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Page 6354, results 158826 - 158850

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Not all publications have extents, not all extents are completely accurate
Thrust and strike-slip faulting in the Plomosa Mountains, southwestern Arizona
F. K. Miller, Edwin H. McKee
1971, Bulletin of the Geological Society of America (82) 717-722
Thrust and strike-slip faulting are recognized in the Plomosa Mountains, southwestern Arizona. The distribution of rock types and the geometry of the thrust faults necessitate that the upper plate moved from east to west. The amount of displacement is not known, but is considered to...
Nomenclature and correlation of some upper Precambrian and basal Cambrian sequences in western Utah and southeastern Idaho
Max D. Crittenden Jr., Frederick E. Schaeffer, D. E. Trimble, Lee A. Woodward
1971, Bulletin of the Geological Society of America (82) 581-602
Recent stratigraphic studies in three widely separated localities in southeastern Idaho and western Utah have revealed a startling continuity of both individual rock units and of rock sequences over a distance of some 300 mi parallel to the strike of a late Precambrian and Cambrian depositional trough. Between 15,000 and...
A further revision of the stratigraphic nomenclature of the Wissahickon Formation in Maryland
Michael W. Higgins, George Wescott Fisher
1971, Bulletin of the Geological Society of America (82) 769-774
The Wissahickon Formation, the thickest and most extensive unit of the Glenarm Series, was divided into lithofacies several years ago. We suggest revision of two of these lithofacies and addition of another. We also suggest that the term lithofacies be shortened to facies. The added...
The functional significance of movements and positions of the pinnae of the African Elephant, Loxodonta africana
I.O. Buss, James A. Estes
1971, Journal of Mammalogy (52) 21-27
Observations of wild African elephants (Loxodonta africana) in Uganda indicated that flapping and spreading the highly vascularized ears are probably important functions for heat dissipation. Ear flapping increased as ambient temperatures rose and decreased or ceased during cold or rainy weather. Rate of ear flapping was inversely related to wind...
Lunar metallic particle ("mini-moon"): An interpretation
D.S. McKay, J.L. Carter, W.R. Greenwood
1971, Science (171) 479-480
A troilite-rich nickel-iron particle ("mini-moon") recovered from the moon may be a mound detached from a sphere of silicate glass. Erosion and pitting of the particle may have been caused by passage through a cloud of hot gas and particulate matter formed by meteorite impact on the lunar surface. This...
Deformation of lee-side laminae in eolian dunes
Edwin D. McKee, John R. Douglass, Suzanne Rittenhouse
1971, Bulletin of the Geological Society of America (82) 359-378
Processes responsible for structures in sand dunes consist of (l) primary deposition by saltation and creep and by settling from suspension, (2) redeposition accompanying avalanching, and (3) penecontemporaneous erosion. Characteristics of dune structures were examined in the field by introducing marker beds of magnetite at times of sand deposition, thus...
Related strontium isotopic and chemical variations in oceanic basalts
Zell E. Peterman, Carl E. Hedge
1971, Bulletin of the Geological Society of America (82) 493-499
Sr87/Sr86 values in oceanic basalts range from 0.7012 to 0.7057 and correlate with basalt composition as measured by the ratio K2O/(Na2O + K2O). The distribution of data points on this plot can be approximated by the following ranges in Sr87/Sr86 and K2O/(K2O + Na2O) respectively: (l) ocean...
Interstitial water studies on small core samples, Deep Sea Drilling Project, Leg 6
F.T. Manheim, F.L. Sayles
1971, Initial reports of the Deep Sea Drilling Project (6) 811-821
Sediments from Leg 6 sites, west of the Hawaiian Islands, consisted primarily of various combinations of deep-sea biogenic oozes, volcanic ash, and its breakdown products. Pore fluids from most of the sites were similar in composition to present day ocean water, and in some sties almost identical. However, interstitial fluids...
Coronadite — Modes of occurrence and origin
D. F. Hewett
1971, Economic Geology (66) 164-177
The lead manganate, "coronadite," was first recognized at the Coronado mine in the Morenci district, Arizona, by Lindgren in 1903. Several years later, the identity of the mineral was questioned and it was not until 1932 that Orcel recognized it in material from Morocco. Since...
Pacific geomagnetic secular variation
Richard R. Doell, A. Cox
1971, Science (171) 248-254
We have considered several different types of records of long-period geomagnetic secular variation: direct measurements made in geomagnetic observatories; paleomagnetic measurements on Hawaiian lava flows with accurately known ages in the interval 0 to 200 years; paleomagentic measurements on Hawaiian lava flows with loosely determined ages within the interval 200...
Floods in the Wapsipinicon River Basin, Iowa
Harlan H. Schwob
1971, Report
Flood information is reported for 338 miles of the main stem and six tributaries of the Wapsipinicon River. The information will be of use to those concerned with the design of bridges and other structures and the conduct of various operations on the flood plains of the streams. Included in...
Sedimentation in the Middle Fork Eel River Basin, California
J. M. Knott
1971, Report
The Middle Fork Eel River basin has a drainage area of 753 square miles and is in a mountainous area on the western flank of the coast ranges in northern California. Elevations in the basin range from about 860 feet above mean sea level at the confluence with the Eel...