The study looked at water resources near the proposed Cabin Creek coal mine in British Columbia. Researchers examined the Flathead River valley to understand the relationship between ground and surface water. They found that the river gains and loses water flow in different areas, with bedrock affecting the aquifer system. Water quality varied in different creeks, with changes in calcium, magnesium, sulfates, and alkalinity downstream. Overall, the research shows how water moves through the area and how it can be influenced by different factors.