Geophysical instrumentation near Parkfield
W. H. Bakun
1988, Earthquakes & Volcanoes (USGS) (20) 60-71
The geophysical instrumentation operated by the U.S Geological Survey and others near Parkfield is designed to monitor ongoing tectonic processes that generate earthquakes and to record the strong shaking that results from larger shocks and its effects. this discussion focuses on the former objectives; the latter is discussed in the...
Using side scan sonar data in a geographic information system to locate and display lake trout spawning habitat in the Great Lakes
Charles L. Brown, Thomas A. Edsall, Robert G. Waltermire, Barbara White
1988, Conference Paper, Proceedings of the Fifth National MOSS User's Workshop
The National Fisheries Research Center-Great Lakes of the U.S. Fish and Wildlife Service has extensively used a side scan sonar to survey and pinpoint lake trout spawning grounds in the Great Lakes. The Geographic Information System (GIS) of the National Ecology Research Center produced maps from the side scan sonar...
Fishery research in the Great Lakes using a low-cost remotely operated vehicle
Gregory W. Kennedy, Charles L. Brown, Ray L. Argyle
1988, Conference Paper, Inshore '88 Conference Proceedings
We used a MiniROVER MK II remotely operated vehicle (ROV) to collect ground-truth information on fish and their habitat in the Great Lakes that have traditionally been collected by divers, or with static cameras, or submersibles. The ROV, powered by 4 thrusters and controlled by the pilot at the surface,...
Applications of satellite telemetry to wildlife research and management in Alaska
S.G. Fancy, R.B. Harris, David C. Douglas, L.F. Pank, Kenneth R. Whitten, Thomas R. McCabe, Steven C. Amstrup, G.W. Garner
1988, Conference Paper, Acte du colloque international: Suivi des vertebres terrestres par radiotelemetrie
Since 1984, the Alaska Fish and Wildlife Research Center, in cooperation with the Alaska Department of Fish and Game and several other agencies, has used the Argos Data Collection and Location System to address wildlife research and management problems in Alaska and other parts of North America. The use of...
Using GIS to evaluate map data
Michael E. Madigan, J. A. Sturdevant, C.A. Roberts
1988, Geotimes (33) 14-15
No abstract available....
The aqueous geochemistry of uranium in a drainage containing uraniferous organic-rich sediments, Lake Tahoe area, Nevada, USA
R. A. Zielinski, J. K. Otton, R. B. Wanty, C. T. Pierson
1988, Uranium (4) 281-305
Anomalously uraniferous waters occur in a small (4.2 km2) drainage in the west-central Carson Range, Nevada, on the eastern side of Lake Tahoe. The waters transport uranium from local U-rich soils and bedrock to organic-rich valley-fill sediments where it is concentrated, but weakly bound. The dissolved U and the U...
Determining transit losses for water deliveries by use of stream-aquifer models
Russell K. Livingston
1988, Conference Paper
Hydrologic modeling of stream-aquifer interaction commonly has been used to quantify transit losses associated with water deliveries, such as those from reservoir storage. This technique requires estimation of model parameters that include stage-discharge relations, channel-storage coefficient, aquifer transmissivity, and aquifer-storage coefficient. Because data to reliably estimate or calibrate these parameters...
Simulation technique for modeling flow on floodplains and in coastal wetlands
Raymond W. Schaffranek, Robert A. Baltzer
1988, Conference Paper
The system design is premised on a proven, areal two-dimensional, finite-difference flow/transport model which is supported by an operational set of computer programs for input data management and model output interpretation. The purposes of the project are (1) to demonstrate the utility of the model for providing useful highway design...
Three-dimensional gravity modeling of the geologic structure of Long Valley caldera
S. F. Carle
1988, Journal of Geophysical Research Solid Earth (93) 13237-13250
A 48-mGal gravity low coincides with Long Valley caldera and is mainly attributed to low-density caldera fill. Gravity measurements by Unocal Geothermal have been integrated with U.S. Geological Survey data, vastly improving gravity station coverage throughout the caldera. A strong regional gravity trend is mainly attributed to isostasy. A “best...
