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2.04.7(1)(a)(iii) <br />(b) Specific surface water information. <br />• <br />The location of the springs within and adjacent to the Bear :line <br />permit area are shown on Drawing 2.04.7(2)(a)-1. Note that some <br />of the springs are located above the "F" seam and some below. <br />The measured yields of springs and results of water quality <br />analysis can be found on Table 2.04.7(2)(a)-2, 2.04.7(2)(a)-3, and <br />2.04.7(2)(a)-4. Spring flows generally decrease from high flora during the early <br />summer to low flows in the early fall, with many of the springs drying <br />up during the same period. This is an indication that the <br />recharge and discharge points of the springs are close together. <br />The approximate location of decreed springs on and near the <br />permit area can be found on Drawing 2.04.7(2)(a)-1. <br />Drawing 2.04.7(2)(a)-2 shows the location of springs in and <br />adjacent to the Bear r'ine permit area with respect to lineaments, <br />landslide deposits, and rock fall areas. Easically what this <br />• map shows is that the springs occur in valleys and the valleys <br />follow linear trends. The source of the water for almost all <br />the springs is felt to be discontinuous lenticular sands, because <br />if only fratures were involved the springs would not he able <br />to flow for any length of time. Yowever, some of the springs may <br />also be associated with fractures. <br />(i) Flow records. <br />The dip of the beds in the Bear Mine permit area is toward the <br />main portal in the northeast. As described more fully on page <br />42, there is no water generated in the Bear Mine. The only <br />water found in the mine is t'~e result of the dust suppression <br />system and the mining operation. These small accumulations <br />do not drain from the mine due to the presence of folding and <br />local low spots. There is no discharge from the Bear ;line. <br />~' The mine area is drained by Sylvester Gulch and one other small <br />ephemeral stream directly into the ':orth Fork of the Gunnison <br />River which is part of the Colorado River drainage basin, see <br />Dra:•ling 3.04.7(2) (a)-1. 5-27 <br />.... <br />e <br />C <br />N <br />C.; <br />a <br />0 <br />G <br />E <br />N <br />a <br />a <br />a <br />W <br />E <br />3 <br />a <br />a <br />W <br />3 <br />E <br />N <br />.~ <br />.a <br />N <br />O <br />U <br />'-I <br />.~ <br />U <br />( ~"OJEJ) <br />7CS, IN I'IEix'I~ <br />SSS <br /> <br /> o '•+ o <br />ul ul ul o o In In o In ul <br />V VV VVV yV <br />O O O N NIA I~ Q <br />Ol 1 ON O~'1Ol v~ <br />In f'l vl 1 r r ul ~ ul <br />.i ul <br /> <br />1 I u'f Ill Vl I <br />~/ V ~"l <br />c r o <br />Ill N q <br />I I l0 N u'1 I <br /> r1 <br /> N <br />S G J. N N O N I A O l0 0 t 0 Gl O lD O <br />m N In o ~ r o N oo .c I I r '•+ .-+ I <br />Ifl IA U1 LA l0 l!1 l0 lA N f`1 lD Ol lp <br />.-I .~ <br />Hd .~ r•l rl In In f•l a' ~o ~o .c rl r ~o <br />I I I <br />rrrl~ rrrr rr rr r` <br />>uo/o[;ut o 0 0 o In o 0 0 <br />o l l IA r In I r o f 1 1 0 l ul 1 <br />3JN'dSJi~QNOJ ~c r+ ao .c .~ rl o rn <br />