Laserfiche WebLink
West Elk Mine 2011 Annual Hydrology Report <br />27 <br />3.2.1 Springs above the F -Seam in the North Fork Drainage Basin <br />3.2.1.1 Spring 24 -3 <br />Spring 24 -3 is located in the West Flatiron drainage that is the first tributary <br />entering Raven Gulch from the west, which is tributary to the North Fork of the Gunnison <br />and east of the West Flatiron B -seam longwall panels (Map 2). This spring issues from a <br />sandstone bed above the F -Seam, flows seasonally, and is typically dry or nearly dry in <br />the late summer and fall months. Monitoring at this spring began in 1998. <br />3.2.1.2 Springs E -13 -1, E -13 -2, E -13 -3, E -13 -4 <br />Springs E -13 -1, E -13 -2, E -13 -3, and E -13 -4 are located in the lower West Flatiron <br />drainage that is the first tributary entering Raven Gulch from the west, which is tributary <br />to the North Fork of the Gunnison and east of the West Flatiron B -seam longwall panels <br />(Map 2). These springs issue from sandstone beds above the F -seam, flow seasonally, <br />and are typically dry or nearly dry in the late summer and fall months. These springs <br />have been monitored since 2001. <br />3.2.1.3 Spring 26 -1 <br />Spring 26 -1 is located in a drainage on the west side of Deep Creek between the <br />Upper and Lower Deep Creek monitoring stations (Map 2). Deep Creek is tributary to <br />Raven Gulch and the North Fork. This spring is located above the east side of longwall <br />panel 15 (Box Canyon B -seam longwall panel area) and issues from a sandstone bed <br />above the F -seam. This spring has perennial flow, but shows strong seasonal variations <br />with high flows in the spring months. Monitoring at this spring began in 1996. <br />3.2.1.4 Seep E14 -1 <br />Seep E14 -1 is located in upper Box Canyon which is tributary to the North Fork. <br />It is located above the Box Canyon B -seam longwall panel area (Map 2). This seep <br />issues from a sandstone bed above the E -seam and has not flowed through the period of <br />record. It is damp only during very wet spring months, but is typically dry. Monitoring <br />at this seep began in 1998. This seep was permanently covered by drill -pad construction <br />in WY 2006 and is no longer being monitored. <br />June 2012 HydroGeo, Inc. <br />