Graptolites from the Martinsburg Formation, Lehigh Gap, Eastern Pennsylvania
Jack Burton Epstein, William B. N. Berry
1973, Journal of Research of the U.S. Geological Survey (1) 33-38
Graptolites collected from the uppermost part of the Martinsburg Formation (Pen Argyl Member) at and near the contact with the overlying Shawangunk Formation at Lehigh Gap, Pa., indicate that the uppermost Martinsburg is as young as Edenian to early Maysvillian (upper subzone [Climacograptus spiniferus subzone] of zone 13 | Orthograptus truncatus intermedius zone]). The Martinsburg gradationally...
Effect of septic-tank wastes on quality of water, Ipswich and Shawsheen River basins, Massachusetts
L.G. Toler, George B. Morrill III
1973, Journal of Research of the U.S. Geological Survey (1) 117-120
Many housing projects in the metropolitan area of Boston are beyond the reach of municipal sewer systems. Waste water disposed of through septic-tank or cesspool systems percolates to ground-water reservoirs and eventually reaches the streams. The dissolved-solids load in the streams receiving septic-tank effluent is increased by an amount that can be predicted from the...
Antimony-bearing orpiment, Carlin gold deposit, Nevada
Arthur S. Radtke, Charles M. Taylor, Chris Heropoulos
1973, Journal of Research of the U.S. Geological Survey (1) 85-87
Orpiment, As2S3, containing up to 1.5 percent antimony has been recognized in carbonaceous arsenic-rich gold ores in the unoxidized East ore body of the Carlin gold deposit. Associated hydrothermal minerals include realgar (AsS) and quartz. Stibnite, commonly associated with realgar in the ores, has not been observed associated with this type of orpiment....
Microprobe analysis of biotites - A method of correlating tuff beds in the Green River Formation, Colorado and Utah
George A. Desborough, Janet K. Pitman, John Roswell Donnell
1973, Journal of Research of the U.S. Geological Survey (1) 39-44
Quantitative electron microprobe analyses of biotite grains for iron, magnesium, and titanium from tuff beds in the lacustrineGreen River Formation (Eocene) of Colorado and Utah provide a tentative method of identification and a permissive stratigraphic correlation of tuffs. Tuff beds that have been identified and correlated by stratigraphic means were sampled at five...
Interpretation of depositional environment in the Plympton Formation (Permian), Southern Pequop Mountains, Nevada, from physical stratigraphy and a faunule
Ellis L. Yochelson, George D. Fraser
1973, Journal of Research of the U.S. Geological Survey (1) 19-33
Field mapping in the southern part of the Pequop Mountains has shown the presence of a major structural high which has profoundly affected the stratigraphy of Pennsylvanian and Lower Permian beds; lesser effects of this high persisted into the later Permian. Within the Park City Group (Permian), the Plymton Formation, overlying the Kaibab Limestone,...
The fractionation of humic acids from natural water systems
R.L. Wershaw, D.J. Pinckney
1973, Journal of Research of the U.S. Geological Survey (1) 361-366
Humic acids, the most abundant organic components of natural water systems, are complex mixtures of molecular aggregates of different chemical and physical properties. The first step in the study of such a mixture is the fractionation of the mixture. The most common approach with humic acids is to attempt to obtain a molecular weight fractionation...
Accessory apatite from hybrid granitoid rocks of the southern Snake Range, Nevada
Donald E. Lee, Robert E. Mays, Richard E. Van Loenen
1973, Journal of Research of the U.S. Geological Survey (1) 89-98
Analytical data, optical properties, and unit-cell parameters are presented for 24 samples of accessory apatites recovered from hybrid granitoid rocks of the southern Snake Range, Nev. A complete chemical analysis is given for one. In the Snake Creek-Williams Canyonoutcrop area, where the hybrid rocks grade from granodiorite with 63 percent SiO2 to a...
