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Not all publications have extents, not all extents are completely accurate
Water resources data, Maine, water year 1985
W.P. Bartlett Jr., W.B. Higgins, W.J. Nichols Jr.
1985, Water Data Report ME-85-1
Water resources data for the 1985 water year for Maine consist of records of stage,discharge, and water quality of streams; stage and contents of lakes and reservoirs;and water levels and water quality of ground-water wells. This report contains discharge records for 48 gaging stations; stage only for 2 gaging stations;...
Stratigraphic cross section and coal bed correlations of uppermost Cretaceous and Paleocene rocks between Painted Canyon and Davis Buttes, North Dakota
J.S. Hinds
1985, Miscellaneous Field Studies Map 1766
Recent detailed coal studies in the area between Havelock and Fryburg, N. Dak. (Hinds, 1983; 1985), have resulted in some revised coal-bed correlations that are, in places, in disagreement with previous work (Banet, 1980; Hares, 1928; Lewis, 1979; Menge, 1977; Owen, 1979; Rehbein, 1977; Royse, 1967). The strati graphically most...
Stratigraphic cross sections and correlation of lignites in the Sentinel Butte member and upper part of the Tongue River member of the Fort Union Formation between Amidon and Fryburg, North Dakota
Jim S. Hinds
1985, Miscellaneous Field Studies Map 1765
The Austin Farm bed was once mined form an adit in the SE1/4 sec, T. 136 N., R. 101 W. Its westerly outcrop extends from that point northward along the east side and north end of the valley of Third Creek at elevations between about 2740 and 2800 ft. It...
Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu
Kiyoshi J. Takasaki, John Francis Mink
1985, Water Supply Paper 2217
Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the island of Oahu because they generally underlie the rainiest areas. These reservoirs accumulate the infiltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams...
Traveltime and dispersion in the Potomac River, Cumberland, Maryland, to Washington, D.C.
Kenneth R. Taylor, Robert W. James Jr., Bernard M. Helinsky
1985, Water Supply Paper 2257
A travel-time and dispersion study using rhodamine dye was conducted on the Potomac River between Cumberland, Maryland, and Washington, D.C., a distance of 189 miles. The flow during the study was at approximately the 90-percent flow-duration level. A similar study was conducted by Wilson and Forrest in 1964 at a...
Hydrologic data for Leviathan Mine and vicinity, Alpine County, California, 1981-83
D.P. Hammermeister, S.J. Walmsley
1985, Open-File Report 85-160
The U.S. Geological Survey collected basic hydrologic and water-quality data during 1981-83 to facilitate the geohydrologic evaluation of the Leviathan Mine area and the design of a pollution-abatement project. Surface-water field data included one or more measurements of pH, water temperature, and specific conductance at 45 sites in and adjacent...