Skip to main content
U.S. flag

An official website of the United States government

Dot gov

Official websites use .gov
A .gov website belongs to an official government organization in the United States.

Https

Secure .gov websites use HTTPS
A lock ( ) or https:// means you’ve safely connected to the .gov website. Share sensitive information only on official, secure websites.

Search Results

164482 results.

Alternate formats: RIS file of the first 3000 search results  |  Download all results as CSV | TSV | Excel  |  RSS feed based on this search  |  JSON version of this page of results

Page 5524, results 138076 - 138100

Show results on a map

Publication Extents

Not all publications have extents, not all extents are completely accurate
Some aspects of aquatic insect populations of pools and riffles in gravel bed streams in western United States
Bruce W. Lium
1974, Journal of Research of the U.S. Geological Survey (2) 379-384
Relationships were studied between aquatic-insect populations on rocks of different sizes and variations of populations between different stream localities. All aquatic insects were counted and identified on streambed gravels and cobbles chosen at random from four rivers on three to four types of locations ranging from riffles to pools. The...
The soil creep-curved tree fallacy
Richard L. Phipps
1974, Journal of Research of the U.S. Geological Survey (2) 371-377
No evidence has been found in eastern deciduous forests to substantiate statements that curved tree trunks, downslope tilted tree trunks, and upslope trailing tree root systems are the result of soil creep. Curvature and tilting of trunks are described as geotropic and phototropic responses to physical and physiological conditions unrelated...
Occurrence of dissolved organic carbon in selected ground-water samples in the United States
J. A. Leenheer, Ronald L. Malcolm, P. W. McKinley, Lawrence A. Eccles
1974, Journal of Research of the U.S. Geological Survey (2) 361-369
A study of nonvolatile DOC (dissolved organic carbon) in ground water was conducted to establish base levels of naturally occurring dissolved organic materials. Samples of ground water were obtained at 100 sites in 27 States. Samples were pressure filtered at the time of collection and immediately frozen on dry ice....
Spectrophotometric determination of silica at high concentrations using fluoride as a depolymerizer
Leonard Shapiro
1974, Journal of Research of the U.S. Geological Survey (2) 357-360
Solutions containing in excess of 200μg/ml of silica form polymers which do not react with molybdate in the spectrophotometric determination of silica. Fluoride ions catalyze the depolymerization of silica so that precise spectrophotometric determinations of silica can be made, even when silica is present predominantly as polymers....
Spectrophotometric determination of niobium in rocks
L. Paul Greenland, E.Y. Campbell
1974, Journal of Research of the U.S. Geological Survey (2) 353-355
After acid decomposition and evaporation to volatilize silica, samples containing 0.5 6 μg Nb are fused with pyrosulfate and dissolved in hydrochloric acid tartaric acid. Niobium is separated by thiocyanate extraction with amyl alcohol and back-extracting from the organic solvent with dilute hydrofluoric acid. Niobium is reacted with 4-(2-pyridylazo)-resorcinol to...
Chemical variations across the Alaska-Aleutian Range batholith
Bruce L. Reed, Marvin A. Lanphere
1974, Journal of Research of the U.S. Geological Survey (2) 343-352
A study of 79 chemical analyses of plutonic rocks in the northern part of the Alaska-Aleutian Range batholith shows that K2O and SiO2 in Late Cretaceous and Tertiary rocks decrease toward the Pacific margin and that Al2O3 and CaO increase. Plots for Fe2O3, FeO, MgO, and TiO2 suggest a...
Thallium-bearing orpiment, Carlin gold deposit, Nevada
Arthur S. Radtke, Charles M. Taylor, F. W. Dickson, Chris Heropoulos
1974, Journal of Research of the U.S. Geological Survey (2) 341-342
A variety of orpiment, As2S3 , containing a significant amount of thallium has been identified in the unoxidized East ore body of the Carlin gold deposit. The mineral occurs in small veinlets with barite, calcite, quartz, and realgar....
Coloradoite, acanthite, and jarosite from the Cripple Creek district, Teller County, Colorado
Fred A. Hildebrand, Garland B. Gott
1974, Journal of Research of the U.S. Geological Survey (2) 339-340
