A lead story in the Star Tribune on Sept. 1 suggested that water from PolyMet's mine could impact the Boundary Waters Canoe Area Wilderness (BWCA). A letter submitted to regulators late in the environmental review process by John Coleman, a wildlife ecologist who works for the Great Lakes Indian Fish and Wildlife Commission, asserts that groundwater could flow north from the PolyMet site to the Peter Mitchell taconite mine and eventually into the Boundary Waters some 20 miles away. This is simply not the case.
The reality is, existing field data from monitoring wells and surrounding lake elevations strongly support the conclusion that project groundwater will not move through the bedrock toward the Boundary Waters. All water quality and quantity data, as well as modeling analyses in the environmental-impact statement used to determine the impacts of the NorthMet project, are appropriate and adequate.
As part of the environmental review process, the co-lead agencies (the Minnesota Department of Natural Resources, the U.S. Army Corps of Engineers and the U.S. Forest Service) and their independent environmental engineering consultant have considered Coleman's allegations. A June 22 technical memo from the agencies concludes: "[T]he lack of hydrologic response at the proposed NorthMet project mine site supports a conceptual model whereby water from the proposed NorthMet pits would not flow into the Northshore pits." It continues: "[A]dditional modeling of flowpaths … would not be beneficial."
In a letter dated Aug. 5, the Environmental Protection Agency (EPA) submitted its comments on the preliminary final environmental-impact statement to the co-lead agencies. The EPA specifically addressed the "potential post-closure northward flow path in bedrock groundwater" and concluded that "the proposed strategy [is] an appropriate response."
This is exactly how the environmenta-review process is supposed to work.
In an e-mail to the agencies, Coleman admits that he is not "a groundwater modeling professional" and that "any analysis should be redone by professionals in the field of groundwater modeling." Coleman changed inputs to the environmental-impact statement model to show that groundwater could flow north. Of course, changing any inputs would affect the outputs. But those new outputs do not reflect reality.
The same assumptions that predict a north flow path would also predict that the Partridge River would be dry during much of the year. Additionally, the model would predict that current dewatering of the Peter Mitchell pit would already have caused a drawdown of water levels in wells that PolyMet already has in place, which is not the case. The changes that Coleman made to the model do not accurately portray actual conditions.
The questions raised by Coleman are intended to delay the environmental-review process, not improve it. The Rainy River Watershed and the BWCA will not be impacted by the PolyMet project.