Abstract

Objectives of baseline hydrologic monitoring are dependent on and derived from the ultimate use of the data. Baseline hydrological data collection for mining projects typically has several functions including: 1) assembly of adequate information to obtain an understanding of hydrologic and hydrogeologic systems; 2) documentation of baseline conditions for permitting and public disclosure purposes; and 3) documentation of baseline conditions for comparison with future conditions to be measured during mine operation. The scope of such investigations and level of detail required for these different objectives may vary significantly. It is in the interest of mining project proponents, the public and the regulatory agencies to ensure that baseline studies are adequate to meet these objectives.

Collection of adequate information to understand the hydrologic system typically requires an inventory of surface and ground water features, characterization of surface and ground water quality, identification and quantification of ground water flow regimes, depth to groundwater, aquifer characteristics, determination of stream flow variation, and establishment of the degree of seasonal variation in these parameters.

The baseline water resources monitoring program conducted by ASARCO, Inc. for the proposed Rock Creek Mine near Noxon, Montana illustrates several issues relating to baseline hydrologic monitoring for mining projects. ASARCO has developed a comprehensive database and has collected more hydrologic baseline data than any mining project in Montana. The proposed Rock Creek Mine is located in the headwaters of Rock Creek, which is a tributary of the Clark Fork River (Figure 1). The Rock Creek ore body underlies the Cabinet Mountain Wilderness Area and will be mined by underground mining techniques from an access point outside of the wilderness area. The proposed mine related surface facilities would be in the Rock Creek drainage except for portions of the tailings impoundment, which is near the Clark Fork River. Rock Creek is an intermittent stream with a drainage area of approximately 33 square miles al its confluence with the Clark Fork River just below the Noxon Rapids Dam, about twenty miles east of the Montana/Idaho stale line. Baseline monitoring has focused on surface water and ground water in the Rock Creek drainage near the proposed facilities in the tailings impoundment area.

Start Date

20-4-1990 3:40 PM

End Date

20-4-1990 4:00 PM

Document Type

Presentation

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Apr 20th, 3:40 PM Apr 20th, 4:00 PM

Baseline Hydrologic Monitoring for Mining Projects

Objectives of baseline hydrologic monitoring are dependent on and derived from the ultimate use of the data. Baseline hydrological data collection for mining projects typically has several functions including: 1) assembly of adequate information to obtain an understanding of hydrologic and hydrogeologic systems; 2) documentation of baseline conditions for permitting and public disclosure purposes; and 3) documentation of baseline conditions for comparison with future conditions to be measured during mine operation. The scope of such investigations and level of detail required for these different objectives may vary significantly. It is in the interest of mining project proponents, the public and the regulatory agencies to ensure that baseline studies are adequate to meet these objectives.

Collection of adequate information to understand the hydrologic system typically requires an inventory of surface and ground water features, characterization of surface and ground water quality, identification and quantification of ground water flow regimes, depth to groundwater, aquifer characteristics, determination of stream flow variation, and establishment of the degree of seasonal variation in these parameters.

The baseline water resources monitoring program conducted by ASARCO, Inc. for the proposed Rock Creek Mine near Noxon, Montana illustrates several issues relating to baseline hydrologic monitoring for mining projects. ASARCO has developed a comprehensive database and has collected more hydrologic baseline data than any mining project in Montana. The proposed Rock Creek Mine is located in the headwaters of Rock Creek, which is a tributary of the Clark Fork River (Figure 1). The Rock Creek ore body underlies the Cabinet Mountain Wilderness Area and will be mined by underground mining techniques from an access point outside of the wilderness area. The proposed mine related surface facilities would be in the Rock Creek drainage except for portions of the tailings impoundment, which is near the Clark Fork River. Rock Creek is an intermittent stream with a drainage area of approximately 33 square miles al its confluence with the Clark Fork River just below the Noxon Rapids Dam, about twenty miles east of the Montana/Idaho stale line. Baseline monitoring has focused on surface water and ground water in the Rock Creek drainage near the proposed facilities in the tailings impoundment area.