J. H. Morgan
1965, Hydrologic Atlas 158
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Publication Extents
Not all publications have extents, not all extents are completely accurateJohn R. Williams
1965, Water Supply Paper 1792
Douglas C. Alverson
1965, Water Supply Paper 1576-F
The Fort Belknap Indian Reservation includes an area of 970 square miles in north-central Montana. At its north edge is the Milk River valley, which is underlain by Recent alluvium of the Milk River, glacial deposits, and alluvial deposits of the preglacial Missouri River, which carved and occupied this valley...
Lorin D. Clark, Fred K. Miller
1965, Open-File Report 65-32
Herbert G. Hinson
1965, Circular 517
The magnitude and frequency of floods are defined regionally for small streams (drainage area, 1 to 150 sq mi) in North Carolina. Composite frequency curves for each of two regions relate the magnitude of the annual flood, in ratio to the mean annual flood, to recurrence intervals of 1.1 to...
F. H. Pauszek, Frederick H. Ruggles
1965, Water Supply Paper 1809-N
Paul Charles Bateman
1965, Geologic Quadrangle 428
G. R. Boynton, Peter Popenoe, G. L. Zandle
1965, Geophysical Investigations Map 531
Richard W. Bayley
1965, Geologic Quadrangle 458
G. R. Boynton, Peter Popenoe, G. L. Zandle
1965, Geophysical Investigations Map 533
No abstract available....
Richard W. Bayley
1965, Geologic Quadrangle 460
G. R. Boynton, C. W. Smith
1965, Geophysical Investigations Map 547
No abstract available....
Richard W. Bayley
1965, Geologic Quadrangle 461
William Back, Ivan Barnes
1965, Professional Paper 498-C
This study was undertaken to develop means of measuring oxidation potentials in aquifer systems and to use the measured values in interpreting the behavior of iron in ground water. Anne Arundel County, Md., was selected as the area of study because of the wide range of concentration of iron-nearly zero...
Paul R. Seaber
1965, Professional Paper 498-B
This investigation describes the variations in the chemical character of the water in the Englishtown Formation of Late Cretaceous age in the Atlantic Coastal Plain of New Jersey, and demonstrates the application of the concept of hydrochemical mapping to the study and evaluation of water-bearing materials. The chemistry of ground water...
Stewart L. Udall
1965, Photogrammetric Engineering (31) 63-75
Aerial survey methods are speeding acquisition of survey data needed to provide and manage the nation's resources. These methods have been applied to topographic mapping for a number of years and the record clearly shows their advantages in terms of cost and speed in contrast to the ground methods that...
Charles J. Robinove
1965, Journal - American Water Works Association (57) 834-840
This article briefly describes the characteristics of infrared radiation and demonstrates how infrared photography and infrared imagery can be applied to water resources research, specifically to the identification and description of hydrologic features....
R.J. Hackman
1965, Photogrammetric Engineering (31) 604-610
Aerial photographs taken after the March 27, 1964, Good Friday, Alaskan earthquake were examined stereoscopically to determine effects of the earthquake in areas remote from the towns, highways, and the railroad. The two thousand black and white photographs used in this study were taking in April, after the earthquake,...
Peter C. Badgley, William A. Fischer, Ronald J. P. Lyon
1965, Geotimes (10) 11-14
The National Aeronautics & Space Administration is planning geologic exploration from orbiting spacecraft. For that purpose it is evaluating new and refined exploration tools, often called remote sensors, including devices that are sensitive to force fields, such as gravity gradient systems, and devices that record the reflection or emission of...
Water Resources Division, U.S. Geological Survey
1965, Water Data Report IN-65-1
The surface-water records for the 1965 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the...
B.B. Hanshaw, E-An Zen
1965, Geological Society of America Bulletin (76) 1379-1385
The two principal suggested modes of facilitating overthrust faulting are (1) lubrication at the sole by evaporite beds or micaceous shales and (2) flotation due to anomalously high (> hydrostatic) pore-water pressures. Past rapid sedimentation and tectonic compression have been suggested as important causes of anomalously high water pressure (Hubbert...
George W. Andrews
1965, Bulletin of the Geological Society of America (76) 113-124
The lower Chippewa Valley in west-central Wisconsin extends 65 miles from the Cary terminal moraine in Chippewa County to the Mississippi River Valley. The Chippewa Valley and its tributaries were filled with a valley train of sand and gravel during the maximum stand of the Cary ice, and entrenchment of...
A. S. Van Denburgh, J. H. Feth
1965, Water Resources Research (1) 537-541
The estimated average rates of annual solute erosion in 11 important western river basins range from 180 tons per square mile (Willamette basin) to 4.2 tons per square mile (Gila basin). An average rate of 58 tons per square mile is indicated for the entire 545,000‐square‐mile area drained by the...
Frank T. Manheim
1965, Undersea Technology (6) 22-25
No abstract available....
Michael Churkin Jr., Earl E. Brabb
1965, American Association of Petroleum Geologists Bulletin (49) 172-185
A predominantly shale and chert sequence has been mapped from the Canadian border at Latitude 65°00′ N. to the Nation River about 25 miles northwest. It has Ordovician and Silurian graptolites in the lower half, and Middle Devonian corals and Upper Devonian spores in the upper half.The lower half of...