Ongoing development in the Flathead Valley is increasing the demand for water. Balancing water management, development, and conservation requires a thorough understanding of how the shallow and deep aquifers and the surface waters interact. In particular, evaluating the continuity and permeability of the confining layer will help determine the extent to which the deep and shallow aquifers are connected.
This study will provide a detailed understanding of the interconnection between groundwater and surface waters on the east side of Flathead Valley and will evaluate groundwater availability as the demand increases with residential and commercial development.
The project scope includes developing the hydrogeologic framework, water budget, and constructing a numerical groundwater model to simulate hydrologic conditions and predict the effects of pumping on the hydrogeologic system.
Groundwater and surface-water monitoring is complete, including aquifer tests. Modeling and aquifer test reports have been published (see below). Final report writing and editing are underway.
This study shows that the confining layer is not continuous throughout the East Flathead area, and groundwater withdrawals from both the shallow and deep aquifers will eventually cause stream depletion. The magnitude of this stream depletion on the Flathead River is likely to be too small to measure. Modeling also indicates that natural variations in groundwater recharge at the Swan Range front is likely to cause more noticeable variations in groundwater levels and groundwater discharge to surface waters than groundwater pumping.
Andy Bobst | Senior Hydrogeologist, Project Manager |
Ali Gebril | Associate Research Hydrogeologist |
Data collected for this project can be accessed through the Ground Water Information Center (GWIC) database:
Download project data from GWIC
Content last updated: 5/11/2022 10:50:59 AM
Program Resources
Contact Information
Program Information
Ginette Abdo, GWIP Manager
(406) 496-4152 | Email