Assessing the Birkenes Model of stream acidification using a multisignal calibration methodology
Richard P. Hooper, Alex Stone, Nils Christophersen, de Grosbois, Hans M. Seip
1988, Water Resources Research (24) 1308-1316
A revision of the Birkenes model of streamwater acidification has been attempted to incorporate additional chemical and hydrologic information gained in the last 6 years since its original construction. The first stage of this effort has been an analysis of the hydrologic submodel with the goal of extending it to...
Acid rain damage to carbonate stone: a quantitative assessment based on the aqueous geochemistry of rainfall runoff from stone
M.M. Reddy
1988, Earth Surface Processes and Landforms (13) 335-354
An onsite experimental procedure was used to identify and quantify acid rain damage to carbonate stone, based on the change in rain runoff chemical composition. Onsite data obtained during the summer and fall of 1984 at three locations in the northeastern United States indicate that carbonate stone surface recession is...
Geothermal gradients in the conterminous United States
M. Nathenson, M. Guffanti
1988, Journal of Geophysical Research Solid Earth (93) 6437-6450
Geothermal gradients from published temperature/depth measurements in drill holes generally deeper than 600 m are used to construct a temperature gradient map of the conterminous United States. The broadly contoured map displays 284 temperature gradients that are applicable to a depth of 2 km. In terms of the number of...
Compositional evolution of the zoned calcalkaline magma chamber of Mount Mazama, Crater Lake, Oregon
C. R. Bacon, T. H. Druitt
1988, Contributions to Mineralogy and Petrology (98) 224-256
The climactic eruption of Mount Mazama has long been recognized as a classic example of rapid eruption of a substantial fraction of a zoned magma body. Increased knowledge of eruptive history and new chemical analyses of ∼350 wholerock and glass samples of the climactic ejecta, preclimactic rhyodacite flows and...
Waveform modelling using locked-mode synthetic and differential seismograms: application to determination of the structure of Mexico
J.S. Gomberg, T. Guy Masters
1988, Geophysical Journal International (94) 193-218
We have developed algorithms for modelling seismic waveforms to constrain regional Earth structure. The seismogram is represented as a sum of locked-mode travelling waves in a layered medium. This representation is convenient as it allows us to model structures with slowly varying heterogeneity and to construct differential seismograms. Describes the...
Seismic-reflection technique used to verify shallow rebound fracture zones in the Pierre Shale of South Dakota
T. C. Nichols Jr., K. W. King, D. S. Collins, R. A. Williams
1988, Canadian Geotechnical Journal (25) 369-374
Shallow seismic-reflection data are presented to demonstrate their usefulness for locating and showing the continuity and lateral extent of rebound fracture zones in the Pierre Shale. Rebound fracture zones, identified in boreholes near Hayes, South Dakota, have variable depth, thickness, and character, thus making questionable the correlation of these zones...
Multi-model approach to petroleum resource appraisal using analytic methodologies for probabilistic systems
R. A. Crovelli
1988, Mathematical Geology (20) 955-972
The geologic appraisal model that is selected for a petroleum resource assessment depends upon purpose of the assessment, basic geologic assumptions of the area, type of available data, time available before deadlines, available human and financial resources, available computer facilities, and, most importantly, the available quantitative methodology with corresponding computer...
Knowledge-based GIS techniques applied to geological engineering
E. Lynn Usery, Phyllis Altheide, Robin R. P. Deister, David J. Barr
1988, Photogrammetric Engineering and Remote Sensing (54) 1623-1628
A knowledge-based geographic information system (KBGIS) approach which requires development of a rule base for both GIS processing and for the geological engineering application has been implemented. The rule bases are implemented in the Goldworks expert system development shell interfaced to the Earth Resources Data Analysis System (ERDAS) raster-based GIS...
