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43 percent sand 80 percent acre-feet acre-ft altitude amount of sediment approximately Ashland boulders CAPACITY AND SEDIMENT coarse core cubic foot deposited sediment drainage area drainage basin end marker erosion flow gaging station Graphs gravel Hindall Lake Superior layers light red-brown ment method mg/L mm/yr north edge northwestern Wisconsin original capacity replaced original depth particle particle size particle-size photopeak point bar pool area pool elevation Power Company powerhouse Precambrian PRERESERVOIR TOPOGRAPHY range line 9 RATES OF SEDIMENT red-clay area replaced by sediment reser RESERVOIR CAPACITY reservoir history reservoir reservoir reservoir was drained RESERVOIR-SEDIMENT CHARACTERISTICS runoff sedi sediment density sediment deposited sediment surface sediment thickness SEDIMENT VOLUME sedimentation rate September 1976 soils square kilometer square mile stream stream-gaging station streamflow surface runoff suspended-sediment discharge tainter gates test holes tons/mi trap efficiency U.S. Geological Survey upstream end valley vertical voir volume of deposited White River Reservoir
Page 20 - Rää bay the maximum value was used (p. 191). In a symmetrical grain size distribution with one maximum size the Md lies close to the real maximum of the sediment (BRAND, p. 97, BRESSAU. p. 68). b. The coefficient of sorting (STr...