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Page 6598, results 164926 - 164950

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Publication Extents

Not all publications have extents, not all extents are completely accurate
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....
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...
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...
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...
Calcium and bromide contents of natural waters
R.J. Anderson, D. L. Graf, B.F. Jones
1966, Science (153) 1637-1638
The linear relation observed in a log Ca++ versus log Br- plot for subsurface Cl- waters is attributed to ultrafiltration by shale of sea water and fresh water that have passed through sedimentary rocks since their formation. Reactions between these solutions and sedimentary minerals, particularly dolomitization, must have contributed additional Ca++ to solution....
Airborne geophysical study in the Pensacola Mountains of Antarctica
John C. Behrendt, L. Meister, J. R. Henderson
1966, Science (153) 1373-1376
A seismic reflection, gravity, and aeromagnetic reconnaissance was made in the Pensacola Mountains, Antarctica, during the 1965-66 austral summer. Prominent ice streams located between the Neptune and Patuxent Ranges and east of the Forrestal Range overlie...
Genetic relations of oceanic basalts as indicated by lead isotopes
M. Tatsumoto
1966, Science (153) 1094-1101
The isotopic compositions of lead and the concentrations of lead, uranium, and thorium in samples of oceanic tholeiite and alkali suites are determined, and the genetic relations of the oceanic basalts are discussed. Lead of the oceanic tholeiites has a varying lead-206 : lead-204 ratio between 17.8 and 18.8, while...
Oxygen fugacities directly measured in magmatic gases
M. Sato, T. L. Wright
1966, Science (153) 1103-1105
An electrochemical device was used to measure the fugacity of oxygen (fO2) in holes drilled through the crust of Makaopuhi lava lake, Kilauea Volcano, Hawaii. Results obtained within 6 months of the lake formation show that log fO2 normally varies linearly with the reciprocal of the absolute temperature, and that chemical changes...
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....
Luna 9 photographs: Evidence for a fragmental surface layer
D. E. Gault, W.L. Quaide, V.R. Oberbeck, H. J. Moore
1966, Science (153) 985-988
The morphological features of the lunar surface photographed by Luna 9 indicate a surficial layer of weakly cohesive to noncohesive fragmental material. Most of this material is finer than a centimeter and probably finer than a few millimeters, although objects of centimeter size and larger are plentiful....
Exposure of basement rock on the continental slope of the Bering Sea
D.W. Scholl, E. C. Buffington, D.M. Hopkins
1966, Science (153) 992-994
Profiles of repetitive seismic reflections reveal that the Bering continental slope, outer shelf, and rise overlay an acoustically reflective "basement" which extends at least 750 kilometers parallel to the trend of the slope. This acoustic basement is usually covered by several hundred meters of stratified sediments at the top and...
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...
Drifting organisms in the Precambrian Sea
D.J. Milton
1966, Science (153) 293-294
Drag marks in the Upper Precambrian Winnall Beds of central Australia were made by semibuoyant flexible objects at least 15 centimeters long, which presumably were algae. This find extends the range of such marks into the Precambrian era and supplements the discovery of microflora in the same sedimentary sequence....
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...