Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1977
J.B. Townshend, J.E. Papp, M.J. Moorman, C.E. Deadmon, S.P. Tilton
1977, Open-File Report 77-300-D
The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory;...
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: March 1977
J.B. Townshend, J.E. Papp, M.J. Moorman, C.E. Deadmon, S.P. Tilton
1977, Open-File Report 77-300-C
The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory;...
Frequency analysis of Illinois floods using observed and synthetic streamflow records
George W. Curtis
1977, Water-Resources Investigations Report 77-104
Equations, applicable Statewide, for estimating flood magnitudes having recurrence intervals ranging from 2 to 500 years for unregulated rural streams, with drainage areas ranging from 9.02 to 10,000 square miles (0.05 to 25,900 sqiiare kilometers), were derived by multiple regression an. A rainfall-runoff model was used in the synthesis of...
Geologic map and sections of the Rincon Valley Quadrangle, Pima County, Arizona
Harald Drewes
1977, IMAP 997
Computation of records of streamflow at control structures
Dannie L. Collins
1977, Water-Resources Investigations Report 77-8
Traditional methods of computing streamflow records on large, low-gradient streams require a continuous record of water-surface slope over a natural channel reach. This slope must be of sufficient magnitude to be accuratly measured with available stage measuring devices. On highly regulated streams, this slope approaches zero during periods of low...
Digital model analysis of the principal artesian aquifer, Savannah, Georgia area
H. B. Counts, R.E. Krause
1977, Water-Resources Investigations Report 76-133
A digital model of the principal artesian aquifer has been developed for the Savannah, Georgia, area. The model simulates the response of the aquifer system to various hydrologic stresses. Model results of the water levels and water-level changes are shown on maps. Computations may be extended in time, indicating changes...
Ground-water resources of Chester County, Pennsylvania
Laurence J. McGreevy, Ronald A. Sloto
1977, Water-Resources Investigations Report 77-67
Fifty gallons per minute (3 liters per second) or more may be obtained from wells in almost all parts of the county, but not at all locations. Adequate exploration to find fracture or solution openings is required. Five hundred gallons per minute (30 liters per second) or more may be...
Digital flow model of the Chowan River estuary, North Carolina
C.C. Daniel
1977, Water-Resources Investigations Report 77-63
A one-dimensional deterministic flow model based on the continuity equation had been developed to provide estimates of daily flow past a number of points on the Chowan River estuary of northeast North Carolina. The digital model, programmed in Fortran IV, computes daily average discharge for nine sites; four of these...
Mineral resources of the Jarbidge Wilderness and adjacent areas, Elko County, Nevada, with a section on interpretation of aeromagnetic data
Robert Roy Coats, R.C. Green, L.D. Cress, L. Y. Marks, W. E. Davis
1977, Bulletin 1439
Geologic map of the Syrtis Major Quadrangle of Mars
J.D. Meyer, M. J. Grolier
1977, IMAP 995
The Syrtis Major quadrangle is located in the equatorial belt of Mars across the boundary between the cratered plateau region to the south and west and the northern lowland plains. The cratered plateau is part of the northern extension of cratered highlands, which generally stands at altitudes greater than 4...
Preliminary report on the lignite resources of the Niobe area, Burke and Ward counties, North Dakota
Hal E. Owen
1977, Open-File Report 77-379
Two lignite beds, the Niobe and the Bonus, occur at strippable depths within the Niobe area. The Niobe bed averages 5 feet (1.5 meters) in thickness and the Bonus bed averages 8 feet (2.4 meters) in thickness. These beds lie in the lower part of the Sentinel Butte Member of...
Stratigraphic diagrams with electric logs of Upper Cretaceous rocks, Powder River basin, Natrona, Converse, and Niobrara Counties, Wyoming, section C-C'
E.A. Merewether, W. A. Cobban, R.M. Matson, W.J. Magathan
1977, Oil and Gas Investigation Chart 75
Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: September 1977
J.B. Townshend, J.E. Papp, M.J. Moorman, C.E. Deadmon, S.P. Tilton
1977, Open-File Report 77-300-I
The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory;...
Geologic map of the Harper Quadrangle, Liberia
M. R. Brock, A.H. Chidester, M.W.G. Baker
1977, IMAP 780-D
Electrical properties of water saturated basalt: preliminary results to 506K (233 degrees C)
Gary R. Olhoeft
1977, Open-File Report 77-688
Water-table map of Cape Cod, Massachusetts, May 23-27, 1976
Denis R. LeBlanc, John H. Guswa
1977, Open-File Report 77-419
Mineralogical, chemical, and physical properties of the regolith overlying crystalline rocks, Fairfax County, Virginia: a preliminary report
Gerhard W. Leo, M.J. Pavich, Stephen F. Obermeier
1977, Open-File Report 77-644
Undisturbed cores of saprolite developed on crystalline rocks of the Piedmont Province in Fairfax County, Virginia have been obtained using a combination of Shelby tubes, Denison sampler, and modified diamond core-drilling. The principal purpose of the core study is to correlate variations in chemistry, mineralogy and texture with engineering properties...
Geologic map of the Custer quadrangle, Breckinridge and Hardin Counties, Kentucky
Dewey Harold Amos
1977, Geologic Quadrangle 1367
No abstract available....
Catalog of earthquakes in the Santa Barbara Channel area for the period January 1, 1972 to December 31, 1973
Sharon L. Kirkman, William L. Ellsworth
1977, Open-File Report 77-302
Quality of rivers of the United States, 1975 water year; based on the National Stream Quality Accounting Network (NASQAN)
John C. Briggs, John F. Ficke
1977, Open-File Report 78-200
The National Stream Quality Accounting Network (NASQAN) was established by the U.S. Geological Survey to provide a nationally uniform basis for continuously assessing the quality of U.S. rivers. Stations generally are at the downstream end of hydrologic accounting units in order to measure the quantity and quality of water flowing...
A digital model of ground-water flow in Spanish Valley, Grand and San Juan counties, Utah
James H. Eychaner
1977, Open-File Report 77-760
No abstract available....
Genesis of a zoned granite stock, Seward Peninsula, Alaska
Travis Hudson
1977, Open-File Report 77-35
A composite epizonal stock of biotite granite has intruded a diverse assemblage of metamorphic rocks in the Serpentine Hot Springs area of north-central Seward Peninsula, Alaska. The metamorphic rocks include amphibolite-facies orthogneiss and paragneiss, greenschist-facies fine-grained siliceous and graphitic metasediments, and a variety of carbonate rocks. Lithologic units within the...
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
Strong ground motion in the Tularosa Basin, New Mexico
John P. Hoffman, Samuel T. Harding
1977, Open-File Report 77-143
Late Pleistocene and Recent geology of the Housatonic River region in northwestern Connecticut
George C. Kelley
1977, Open-File Report 77-545
An investigation of Late Pleistocene and Recent surficial deposits in western Connecticut and adjacent areas was undertaken, to determine characteristics of Wisconsin glaciation and the history and chronology of deglaciation in part of the finely dissected New England Uplands. The study area lies along the midreach of the Housatonic River...