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indicate typical saasoaal variation due to enormalt runoff Sa the epzinq. The fist <br />l~ydsograph euppliad shore data for 1995, the second ahors all data collected ^iaca the • <br />•ita bagsa diaehargiaq. 'NO floc' observations era not +^w:csted oa these or nay other <br />surface rater hydrographe. <br />The yearly svaraga floc (lrom reekly meaeuramante) since this pond begea to Qischarga arai <br />1995 0.106 cf^ <br />1994 0.010 cE^ <br />1993 0.1]7 efs <br />1997 0.036 e!s <br />1991 0.067 ef^ <br />1990 0.055 ef^ (pond did not eo~letely till until Mszch 79, 1990). <br />The above table, along rich the hydrographs, indicates high flora for this year. Ravier <br />o! the TDB plot indicates a recently Qaczeasiag trend, most likely Qua to high spring <br />runoCl. The TDB average at the site prior to the eoastructioa of the HPDHB pond (Bits <br />NeH6) ran 1969 mQ/1. <br />8urfsce Nntar Bita BN•B7N-FG1 (NeByl). Thl^ •it• i^ locnteQ oa Hubbarsoa Gulch dornstrasm • <br /> <br />of the 006 Ouleh eoafluenea. It has bean moaitorad since July, 1979. 8aviar of it^ <br />hyQrograDh reveals the high Daak llor ^Saca 1986. Tha TDB plot iadieatae a deczaaaiag <br />traaQ. <br />NPDBB 005 (NpD885I. Thi^ sadlmea[ poa6 i^ located Sa the mrth mining area oa a tributary <br />to Dry Crask safasraQ to as the 005 Culch. Construetioa of thi^ pond ras eo~lated is <br />JLly, 199] sad the fist discharge occurred oa April ]7, 1993. Doe to for pzaeipitstioa, <br />ao floc ran obearved from thi• ^Ste is 1994. Floc at thi^ site raeumeQ Sa Nay, 1995. Hot <br />enough aa~las have bean collected at this site to indicate aqy apparent TD8 Grand. <br />8urfsce Nater Bite BN•87N•BGS (NeD9). Thi• ^ite i^ located oa Dry Creek and is the <br />furthaet Qoraetraem aurfsce rstar aita !or Beneea II-N. Moaitozlaq at thi^ site began in <br />March, 1983. $aviar of its 1lydzograph again abors the highest Deak floc since 1997 sad <br />1988. The TDB Dlot Sndicates s dacraneiaq tread. <br />• <br />8 <br />