Coloradoite (HgTe), acanthite (Ag2 S), and jarosite (KFe3(S04)2 (OH)6) have been identified in rocks from the Cripple Creek district, Colorado. Neither acanthite nor jarosite has previously been reported from this mining district. Although the occurrence of coloradoite was reported, its identification was never actually verified. The presence of acanthite may...
Paleozoic tectonics in the Edna Mountain quadrangle, Nevada
R. L. Erickson, S. P. Marsh
1974, Journal of Research of the U.S. Geological Survey (2) 331-337
Geologic mapping at scale 1:24,000 of the Edna Mountain 15-minute quadrangle, Humboldt County, Nev., revealed two episodes of pre-Mesozoic deformation that are difficult to reconcile with either the Antler or the Sonoma orogeny. We believe that the older episode predated the Antler orogeny and may be as old as Late...
The Border Ranges Fault in south-central Alaska
E. M. MacKevett, George Plafker
1974, Journal of Research of the U.S. Geological Survey (2) 323-329
The Border Ranges fault, a major fault of southern Alaska, can be traced for more than 1,000 km arcuately eastward from Kodiak Island to the St. Elias Mountains. Throughout its extent, the fault juxtaposes upper Paleozoic and lower Mesozoic rocks on the north against upper Mesozoic and Tertiary rocks. This...
Generalized geology and structure of the Winkelman 15-minute quadrangle and vicinity, Pinal and Gila Counties, Arizona
M. H. Krieger
1974, Journal of Research of the U.S. Geological Survey (2) 311-321
A. northwest-trending belt of steeply east-dipping Precambrian and Paleozoic sedimentary rocks extends across the Winkelman 15-minute quadrangle and separates areas of contrasting structures. To the southwest for 60 mi is an expanse of Precambrian basement, largely granite; to the northeast the Precambrian and Paleozoic sedimentary rocks are gently tilted and...
Silicoflagellate zonation of upper Cretaceous to lower Miocene deep-sea sediment
David Bukry, J. H. Foster
1974, Journal of Research of the U.S. Geological Survey (2) 303-310
A stratigraphic zonation based on silicoflagellates is proposed for the division of Upper Cretaceous to lower Miocene deep-sea sediments into eight independent zones. The occurrence of silicoflagellate siliceous microfossils from Mesozoic and lower Cenozoic sediment has been poorly known in all but the middle Eocene. The most diagnostic occurrences in...
Artificial Recharge — State of the Art
R. F. Brown, D. C. Signor
1974, Groundwater (12) 152-160
The largest potential reservoir for the storage of potable water is in the unsaturated zone. Use of this space for the storage and retrieval of potable water is a multifaceted problem which requires application of the best talent from the scientific community.Artificial recharge has many similarities to liquidwaste disposal through...
Palaeomagnetism and magnetic–polarity zonation in some Oligocene volcanic rocks of the San Juan Mountains, south–western Colorado
J. F. Diehl, Myrl E. Beck, Peter W. Lipman
1974, Geophysical Journal International (37) 323-332
Palaeomagnetic results have been obtained from thirty sites in intrusive and extrusive rocks of Oligocene age from the San Juan Mountains, south-western Colorado. All specimens from each site were subjected to af demagnetization, and the reliability of each site determined. Twenty-three sites gave reliable results. Because five sites from the...
Tectonic transition zone in the northeastern Caribbean
Michael S. Marlow, Louis E. Garrison, Ray G. Martin, James V. A. Trumbull, Alan K. Cooper
1974, Journal of Research of the U.S. Geological Survey (2) 289-302
Seismic reflection data indicate that the Atlantic plate has been underthrust beneath the Caribbean plate east of the Lesser Antilles. The data further reveal that the transition from underthrust to strike-slip plate motion occurs near lat 19.3° N. and long 62° W. in alinement with the Anegada Trough. Oceanic basement...
Some morphometric properties of experimentally cratered surfaces
Alfred H. Truesdell, Wendy Singers
1974, Journal of Research of the U.S. Geological Survey (2) 279-288
The temperature and chemical conditions (pH, gas pressure, and ion activities) in a geothermal aquifer supplying a producing bore can be calculated from the enthalpy of the total fluid (liquid + vapor) produced and chemical analyses of water and steam separated and collected at known pressures. Alternatively, if a single...
