Geology of the Franklin D. Roosevelt Reservoir Shoreline: Glacial geology, terraces, landslides, and lineaments
Kiver EP and Stradling DF. 1995. Geology of the Franklin D. Roosevelt Reservoir Shoreline: Glacial geology, terraces, landslides, and lineaments. Grand Coulee Power Office; Bureau of Reclamation, Pacific Northeast Region. Grand Coulee, WA
Surficial deposits along the flooded valleys of the Columbia River and its tributariesfrom Grand coulee Dam to Canada were studied during the 1983 to 1985 field seasonsas part of the shoreline investigation studies of 151-mile (242 km) long Lake Roosevelt.Minor manuscript updates and review of maps were completed in 1994. Anunderstanding of the geologic events that affected the Columbia River valley andsurrounding area is basic to intelligently evaluating the nature of the sediments alongLake Roosevelt and their stability.