. This coarse alluvium is capped by finer sands and silts. The North Fork alluvium in the area of the Hawk's Nest, Bear, West Elk and Somerset Mines is fairly narrow in width and between 50 to 70 feet thick. About a mile below the town of Somerset, Colorado, the width of alluvium increases ~dhile the thickness of alluvium decreases to about 35 feet. DESCRIPTION OF THE GROUND WATER REGIME Four categories of potential aquifers occur in the Somerset Coal field. These are: the alluvial and terrace deposits associated with the North Fork of the Gunnison River; the localized, shallow alluvium along creeks tributary to the North fork; the discontinuous, lenticular and laminar sandstones of the Mesaverde Formation; and the Rollins sandstone. The most significant occurrence of ground water in the region is associated with the alluvium of the North Fork of the Gunnison River. Significant thicknesses of alluvial sand and gravel between 30 to 80 feet exist along the North Fork. Numerous wells are developed in the alluvium with an average yield of 17.4 gpm. The Terror Creek Loadout draws 450 gpd from the alluvium of the North Fork of the Gunnison. A pump test conducted by Bear Coal Company on an alluvial well near the site of the Bear No. 3 Mine yielded a value of 806.5 g/ft/d for transmissivity and 0.2 for storativity. Three water quality analyses were conducted for the Bear No. 3 Mine on three wells completed in the North Fork alluvium. Two wells exceeded drinking water -6-