A digital-computer model for estimating drawdowns in the sandstone aquifer in Dane County, Wisconsin
R.S. McLeod
1975, Open-File Report 74-59
A digital-computer program was developed to compute nonsteady and steady-state hydrologic changes caused by pumping from a confined aquifer. The program computes head changes in the confined aquifer and the rate and volume of water withdrawn from aquifer boundaries.The program was used to model the sandstone aquifer underlying Dane County,...
A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin
R.S. McLeod
1975, Open-File Report 75-304
A finite-element model of a two-dimensional, single-phase heat transport in a porous medium
James W. Mercer, George Francis Pinder
1975, Open-File Report 75-574
Availability of ground water in Marion County, Indiana
William R. Meyer, J. P. Reussow, D. C. Gillies, W. J. Shampine
1975, Open-File Report 75-312
County constitute the most extensive aquifers in the county. Four areally distinct sand and gravel aquifers were mapped in the drift during the course of this study. The aquifer of greatest economic importance consists of sand and gravel deposits of glacial-outwash origin which coincide with the courses of the White...
A reconnaissance study of the U and Th contents of plutonic rocks of the southeastern Seward Peninsula, Alaska
Thomas P. Miller, Carl M. Bunker
1975, Open-File Report 75-217
Large granitic Cretaceous plutons are exposed along and adjacent to an arcuate belt of igneous and high-grade metamorphic rocks in the southeastern Seward Peninsula of Alaska. Reconnaissance studies of these plutons have shown that the Darby pluton has well above average amounts of U and Th (11.2 ppm and 58.7...
U, Th, and K analyses of selected plutonic rocks from west-central Alaska
Thomas P. Miller, Carl M. Bunker
1975, Open-File Report 75-216
Numerous samples of plutonic rocks collected during reconnaissance mapping in western Alaska have been analyzed for K, U, and Th. The U and Th content of the plutonic rocks from the southeastern Seward Peninsula have been discussed in a separate report (Miller and Bunker, 1975); because of the current interest...
Geology of the middle Tertiary formations of Puerto Rico
Watson Hiner Monroe
1975, Open-File Report 75-313
Acoustic-reflection profiles, R/V Polaris, Nov.-Dec. 1970, offshore southern California, Port Hueneme to Point La Jolla
George William Moore
1975, Open-File Report 75-629
No abstract available....
Acoustic-reflection profiles, M/V Oil City, June 1969, offshore southern California
George William Moore, David S. McCulloch
1975, Open-File Report 75-347
No abstract available....
Chemical characteristics of hydrothermal alteration at Bingham, Utah
William J. Moore
1975, Open-File Report 75-649
Digital-model analysis of the effects of water-use alternatives on spring discharges, Gooding and Jerome Counties, Idaho
Joe A. Moreland
1975, Open-File Report 75-615
Ground water in the Grand (Neosho) River basin, Kansas and Oklahoma
Robert B. Morton, Stuart W. Fader
1975, Open-File Report 75-366
Ground water in the Grand (Neosho) River basin occurs in both consolidated rocks and unconsolidated deposits. Water for domestic and stock supplies generally can be obtained from wells in either of the above deposits. Water for municipal, industrial, and irrigation supplies generally can be obtained in limited quantities from the...
Abundances of uranium, thorium and potassium from some plutonic rocks in northern Washington
Robert J. Munroe, J.H. Sass, C. M. Bunker, C. A. Bush
1975, Open-File Report 75-221
No abstract available....
Reconnaissance of the geology and ore mineralization in part of the Chagai District, Pakistan
Raymond H. Nagell
1975, Open-File Report 75-550
The Chagai District of the Quetta Division is in the northwestern part of Pakistan. Igneous activity during the Himalayan orogeny included the extrusion of horizontally layered andesites of the Cretaceous Sinjrani Volcanic Group, emplacement of monzonitic stocks of the Cretaceous Chagai intrusions, and the extrusion of flows and tuffs of the...
Sulfur, fluorspar, magnesite, and aluminous chromite in Pakistan
Raymond H. Nagell
1975, Open-File Report 75-496
Reports and analyses on elemental sulfur, fluorspar, magnesite, and aluminous chromite were reviewed for the purpose of identifying and categorizing the known deposits, and to indicate those which seem to merit further study on the basis of available information. General conclusions drawn from the study are: (1) Although aluminous chromite...
Exploration for uranium deposits in meta-sedimentary rocks in the light of geologic studies of the Midnite Mine, Washington
J. Thomas Nash
1975, Open-File Report 75-638
Geology of the Midnite uranium mine, Stevens County, Washington; a preliminary report
J. Thomas Nash, Norman J. Lehrman
1975, Open-File Report 75-402
The Midnite mine is one of only two mines in the United States currently producing uranium from discordant deposits in crystalline host rocks. Ore bodies are in metamorphosed steeply dipping Precambrian pelitic and calcareous rocks of a roof pendant adjacent to a Cretaceous(?) porphyritic quartz monzonite pluton. Production during 14...
Investigations of the 7 June 1975 earthquake in Humboldt County, California
Robert Nason, Edwin L. Harp, Harry LaGesse, Richard P. Maley
1975, Open-File Report 75-404
Physical factors determining the fraction of stored energy recoverable from hydrothermal convection systems and conduction-dominated areas
Manuel Nathenson
1975, Open-File Report 75-525
This report contains background analyses for the estimates of Nathenson and Muffler (1975) of geothermal resources in hydrothermal convection systems and conduction-dominated areas. The first section discusses heat and fluid recharge potential of geothermal reservoirs. The second section analyzes the physical factors that determine the fraction of stored energy obtainable...
Some reservoir engineering calculations for the vapor-dominated system at Larderello, Italy
Manuel Nathenson
1975, Open-File Report 75-142
Various reservoir properties are calculated for the Larderello vapor-dominated system using available published data. Bottom-hole flowing properties are calculated from measured wellhead data. Whereas wellhead temperatures measured at a particular time tend to change systematically with changes in flow and pressure, calculated bottom-hole temperatures tend to be constant for two...
Seismic attenuation studies at the Idaho National Engineering Laboratory
Richard Navarro
1975, Open-File Report 75-512
Water availability of Washington County, Alabama
John G. Newton, Jerald F. McCain, James D. Turner
1975, Open-File Report 75-476
Large quantities of ground water and surface water are available in Washington County. Major sources of ground water are the Gosport Sand and Lisbon Formation undifferentiated, the Miocene Series undifferentiated, and alluvium and low terrace deposits. The Miocene, the most productive source of ground water, will yield 0.5 to 1.0...
The Decaturville, Missouri, impact structure; a geologic summary with map
Terry W. Offield, Howard A. Pohn
1975, Open-File Report 75-310
Preliminary hydrogeologic appraisal of selected hydrothermal systems in northern and central Nevada
F. H. Olmsted, P.A. Glancy, J. R. Harrill, F. E. Rush, A. S. Van Denburgh
1975, Open-File Report 75-56
Several hydrothermal systems in northern and central Nevada were explored in a hydrogeologic reconnaissance. The systems studied comprise those at Stillwater and Soda Lakes-Upsal Hogback in the Carson Desert, Gerlach, Fly Ranch-Granite Range, and Double Hot Springs in the Black Rock Desert, Brady's Hot Springs, Leach Hot Springs in Grass...
Second EROS/AID international course on remote sensing
Donald G. Orr
1975, Open-File Report 75-48
No abstract available....