Batholithic rocks of Southern California: A model for the petrochemical nature of their source materials
A. K. Baird, A.T. Miesch
1984, Professional Paper 1284
No abstract available....
Hydrogeology of the Verna well-field area and management alternatives for improving yield and quality of water, Sarasota County, Florida
C. B. Hutchinson
1984, Water-Resources Investigations Report 84-4006
About 8 million gallons of water are pumped daily from the 3-square-mile Verna well field to supply the city of Sarasota. Pumping has resulted in water-level declines and changes in water quality. Drawdowns of at least 30 feet have occurred in the producing zone at the well-field boundaries. Sulfate concentrations...
Downstream effects of dams on alluvial rivers
G. P. Williams, M. G. Wolman
1984, Professional Paper 1286
Huebnerite veins near Round Mountain, Nye County, Nevada
D. R. Shawe, E.E. Foord, N. M. Conklin
1984, Professional Paper 1287
Glastonbury Gneiss and mantling rocks (a modified Oliverian dome) in south-central Massachusetts and north-central Connecticut: Geochemistry, petrogenesis, and isotopic age
G. W. Leo, R. E. Zartman, D. G. Brookins
1984, Professional Paper 1295
The Glastonbury dome is a long, narrow structure trending approximately 70 km north-northeast through Connecticut and Massachusetts along the west side of the Bronson Hill anticlinorium. Structurally and stratigraphically the dome is analogous to the Oliverian domes of New Hampshire. It is cored by Glastonbury Gneiss and is mantled by...
Igneous activity and related ore deposits in the western and southern Tushar Mountains, Marysvale volcanic field, west-central Utah
Thomas A. Steven, editor(s)
1984, Professional Paper 1299-A,B
PART A: Igneous activity in the Marysvale volcanic field of western Utah can be separated into many episodes of extrusion, intrusion, and hydrothermal activity. The rocks of the western Tushar Mountains, near the western part of the volcanic field, include intermediate-composition, calc-alkalic volcanic rocks erupted from scattered volcanoes in Oligocene...
The Schultze granite, the Tea Cup granodiorite, and the Granite Basin porphyry: A geochemical comparison of mineralized and unmineralized stocks in southern Arizona
S.C. Creasey
1984, Professional Paper 1303
No abstract available....
Chemical data for soils over and around the Velma oil field, Stephens County, Oklahoma
S.S. Roeming, T.J. Donovan
1984, Open-File Report 84-262
Determination of the Total, Commonality, and Uniqueness of Interpreted Structural Elements from Remotely Sensed Data in Alaska
George H. Rosenfield
1984, Open-File Report 83-876
Stratigraphy and sedimentary facies of the Madison Limestone and associated rocks in parts of Montana, Nebraska, North Dakota, South Dakota, and Wyoming
J.A. Peterson
1984, Professional Paper 1273-A
Geohydrology of the Madison and associated aquifers in parts of Montana, North Dakota, South Dakota, and Wyoming
J. S. Downey
1984, Professional Paper 1273-G
Geohydrologic data for test well USW G-4, Yucca Mountain area, Nye County, Nevada
C.B. Bentley
1984, Open-File Report 84-63
Data are presented on drilling operations, lithology, borehole geophysics, hydrologic monitoring, core analysis, water chemistry, pumping tests, and packer-injection tests for test well USW G-4. The well is one of a series of test wells drilled in and near the southwestern part of the Nevada Test Site, Nye County, Nevada,...
An evaluation of rainfall-runoff data for the Denver Federal Center, Lakewood, Jefferson County, Colorado
R.D. Jarrett, J.E. Veenhuis
1984, Water-Resources Investigations Report 84-4050
An investigation was made to monitor the storm runoff in McIntyre Gulch basin to determine the rainfall-runoff chracteristics. Results may now be used to evaluate the effects of future development on storm runoff from the Denver Federal Center, which is located in the McIntyre Gulch basin in Lakewood , CO....
