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Bowie Resources Limited <br />• <br />Bowie No. 2 Mine <br />Hydrologic Monitoring Data (1997 - 1999) <br />S2-5 Hubbard Creek • Sorinc 2.5 Elev. 6720 <br />• <br />Field Parameters °°"' °"" °"" ""' °'"' °"" °"'° "'°' <br />Flow Rate (gpm) a.e a.o o.o °.° o.o °.° a.o o.o <br />Water level °n' °n °"' ~' °n' or ort <br />pH (Standard Units) '~' <br />Conductivity (umhos/cm) xB0 <br />Temperature (C) 1°~' <br />Lab Parameters '' ' '•~~~ <br />~. 5..,; ~.d~~`',!: <br />Thera is no lab analysis /or this point tlu <br />Wet Chemistry MDL tow water levelduringlhisperiodorasr <br />Alkalinity as CaCO (mg/I) <br />Bicarbonate as CaCO (mg/I) ' <br />Carbonate as CaCO (mg/I) t <br />Hydroxide as CaCO (mg/I) ~ <br />Chloride (mg/I) ' <br />Conductivity (umhos/cm) ' <br />NiVate (mg/I) °~0~ <br />Nitrate/Nitrite as N, dis. (mg/I) °~03 <br />Nitrite as N, dissolved (mg/I) °'01 <br />pH (Loh Units) °~t <br />Hartlness (mg/I) ' <br />Phosphate (mg/I) °~0' <br />Phosphorous, ortho tlis. (mg/I) °~0m <br />TDS @180 C (mg/I) 10 <br />TSS (mg/I) ° <br />SAR °0' <br />Sulfate (mg/I) 10 <br />Metals <br />Aluminum, total rec. (mg/I) 0.°° <br />Arsenic, total recoverable (mgA) o.ml <br />Cadmium, total recoverable (mgA) °~m' <br />Calcium, total recoverable (mg/I) °~' <br />Copper, local rewverable (mg/I) °~~ <br />Iron, total recoverable (mgll) o.or <br />Lead, local recoverable (mg/I) o~p0 <br />Magnesium, total rec. (mgll) °~~ <br />Manganese, total rec. (mgA) °~' <br />Mercury, total rec. (mg/I) °~0°°t <br />Molybdenum, total rec. (mgA) °~01 <br />Selenium, dissolved (mg/I) °~0°' <br />Sodium. dissolved (mg/I) °J <br />Zinc, dissolved (mg/I) °~01 <br />Organic Analysis <br />Oil and Grease, total rec. (mg/I) ' <br />Requved by current permit. <br />, to low Oows or <br />oted above <br />Surface Water <br />6/tOn 998 to 9/24n999 924/1999 to Present <br />Baseline Onnralinnal <br />Min Max Avg Min Max Avg <br />o.o a.e at a.p p.o °° <br />u >.t >.l <br />tea mo ~m <br />le.t te.l te.t <br />There la no lab analyala for Thera la no lab analysts for <br />this polo/ duo to low flows Nla polo/ tlua to law flows or <br />or water lava) tlurina Ihla water level durlna ibis periatl. <br />padatl. <br />• Baseline Infarma4on for Point 526 is derived Irom events beginning on 6/10/1996 through 9/24/1999, a periatl of -16 months. Point influenced by min,ng on 9/24!1999. <br />the monitoring point IoCdlion for 53-6 (Spring 2-6) is located along Ne upper edge of a souNern lork of the Freeman Gulch Roao as ,1 originates Irom the Hubbard Creek <br />road. Its flow originates Irom the exposed sandstone outcrop totaled high above lne Hubbard Creek Canyon along lha eastern faang walls of the cliffs between the valley <br />created by the North Fork of the Gunnison and Freeman Gulch. <br />MDL =Method Determination Limit BLANK =Not Tested Monitoring Point Table 15 <br />