J. G. Vedder
1968, IMAP 547
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Page 5833, results 145801 - 145825
Publication Extents
Not all publications have extents, not all extents are completely accurateS. E. Rantz
1968, Hydrologic Atlas 298
No abstract available....
James Louis Gualtieri
1968, Geologic Quadrangle 685
C. C. Hawley, Allen L. Meier, Ralph L. Miller
1968, Open-File Report 68-123
Jules A. MacKallor
1968, Open-File Report 68-172
A series of 39 overlapping photographs of the southwestern United States and adjacent areas of Mexico was obtained as part of an experiment of the Gemini IV mission. Twenty-four of these pictures plus one from the Gemini III and four from the Gemini V mission were used to construct a...
Leonard Dorrean Harris
1968, Open-File Report 68-119
Upper part of the Knox Group has previously been divided into three formations; however, because of the lack of regionally recognizable boundaries, there has been a marked inconsistency as to the rocks assigned by different workers to the Longview Dolomite, Kingsport Formation and Mascot Dolomite. Regional stratigraphic studies have pointed...
A. C. Waters, R.H. Vaughan
1968, IMAP 541
Gus H. Goudarzi, Avery E. Smith
1968, Geologic Quadrangle 766
R.L. Hosman, A. T. Long, T. W. Lambert, H. G. Jeffery
1968, Professional Paper 448-D
No abstract available....
M. A. Maroof Khan, Norbert A. Parker
1968, Open-File Report 68-176
The following report covers field work and muffle furnace tests on clays in the immediate vicinity of Dacca, East Pakistan, to determine clay amenability to bloating for the commercial production of light-weight aggregates. It has been established that such clays exist in at least three areas; reserves are sufficient in...
George Walton Walker, Donald A. Swanson
1968, Bulletin 1260-M
William Charles MacQuown
1968, Geologic Quadrangle 767
James A. Pitkin
1968, Professional Paper 516-F
John O. Maberry
1968, Open-File Report 68-170
The Blackhawk Formation at Sunnyside, Utah, was deposited along the western margin of the Western Interior Cretaceous sea during southeastward withdrawal of the sea. Sand was the dominant type of land-derived sediment deposited in the Sunnyside district during the regressive phases. Sand bodies prograded seaward in response to changing sediment...
George Walton Walker, Donald A. Swanson
1968, Bulletin 1260-L
C.M. Swinney, A. C. Waters, C. P. Miller
1968, IMAP 543
A. C. Waters
1968, IMAP 542
Edwin H. McKee
1968, Geologic Quadrangle 770
Ellis Leon Yochelson, Clive R. Jones
1968, Professional Paper 613-B
Gus H. Goudarzi
1968, Geologic Quadrangle 741
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...
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...
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...
Charles Floyd Berkstresser
1968, Report
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...