S. F. Personius, W. E. Scott
1990, Miscellaneous Field Studies Map 2114
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Page 4368, results 109176 - 109200
Publication Extents
Not all publications have extents, not all extents are completely accurateK.T. Gunard, J.H. Hess, J.L. Zirbel, C.E. Cornelius
1990, Water Data Report MN-88-1
J. R. Donnell, W. E. Yeend, M. C. Smith
1990, Miscellaneous Field Studies Map 2113
Robert A. Crovelli, Richard H. Balay
1990, Open-File Report 90-509-A
H. R. Covington, Jean N. Weaver
1990, IMAP 1947-A
The Snake River Plain is a broad, arcuate region of low relief that extends more than 300 mi across southern Idaho. The Snake River enters the plain near Idaho Falls and flows westward along the southern margin of the eastern Snake River Plain (fig. 1), a position mainly determined by...
Kernell G. Ries III
1990, Water-Resources Investigations Report 89-4164
B. P. Sargent, T. V. Fusillo, D. A. Storck, J. A. Smith
1990, Water-Resources Investigations Report 90-4057
R. P. Hooper, C.T. West, N.E. Peters
1990, Water-Resources Investigations Report 90-4000
Anne B. Hoos
1990, Water-Resources Investigations Report 90-4044
Storm-related water-quality data were collected at a drainage-well site and at a spring site in Clarksville, Tennessee, to define the effects of storm-water runoff on the quality of ground water in the area. A dye-trace test verified the direct hydraulic connection between the drainage well and Mobley Spring. Samples of...
V. A. Leidy, E. E. Morris
1990, Water-Resources Investigations Report 90-4099
J. D. Powell, W. G. Wright, D.L. Nelms, R.J. Ahlin
1990, Water-Resources Investigations Report 90-4113
E.G. Jensen
1990, Open-File Report 90-346
S. M. Eberts, E. Scott Bair, J.T. De Roche
1990, Water-Resources Investigations Report 90-4026
D.L. McClain
1990, Open-File Report 90-158
The flood of February 1989 in Kentucky was the result of two storms that caused as much as 13.37 inches of rain at one site during the period of February 13-22. The heaviest rainfall was in western Kentucky where rainfall amounts of 10 to 13 inches were common. Eastern Kentucky...
W. S. Parks, J. K. Carmichael
1990, Water-Resources Investigations Report 88-4181
The Cockfield Formation of the Claiborne Group of Tertiary age underlies approximately 4,000 sq mi in western Tennessee. The formation consists primarily of lenticular beds of very fine to coarse sand, silt, clay, and lignite. The Cockfield Formation has been extensively eroded, and the original thickness is preserved only in...
George H. Billingsley
1990, Open-File Report 90-644
George W. Moore, Manuel G. Bonilla, Richard H. Rapp, W.A. Rinehart, Lee Siebert, Tom Simkin, D. R. Soller, M.L. Zoback, Frank J. Sidlauskas Jr.
1990, Circum-Pacific Map 38
Russell E. Needham
1990, Open-File Report 88-556-B
G.A. Nowlan, F. H. Howd, F. C. Canney, J. A. Domenico
1990, IMAP 1898-C
No abstract available....
Walter J. Bawiec, Gerda A. Abrams, Carol A. Finn, James A. Pitkin, Jean L. Ryder, Steven M. Smith, Paul K. Theobald, Dean B. Vander Meulen, George W. Walker
1990, Open-File Report 89-177
No abstract available....
G.A. Nowlan, F. H. Howd, F. C. Canney, J. A. Domenico
1990, IMAP 1898-B
No abstract available....
Jeffrey L. Imes
1990, Hydrologic Atlas 711-F
No abstract available....
William L. Dam, J. M. Kernodle, C. R. Thorn, G. W. Levings, S. D. Craigg
1990, Hydrologic Atlas 720-D
This report is one in a series resulting from the U.S. Geological Survey's Regional Aquifer System Analysis (RASA) study of the San Juan structural basin that began in October 1984. The purposes of the study (Welder, 1986) are to: (1) Define and evaluate the aquifer system; (2) assess the effects...
G.A. Nowlan, F. H. Howd, F. C. Canney, J. A. Domenico
1990, IMAP 1898-A
1990, Open-File Report 90-83
No abstract available....