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Page 6031, results 150751 - 150775

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Paleozoic seas of central Idaho
Clyde P. Ross
1962, Geological Society of America Bulletin (73) 769-793
Some recent paleogeographic maps indicate that central Idaho was part of a major geosyncline throughout Paleozoic time. This concept, apparently based on thick marine accumulations far apart on the margins of the region, is inconsistent with field data. Within the area of the Idaho batholith, Permian(?) volcanic rocks rest either on batholithic rocks...
Magnetic anomalies and magnetizations of the Biwabik iron-formation, Mesabi area, Minnesota
G. D. Bath
1962, Geophysics (27) 627-650
In a study of the relationship of magnetic anomalies to the magnetite content and structure of layered Precambrian iron-formations, the effective induced and remanent magnetizations of the Biwabik iron-formation were determined by analyses of aeromagnetic anomalies recorded 1,000 ft above the Biwabik in areas of known geology. The induced magnetization along the layers is relatively insignificant...
Erosion on miniature pediments in badlands national monument, South Dakota
S. A. Schumm
1962, Bulletin of the Geological Society of America (73) 719-724
Measurements of erosion on miniature pediments in Badlands National Monument, South Dakota, show that during almost eight years, the pediments were lowered by sheetwash. The adjacent hillslopes have retreated leaving a belt of newly formed pediment from 6 to 12 cm wide at their bases. The hillslopes are rough and relatively permeable; the <span...
Tertiary landslides, northwestern South Dakota and Southeastern Montana
J. R. Gill
1962, Bulletin of the Geological Society of America (73) 725-735
Landslide blocks of latest Oligocene or earliest Miocene age are preserved at several localities in northwestern South Dakota and southeastern Montana. These tilted blocks contain Late Cretaceous to late Oligocene rocks and are unconformably overlain by nearly horizontal strata of the Arikaree Formation of Miocene age. Undisturbed rocks of late Oligocene...
Temperature correction in conductivity measurements
Stanford H. Smith
1962, Limnology and Oceanography (7) 330-334
Electrical conductivity has been widely used in freshwater research but usual methods employed by limnologists for converting measurements to conductance at a given temperature have not given uniformly accurate results. The temperature coefficient used to adjust conductivity of natural waters to a given temperature varies depending on the kinds...
Correlation of the Carrizo Sand in Arkansas and adjacent states
R.L. Hosman
1962, Geological Society of America Bulletin (73) 389-394
The Carrizo Sand (Eocene), the basal unit of the Claiborne Group, can be recognized in the subsurface throughout much of southeastern Arkansas and is correlated with the Carrizo Sand of Louisiana and the Meridian Sand Member of the Tallahatta Formation of Mississippi. The term Carrizo Sand is appropriate for use in Arkansas, as the stratigraphic terminology...
Lava tree molds of the September 1961 eruption, Kilauea Volcano, Hawaii
James G. Moore, D.H. Richter
1962, GSA Bulletin (73) 1153-1158
Well-developed lava tree molds were formed during the September 1961 eruption along the east rift zone of Kilauea Volcano. The upright molds were produced where fluid lava, flowing through dense tropical forest, became chilled against the larger trees and tree ferns and later drained away. Where the lava ponded temporarily...
Metallogenetic provinces of Chile, S. A
F. C. Martinez-Ruiz, G. E. Ericksen
1962, Economic Geology (57) 91-106
The metalliferous deposits of Chile tend to be restricted to well denned metallogenetic provinces, each characterized by a dominant mineral or mineral assemblage. The most important ore deposits are those of copper, iron, silver, gold, and manganese. The primary minerals are few in number and most are simple sulfides and...
Records of wells and ground-water quality in Burlington County, New Jersey
F. Eugene Rush
1962, Report
<This basic-data report is limited to the presentation of selected drillers' logs and their geologic correlations, well data, and chemical analyses of water from wells in Burlington County, N. J. The county lies within the Coastal Plain province; it is underlain by unconsolidated sediments of Quarternary, Tertiary, and Cretaceous...
Generalized structure contour maps of the New Jersey coastal plain
Hoarce G. Richards, F. H. Olmsted, James L. Ruhle
1962, Geologic report (New Jersey) 4
Twelve generalized structural contour maps were prepared from a study of 169 well logs or sample logs of drill cuttings from the Coastal Plain of New Jersey, Delaware, and the E astern Shore of Maryland. The configuration of the tops of the nonmarine Cretaceous deposits (Patuxent , Patapsco, Raritan, and Magothy formations) and...
Physical properties of evaporite minerals
Eugene C. Robertson
1962, Trace Elements Investigations 821
The data in the following tables were abstracted from measurements of physical properties of evaporite minerals or of equivalent synthetic compounds. The compounds considered are the halide and sulfate salts which supposedly precipitated from evaporating ocean water and which form very extensive and thick "rock salt" beds. These beds are...
Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah
L.C. Huff, F. G. Lesure
1962, Economic Geology (57) 226-237
Uranium-vanadium deposits in the Salt Wash Member of the Morrison Formation in Montezuma Canyon, San Juan County, Utah, exhibit zoning that is interpreted as a result of metal transport by diffusion. The concentric zones consist of a brown nonmineralized core, an olive-gray mineralized shell, and a gray nonmineralized outer zone. The...
Diatremes and uranium deposits in the Hopi Buttes, Arizona
Eugene Merle Shoemaker, C. H. Roach, F. M. Byers Jr.
A.E.J. Engel, Harold L. James, B. F. Leonard, editor(s)
1962, Book chapter, Petrologic studies: A volume in honor of A. F. Buddington
The Hopi Buttes diatremes erupted in a shallow lake that was filled in as volcanic activity progressed in Pliocene time. At the end of the period of volcanism the landscape included low lava domes capping some of the diatremes, a few flows, and numerous craters of the maar type, surrounded...
Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid
D. B. Stewart, E. H. Roseboom Jr.
1962, Journal of Petrology (3) 280-315
Geological and experimental evidence indicate that the three-phase field, plagioclase-alkalifeldspar-liquid, may terminate in several different ways. The possible terminations have been developed from Schreinemakers' rules governing the disappearance of three-phase fields. In igncous rocks, these different terminations may arise from variations in the relative amounts of additional components in magmas, or from...