Surface water records of Nepal: Supplement no. 1
Nepal Hydrological Survey Department.
1966, Book
No Abstract available....
Selected flow characteristics of streams in the Willamette River Basin, Oregon
C. H. Swift III
1966, Report
Flow-duration, annual low-flow, and annual high-flow tables through September 30, 1963, are given in this report for 110 stream-gaging stations in the Willamette and Sandy River basins. These tables summarize the basic data needed to define the streamflow characteristics at the gaging stations. The content of each of the three...
Floods of June 24-25, 1966 in southwest-central North Dakota
Orlo A. Crosby
1966, Report
A severe thunderstorm accompanied by much hail swept through southwest-central North Dakota on the afternoon of June 24. Rainfall of up to 13 inches caused floods higher than any previously known in the area. The isohyetal map (fig. 1) indicates the extent and magnitude of the storm. This map was...
Jura tectonics as a décollement
W. G. Pierce
1966, Geological Society of America Bulletin (77) 1265-1276
For many years the structure of the Jura Mountains was interpreted as a décollement whose origin was related to the Alps; in recent years, however, this mode of origin has been questioned. Most of the alternative explanations recognize a décollement to some extent, but attribute it to movement of the...
Insecticide contaminations in wetland habitats and their effects on fish- eating birds
James O. Keith
1966, Journal of Applied Ecology (3) 71-85
An unusual mortality of fish-eating birds occurred at the Tule Lake National Wildlife Refuge in California between 1960 and 1962. Over 1100 dead birds of ten species were found during that period. Investigations of the mortality indicated that birds died as a result of their exposure to toxaphene, which was...
Field continuation and the step model in aeromagnetic interpretation
Roland G. Henderson
1966, Geophysical Prospecting (14) 528-546
Downward continuation of the field in the neighborhood of a singularity of a magnetic anomaly is used to render the anomaly more two‐dimensional, to make the bottom of the causal body more remote, and to obtain an auxiliary function, φ (O, z), by means of which the anomaly may be...
Hydration of natural glass and formation of perlite
I. Friedman, R.L. Smith, W.D. Long
1966, Geological Society of America Bulletin (77) 323-328
The hydration rate of rhyolitic glass has been determined at temperatures ranging from 5° C to 100° C. The relationship between the depth of hydration, x, and time, t is x2 = kt; k varies from 0.4 μ2/103 years at 5° C to 104 μ2/103 years at 100° C; k is independent of the...
The Bandelier Tuff: A study of ash-flow eruption cycles from zoned magma chambers
R.L. Smith, R. A. Bailey
1966, Bulletin Volcanologique (29) 83-103
No abstract available. ...
Tropical lakes, copropel, and oil shale
W.H. Bradley
1966, GSA Bulletin (77) 1333-1337
During a long-continued study of the lacustrine beds of the Eocene Green River Formation, I have tried to interpret past events from observation of present-day processes. After a search of some 40 years, four lakes have been found that are producing a kind of organic ooze judged to be a...
Geologic evaluation of aerial radar photographs of southwestern Oregon
William P. Irwin
1966, General Technical Report NASA-23
No abstract available....
Geology of the Klamath Mountains province
E. H. Bailey
1966, California Division of Mines and Geology Bulletin 190
No abstract available....
Pesticide residues in the ecosystem
E. H. Dustman, Lucille F. Stickel
S. Breth, editor(s)
1966, Book chapter, Pesticides and their effects on soils and water
Pesticide residues have become a component of nearly all living organisms. Nearly all California birds and fish collected in a 1963 pesticide survey contained residues. Discovery of DDT and metabolites in Antarctic animals in 1964 pushed the distribution of pesticides to the remotest portions of the globe. Exchange of pesticides...
San Andreas Fault from San Francisco to Hollister
E. E. Brabb, M. Maddock, R. E. Wallace
1966, California Division of Mines and Geology Bulletin 190
No abstract available....
Sediment transport in a Precambrian ice age: The Huronian Gowganda Formation
David A. Lindsey
1966, Science (154) 1442-1443
The Gowganda Formation of Ontario consists of conglomerates, quartzites, and argillites deposited in a glacial environment. The distribution of varved argillites and silty limestones suggests continental and marine facies, respectively. Pebble and ripple-drift orientations, distribution of limestones, striated pavements, distribution of the underlying Bruce Group, and Huronian quartzite paleocurrents support...
Copper artifacts from prehistoric archeological sites in the Dakotas
W.E. Hill Jr., R.W. Neuman
1966, Science (154) 1171-1173
Thirteen archeological specimens were analyzed spectrographically, and within defined limits they were determined to be native copper. Twelve of the specimens show close elemental homogeneity and are believed to be of Lake Superior ore; the origin of the other specimen is devious....
