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Page 6579, results 164451 - 164475

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Publication Extents

Not all publications have extents, not all extents are completely accurate
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...
Sulfide-mineral zoning in the basal nonesuch shale, Northern Michigan
W. S. White, J.C. Wright
1966, Economic Geology (61) 171-1190
A zone, 1 to 50 feet thick, at the base of the Nonesuch Shale, is relatively rich in copper, chiefly as chalcocite. Pyrite is the characteristic sulfide mineral of the overlying 400 to 600 feet of the formation. The boundary of the cupriferous zone with the pyrite zone regionally transgresses both stratigraphic layering and fades gradations indicative...
Observations on the Life History of Ogcodes rufoabdominalis in Northern Utah (Diptera: Acroceridae)
K.J. Capelle
1966, Journal of the Kansas Entomological Society (39) 641-649
Detailed observations were made on the emergence and feeding habits of the acrocerid parasite Ogcodes rufoabdominalis from lycosid spiders. One hundred and twenty field-collected hosts yielded six parasites in May. Eggs, first and third instars, and pupae are described for the first time, as well as mating and oviposition....
Proportion of recovered goose and brant bands that are reported
R. K. Martinson, J.A. McCann
1966, Journal of Wildlife Management (30) 856-858
A few more than one-third of the goose and brant bands recovered by hunters were reported to the Bird Banding Laboratory (a rate of 0.361) during the 1962-64 hunting seasons. We calculated this band-reporting rate by comparing the estimated number of goose and brant bands recovered by hunters, based on...
Flexible plastic collars compared to nasal discs for marking geese
G.A. Sherwood
1966, Journal of Wildlife Management (30) 853-855
Construction of a flexible plastic collar for marking geese is described. The usefulness of the collars, tried on 468 Canada geese (Branta canadensis) at the Seney National Wildlife Refuge from 1963 to 1965, was compared with that of nasal discs attached to 361 Canada geese at Seney in 1961 and...
Breeding ecology of the redhead duck in western Montana
J. T. Lokemoen
1966, Journal of Wildlife Management (30) 668-681
The habits of the redhead duck (Aythya americana) were studied in the Flathead Valley of western Montana in 1960 and 1961 to determine their habitat preferences in this pothole breeding ground. The 2,600-acre study area, surrounding the Ninepipe Reservoir, contained 686 potholes. Redheads usually were paired by the time they...
Use of analog model to predict streamflow depletion, big and little Blue River basin, Nebraska
P. A. Emery
1966, Groundwater (4) 13-19
The States of Nebraska and Kansas are negotiating a compact for apportionment of the waters of the Big and Little Blue Rivers. So that the negotiating officials could allocate the water equitably, the amount of streamflow depletion caused by ground‐water withdrawals upgradient from the State line needed to be determined. At the request of the Nebraska officials, the U. S. Geological Survey...
Frequency distribution of dissolved solids in ground water
G.H. Davis
1966, Groundwater (4) 5-12
The frequency distribution of dissolved‐solids content of ground waters in geologically and climatologically homogeneous terrane units commonly approximates a log‐normal distribution. A graphic logarithmic transformation is de‐scribed which permits rapid calculation of approximate values for the mean, standard deviation, and coefficient of variation. Statistical parameters calculated by this method show good agreement with known physical conditions in the terranes studied and are...
The effect of climate on drainage density and streamflow
C.W. Carlston
1966, International Association of Scientific Hydrology - Bulletin (11) 62-69
Sir Charles Cotton (1964) has pointed out that in an earlier paper (Carlston, 1963) which related drainage density to hydrology, there was insufficient emphasis on the role of climate in its effect on drainage density. Re-examination of the relation of drainage density to base flow in the 15 basins originally...
Dawsonite in the green river formation of Colorado
J.W. Smith, C. Milton
1966, Economic Geology (61) 1029-1042
Dawsonite NaAl(OH)2C03 is a rare mineral that occurs in relative abundance over hundreds of square miles in the Piceance Creek Basin of northwestern Colorado, as a rock-forming constituent of the oil shales in the green River Formation. In some specimens it makes up 25 percent by weight of the shale....
Isotopic study of galenas from the upper Mississippi Valley, the Illinois-Kentucky, and some Appalachian Valley mineral districts
A. V. Heyl, M.H. Delevaux, R. E. Zartman, M. R. Brock
1966, Economic Geology (61) 933-961
Analyses of lead isotopes in galena in carbonate rock ore deposits collected from several mineralized districts in the Central and Eastern Interior of the United States support previous studies in establishing that the galena is anomalously radiogenic ("J"type")- This study, using care-fully selected samples to test some géologie relationships, shows region-wide and distrietwide systematic variations in isotope...
Phase relations involving sphalerite in the Fe-Zn-S system
P. B. Barton Jr., Priestley Toulmin
1966, Economic Geology (61) 815-849
The equilibrium diagram for the Fe-Zn-S System has been worked out in détail from 580° to 850° C. Previous work on this System is proven to be seriously in error and températures heretofore estimated from the "sphalerite geothermometer" are without a sound quantitative foundation. Sphalerite solid solutions lie essentially along the FeS-ZnS join. Neither pyrite nor pyrrhotite takes up appréciable amounts of...
Breeding behavior of immature mourning doves
Harold D. Irby, Lytle H. Blankenship
1966, Journal of Wildlife Management (30) 598-604
Some immature mourning doves (Zenaidura macroura) are capable of breeding in their first (calendar) year of life. The breeding activities of immatures observed in this study included calling, copulating, and nesting. Development of sexual structures such as cloacal papillae, oviduct openings, and gonads was also regarded as evidence of breeding...
An analysis of ground‐water fluctuations caused by ocean tides in Glynn County, Georgia
D. O. Gregg
1966, Groundwater (4) 24-32
The tidal efficiencies of wells tapping the principal artesian aquifer in Glynn County, Georgia decrease with distance from the influencing tidal body and also decrease with well depth. Although the magnitude of water‐level fluctuation of these wells is largely dependent upon the distance to a large tidal body, the time of a high or a low water level in the wells is...
Pumping test methods for determining aquifer characteristics
S.M. Lang
1966, ASTM Special Technical Publication 35-55
Data describing the shape and manner in which the cone of depression forms about a well discharging at a constant rate are used with various formulas to determine the hydraulic characteristics of aquifer materials. The solutions to these formulas generally are graphical and may be used to detect the presence of hydraulic or geologic...
Digital computer methods for water‐quality data
C.O. Morgan, R.J. Dingman, J.M. McNellis
1966, Groundwater (4) 35-42
The digital computer is used on a routine basis in the ground-water program in Kansas for tasks ranging from the listing of water-quality data in tabular and publishable form to statistically and graphically analyzing a mass of data.In the past year a number of computer programs in FORTRAN IV have...
Use of type curves developed from electric analog studies of unconfined flow to determine the vertical permeability of an aquifer at Piketon, Ohio
S.E. Norris, Richard E. Fidler
1966, Groundwater (4) 43-48
A type‐curve method for determining anisotropy of unconfined aquifers, developed from electric analog simulation, is applied to drawdowns observed near, a well pumping from a glacial outwash aquifer at Piketon, Ohio. The coefficient of vertical permeability, P z'averaged 365 gpd per square foot. Computed drawdown for the pumped well, based on this value, differed by only a small amount from the observed drawdown. The coefficient...