Upper Cretaceous (Maestrichtian) fossils from the Kenai-Chugach Mountains, Kodiak and Shumagin Islands, Southern Alaska
Sandra H. B. Clark, David L. Jones
1973, Journal of Research of the U.S. Geological Survey (1) 125-136
A thick sequence of highly deformed flyschlike metasandstone, slate, and argillite crops out in southern Alaska in the Kenai-Chugach Mountains and on Kodiak and the Shumagin Islands to the southwest. These poorly fossiliferous rocks have long been considered Cretaceous in age because of scattered occurrences of fragmentary shells of Inoceramus. Mainly on the basis of...
Evaluating the reliability of specific-yield determinations
Ronald L. Hanson
1973, Journal of Research of the U.S. Geological Survey (1) 371-376
The specific yield of the alluvial aquifer in the Gila River flood plain in southeastern Arizona has been determined using two methods of analysis - the time-drawdown method and the soil-moisture-content method. Time-drawdown data measured at 17 observation wells during a 3.5-day aquifer test define an average apparent specific yield of 0.13. Soil-moisture-content data...
A precautionary note on the use of mixed solvents in soxhlet extraction procedures
Alan A. Roberts, James George Palacas
1973, Journal of Research of the U.S. Geological Survey (1) 221-222
The variation in solvent composition of a mixed solvent used in Soxhlet extraction of sediments has apparently often been overlooked. Owing to azeotropic distillation of the solvent introduced into the apparatus, care must be taken to determine the composition of the solvent actually doing the extracting....
Geologic bench marks by terrestrial photography
Harold E. Malde
1973, Journal of Research of the U.S. Geological Survey (1) 193-206
A photograph made with a level camera, if taken at a known height above a permanent mark on the ground, can be later repeated with exactness for measurement of changes in terrain. Such a photograph is one of several means for establishing a geologic bench mark and is especially useful for monitoring the subtle...
Magnetizations of some Late Cretaceous glassy tuffs, volcanic breccias, and altered basalts of the Elkhorn Mountains volcanic field, Western Montana
W. F. Hanna
1973, Journal of Research of the U.S. Geological Survey (1) 179-192
New magnetization data for Late Cretaceous glassy welded tuffs, volcanic breccias, and altered basalts from the Elkhorn Mountains volcanic field, together with geologic, mineralogic, and K-Ar data, indicate that (1) the glassy tuffs have unusually strong, uniform remanent magnetizations which are reversely polarized, much of the remanence perhaps residing in submicroscopic single-domain iron oxide particles within...
Radiometric dating of intrusive rocks in the Cottonwood area, Utah
M. D. Crittenden Jr., J. S. Stuckless, R. W. Kistler, T. W. Stern
1973, Journal of Research of the U.S. Geological Survey (1) 173-178
Recently completed fission-track and K-Ar dating of zircon, sphene, apatite, muscovite, biotite, and hornblende indicate that the Clayton Peak stock was intruded 37-41 m.y. ago, the Alta stock about 32-33 m.y. ago, and the Little Cottonwood stock between 24 and 31 m.y. ago. Pb-a ages on zircon, though showing the same sequence, are about twice...
Geology of part of the southern complex, Marquette district, Michigan
W.F. Cannon, George C. Simmons
1973, Journal of Research of the U.S. Geological Survey (1) 165-172
The southern complex, south of the Marquette synclinorium in the Marquette district of Michigan, is dominantly granitic. The granitic parts of the complex have Rb-Sr ages of about 2.5 b.y. and are classed as of Precambrian W age. The rocks are divided into two major units: (1.) Bell Creek Gneiss consisting mostly of...
Age and tectonic implications of some low-grade metamorphic rocks from the Yucatan Channel
J. G. Vedder, N. S. MacLeod, M. A. Lanphere, William P. Dillon
1973, Journal of Research of the U.S. Geological Survey (1) 157-164
Phyllite and marble dredged from the lower part of the continental slope between Cuba and the Yucatan Peninsula seem to support the contention that a pre-early Tertiary metamorphic belt extends from the western Greater Antilles into northern Central America. The minimum K-Ar ages derived from the samples suggest that the metamorphic event was pre-Late Cretaceous,...
