Laserfiche WebLink
Draft West Elk Mine 2005 Annual Hydrology Report 17 <br />3.2.2.2 Spring 1 D-1 <br />Spring 10-1 is located on the east side of lower Box Canyon. It is located north of the Box Canyon <br />Panels and issues from alluvium on slopes tributary to the North Fork. Flow is seasonal and it is <br />typically dry in late summer. <br />3.2.2.3 Sprin Eg 10-2 <br />Spring E10-2 is located on a hillside east of an unnamed drainage tributary to the North Fork <br />between Sylvester Gulch and Box Canyon. This spring is in landslide material below a fractured <br />sandstone cliff. It is located north of the Box Canyon Panels. Flow has not been observed during <br />the past 3 years. <br />3.2.2.4 Wiring IS-1 <br />Spring 15-1 is located on the west side of an unnamed drainage tributary to North Fork between <br />Sylvester Gulch and Box Canyon. This spring is located north of the Box Canyon Panels. The <br />spring issues from alluvium and water is present only during peak flow months. <br />3.2.2.5 Spring_G-Ia <br />• Spring G-la is located in Sylvester Gulch on the west side of the drainage, north of the Box <br />Canyon Panel area. It issues from alluvium and is seasonal with moisture present only during <br />periods of snow melt or peak flow. <br />3.2.2,6 Spring G-10 <br />Spring G-20 is in middle Sylvester Gulch on the east side of the drainage. It is located north of the <br />Box Canyon Panels and east of the mine facilities. It issues from alluvium or landslide material <br />and disperses water through a grassy area. <br />3.2.3 Springs above the B Seam in the Jumbo Mountain Area in the <br />North Fork Drainage Basin <br />3.2.3.1 Sprin Cg R-12 <br />Spring CR-12 (decreed spring #12) is located in Lone Pine Gulch north of the NW mine panels. It <br />issues from alluvium on the south side of the gulch. This is a perennial spring, but the volume of <br />flow diminishes in summer and autumn. <br />_~ <br />September 2006 HydroGeo, Inc. <br />