L.L. Hubbard, T.D. Parks, D.L. Weiss, L.E. Hubbard
1983, Water Data Report OR-82-2
No abstract available....
Search Results
165549 results.
Alternate formats: RIS file of the first 3000 search results | Download all results as CSV | TSV | Excel | RSS feed based on this search | JSON version of this page of results
Page 4700, results 117476 - 117500
Publication Extents
Not all publications have extents, not all extents are completely accurateCarol J. Lind
1983, Water Supply Paper 2204
Abstract contains content that can not be displayed, please see the publication for abstract...
B. A. Hopkins
1983, Open-File Report 83-577
No abstract available....
E.E. Denis
1983, Open-File Report 82-116
The Tonto basin area includes about 955 mi2 in central Arizona. The area is bounded on the north by the Mogollon Rim, on the east by the Sierra Ancha Mountains, on the west by the Mazatzal Mountains, and on the south by Theodore Roosevelt Lake. The area is drained by...
E.G. Boyce, Robert M. Turner
1983, Open-File Report 83-155
R. E. Curtis Jr., P. W. McKinley, H. M. Colon-Ramos
1983, Water Data Report PR-81-82-1
No abstract available. ...
N. S. MacLeod, E. M. Taylor, D. R. Sherrod, G. W. Walker, J. D. Causey, S. L. Willett
1983, Open-File Report 83-659
No abstract available....
John B. Wesselman
1983, Hydrologic Atlas 654
A study of the hydrogeology of deep sedimentary basins using the Neogene deposits of the northern Gulf of Mexico basin as a model was initiated by the U.S. Geological Survey in the 1960's (Jones, 1969). This study led to investigations of geopressured-geothermal resources in this basin (Papadopulos and others, 1975;...
William Jasper Sando
1983, Professional Paper 1247
J.D. Byerlee, C.A. Morrow, D. Moore
1983, Open-File Report 83-475
M. L. Sorensen, Andrew Griscom, M. D. Conyac, A. R. Buehler, D. E. Graham, T. M. Sweeney
1983, Miscellaneous Field Studies Map 1427-B
No abstract available....
B. R. Lipin, Nicholas Wetzel, S. M. Heinrich
1983, Open-File Report 83-816
The Emma Bell chromite deposit in Siskiyou County, California contains over 5 million tons of dunite averaging about 4 percent Cr2O3. Chromite is not evenly disseminated throughout the dunite, however. For the most part the deposit consists of many chromite-rich bands in sharp contact with, and separated by, common dunite...
Patrick J. Sousa
1983, FWS/OBS 82/10.32
This document is part of the Habitat Suitability Index (HSI) Model Series (FWS/OBS-82/10), which provides habitat information useful for impact assessment and habitat management. Several types of habitat i nformat i on are provided. The Habitat Use Information Section is largely constrained to those data that can be used to...
L. E. Dunlap, Richard J. Lindgren, C. G. Sauer
1983, Open-File Report 83-222
A study was made, in cooperation with the Division of Water Resources, Kansas State Board of Agriculture, to determine geohydrologic conditions in an area comprising nearly 850,000 acres along the Arkansas River valley in Kearny and Finney Counties, southwestern Kansas. The Arkansas River meanders atop and interacts hydraulically with the...
T. E. Reilly, H. T. Buxton, O.L. Franke, R. L. Wait
1983, Water-Resources Investigations Report 82-4045
A computer simulation of Long Island 's regional groundwater system has been used to evaluate the effects that new-installed sewers will have on ground-water levels. Results indicate maximum water-table decliners of as much as up to 18 feet in central Nassau County and about 9 feet in Suffolk County. Total...
G.E. McGill, E.A. King
1983, IMAP 1409
D.F. Huber, S.C. Nelson, E. E. Cather, J.L. Ritchey
1983, Open-File Report 83-482
Edward A. du Bray
1983, Open-File Report 83-370
Sixteen well-defined geochemical anomalies associated with felsic plutons and (or) muscovite-bearing plutons of Proterozoic age have been identified in the eastern and southeastern Arabian Shield. The majority of these plutons are highly evolved, granitophile-element-enriched muscovite-bearing granites that are weakly peraluminous. A followup study of the mineral potential of these plutons included...
W.H. Lee, D.L. Scharre, G.R. Crane
1983, Open-File Report 83-518
John C. Behrendt, M. S. Grim
1983, Geophysical Investigations Map 956
No abstract available....
Lawrence J. Drew, G.C. Grender, R. M. Turner
1983, Open-File Report 83-75
Timothy J. Durbin
1983, Open-File Report 81-688
The Gauss optimization technique can be used to identify the parameters of a model of a groundwater system for which the parameter identification problem is formulated as a least squares comparison between the response of the prototype and the response of the model. Unavoidable uncertainty in the true stress on...
Water Resources Division, U.S. Geological Survey
1983, Water Data Report NM-82-1
Water resources data for the 1982 water year for New Mexico consist of records of discharge and water quality of streams; stage, contents and water quality of lakes and reservoirs; and water levels and water quality in wells and springs. This report contains discharge records for 197 gaging stations; stage and...
J. B. Miller, J.L. Oberg, T. Sieger Jr.
1983, Water Data Report MI-82-1
Water resources data for the 1982 water year for Michigan consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water temperature of ground water. This report contains discharge records for 169 gaging stations; stage only...
Water Resources Division, U.S. Geological Survey
1983, Open-File Report 83-377
The Climax stock is a composite granitic intrusive of Cretaceous age, composed of quartz monzonite and granodiorite, which intrudes rocks of Paleozoic and Precambrian age. Tertiary volcanic rocks, consisting of ashflow and ash-fall tuffs, and tuffaceous sedimentary rocks overlie the sedimentary rocks and the stock. Erosion has removed much of...