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Page 1065, results 26601 - 26625

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Not all publications have extents, not all extents are completely accurate
Water supply potential of the Lake Sally System, Marquette County, Michigan
Norman G. Grannemann
1978, Open-File Report 78-1046
Six lakes in the headwaters of Ely Creek form the Lake Sally system. This system is the source of water for Ishpeming and several small communities in the central part of Michigan's Upper Peninsula. During years of average precipitation, more water is used from the system than is supplied to...
Analyses and description of geochemical samples, Craggy Mountain Wilderness Study area, Buncombe County, North Carolina
Jerry M. Motooka, John D. Sharkey, Frank Gardner Lesure
1978, Open-File Report 78-856
Semiquantitative spectrographic analyses for 30 elements and atomic absorption analyses for gold and zinc on 24 bulk stream sediments, 22 panned concentrates, and 50 rock samples from the Craggy Mountain Wilderness Study area and vicinity, Buncombe County, North Carolina, are reported here in detail. Locations for all samples are given...
Overburden chemistry and mineralogy at Hanging Woman Creek, Big Horn County, Montana, and recommendations for sampling at similar sites
Todd K. Hinkley, Richard John Ebens, Josephine G. Boerngen
1978, Open-File Report 78-393
Cored overburden rock of the Fort Union Formation at the Hanging Woman Creek potential coal mine site was classified in hand specimen on the basis of color and grain size into 3 types: sandstone. siltstone-plus-shale, and dark shale. The samples were analyzed for bulk chemistry and mineralogy. In general the...
Results and interpretation of geophysical studies near the Picacho Fault, south-central Arizona
Leroy W. Pankratz, Hans D. Ackermann, Robert C. Jachens
1978, Open-File Report 78-1106
Earth fissuring attributed to ground-water withdrawal occurs throughout south-central Arizona. A large zone of active fissures is located near Picacho, Arizona on the eastern rim of a large subsidence bowl. The main fissure has been named the Picacho fault. During February and March 1977, approximately 6.5 km of seismic-refraction lines...
Geohydrologic data from twenty-four test holes drilled in the Piceance Basin, Rio Blanco County, Colorado, 1975-76
Frank A. Welder, George J. Saulnier
1978, Open-File Report 78-734
Twenty-four test holes were drilled in the Piceance basin, northwestern Colorado, to obtain geohydrologic data from the Uinta and Green River Formations of Eocene age. Depths of test holes ranged from 640 to 2,800 feet. The maximum quantity of water discharged during the air drilling of individual test holes ranged...
Report on laboratory testing of shallow sediments, Middle Atlantic Outer Continental Shelf
Daniel P. LaGatta, Karl Dalenberg, H.J. Knebel, D.A. Sangrey
1978, Open-File Report 78-578
This report contains the results of geotechnical engineering testing on cores taken by the U.S. Geological Survey to evaluate the characteristics of the sea floor within the Baltimore Canyon Trough area. The coring took place in September, 1977 aboard the R/V ANNANDALE. During the cruise (AN-01-77), 20 vibracores were taken...
Mineral resources of the Craggy Mountain Wilderness Study Area, Buncombe County, North Carolina
Frank Gardner Lesure, A. E. Grosz, B. B. Williams, Gertrude C. Gazdik
1978, Open-File Report 78-1091
The Craggy Mountain Wilderness Study Area covers about 550 hectares of the Pisgah National Forest in the Blue Ridge Mountains of western North Carolina (fig. 1). The area is 21 km northeast of Asheville, Buncombe County, N.C., and 11 km southwest of Mount Mitchell, the highest point in eastern North...
Maps showing formation temperatures and configurations of the tops of the Minnelusa Formation and the Madison Limestone, Powder River basin, Wyoming, Montana, and adjacent areas
William J. Head, Kevin Thomas Kilty, Richard K. Knottek
1978, Open-File Report 78-905
This report is part of a study to describe the hydrogeologic framework needed to evaluate the water resources of the Paleozoic age aquifers in the Northern Great Plains coal region. Preliminary studies by the U.S. Geological Survey and State agencies in Wyoming, Montana, and South Dakota have indicated that these...
Low-flow and flow duration of Tennessee streams
Robert L. Gold
1978, Open-File Report 78-807
Low-flow frequency and duration data are presented to define variations of the low flow of Tennessee streams both in time and place. Analysis has been made of 204 continuous record stations, both regulated and unregulated and 651 partial-record stations operated either by the U.S. Geological Survey or Tennessee Valley Authority...
Hydrologic information for land-use planning, Fairbanks vicinity, Alaska
Gordon L. Nelson
1978, Open-File Report 78-959
The flood plain on the Chena and Tanana Rivers near Fairbanks, Alaska, has abundant water in rivers and in an unconfined alluvial aquifer. The principal source of ground water is the Tanana River, from which ground water flows northwesterly to the Chena River. Transmissivity of the aquifer commonly exceed 100...