Maxwell E. Gardner
1969, Open-File Report 69-102
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateCarl G. Kroll, George Porterfield
1969, Open-File Report 69-146
J. A. Moreland, J.A. Singer
1969, Open-File Report 69-175
Roy Newcome Jr., F.H. Thomson
1969, Open-File Report 69-183
R.H. Ollman
1969, Open-File Report 69-187
Adel A. R. Zohdy, D. B. Jackson, R.E. Mattick, D. L. Peterson
1969, Open-File Report 69-326
A.M. Moore
1969, Open-File Report 69-173
Henry C. Berg
1969, Open-File Report 69-19
Water Resources Division, U.S. Geological Survey
1969, Open-File Report 72-398 to 72-403, 73-326
J.D. Larsen, J. E. Weir Jr.
1969, Open-File Report 69-148
John C. Roller, Jerry P. Eaton, William Hung Kan Lee
1969, Open-File Report 69-229
M. J. Grolier, J.W. Bingham
1969, Open-File Report 69-111
W. F. Hardt
1969, Open-File Report 69-118
N.L. Hawley, B.L. Jones
1969, Open-File Report 69-124
G.E. Seaburn
1969, Professional Paper 627-B
The study described in this report is concerned with the effects of intensive urban development on direct runoff to East Meadow Brook, a southward-flowing stream in central Nassau County, N.Y., during the period 1937-66. The specific objectives of the study were (a) to relate indices of urban development to increases...
C.H. Miller, G. D. Bath
1969, Geophysical Investigations Map 693
G. D. Robinson, M. E. McCallum, William Henry Hays
1969, Geologic Quadrangle 840
J.G. Cronin
1969, Hydrologic Atlas 330
The Ogallala Formation of Tertiary (Pliocene) age is the principal aquifer in the Southern High Plains of western Texas and eastern New Mexico. This heavily pumped aquifer supplies practically all the water used for irrigation, municipal, industrial (except oil-field repressuring), and domestic purposes. Although the ground water in the Ogallala Formation...
Edwin H. McKee, John H. Stewart
1969, Open-File Report 69-159
Water Resources Division, U.S. Geological Survey
1969, Circular 622
John H. Stewart, Edwin H. McKee
1969, Open-File Report 69-269
Donald E. White
1969, Journal of Geophysical Research (74) 5191-5201
Local differences in rate of heat transfer in vapor and by conduction through the ground in hot spring areas are difficult and time-consuming to measure quantitatively. Individual heavy snowfalls provide a rapid low-cost means of measuring total heat flow from such ground. After a favorable snowfall (heavy, brief duration, little...
George E. Stoertz, William R. Hemphill, David A. Markle
1969, Marine Technology Society Journal (3) 11-26
An experimental Fraunhofer line discriminator detected solar-stimulated yellow fluorescence (5890 A) emitted by Rhodamine WT dye in aqueous solutions. Concentration of 1 part per billion was detected in tap water 1/2-meter deep. In extremely turbid San Francisco Bay, dye was monitored in concentrations of less than 5 parts per billion...
Charles J. Robinove, Daniel G. Anderson
1969, Journal of the American Water Resources Association (5) 10-19
Remote sensing in the field of hydrology is beginning to be applied to significant problems, such as thermal pollution, in many programs of the Federal and State Governments as well as in operation of many private organizations. The purpose of this paper is to guide the hydrologist to a better...
Robert G. Reeves
1969, Geological Society of America Bulletin (80) 2159-2164
Certain structural geologic features may be more readily recognized on sidelooking airborne radar (SLAR) images than on conventional aerial photographs, other remote sensor imagery, or by ground observations. SLAR systems look obliquely to one or both sides and their images resemble aerial photographs taken at low sun angle with the...