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Page 5876, results 146876 - 146900

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.
John Vecchioli, William D. Nichols, Bronius Nemickas
1967, New Jersey Division of Water Policy and Supply Water Resources Circular 17
The continued drought in northeastern New Jersey through the summer of 1966 with its attendant water-supply problems resulted in an extension of the drought-disaster test-drilling program originally requested by the Office of Emergency Planning on August 30, 1965. Authorization to continue test drilling was fiven by the Office of Emergency...
Mountains and plains Denver's geologic setting
Water Resources Division, U.S. Geological Survey
1967, Report
A slice of geologic history is exposed to view in the Denver, Colorado area. Denver is situated on the High Plains near the east front of the Rocky Mountains. As one travels westward from Denver toward the mountains, successively older rocks are crossed from the geologically young rocks of the...
An electrical analog study of the geometry of limestone solution
M. S. Bedinger
1967, Groundwater (59) 24-24
This study of the geometry of limestone solution is based on the following conditions: (1) the limestone is impermeable but contains and transmits water in joints, fractures, bedding‐plane partings, and solution channels; (2) at depth, the limestone aquifer is underlain by impermeable rock; (3) ground water in the limestone is under water‐table conditions; (4) recharge to the limestone is by infiltration of precipitation through the overlying rock...
Scapolite in the Belt Series in the St. Joe-Clearwater Region, Idaho
Anna Hietanen
1967, GSA Special Papers (86) 1-54
Scapolite is a common rock-forming mineral in parts of the Belt Series of Precambrian age in southern Shoshone County and adjoining parts of Clearwater County, Idaho. It is most abundant in moderately metamorphosed calcareous shaly layers of the Wallace Formation but occurs also in their highly metamorphosed equivalents and in...
Mineral appraisal of the Poker Jim Ridge and Fort Warner areas of the Hart Mountain National Antelope Refuge, Lake County, Oregon
George W. Walker, Donald A. Swanson
1967, Report
The Poker Jim Ridge and Fort Warner areas, which are candidate areas for inclusion in the National Wilderness Preservation System, are in the Hart Mountain National Antelope Refuge in east-central Lake County, south-central Oregon. The two areas form part of an upraised and tilted fault block--a structural element that is...
Geochemistry and ground-water movement in northwestern Minnesota
R.W. Maclay, T. C. Winter
1967, Groundwater (5) 11-19
The relation between water quality and water movement within the ground-water reservoir may be better understood if studies of flow systems are used in conjunction with hydrochemical methods. Within small watersheds, local, intermediate, and regional flow systems may develop, depending upon the shape, the relief, and the thickness of the...
Pre-Olympia Pleistocene stratigraphy and chronology in the central Puget Lowland, Washington
D. J. Easterbrook, Dwight R. Crandell, Estella B. Leopold
1967, GSA Bulletin (78) 13-20
Drifts of two pre-Olympia glaciations separated by nonglacial sediments are widespread in the central Puget Lowland of western Washington. The Double Bluff Drift (older) and Possession Drift represent advances of the Puget lobe of the Cordilleran ice sheet more than 40,000 years ago. The nonglacial Whidbey Formation between the drifts...
Water resources of the Guanica area, Puerto Rico: A preliminary appraisal, 1963
Neal E. McClymonds
1967, Report
Guánica and the lower Rio Loco valley lie between the extensive agricultural development in Lajas Valley to the west and the industrial development at Guayanilla to the east. Having a protected deep-water port, the Guánica area is particularly well suited to further development. The economic growth of the area depends,...
Devonian of the Northern Rocky Mountains and plains
Charles A. Sandberg, William J. Mapel
1967, Conference Paper, International symposium on the Devonian system
The Devonian System, represented predominantly by shallow-water marine carbonate, is widespread in Montana, Wyoming, eastern Idaho, North Dakota, South Dakota, and northwestern Nebraska. It comprises cratonic rocks in the east and miogeosynclinal rocks in the west. The cratonic rocks thicken generally northward from their southern limit in Wyoming across...
Devonian of the Southwestern United States
F. G. Poole, D.L. Baars, H. Drewes, P. T. Hayes, K. B. Ketner, E. D. McKee, C. Teichert, J. S. Williams
1967, Conference Paper, International symposium on the Devonian system
The structural framework that controlled Devonian deposition consisted of, from west to east: (1) a eugeosynclinal area in northern California and western Nevada; (2) a miogeosynclinal area in southeastern California, eastern Nevada, and western Utah; and (3) a cratonic area in Arizona, eastern Utah, Colorado, New Mexico, and western...
Succession of rugose coral faunas in the Lower and Middle Devonian of eastern North America
William Albert Oliver Jr.
1967, Conference Paper, International symposium on the Devonian system
Rocks of Early Devonian age are widely but sporadically distributed in the eastern half of North America and coral studies are based on a very incomplete record. Middle Devonian rocks are thicker and cover a greater area. Both Early and Middle Devonian corals are more similar to western European species...
Devonian of the Appalachian Basin, United States
William A. Oliver, Wallace De Witt, John M. Dennison, D.M. Hoskins, John W. Huddle
1967, Conference Paper, International symposium on the Devonian system
Although Devonian rocks in the Appalachians have been studied for more than 150 years, they are poorly known in most of the area. The nearly complete Devonian sequence in New York has been established as the North American standard of reference. The structural belt that includes unmetamorphosed Devonian geosynclinal...
Northern part, Ten Mile and Taunton River basins
John R. Williams, Richard E. Willey
1967, Massachusetts Hydrologic - Data Report 10
The northern part of the Ten Mile and Taunton River basins is an area of about 195 square miles within Norfolk, Plymouth, and Bristol Counties in southeastern Massachusetts. The northern boundary of the area (plate 1) is the drainage divide separating these basins from that of the Charles, Neponset, and...
Growth of lake trout in Lake Superior before the maximum abundance of sea lampreys
Jerold F. Rahrer
1967, Transactions of the American Fisheries Society (96) 268-277
The growth in length of lake trout (Salvelinus namaycush) from the inshore water of Lake Superior in 1953 increased with age from the 3rd to 9th year, and was nearly constant from the 9th to the 12th year. Growth was greatest in the 1st year (4.0 inches) and least in...
Yakima basalt of the Tieton River area, south-central Washington
Donald A. Swanson
1967, Geological Society of America Bulletin (78) 1077-1110
Up to 1700 feet of the upper Miocene-lower Pliocene Yakima Basalt of the Columbia River Group underlie much of the eastern flank of the Cascade Range in the Tieton River area, Yakima County, Washington. Local prebasalt relief was more than 1700 feet, so thicknesses of each of the 15...