Hydrology of the Ferron Sandstone aquifer and effects of proposed surface-coal mining in Castle Valley, Utah, with a section on stratigraphy and a section on leaching of overburden
Gregory C. Lines, Daniel J. Morrissey, Thomas A. Ryer, Richard H. Fuller
1983, Water Supply Paper 2195
Coal in the Ferron Sandstone Member of the Mancos Shale of Cretaceous age has traditionally been mined by underground techniques in the Emery Coal Field in the southern end of Castle Valley in east-central Utah. However, approximately 99 million tons are recoverable by surface mining. Ground water in the Ferron...
Ground water for oil-shale development, Piceance Basin, Colorado
W.M. Alley
1983, Ground Water (21) 456-464
Vast deposits of oil shale are contained in the Piceance basin in northwestern Colorado. The basin may contain as much as 40 million acre-feet of stored water associated with these deposits, much of which may have to be drained for mining. Yet, most analyses of...
Remote detection of metal anomalies on Pilot Mountain, Randolph County, North Carolina
N.M. Milton, W. Collins, Sheng-Huei Chang, R. G. Schmidt
1983, Economic Geology (78) 605-617
Pilot Mountain, a hydrothermally altered monadnock within the Carolina slate belt, contains areas of anomalously high amounts of Cu, Mo, and Sn in the soils. Leaves of canopy trees in the mineralized zone also contain more copper than trees in a nearby control area. Spectral data were processed using a...
Sorption of radium-226 from oil-production brine by sediments and soils
E. R. Landa, D.F. Reid
1983, Environmental Geology (5) 1-8
The sorption of226Ra from oil-production brine by soils and sediments was investigated. Sorption was rapid, and the percentage sorbed increased with brine dilution. Greatest removals of226Ra from sediments in the laboratory occurred with alkaline DTPA, HCl, and BaCl2, with lesser removals using CaCl2 and NaCl solutions. Digestion of sediments with...
SPONTANEOUS COAL COMBUSTION; MECHANISMS AND PREDICTION.
James R. Herring, Fredrick J. Rich
1983, Conference Paper
Spontaneous ignition and combustion of coal is a major problem to the coal mining, shipping, and use industries; unintentional combustion causes loss of the resource as well as jeopardy to life and property. The hazard to life is especially acute in the case of underground coal mine fires that start...
Mine drainage and rock type influences on eastern Ohio stream water quality
D.R. Helsel
1983, Water Resources Bulletin (19) 881-887
Stream water during fair weather (base flow) is largely ground water discharge, which has been in contact with minerals of the underlying aquifer. Base flow water quality should therefore reflect aquifer mineralogy as well as upstream land use. Three upstream mining categories (unmined lands, abandoned coal mines, and reclaimed coal...
Chemical reactions accompanying fluid flow through granite held in a temperature gradient
Diane E. Moore, C.A. Morrow, J.D. Byerlee
1983, Geochimica et Cosmochimica Acta (47) 445-453
Distilled water was passed at a low rate down a temperature gradient through cylinders of Barre and Westerly Granite. Temperatures ranged from 80–100°C at the outer edges of the cylinders to 250–300°C in central, drilled holes which housed the heating coils. The measured permeabilities of the granite cylinders decreased by...
Distribution of oceanic and continental leads in the Arabian-Nubian Shield
J. S. Stacey, D. B. Stoeser
1983, Contributions to Mineralogy and Petrology (84) 91-105
New common lead data for feldspar, whole-rock, and galena samples from the Arabian-Nubian Shield, together with data from previous work, can be divided into two main groups. Group I leads have oceanic (mantle) characteristics, whereas group II leads have incorporated a continental-crustal component of at least early Proterozoic age. The...