Geochemical indicators of subsurface temperature: Part 2, estimation of temperature and fraction of hot water mixed with cold water
R.O. Fournier, A. H. Truesdell
1974, Journal of Research of the U.S. Geological Survey (2) 263-270
The water in many warm springs with large rates of flow consists of mixtures of hot water that has come from depth and of shallow cold water. Under favorable conditions the original temperature of the hot water and the fraction of the cold water in the mixture can be estimated...
Geochemical indicators of subsurface temperature: Part 1, basic assumptions
R.O. Fournier, D. E. White, A. H. Truesdell
1974, Journal of Research of the U.S. Geological Survey (2) 259-262
The chemical and isotopic compositions of hot-spring water and gas are used to estimate subsurface temperatures. The basic assumptions inherent in the methods are seldom stipulated. These assumptions include (1) a temperature-dependent reaction at depth, (2) a supply of the solid phase involved in the reaction to permit saturation of...
Stabilities of calcite and aragonite
C. L. Christ, P. B. Hostetler, R. M. Siebert
1974, Journal of Research of the U.S. Geological Survey (2) 175-184
A revaluation of the 25° C activity-product constants of calcite (KC) and aragonite (KA) was made on the basis of the known solubilities of these phases for which the activity of total dissolved calcium was corrected for the presence of the ion pair CaHCO3+ in the aqueous phase. The value...
Remote sensing for identification and classification of wetland vegetation
L.M. Cowardin, V.I. Myers
1974, Journal of Wildlife Management (38) 308-314
Multispectral photography and ground truth were obtained on an area 12 miles (19.3 km) east of Bemidji, Minnesota, to identify and map wetlands less than 2 acres (0.8 hectare) in size, to map emergent vegetation in lakes, and to explore the feasibility of classifying vegetation from aerial photographs. Wetlands less...
Effects of radio packages on wild ducks
D.S. Gilmer, I.J. Ball, L.M. Cowardin, J. H. Riechmann
1974, Journal of Wildlife Management (38) 243-252
A total of 211 wild, free-flying mallards (Anas platyrhynchos) and wood ducks (Aix sponsa) were equipped with breast-mounted radio packages during the breeding seasons of 1968-72. Known predation loss was 7.6 and 12.0 percent for mallards and wood ducks respectively, 60 percent occurred within 3 weeks of instrumentation. The highest...
Hydrology and trout populations of cold-water rivers of Michigan and Wisconsin
G. E. Hendrickson, R. L. Knutilla
1974, Transactions of the Wisconsin Academy of Sciences, Arts, and Letters (62) 181-193
Statistical multiple-regression analyses showed significant relationships between trout populations and hydrologic parameters. Parameters showing the higher levels of significance were temperature, hardness of water, percentage of gravel bottom, percentage of bottom vegetation, variability of streamflow, and discharge per unit drainage area. Trout populations increase with lower levels of annual maximum...
Supplemental feeding program for California condors
S.R. Wilbur, W.D. Carrier, J.C. Borneman
1974, Journal of Wildlife Management (38) 343-346
A 2-year supplemental feeding program for the endangered California condor (Gymnogyps californianus) was of insufficient length to definitely show that a dependable food supply will stimulate additional breeding; however, production did increase during the study, and food supply appears a likely cause. Because no undesirable effects of feeding were noted,...
Upland duck nesting related to land use and predator reduction
Harold F. Duebbert, H.A. Kantrud
1974, Journal of Wildlife Management (38) 257-265
Duck nesting was studied during 1971 in north-central South Dakota under four conditions: in idle, five or six year old fields of domestic grass-legume mixtures in an area where predators including the red fox (Vulpes fulva), raccoon (Procyon lotor), striped skunk (Mephitis mephitis), and badger (Taxidea taxus) were (1) reduced...
Estimating survival rates from banding of adult and juvenile birds
Douglas H. Johnson
1974, Journal of Wildlife Management (38) 290-297
The restrictive assumptions required by most available methods for estimating survival probabilities render them unsuitable for analyzing real banding data. A model is proposed which allows survival rates and recovery rates to vary with the calendar year, and also allows juveniles to have rates different from adults. In addition to...