The concept of growth and maturity of ore-stage pyrite in roll-type uranium deposts
C. G. Warren, H.C. Granger
1973, Journal of Research of the U.S. Geological Survey (1) 151-155
Roll-type uranium deposits contain both ore-stage pyrite and preore or diagenetic pyrite that was present in the host rock before the deposits began to form. Ore-stage pyrite forms as the result of redistribution and accretion from the preore pyrite. Accretion of the ore-stage pyrite seems to be governed by natural laws that limit its concentration...
A second specimen of Parahyus vagus Marsh, 1876
G. Edward Lewis
1973, Journal of Research of the U.S. Geological Survey (1) 147-149
The occurrence of the second known specimen of Parahyus vagus, from the Tepee Trail Formation, Wyoming, is recorded. As the first specimen was reported from the lower Eocene, this second occurrence casts doubt on the supposed age ranges of both Parahyus and the Tepee Trail....
Lithostrotion reiseri n. sp., a cerioid colonial coral from Meramec-age beds, Lisburne Group, arctic Alaska
Augustus K. Armstrong
1973, Journal of Research of the U.S. Geological Survey (1) 137-145
Lithostrotion reiseri n. sp. is a cerioid, colonial coral, index fossil for microfossil zones 12-13 (Meramec) in the Lisburne Group in the central and eastern Brooks Range, arctic Alaska....
A preliminary classification of wetland plant communities in north-central Minnesota
L.M. Cowardin, Douglas H. Johnson
1973, Special Scientific Report - Wildlife 168
A classification of wetland plant communities was developed for a study area in north-central Minnesota in order to analyze data on waterfowl use of habitat that were gathered by radio telemetry. The classification employs features of several earlier classifications in addition to new classes for bogs and lakeshore communities. Brief...
Preparation and properties of quinaldine sulfate, an improved fish anesthetic
J. L. Allen, J.B. Sills
1973, Investigations in Fish Control 47
Abstract not submitted to date...
Unharvested fishes in the U. S. commercial fishery of western Lake Erie in 1969
Harry D. Van Meter
1973, Special Scientific Report - Fisheries 670
Potential commercial fish production was estimated for U.S. waters of western Lake Erie in 1969 from pounds landed and pounds discarded. Periodic observations of catches in haul seines and trap nets revealed that about 37% of the catch (by weight) in haul seines and 26% of that in trap nets...
The microgravimetric determination of acid-insoluble impurities in the complete analysis of small samples of acid-soluble minerals
Robert Meyrowitz
1973, Journal of Research of the U.S. Geological Survey (1) 207-209
The acid-insoluble impurities of small samples of minerals are determined by a microgravimetric procedure. A Schwarz von Bergkampf glass filter stick with paper filter medium is used to separate the insoluble material. The filtration apparatus and procedural details are described....
Scolecobasidium humicola, a fungal pathogen of fish
A. J. Ross, W. T. Yasutake
1973, Journal of the Fisheries Research Board of Canada (30) 994-995
Scolecobasidium humicola, a previously undescribed fungal pathogen of fish was isolated from coho salmon (Oncorhynchus kisutch). In natural infections the kidney was the organ most affected. The disease was difficult to transmit experimentally and appeared to be only weakly contagious....
Radiochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, July 1972
Wilbur C. Ballance, L.J. Schroder
1973, Report
The U.S. Geological Survey established a sampling program on Amchitka Island in 1967 in cooperation with the U.S . Atomic Energy Commission. Water samples are analyzed routinely for tritium, gross alpha, and gross beta/gamma content, Frequency of sampling was semiannually prior to Cannikin and has been bimonthly since the Cannikin...
Ground water in selected areas in the Klamath Basin, Oregon
A.R. Leonard, A.B. Harris
1973, Report
GROUNDWATER FEATURES OF SIX LOWLAND AREAS IN THE KLAMATH BASIN OF OREGON--KLAMATH MARSH AREA, AND SPRAGUE RIVER, SWAN LAKE, YONNA, POE, AND LANGELL VALLEYS--ARE DESCRIBED. RUGGED MOUNTAINS AND RIDGES SURROUND AND SEPARATE THESE LOWLANDS WHERE FLOORS RANGE IN ALTITUDE FROM 4,100 FEET IN POE...