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• components (figure 5), which are about a mile and a <br />half apart. Both are on dissected dip slopes that <br />drain southwestward at Gradients of 700-1,000 ft/ni, <br />The western tract, the laf•Gest of the two, is traversed <br />by ephemeral streams that head on the drainage divide <br />between Fish and elk Creeks and drain Generally scuth- <br />eastward to Fish Creek at gradients of 80 to 260 ft:mi, <br />The eastern tract has no well-draiaed strew channe_s <br />and drains directly to nearby Trout Creek, <br />Foidel Creei< is *.ributary to t5iddle Creek which in Burn <br />enters Trout Creek about 0,3 mile northwest of the <br />eastern tract of C-22676 (figure 5). both Foidel a-d <br />• t•]:ddle Creeks drain coal areas and are intermittent <br /> streams that have insuf_` icient ground-water dischara_ <br />to maintain perennial base flow, Trout Creek heads on <br />the Flat Tops Area in Routt tlational Forest and flews <br />i <br />~ generally northward, entering the Yampa River near <br />i <br />Milner, Colorado, Trout Creek is perennial and has a <br />base flow of 10-15 efs (cubic feet per second). Fish <br />Creek, which is also perennial with a Lase flow of 1-2 <br />efs, heads on the Dunkley Flat Tops west of the Tr cut <br />Creek headwaters and enters Trout Creek about half a <br />mile east of C-22676 (west) (figure 51. <br />No long-term precipitation data are available for the <br />M <br />36 <br />