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This is an active fault that has been identified by seismic and gravity evidence as spanning the width of the Rocky Mountain Trench. The maximum historic event attributed to this fault was a magnitude 5 event in 1975. North of the fault, the depth to bedrock in the trench increases, and the orientation of the trench swings from N to NW. At the same latitude (48 0 10' N) the thrust ranges to the east show a similar orientation change. Leaving Hungry Horse Dam, the excursion will again cross the Rocky Mountain Trench and pass into the more subdued ranges of the western belt of the Northern Rocky Mountains, passing a chain of lakes called the Thompson Lakes and entering the Libby Trough.
Drainage adi! No. I Downie slide, geologic section looking south (downstream). /'" / 7 //Heod scarp reservoir started filling in October 1983. The reservoir sloughing does not jeopardize the stability of the large was kept 30 ft (9 m) below normal full pool until slide mass. stabilization measures were complete. Filling was Mica Dam completed by the summer of 1984. Movement of the Stop '-2: slide mass has been insignificant, and water pressures The Mica Dam (Figure 7-4,) lies within low-to have remained low.
A 3-ft- (1 m) thick interbed separates it from the overlying Ginkgo flow. The Grande Ronde Basalt is exposed below the falls and along the lower part of the canyon, which extends to the Palouse canyon confluence with the Snake River canyon at Lyons Ferry less than 5 mi (8 km) south (Swanson and Wright, 1981). Stop 3-7: Little Goose Dam The Snake River canyon at Little Goose Dam (Figure 3-8) is cut in of upper Grande Ronde Basalt flows with the Frenchman Springs and Roza members of the Wanapum Basalt are exposed high on the canyon walls.