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Draft West Elk Mine 2005 Annual Hy <br />3.2.1.9 <br />16 <br />• Spring G-7 is located in a western tributary to Sylvester Gulch and is south of the NE mine panel <br />azea and north of the SE panel azea. This spring issues from joints in a sandstone ledge and has <br />perennial flow, but shows strong seasonal variations with high flows in the spring months. <br />3.2.1.10~ring_G-16 <br />Spring G-16 is located in Sylvester Gulch east of the NE mine panel area. This spring issues from <br />a sandstone bed above the F Coal Seam and flows seasonally. It is typically dry in the ]ate summer <br />and fall. <br />3.2.1.11Spring G-24 <br />Spring G-24 (decreed spring #8) is located in Sylvester Gulch east of the NE mine panel area. This <br />spring issues from alluvium and is measured at the outflow of a plastic drainage pipe. It flows <br />seasonally and is typically dry in the late summer and fall. <br />3.2.1.12Saring G-14 <br />Spring G-14 (decreed spring #7) is located in Sylvester Gulch east of the NE mine panel area. This <br />. spring issues from fractures in the base of a sandstone bed. It flows seasonally and is typically dry <br />in the late summer and fall. <br />3.2.1.13Snring G=22 <br />Spring G-22 (decreed spring #3) is located in the Sylvester Gulch drainage on a hillside on the west <br />side of the drainage just south of a mine ventilation shaft and east of the NE mine panel area. It <br />issues from alluvium over a wide area and feeds a wetland on the west side of Sylvester Gulch. <br />Flow diminishes in late summer and autumn. <br />3.2.2 Springs above the B Seam in the Box Canyon Area in the North <br />Fork Drainage Basin <br />3.2.2.1 Spring 11-2 <br />Spring I I-2 is located east of Box Canyon on a hillside on the south side of the North Fork. This <br />spring is north of the Box Canyon Panels. It issues from alluvium below a sandstone cliff, has <br />seasonal flow, and is often dry in summer and autumn. <br />u <br />September zo06 HydrOGeq Inc. <br />