Geologic sketch map of eastern Connecticut
Richard Goldsmith
1963, Open-File Report 63-37
Effects of drought in basins of interior drainage: Chapter E in Drought in the Southwest, 1942-56
H. E. Thomas
1963, Professional Paper 372-E
The effects of the recent drought 1942-56 have varied widely in the Southwestern basins of interior drainage which include, in addition to the Great Basin of Nevada, Utah, and California many smaller basins in Texas, New Mexico, and Arizona. These closed basins are characteristically separate hydrologic units, and their water...
Geologic maps of the Marquette and Sands quadrangles, Michigan
Jacob Eugene Gair, Blair F. Jones
1963, Open-File Report 63-35
Dispersion in ground water flowing through heterogeneous materials
H.E. Skibitzke, G.M. Robinson
1963, Professional Paper 386-B
Effects of drought in the Colorado River basin: Chapter F in Drought in the Southwest, 1942-56
H. E. Thomas
1963, Professional Paper 372-F
The prolonged drought of 1942-56 affected chiefly the lower part of the Colorado River basin and did not extend into the upper basin (the chief water-producing area) until 1953. Areas served by the Colorado River had adequate water supplies in spite of the local deficiency of precipitation. In the Gila...
Fluid impact craters and hypervelocity - high velocity impact experiments in metals and rocks
H. J. Moore, R.W. MacCormick, D. E. Gault
1963, Open-File Report 63-100
The impact phenomena of hypervelocity and high-velocity projectiles with rock and metal targets are being studied in a cooperative research program conducted by the U.S. Geological Survey and the Ames Research Center of the National Aeronautics and Space Administration. This paper deals with the comparison of: (1) fluid-impact craters produced...
Probability distribution of low flows
N.C. Matalas
1963, Professional Paper 434-A
Effects of drought in the Rio Grande basin: Chapter D in Drought in the Southwest, 1942-56
H. E. Thomas
1963, Professional Paper 372-D
In headwater areas of the Rio Grande and its principal tributaries, variations in streamflow and in ground-water storage and discharge depend upon fluctuations in precipitation, with modifications by geologic factors and by the pattern of water development and use. In downstream areas the surfaceand ground-water resources are replenished not only...
Uptake and transport of radionuclides by stream sediments
W.W. Sayre, H.P. Guy, A.R. Chamberlain
1963, Professional Paper 433-A
Quantitative and qualitative analysis of the family Bolivinidae
P.B. Smith
1963, Professional Paper 429-A
Economic geology of the Keysville quadrangle, Florida
James Bachelder Cathcart
1963, Bulletin 1128
No abstract available....
Surficial geology and geomorphology of the Lake Tapps quadrangle, Washington
D. R. Crandell
1963, Professional Paper 388-A
Aeromagnetic map of the Twin Buttes area, Pima and Santa Cruz Counties, Arizona
G. E. Andreasen, J. A. Pitkin
1963, Geophysical Investigations Map 426
No abstract available....
Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California
R. E. Evenson, G.A. Miller
1963, Water Supply Paper 1619-F
Low-flow frequency curves for selected long-term stream gaging stations in eastern United States
Clayton H. Hardison, Robert O.R. Martin
1963, Water Supply Paper 1669-G
Curves showing the magnitude and frequency of annual low flow at 85 streamgaging stations located in 17 States east and 5 States west of the Mississippi River have been smoothed and adjusted to one of four long-term periods. They are presented to show the similarity and dissimilarity of curves even...
Reconnaissance of Headwater Springs in the Gila River Drainage Basin, Arizona
John Henry Frederick Feth, John David Hem
1963, Water Supply Paper 1619-H
Studies of artificial recharge in the Grand Prairie region, Arkansas; environment and history
Kyle Engler, F. H. Bayley, Richard T. Sniegocki
1963, Water Supply Paper 1615-A
No abstract available....
Aeromagnetic map of the Moosehead Lake quadrangle and part of the First Roach Pond quadrangle, Piscataquis and Somerset Counties, Maine
J. R. Henderson, C. W. Smith
1963, Geophysical Investigations Map 334
Ground-water contamination and legal controls in Michigan
Morris Deutsch
1963, Water Supply Paper 1691
The great importance of the fresh ground-water resources of Michigan is evident because 90 percent of the rural and about 70 percent of the total population of the State exclusive of the Detroit metropolitan area are supplied from underground sources. The water-supply and public-health problems that have been caused by...
Aeromagnetic map of part of the Mooseleuk Lake quadrangle, Aroostook and Piscataquis Counties, Maine
L. A. Anderson, N.W. Natof
1963, Geophysical Investigations Map 373
Ground-water reconnaissance of American Samoa
Daniel Arthur Davis
1963, Water Supply Paper 1608-C
The principal islands of American Samoa are Tutuila, Aunuu, Ofu, Olosega, and Ta'u, which have a total area of about 72 square miles and a population of about 20,000. The mean annual rainfall is 150 to 200 inches. The islands are volcanic in origin and are composed of lava flows,...
Geology and ground-water resources of Winkler County, Texas
Sergio Garza, John B. Wesselman
1963, Water Supply Paper 1582
Winkler County, in west Texas, is adjacent to the southeast corner of New Mexico. Most of the county lies in the Pecos Valley; the remainder, in the northeastern part of the county, is part of the Llano Estacado, or the High Plains. Its principal industries are those related to the...
Geology of the Varilla quadrangle, Kentucky-Virginia
Kenneth John Englund, Edwin R. Landis, Henry L. Smith
1963, Geologic Quadrangle 190
Hydrology of small watersheds in western states
Harold V. Peterson
1963, Water Supply Paper 1475-I
No abstract available....
Availability of fresh ground water, Montauk Point area, Suffolk County, Long Island, New York
Nathaniel Matthew Perlmutter, Frank A. DeLuca
1963, Water Supply Paper 1613-B
Ground water is the only source of supply at the Montauk Air Force Station n eastern Suffolk County. The water is contained in the upper 200 feet of deposits of late Pleistocene age, which are broadly divided into an upper unit of undifferentiated till and stratified drift and a lower...