Wetland Boundary Determination in the Great Dismal Swamp Using Weighted Averages
Virginia Carter, Mary Keith Garrett, Patricia T. Gammon
1988, Water Resources Bulletin (24) 297-306
A weighted average method was used to analyze transition zone vegetation in the Great Dismal Swamp to determine if a more uniform determination of wetland boundaries can be made nationwide. The method was applied to vegetation data collected on four transects and three vertical layers across the wetland-to-upland transition zone...
Groundwater flow and transport modeling
Leonard F. Konikow, J.W. Mercer
1988, Journal of Hydrology (100) 379-409
Deterministic, distributed-parameter, numerical simulation models for analyzing groundwater flow and transport problems have come to be used almost routinely during the past decade. A review of the theoretical basis and practical use of groundwater flow and solute transport models is used to illustrate...
Regression estimates for topological‐hydrograph input
Michael R. Karlinger, D. Phillip Guertin, Brent M. Troutman
1988, Journal of Water Resources Planning and Management (114) 446-456
Physiographic, hydrologic, and rainfall data from 18 small drainage basins in semiarid, central Wyoming were used to calibrate topological, unit‐hydrograph models for celerity, the average rate of travel of a flood wave through the basin. The data set consisted of basin characteristics and hydrologic data for the 18 basins and...
Climatological observations and predicted sublimation rates at Lake Hoare, Antarctica.
G.D. Clow, C.P. McKay, G.M. Simmons Jr., R.A. Wharton Jr.
1988, Journal of Climate (1) 715-728
In December 1985, an automated meteorological station was established at Lake Hoare in the dry valley region of Antarctica. Here, we report on the first year-round observations available for any site in Taylor Valley. This dataset augments the year-round data obtained at Lake Vanda (Wright Valley) by winter-over crews during...
The plumbotectonic model for Pb isotopic systematics among major terrestrial reservoirs: A case for bi-directional transport
R. E. Zartman, S.M. Haines
1988, Geochimica et Cosmochimica Acta (52) 1327-1339
Version IV of plumbotectonics expands and refines the original model of Doe and Zartman (1979) and Zartman and Doe (1981) for explaining Pb (Sr, and Nd) isotopic systematics among major terrestrial reservoirs. A case for bi-directional transport among reservoirs is based on the observed isotopic compositions for different tectonic settings, and finds a rationale...
Oxygen isotope variations in granulite-grade iron formations: constraints on oxygen diffusion and retrograde isotopic exchange
Z.D. Sharp, J. R. O’Neil, E.J. Essene
1988, Contributions to Mineralogy and Petrology (98) 490-501
The oxygen isotope ratios of various minerals were measured in a granulite-grade iron formation in the Wind River Range, Wyoming. Estimates of temperature and pressure for the terrane using well calibrated geothermometers and geobarometers are 730??50?? C and 5.5??0.5 kbar. The mineral constraints on fluid compositions in the iron formation...
Paleoecology of Middle Pennsylvanian-age peat-swamp plants in Herrin coal, Kentucky, U.S.A.
R.B. Winston
1988, International Journal of Coal Geology (10) 203-238
To develop a method for quantifying the vegetation of Pennsylvania-age coal beds, of four coal-ball (permineralized peat) profiles and four coal column samples from the Herrin coal bed (Kentucky No. 11) Carbondale Formation in western Kentucky were compared. An estimated 89.5%...
Statistical Methods and Sampling Design for Estimating Step Trends in Surface-Water Quality
Robert M. Hirsch
1988, Water Resources Bulletin (24) 493-503
This paper addresses two components of the problem of estimating the magnitude of step trends in surface water quality. The first is finding a robust estimator appropriate to the data characteristics expected in water-quality time series. The J. L. Hodges-E. L. Lehmann class of estimators is found to be robust...