Atlantic Continental Shelf and Slope of the United States - Physiography
Elazar Uchupi
1968, Professional Paper 529-C
Geologic map of the Grand Valley quadrangle, Garfield County, Colorado
John R. Donnell, Warren E. Yeend
1968, Open-File Report 68-77
Biostratigraphy of the Phosphoria, Park City, and Shedhorn Formations, with a section on fish
E. L. Yochelson, D. H. Van Sickle
1968, Professional Paper 313-D
Map of northern half of Wisconsin showing geologic data of Precambrian area
Carl E. Dutton, Reta E. Bradley
1968, Open-File Report 68-91
Geology of the Scranton and New Blaine quadrangles, Logan and Johnson Counties, Arkansas
B.R. Haley
1968, Professional Paper 536-B
Preliminary geologic map of the Eagle B-1 and C-1 quadrangles, Alaska
Helen L. Foster, Terry C. Keith
1968, Open-File Report 68-103
Geologic map of the Quartzsite quadrangle, Arizona
Fred K. Miller
1968, Open-File Report 68-180
Petrography of sedimentary rocks in the Slick Rock district, San Miguel and Dolores Counties, Colorado
D. R. Shawe
1968, Professional Paper 576-B
Preliminary geologic map of Ellipse II-11-2 and vicinity
N.J. Trask
1968, Open-File Report 68-271
Geology of the Comstock-Indian Wells area, Val Verde, Terrell, and Brewster Counties, Texas
V. L. Freeman
1968, Professional Paper 594-K
No abstract available....
New Upper Cretaceous Amphineura (Mollusca)
A.G. Smith, N. F. Sohl, E. L. Yochelson
1968, Professional Paper 593-G
Geologic map of the Muddy Gap quadrangle, Carbon County, Wyoming
Mitchell W. Reynolds
1968, Geologic Quadrangle 771
Phase test wells, White Sands Missile Range, Dona Ana County, New Mexico
G.C. Doty
1968, Open-File Report 68-82
Water resources data for Wisconsin, 1967; Part 1. Surface water records and Part 2. Water quality records
Water Resources Division, U.S. Geological Survey
1968, Water Data Report WI-67-1-2
Color photographs for water resources studies
William J. Schneider
1968, Photogrammetric Engineering (34) 257-262
Air-photo interpretation is very well suited to water resources studies where limited observations of hydrologic data must be extended to regional characteristics for large areas. It is also useful in monitoring the hydrologic regimen of an area to detect possible changes. Color aerial photography is generally superior to black-and-white photography...
Geological interpretation of a Gemini photo
William R. Hemphill, Walter Danilchik
1968, Photogrammetric Engineering (34) 150-154
Study of the Gemini V photograph of the Salt Range and Potwar Plateau, West Pakistan, indicates that small-scale orbital photographs permit recognition of the regional continuity of some geologic features, particularly faults and folds that could he easily overlooked on conventional air photographs of larger scale. Some stratigraphic relationships can...
Early lessons in space observations and Earth resources
William A. Fischer
1968, Astronautics & Aeronautics (6) 1-1
No abstract available....
EROS: viewing the earth from space
William A. Fischer
1968, Geoscience News (1) 16-19
No abstract available....
False-color film fails in practice
G. Ross Cochrane
1968, Photogrammetric Engineering (34) 1142-1146
No abstract available....
Evaporation study at Warm Springs Reservoir, Oregon
D.D. Harris
1968, Report
The mass transfer-water budget method of computing reservoir evaporation was tested on Warm Springs Reservoir, whose contents and surface area change greatly from early spring to late summer. The mass-transfer coefficient computed for the reservoir is two to three times greater than expected and results in a computed evaporation much...
Data for springs in the southern coast, transverse, and peninsular ranges of California
Charles Floyd Berkstresser
1968, Report
Ground-water resources of Monmouth County, New Jersey
Leo A. Jablonski
1968, New Jersey Division of Water Policy and Supply Special Report 23
Monmouth County includes an area of 538 square miles in east-central New Jersey. The climate is characterized by moderate temperature, moderate humidity, and moderate precipitation. The exposed rocks in the area are chiefly sands and clays, which range in age from Late Cretaceous through Recent. The formations strike northeast-southwest and dip...
Data for springs in the northern coast ranges and Klamath Mountains of California
Charles Floyd Berkstresser
1968, Report
Pedogenic formation of montmorillonite from a 2:1-2:2 intergrade clay mineral
Ronald L. Malcolm, W.D. Nettleton, R. J. McCracken
1968, Clays and Clay Minerals (16) 405-414
Montmorillonite was found to be the dominant clay mineral in surface horizons of certain soils of the North Carolina Coastal Plain whereas a 2:1-2:2 intergrade clay mineral was dominant in subjacent horizons. In all soils where this clay mineral sequence was found, the surface horizon was low in pH (below...
Geology of the Magruder Mountain area, Nevada-California
Edwin H. McKee
1968, Bulletin 1251-H
No abstract available....