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Page 2424, results 60576 - 60600

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Nodal tidal cycle of 18.6 yr.: Its importance in sea-level curves of the east coast of the United States and its value in explaining long-term sea-level changes
Clifford A. Kaye, Gary W. Stuckey
1973, Geology (1) 141-144
The 18.6-yr cycle of the Moon's nodes dominates the annual means of high water, low water, and range at Boston and at other East Coast harbors. The maxima and minima of the high-water and range curves agree closely with the 180° and 0° long. yr, respectively, of the Moon's ascending...
Flow characteristics of a subsurface-controlled recharge basin on Long Island, New York
Robert C. Prill, Donald B. Aaronson
1973, Journal of Research of the U.S. Geological Survey (1) 735-744
Ponding studies at the Woodbury recharge basin on Long Island, N.Y., show that the principal zones controlling infiltration are a surface-loam stratum and an intermediate gravelly, sandy loam stratum. The saturated hydraulic conductivities of these strata are 0.90 and 0.1 ft per day, respectively. The surface loam acts as the principal zone controlling infiltration until...
Problems of underground storage of wastes
Raymond L. Nace
1973, Journal of Research of the U.S. Geological Survey (1) 719-723
Problems of underground storage of waste involve geology in its broadest sense, including hydrology, geochemistry, and geophysics. Wastes may be solid, liquid, or gaseous, and they may be chemically toxic or noxious, esthetically offensive, or radioactive. Some wastes require only temporary containment, whereas others must be isolated for indefinitely long periods. The means and locale...
Loss of volatiles during fountaining and flowage of basaltic lava at Kilauea Volcano, Hawaii
Donald A. Swanson, Brent P. Fabbi
1973, Journal of Research of the U.S. Geological Survey (1) 649-658
The amount of water and sulfur in pumice erupted during periods of vigorous activity during the 1969-71 Mauna Ulu eruption varied inversely with fountain height because of degassing during the fountaining. The pumice lost about 0.05 wt percent water and 0.003 wt percent sulfur during fountaining to heights of 400-540 m. Analyses suggest that the...
Fluorescent spectroscopy, a technique for characterizing surface films
Marvin C. Goldberg, David H. Devonald III
1973, Journal of Research of the U.S. Geological Survey (1) 709-717
A relationship is established between fluorescent spectra obtained by using a light path through the liquid solution and the fluorescent spectra obtained by a direct reading of surface reflection (remote sensing). A brief review of quantum fundamentals provides the necessary information to conclude that "see-through" and reflectance spectra are identical in wavelength response. Many floating...
Effects of migratory waterfowl on water quality at the Montezuma National Wildlife Refuge, Seneca County, New York
Mark A. Have
1973, Journal of Research of the U.S. Geological Survey (1) 725-734
This study was done in response to the shellfish industry's concern that bacteria in effluent from the national wildlife refuges along the northeast coast of the United States may be adversely affecting the harvest of shellfish. A line graph shows inconsistent relationships between bird population at the Montezuma refuge and total coliform, fecal coliform, and...
An accurate Invar-wire extensometer
W. A. Duffield, Robert O. Burford
1973, Journal of Research of the U.S. Geological Survey (1) 569-577
Stevens Type F water-level recorders have been modified to measure changes in the distance between two points, with amplification of up to 10 times. Such recorders are capable of measuring strains of 10-5 and possibly 10-6 over 10-m distances when corrections are made for frictional effects and temperature. In two...
Karst hydrology: A review
H. E. LeGrand, V. T. Stringfield
1973, Journal of Hydrology (20) 97-120
Karst regions of the world are characterized by limestones and other soluble rocks at or near land surface that have been modified by solutional erosion. Such surface features as sinks, long dry valleys, sparse streams, and bare rock and such subsurface features as caverns, arterial solution openings leading to large...
Water projects design with inadequate data: Madrid, Spain June 4-9, 1973
I. C. James II
1973, Eos, Transactions, American Geophysical Union (54) 935-937
The Symposium on the Design of Water Resources Projects with Inadequate Data drew 300 participants, representing more than 60 countries. The symposium was planned within the framework of the International Hydrological Decade and was convened by Unesco and WMO. Organization of the symposium was carried out by Unesco and the...
Stable isotope and chemical relations during mineralization in the Bodie mining district, Mono County, California
J. R. O’Neil, M.L. Silberman, B.P. Fabbi, C. W. Chesterman
1973, Economic Geology (68) 765-784
Stable isotope and chemical relations have been determined in a typical epithermal Au-Ag deposit located in the Bodie mining district of California. Analyses were made of altered host rocks, vein minerals, alteration clays, fluid inclusions, modern spring waters, and unaltered rocks of the area.The results indicate that a hydrothermal convection...
Tests of rhodamine WT dye for toxicity to oysters and fish
Garald G. Parker Jr.
1973, Journal of Research of the U.S. Geological Survey (1) 499-499
Because of the toxicity to oyster larvae and eggs of rhodamine B dye in concentrations greater than 1 mg/l in earlier tests, there was a concern that rhodamine WT, a similar tracer dye, would have a detrimental effect on marine life being developed under the aquaculture program of the Lummi...
Aquifer diffusivity of the Ohio River alluvial aquifer by the flood-wave response method
Harold H. Zehner, Hayes F. Grubb
1973, Journal of Research of the U.S. Geological Survey (1) 597-601
Aquifer diffusivity (T/S) was calculated for 10 sites in the alluvial aquifer adjacent to the Ohio River by observing the response of the aquifer to a flood wave in the river. The calculated type curves matched the observed aquifer response reasonably well at eight of the 10 sites. The diffusivities ranged from 0.4 ft2...
