George William Holmes
1964, Open-File Report 64-79
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateH. D. Zeller, E. V. Stephens
1964, Miscellaneous Field Studies Map 289
H. D. Zeller, E. V. Stephens
1964, Miscellaneous Field Studies Map 285
Merritt B. Smith
1964, Oil and Gas Investigation Map 215
No abstract available. ...
Weldon W. Rau
1964, Professional Paper 374-G
Foraminifera from a Tertiary sequence that crops out on the northern part of the Olympic Peninsula, Wash., show stratigraphic and ecologic significance. Forty-two species that are important both to correlations and to ecologic interpretations are illustrated and systematically discussed. The Foraminifera indicate that some of the rocks may be as...
George William Holmes
1964, Open-File Report 64-84
No abstract available....
George William Holmes
1964, Open-File Report 64-82
No abstract available....
G.E. Becraft
1964, Miscellaneous Field Studies Map 283
H.E. Skibitzke
1964, Professional Paper 411-F
The tensor nature of permeability and its effect in a given ground-water flow regime have been acknowledged by various investigators. The effect on the spread of a given dissolved substance can be qualitatively discussed on the basis of the tensor characteristic of the permeability coefficient. The correlation between the dispersion...
Milton Theurer Wilson, Harold E. Thomas
1964, Professional Paper 417-C
Navajo Lake, whose entire outflow disappears underground, is on the high Markagurit Plateau where the average annual precipitation is more than 30 inches. It nestles among the headwaters of several streams that flow into arid regions where competition for municipal, industrial, and irrigation water sup- plies is very keen. Several...
H. D. Zeller, E. V. Stephens
1964, Miscellaneous Field Studies Map 293
Arthur A. Baker
1964, Geologic Quadrangle 239
No abstract available....
H. D. Zeller, E. V. Stephens
1964, Miscellaneous Field Studies Map 297
Philip M. Cohen, Omar J. Loeltz
1964, Water Supply Paper 1779-S
Practically all the ground water of economic importance in the Truckee Meadows area, an alluviated intermontane basin in western Nevada is in the valley fill, which consists of unconsolidated and partially consolidated sedimentary deposits. The Mesozoic and Cenozoic consolidated rocks of the mountains bordering the valley contain some water in...
Burdge Irelan, H.B. Mendieta
1964, Water Supply Paper 1779-K
The Brazos River basin, which makes up 15 percent of the land area of Texas, extends from the High Plains, where altitudes reach 4,200 feet and the average precipitation ranges from 15 to 20 inches a year, to the Gulf of Mexico where the annual rainfall is 45-^50 inches. Large...
Ronald C. Phillips
1964, Special Scientific Report - Wildlife 79
H. D. Zeller, E. V. Stephens
1964, Miscellaneous Field Studies Map 292
H. D. Zeller, E. V. Stephens
1964, Miscellaneous Field Studies Map 294
H. D. Zeller, E. V. Stephens
1964, Miscellaneous Field Studies Map 296
H. D. Zeller, E. V. Stephens
1964, Miscellaneous Field Studies Map 288
H. D. Zeller, E. Vernon Stephens
1964, Miscellaneous Field Studies Map 286
Thomas H. Woodard, Sumner Griggs Heidel
1964, Water Supply Paper 1786
This inventory contains a list of published and unpublished chemical analyses obtained through September 30, 1961, by agencies associated with the Subcommittee on Hydrology. Bulletin 6 of Subcommittee on Hydrology includes references to all surface-water analyses for states east of the Mississippi River known to exist in the files of...
George Frank Worts
1964, Water Supply Paper 1608-E
In 1961 a reconnaissance of the geology and ground-water hydrology of Poro Point, on the west coast of Luzon Island, Philippines, was made on behalf of the U.S. Department of the Navy. Poro Point, which marks the northern end of Lingayen Gulf, is about half a mile wide and projects...
Edward D. Jenkins, Robert E. Glover
1964, Water Supply Paper 1583
The part of Fountain Valley considered in this report extends from Colorado Springs to the Pueblo County line. It is 23 miles long and has an area of 26 square miles. The part of Jimmy Camp Valley discussed is 11 miles long and has an area of 9 square miles....
William Albert Oliver Jr.
1964, Professional Paper 483-B