New Publications
A ravenous river reclaims its true course: the tale of Marmot Dam's demise. Science Findings. March 2009 (Issue 111). Portland, OR. U.S.D.A.Forest Service, Pacific Northwest Research Station. 6p.

Major et al., 2008. Initial Fluvial Response to the Removal of Oregon's Marmot Dam, EOS 89(27): 241-252.

Jefferson, A., Nolin, A., Lewis, S., and Tague, C., 2008. Hydrogeologic controls on streamflow sensitivity to climatic variability, Hydrological Processes, 22: 4371–4385. DOI: 10.1002/hyp.7041.

Grant, G.E., Lewis, S.L., Swanson, F., Cissel, J. & McDonnell, J., 2008. Effects of forest practices on peakflows and consequent channel response: a state-of-science report for western Oregon and Washington. General Technical Report PNW-GTR-760. Portland, Oregon: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 76 p.

O'Connor, J., Major, J., Grant G. Down with Dams: Unchaining US Rivers. Geotimes March 2008

Burkholder BK, Grant GE, Haggerty R, Wamper PJ, Khangaonkar T. 2008. Influence of Hyporheic Flow and Geomorphology on Temperature of a Large, Gravel-bed River, Clackamas River, Oregon, USA. Hydrological Processes DOI: 10.1002/hyp.6984.

Wallick, J.R., Grant, G.E, Lancaster, S.T., Bolte J.P. and R.P. Denlinger. 2008. Patterns and controls on historical channel change in the Willamette River, Oregon USA. In Gupta A.V., ed. Large Rivers: Geomorphology and Management. John Wiley and Sons. p491-516. (buy this book)

Tague, C., Farrell, M., Grant, G. Choate, J., and Jefferson A. 2008. Deep groundwater mediates streamflow response to climate warming in the Oregon Cascades, Climatic Change 86: 189-210

Marmot Dam (Sandy River, Oregon)
prior to removal in summer 2007
additional information

Video Presentations
Hydrology and Geomorphic Evolution of Basaltic Landscapes, High Cascades, Oregon
Anne Jefferson (2006)

The Geomorphic Response of Rivers to Dam Removal
Gordon Grant (2003)