The subenvelope map as a tool for delineating linear features in the Georgia Piedmont and coastal plain
Larry Mayer, David C. Prowell, Juergen Reinhardt
1977, Open-File Report 77-695
Land use and land cover and associated maps for Hattiesburg, Mississippi; Alabama (Alabama portion only)
Water Resources Division, U.S. Geological Survey
1977, Open-File Report 77-50
Time of travel of solutes in selected reaches of Ohio streams, 1973 and 1975
Arthur O. Westfall
1977, Water-Resources Investigations Report 77-116
The basic field data for time-of-travel measurements on six streams in Ohio are presented. In general, additional data on stream cross sections, tributary inflows, and chemical analyses for mainstream and tributary flows are given. Insufficient data were obtained to establish time-distance or time-discharge relationships....
Deep drilling data, Raft River Geothermal Area, Idaho; Raft River Geothermal Exploration Well No. 1
H. R. Covington
1977, Open-File Report 77-226
Preliminary geologic map of the Pillar Butte, Pillar Butte NE, Pillar Butte SE, and Rattlesnake Butte quadrangles, Bingham, Blaine, and Power counties, Idaho
H. R. Covington
1977, Open-File Report 77-779
Mercury in the conterminous United States: computerized data file and computer-plotted map of occurrences
Jocelyn A. Peterson, Joel R. Bergquist, Judith S. Gassaway
1977, Open-File Report 77-859
Albuquerque Basin seismic network
Lawrence H. Jaksha, Jerry Locke, J.B. Thompson, Alvin Garcia
1977, Open-File Report 77-865
The U.S. Geological Survey has recently completed the installation of a seismic network around the Albuquerque Basin in New Mexico. The network consists of two seismometer arrays, a thirteen-station array monitoring an area of approximately 28,000 km 2 and an eight-element array monitoring the area immediately adjacent to the Albuquerque...
Thickness of overburden map of Fairfax County, Virginia
A.J. Froelich, T.L. Heironimus
1977, Open-File Report 77-797
Preliminary bedrock geologic map of the Georgetown Quadrangle, Essex County, Massachusetts
Kenneth Granville Bell, A. F. Shride, Norman P. Cuppels
1977, Open-File Report 77-179
Land use and land cover and associated maps for Greeley, Colorado, Wyoming
Water Resources Division, U.S. Geological Survey
1977, Open-File Report 77-394
Distribution and relationships of 4-10 km diameter craters to global geologic units on Mars
Christopher D. Condit
1977, Open-File Report 77-421
Analog-model analysis of effects of waste-water management on the ground-water reservoir in Nassau and Suffolk counties, New York; Report III: Reduction and redistribution of ground-water pumpage
Arlen W. Harbaugh, Thomas E. Reilly
1977, Open-File Report 77-148
Chemical, physical, biochemical, and bacteriological characteristics at selected stream sites in Puerto Rico, 1975-76
Ferdinand Quinones-Marquez, Pedro Vazquez, Rafael Pena
1977, Open-File Report 77-237
A device for automatic photoelectric control of the analytical gap for emission spectrographs
John A. Dietrich, Elmo F. Cooley, Kenneth J. Curry
1977, Circular 748
A photoelectric device has been built that automatically controls the analytical gap between electrodes during excitation period. The control device allows for precise control of the analytical gap during the arcing process of samples, resulting in better precision of analysis....
Availability of ground water in the lower Connecticut River basin, southwestern New Hampshire
J. E. Cotton
1977, Water-Resources Investigations Report 77-79
This map scale 1:125,000 presents a preliminary assessment of the availability of ground water in the lower Connecticut River basin in southwestern New Hampshire. It is a generalization of several hydrogeologic factors and provides a guideline for ground-water exploration useful in water- and land-use planning. It does not describe the...
Joints, fissures, and voids in rhyolite welded ash-flow tuff at Teton damsite, Idaho
Harold J. Prostka
1977, Open-File Report 77-211
Several kinds of joints, fissures, and voids are present in densely welded rhyolite ash-flow tuff at Teton damsite. Older fissures and voids probably were formed in the ash-flow sheet during secondary flowage, which probably was caused by differential compaction or settling over irregular topography. The younger, more abundant fissures are...
Flood-plain delineation for Pohick Creek Basin, Fairfax County, Virginia
Pat LeRoy Soule
1977, Open-File Report 76-444
Image analysis as a method for determining grain-size distributions in sandstones
Michael B. Sawyer
1977, Open-File Report 77-280
Assessment of increased thermal activity at Mount Baker, Washington, March 1975-March 1976
David Frank, Mark Frederick Meier, Donald A. Swanson, James W. with contributions by Babcock, Marvin O. Fretwell, Stephen D. Malone, Charles L. Rosenfeld, Ronald L. Shreve, Ray E. Wilcox
1977, Professional Paper 1022-A
In March 1975 Mount Baker showed a large increase in thermal emission, which has persisted for more than 1 year. Fumarole ejecta accompanied the thermal activity from March to September, but the ejecta had no constituents that suggest a magmatic source. Estimates of that part of the total heat flux...
CENTO workshop on application of remote sensing data and the methods held at Lahore, Pakistan, March 2-8, 1975
Raymond W. Fary (compiler)
1977, Open-File Report 77-488
Lithologic logs of Lisburne Group in Lawrence Livermore Laboratory drill holes 1 and 2, Confusion Creek, Chandler Lake Quadrangle, northern Alaska
William Peters Brosge, Augustus K. Armstrong
1977, Open-File Report 77-26
Chemical analyses of 97 stream-sediment samples from the Coleen and Christian quadrangles, northern Alaska
William Peters Brosge, H. N. Reiser, Thomas E. Moore
1977, Open-File Report 77-458
Water resources in western Cortland County, New York: hydrologic data for 1972-75 and progress report
Harold L. Shindel, William Buller, William H. Johnston
1977, Open-File Report 77-525
Basic data on the surface water, ground water, and water quality of Cortland County, New York, are presented with a short explanatory text. Seepage investigations showed that during periods of base flow, the surface-water regime cannot be predicted on the basis of flow-duration figures alone. The investigations also indicate that...
Water consumption by nuclear powerplants and some hydrological implications
Ennio V. Giusti, E.L. Meyer
1977, Circular 745
Published data show that estimated water consumption varies with the cooling system adopted, being least in once-through cooling (about 18 cubic feet per second per 1,000 megawatts electrical) and greatest in closed cooling with mechanical draft towers (about 30 cubic feet per second per 1,000 megawatts electrical). When freshwater is...
A review of the effects of earthquakes on underground mines
Peter R. Stevens
1977, Open-File Report 77-313