Selective dissolution of siliceous microfossils observed in a box core from the north-east equatorial Pacific
D. Kadko, J. R. Blueford, L.H. Burckle, J. Barron
1983, Nature (302) 139-141
A box core taken at 11??50.3??? N and 137??28.2??? W in the Central Pacific manganese nodule province was studied to determine the pattern of diatom and radiolarian preservation with depth in the sediment, as well as to observe downcore variations in clay mineralogy. We observed marked deterioration of the siliceous...
Talc in the suspended matter of the northwestern Atlantic
Lawrence J. Poppe, John C. Hathaway, Carol M. Parmenter
1983, Clays and Clay Minerals (31) 60-64
Knowledge of the distribution, concentration, and composition of suspended particulate matter in seawater is important to the understanding of sedimentation processes on the Continental Shelf. Because the surfaces of both organic and inorganic particles have high affinities for pollutants, such as certain trace metals, chlorinated hydrocarbons, and petroleum (Bothner et...
Harding Iceland spar: A new δ18O−δ13C carbonate standard for hydrothermal minerals
G. P. Landis
1983, Chemical Geology (41) 91-94
An isotopically homogeneous calcite, Harding Iceland Spar (HIS), having 6180 = +11.78 ± 0.07‰ (= +22.15‰ for CO2) and δ13C = −4.80 ± 0.02‰, has been prepared in quantities suitable for use as a working standard in mass spectrometric analysis. The isotopic values are well-suited for analysis of minerals of hydrothermal...
Tectonics and metallogenic provinces
P. W. Guild
1983, Advances in Space Research (3) 9-16
Various theories have been advanced to explain the well-known uneven distribution of metals and ore-deposit types in space and time. Primordial differences in the mantle, preferential concentration of elements in the crust, the prevalence of ore-forming processes at certain times and (or) places, and combinations of one or several of...
The mobility and distribution of heavy metals during the formation of first cycle red beds
R. A. Zielinski, S. Bloch, T.R. Walker
1983, Economic Geology (78) 1574-1589
Holocene-Pliocene sequence sampled in northern Baja California. Geochemical data supported by petrographic, X-ray, and SEM observations of mineralogical transformations, fission-track radiography, and uranium decay series measurements. Results indicate that metal content of the studied samples is inherited from constituent detrital minerals and that reddening of whole-rock samples does not promote...
Process and rate of dedolomitization: Mass transfer and C14 dating in a regional carbonate aquifer
W. Back, B.B. Hanshaw, Niel Plummer, P.H. Rahn, C.T. Rightmire, M. Rubin
1983, Geological Society of America Bulletin (94) 1415-1429
Regional dedolomitization is the major process that controls the chemical character of water in the Mississippian Pahasapa Limestone (Madison equivalent) surrounding the Black Hills, South Dakota and Wyoming. The process of dedolomitization consists of dolomite dissolution and concurrent precipitation of calcite; it is...
Comparison of rapid methods for chemical analysis of milligram samples of ultrafine clays
S.L. Rettig, J.W. Marinenko, Hani N. Khoury, B.F. Jones
1983, Clays and Clay Minerals (31) 440-446
Two rapid methods for the decomposition and chemical analysis of clays were adapted for use with 20–40-mg size samples, typical amounts of ultrafine products (≤0.5-µm diameter) obtained by modern separation methods for clay minerals. The results of these methods were compared with those of “classical” rock analyses. The two methods...
Areal extent of a plume of mineralized water from a flowing artesian well in Dade County, Florida
Bradley G. Waller
1982, Water-Resources Investigations Report 82-20
A flowing artesian well that taps the Floridan aquifer at Chekika Hammock State Park is contaminating the overlying Biscayne aquifer with saline water. The plume of mineralized water extends approximately 7 miles southeast of the well and ranges in width from 1 to 2 miles. The areal extent of contamination...
Water resources inventory of Connecticut Part 10: Lower Connecticut River basin
Lawrence A. Weiss, James W. Bingham, Mendall P. Thomas
1982, Connecticut Water Resources Bulletin 31
The lower Connecticut River basin study area in south-central Connecticut includes 639 square miles and is drained principally by the Connecticut River and by seven smaller streams that flow directly to Long Island Sound between the West River on the west and the Connecticut River on the east. The population...
