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The North Fork of the Gunnison River drains an area of approximately 526 square miles. The average annual yield of the North Fork of the Gunnison River from October 1993 to September 1994 was approximately 330,500 acre-feet. The quantity and quality of this river is influenced significantly by agricultural and municipal uses. Near Somerset, Colorado, the water in the North Fork of the Gunnison River is acalcium-bicarbonate type, and total dissolved solids concentrations range from approximately 100 milligrams per liter (mg/1) to approximately 400 mg/l. Tenor Creek is a perennial stream which drains approximately 29 squaze miles, and Hubbard Creek is a perennial stream which drains approximately 35 squaze miles. Freeman Gulch is a significant drainage which is tributary to Hubbazd Creek. Freeman Gulch exhibited flow during the snowmelt period of Spring 1995, and may be considered an intermittent stream. Stephans Draw is also an intermittent stream, and Stockpond P-1 is located along Stephans Draw. The drainages of A-Gulch, B-Gulch, C-Gulch, D-Gulch, Sheep Corral Gulch and a portion of Dove Gulch probably exhibit ephemeral flow regimes. A portion of Dove Gulch can be considered perennial. There aze twelve (12) stock ponds located in the permit and adjacent azeas. These include Pond P-1, mentioned above, and all of the ponds aze manmade. The ponds collect spring season runoff, and any available seep water. Groundwater in the area is located within the alluvial deposits along the North Fork of the Gunnison River and Hubbazd and Terror Creeks, within the steep sloped colluvial deposits found within some of the drainages, in perched water zones located within the lenticulaz sandstones of the Mesa Verde formation and in the Rollins Sandstone. The Rollins Sandstone is a recognized aquifer in the azea. The groundwater associated with the alluvial deposits of the North Fork of the Gurmison River has been developed for domestic and agricultural uses. The localized groundwater resources associated with the alluvial deposits of Hubbazd and Tenor Creeks aze not significantly developed. The groundwater associated with local colluvial deposits is rechazged by snowmelt, and the water dischazges through local intermittent springs and seeps. Most of this colluvial water is lost due to evaporation. Bedrock groundwater is not abundant in the permit azea. The groundwaters of the locally perched bedrock water zones and of the Rollins Sandstone are not significantly developed in the permit and surrounding area, due to relatively poor water quality and low potential quantity yields. The general bedrock groundwater flow direction in the sandstone strata of the Mesaverde formation is from the rechazge azea near the outcrop of these strata, north towazd the lower parts of the basin. Climatological Information - Detailed climate information is presented in Section 2.04.8 of the Bowie No. 2 Mine permit application document, and the information is summarized below. The neazest weather station to 14