Surface Water and Riparian Studies Summary

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Surface Water & Riparian

Surface Water & Riparian

TITLE: Baseline Regulatory (100-Year) Hydrology and Average-Annual Runoff RELEASE DATE: March 2010 PREPARED BY: Tetra Tech Brief Summary: Under baseline conditions, stormwater runoff from the Rosemont drainage area flows down four main pathways – McCleary Canyon, Wasp Canyon, and Barrel Canyon and Lower Barrel Canyon – to the general outlet point (Compliance Point) for the watershed to the northeast of the project site. In this report, Tetra Tech provides details on the flow generated in those drainages. Both the peak flow from the 100-year storm event and average runoff conditions at the Rosemont site were calculated. Tetra Tech’s baseline average-annual runoff analysis for watersheds within the project site indicate annual precipitation of approximately 18 inches with the following average annual runoff (provided in acre-feet): McCleary Canyon-322, Wasp Canyon-310, Barrel Canyon-354, Lower Barrel Canyon-142, and Compliance Point-912.

Surface water and riparian studies looked at vegetative cover and riparian mapping to establish baselines and compare potential impacts from Rosemont project operations. 34

rosemont copper

- a bridge to a sustainable future

TITLE: Davidson Canyon Hydrogeologic Conceptual Model and Assessment of Spring Impacts RELEASE DATE: April 2010 PREPARED BY: Tetra Tech Brief Summary: The Rosemont project site comprises approximately 16 percent of the entire Davidson Canyon watershed; therefore, the project has the potential to impact water resources in that drainage, according to this Tetra Tech report. However, the anticipated downstream effects of pit dewatering and the post-mining pit lake may be indiscernible from the existing natural and man-induced regional conditions. During operations, dewatering (taking water out of the pit) will create drawdown in the groundwater table in an area immediately surrounding the pit. The water will follow the path of least resistance or in this case, the most permeable or most fractured rocks. The drawdown will be greatest around the pit and will diminish farther away from the pit, such as in Davidson Canyon, a


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Surface Water and Riparian Studies Summary by Danny Simons - Issuu