Assessment of hydrologic conditions in potential coal-lease tracts in the Warrior coal field, Alabama
Celso Puente, John F. Newton, Roy H. Bingham
1982, Open-File Report 81-540
Assessing the hydrology of potential Federal coal-lease tracts, because of their dissemination and limited data, requires some predictive capability. Four tracts assessed were located in the outcrop of three coal groups and of other relatively impermeable rocks in the Pottsville Formation. Physical settings of the tracts and most other areas...
Hydrologic characteristics of surface-mined land reclaimed by sludge irrigation, Fulton County, Illinois
G. L. Patterson, R.F. Fuentes, L.G. Toler
1982, Water-Resources Investigations Report 82-16
Analyses of water samples collected at four stream-monitoring stations, in an area surface mined for coal and being reclaimed by sludge irrigation, show the principal metals are sodium, calcium, and magnesium and principal non-metals are chloride, sulfate, and bicarbonate. Comparing yearly mean chemical concentrations shows no changing trends since reclamation...
Hydrology of area 15, Eastern Coal province, Kentucky and Tennessee
David W. Leist, Ferdinand Quinones, D. S. Mull, Mary Young
1982, Open-File Report 81-809
Area 15, in Eastern Kentucky and Tennessee consists of 3,095 square miles in the Cumberland, Rockcastle and Laurel River basins. The area is underlain by Permian, Pennsylvanian, Mississippian rocks. The Breathitt Formation of Pennsylvanian age crops out in about 75% of the area and contains most of the coal. About...
Evaluation of the hydrologic system in the New Leipzig coal area, Grant and Hettinger counties, North Dakota
C. A. Armstrong
1982, Open-File Report 82-698
Aquifers in the New Leipzig coal area consist of sandstone beds in the Fox Hills Sandstone, the Hell Creek Formation, the Cannonball and Ludlow Members of the Fort Union Formation, and the basal part of the Tongue River Member of the Fort Union Formation. Aquifers also occur in sandstone and...
Hydrology of potential mining areas in the Warrior coal field, Alabama
Celso Puente, J.G. Newton
1982, Open-File Report 82-105
Hydrologic data for four small basins and for numerous other sites in the Warrior coal field are used to define the potential impact of surface mining on water resources. Bear and Blue Creek basins are underlain predominantly by relatively impermeable consolidated rocks in the Pottsville Formation. Turkey and Yellow Creek...
Hydrology of Salt Wells Creek — A plains stream in southwestern Wyoming
H. W. Lowham, L. L. DeLong, K. R. Collier, E. A. Zimmerman
1982, Water-Resources Investigations Report 81-62
Development of energy minerals in plains areas of Wyoming is expanding rapidly. Such development may affect water resources and hydrologic relations of the plains; however, little information exists concerning hydrologic processes for these areas. This report summarizes results of a hydrologic study made during 1975-78 of Salt Wells creek, a...
Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis
J.K. Felmlee, R. A. Cadigan
1982, Open-File Report 82-324
Multivariate statistical analyses were performed on data from 156 mineral-spring sites in nine Western States to analyze relationships among the various parameters measured in the spring waters. Correlation analysis and R-mode factor analysis indicate that three major factors affect water composition in the spring systems studied: (1) duration of water...
Hydrologic investigations and data-collection network in strippable coal-resource areas in northwestern New Mexico
H.R. Hejl
1982, Open-File Report 82-358
This report presents hydrologic investigations and data collections conducted by the U.S. Geological Survey in the strippable coal areas of northwestern New Mexico. Streamflow, ground-water, and quality-of-water data were collected to provide information about baseline or prevailing hydrologic conditions. A network of hydrologic data-collection sites in the strippable coal areas...