Hydrologic data for the Larimer-Weld regional water-monitoring program, Colorado, 1975-82
S. R. Blakely, J.T. Steinheimer
1984, Open-File Report 84-139
The Larimer-Weld, Colorado, regional Monitoring Program was begun in 1976 to provide information on the quality and quantity of the surface-water resources in the area. Three stations on the big Thompson River and five stations on the Cache La Poudre River were selected for a data-collection network. Four previously established...
The thrust belt in Southwest Montana and east-central Idaho
Edward T. Ruppel, David A. Lopez
1984, Professional Paper 1278
The leading edge of the Cordilleran fold and thrust in southwest Montana appears to be a continuation of the edge of the Wyoming thrust belt, projected northward beneath the Snake River Plain. Trces of the thrust faults that form the leading edge of the thrust belts are mostly concealed, but...
Map showing the distribution and abundance of copper in bedrock samples, western Chichagof and Yakobi Islands Wilderness Study Area, southeastern Alaska
Bruce R. Johnson, Geoffrey S. Elliott
1984, Open-File Report 81-27-D
No abstract available....
Directory of member organizations of the National Water Data Exchange (NAWDEX)
Cassandra D. Blackwell
1984, Open-File Report 84-469
The National Water Data Exchange (NAWDEX) is a national confederation of water-oriented organizations working together to improve access to water data. It consists of member organizations from all sectors of the water-data community. This Directory provides the names, addresses, and telephone numbers of all NAWDEX member organizations and their designated...
Mines and prospects of the Dillon 1 degree x 2 degrees Quadrangle, Idaho and Montana
J. S. Loen, R. C. Pearson
1984, Open-File Report 84-377
No abstract available. ...
Depth and thickness of selected units in Upper Permian, Upper Jurassic, and Lower Cretaceous rocks in southwestern Kansas
Jack Kume, Joseph M. Spinazola
1984, Water-Resources Investigations Report 83-4095
As ground-water reserves decline in the Ogallala aquifer in an area of about 17,400 square miles in 26 counties of southwestern Kansas, sandstone aquifers in underlying Upper Jurassic and Lower and Upper Cretaceous rocks may be developed to supplement or replace the Ogallala as a source of water for some...
Analytical results and sample locality map of stream-sediment and panned-concentrate samples from the Chandler Lake 1° x 3° quadrangle, Alaska
S. J. Sutley, K.A. Duttweiler, R.T. Hopkins
1984, Open-File Report 84-412
No abstract available....
Preliminary mineral resource assessment of the proposed Mt. Wrightson Wilderness, Santa Cruz and Pima Counties, Arizona
Steve Ludington
1984, Open-File Report 84-294
Water resources data for Utah, water year 1983
M. D. ReMillard, G. A. Birdwell, R. B. Garrett, G. W. Sandberg
1984, Water Data Report UT-83-1
No abstract available....
Developing an oil generation model for resource assessment of the Bakken Formation, U.S. portion of the Williston Basin
K. B. Krystinik, Ronald R. Charpentier
1984, Open-File Report 84-694
No abstract available....
Hydrologic data; North Canadian River from Lake Overholser to Lake Eufaula, central Oklahoma
J.S. Havens
1984, Open-File Report 84-808
The data contained in this report were gathered during the period 1982 to 1984 for use in constructing a digital model of the North Canadian River from Lake Overholser, in the western part of Oklahoma City, to Lake Eufaula, in eastern Oklahoma. Locations of test holes and sampling sites are...
Ground-water models as a management tool in Florida
C. B. Hutchinson
1984, Water-Resources Investigations Report 84-4016
Highly sophisticated computer models provide powerful tools for analyzing historic data and for simulating future water levels, water movement, and water chemistry under stressed conditions throughout the ground-water system in Florida. Models that simulate the movement of heat and subsidence of land in response to aquifer pumping also have potential...