Development of permeability and storage in the tertiary limestones of the southeastern states, USA
H. E. LeGrand, V. T. Stringfield
1966, International Association of Scientific Hydrology - Bulletin (11) 61-73
Permeability and storage characteristics in the Tertiary limestone system of southern United States have developed progressively but non-uniformly as circulation of water and solution in the limestone have changed during the geologic and hydrologic history.The limestone formations, predominantly of Eocene age and subordinated of Oligocene and Miocene age, are widespread...
Circular patterns and exfoliation in crystalline terrane, Grandfather Mountain area, North Carolina
John T. Hack
1966, Geological Society of America Bulletin (77) 975-986
Aerial photographs of areas of crystalline rock in the Piedmont and Blue Ridge of western North Carolina reveal numerous large-scale arcuate, circular, and elliptical patterns with diameters from 1000 to more than 4000 feet. They are commonly defined by curving streams, curving ridges, and curving belts of contrasting vegetation. Geologic mapping shows that the circular patterns are not related to primary geologic structures;...
Volcanism in the western San Juan Mountains, Colorado
R. G. Luedke, W. S. Burbank
1966, Bulletin Volcanologique (29) 345-346
Three major cycles of volcanism during the Miocene and Pliocene formed a layered succession of calc-alkaline eruptive materials in the western San Juan Mountains nearly 1.5 miles thick and having a volume greater than 1,000 cubic miles. Each cycle was characterised by major eruptions followed by subsidence in the vent areas, and the resulting structure was a great volcanic plateau surrounding...
Hot shadows on Jupiter
W.T. Plummer, R. Wildey
1966, Science (153) 1418-1419
No abstract available. ...
Crustal study of a continental strip from the Atlantic Ocean to the Rocky Mountains
I. Zietz, Elizabeth R. King, Wilburt Geddes, E.G. Lidiak
1966, Geological Society of America Bulletin (77) 1427-1447
Twenty aeromagnetic profiles over a 100-mile-wide strip along the arc of a great circle passing through Denver, Colorado, and Washington, D. C, reveal large anomalies of major crustal significance. Contoured data disclose several areas of distinct magnetic patterns reflecting basement lithology and structure. The mafic rocks of the Blue Ridge and Piedmont and the Keweenawan mafic belt in...
Magnetic data on the structure of the central Arctic Region
E. R. King, I. Zietz, L.R. Alldredge
1966, Geological Society of America Bulletin (77) 619-646
A study of 23,000 miles of total intensity aeromagnetic profiles in the central Arctic has been made by the U. S. Geological Survey and the U. S. Coast and Geodetic Survey. The profiles were flown at 20,000 feet above sea level and cover approximately 1,350,000 square miles of the Arctic Ocean between the North Pole...
Geochronology of the St. Kevin granite and neighboring precambrian rocks, northern Sawatch Range, Colorado
R. C. Pearson, C. E. Hedge, H.H. Thomas, T.W. Stern
1966, Geological Society of America Bulletin (77) 1109-1120
Radiometric ages have been measured on rocks of a crystalline terrane that includes ancient gneisses and migmatites, two granitic batholiths (St. Kevin Granite and granite of Cross Creek), and various minor intrusive rocks. A whole-rock Rb-Sr isochron age on the St. Kevin Granite establishes it as 1390 ± 60 m.y. old. Mineral ages on the St. Kevin and numerous other rocks are either about the same as the St. Kevin whole-rock age...
Large-scale basin-and-dome pattern resulting from the interference of major folds
O. T. Tobisch
1966, Geological Society of America Bulletin (77) 393-408
The geometry of individual major folds from the Glen Cannich area in the Northern Highlands of Scotland is described. The major folds are isoclinal, and their axial planes and fold limbs strike north or northeast and dip steeply; the fold axes plunge steeply toward the south or southeast. If pairs of individual folds are joined along a common axial-plane trace they form basins, domes, or other unusual...
Eclogitic pyroxenes, ordered with P2 symmetry
J. R. Clark, J. J. Papike
1966, Science (154) 1003-1004
X-ray diffraction crystal-structure analysis of omphacite from eclogite, Tiburon Peninsula, Marin County, California, shows that this clinopyroxene has P2 symmetry with a nearly ordered distribution of the multiple cation content defined by its approximate formula: (Na0.5Ca0.5) (Mg0.4Fe2+0.1Al0.4Fe3+0.1)Si2O6. Na+ and Ca2+ tend to assume alternate locations in the structure, and...
Absence of neutral alkali atoms in rhodizite
G. Donnay, A. N. Thorpe, F. E. Senftle, R. Sioda
1966, Science (154) 889-890
The formula CsB12Be4Al4O28 has been proposed by others for the mineral rhodizite. Electron-spin-resonance and magnetic susceptibility measurements prove the absence of neutral cesium atoms. An ionic formula CsB11Be4Al4O26(OH)2 is proposed....