A study of the distribution of the polychlorinated biphenyls in the aquatic environment
Hans J. Crump-Wiesner, Herman R. Feltz, Marvin L. Yates
1973, Journal of Research of the U.S. Geological Survey (1) 603-607
Data gathered from monitoring activities and project studies indicate the ubiquitous occurrence and distribution of polychlorinated biphenyls in the aquatic environment. Residues have been detected in samples from 19 States, representing nearly every region of the country. Concentrations ranged from 0.1 to 4.0 ug/l in unfiltered water samples and 5.0 to 3,200 ug/kg in bottom...
Soda Creek springs - metamorphic waters in the eastern Alaska Range
D.H. Richter, D.E. Donaldson, R.A. Lamarre
1973, Journal of Research of the U.S. Geological Survey (1) 523-528
The Soda Creek springs are a group of small, cold mineral springs on the southern flank of the eastern Alaska Range. The spring waters contain anomalous concentrations of carbon dioxide, sodium, chlorine, sulfate, boron, and ammonia and are actively precipitating deposits of calcite and aragonite. Sparingly present in these deposits are mixed-layer illite-montmorillonite clays and...
Methane in Lake Kivu: New data bearing on its origin
W.G. Deuser, E.T. Degens, G.R. Harvey, M. Rubin
1973, Science (181) 51-54
Lake Kivu, an African rift lake, contains about 50 cubic kilometers of methane (at standard temperature and pressure) in its deep water. Data resulting from two recent expeditions to the lake and a reevaluation of earlier data suggest that most of the methane was formed by bacteria from abiogenetic carbon...
Hydraulics of sheetlike solution cavities
Gerald K. Moore
1973, Groundwater (11) 4-11
The sheetlike solution cavities that supply water to most wells in central Tennessee are 100 to 2,500 feet wide and less than 0.2 inch high. These dimensions have a scale similar to those in Hele-Shaw models. Both logical and mathematical evidence indicate laminar ground-water flow, except close to pumping wells....
Ground water and geology of Baraga County, Michigan
C. J. Doonan, J.R. Byerlay
1973, Water Investigation 11
Most wells In Baraga County obtain water from beds of sand and gravel in morainal and lakebed deposits or from the Jacobsville Sandstone. Yields of wells range from a few to as much as 115 gallons per minute, but most wells probably yield less than 10 gpm. Large areas, where...
Origin of andesitic and granitic magmas in the northern Sierra Nevada, California
Anna Hietanen
1973, Geological Society of America Bulletin (84) 2111-2118
The early magmas of the northern Sierra Nevada, calc-alkaline andesite of island-arc type and its derivatives, all low in potassium, were generated during the Devonian(?) period, possibly along an eastward-dipping sub-duction zone. These magmas could have been derived from mantle peridotite of the continental plate by introduction of water from...
Petrogenesis of the Superstition-Superior volcanic area as inferred from strontium- and oxygen-isotope studies
John S. Stuckless, James R. O’Neil
1973, Geological Society of America Bulletin (84) 1987-1997
Apparent initial Sr87/Sr86 ratios of five ash-flow tuffs (0.7063 to 0.7139) and several mafic to silicic lavas (0.7055 to 0.7131) indicate that the magmas were derived below the base of the Precambrian granitic crust (0.7231 to 1.0906). Liquidus compositions in the system Q-Or-Ab-H2O and oxygen-isotope geother-mometry suggest that the silicic magmas...
Phase relations of basalts in their melting range at PH2O = 5 kb as a function of oxygen fugacity: Part I. Mafic phases
Rosalind Tuthill Helz
1973, Journal of Petrology (14) 249-302
The phase relations of three basalts, the Picture Gorge tholeiite, the 1921 Kilauea olivine tholeiite, and the 1801 Hualalai alkali basalt, were studied at 5 kb water pressure, 680–1000°C, at the oxygen fugacities of the quartz-fayalite-magnetite (QFM) and hematite-magnetite (HM) buffers.In the range 680–850 °C, the crystalline assemblage...
Mapping of the 1973 Mississippi River floods from the Earth Resources Technology Satellite (ERTS)
Morris Deutsch, F. H. Ruggles, Philip Guss, Edward Yost
1973, Conference Paper, Remote sensing and water resources management
On March 31, and May 4 and 5, 1973, the first Earth Resources Technology Satellite (ERTS-1) obtained multispectral scanner imagery over the Mississippi River below St. Louis, Missouri. The river was in flood, and the ERTS data provided the first opportunity for regional synoptic mapping of the extent of flooding...
Antarctic icebergs as a fresh water resource
W.F. Weeks, W. J. Campbell
1973, Polar Record (16) 661-665
In a recent study (Weeks and Campbell, in press), we made a rather complete examination of the idea that icebergs could advantageously be used as a source of fresh water. The origin of the general idea of transporting icebergs is obscure; it may date from the 1850's when ice was...
Hydrologic changes after clear-cut logging in a small Oregon coastal watershed
D.D. Harris
1973, Journal of Research of the U.S. Geological Survey (1) 487-491
Preliminary graphical analysis indicates that clear-cut logging of a small Oregon watershed has significantly altered certain hydrologic characteristics. After logging, moderate increases were noted in annual runoff, but no significant changes were detected in either peak or minimum flow rates. Both the annual sediment yields and the maximum monthly water temperatures increased greatly after logging; sediment...