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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Atlantic Ocean
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North Atlantic
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Gulf of Mexico
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Mississippi Canyon (1)
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North America
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Appalachians
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Appalachian Plateau (1)
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Central Appalachians (2)
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Great Lakes region (1)
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Saint Lawrence Lowlands (1)
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United States
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Nevada
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Nye County Nevada
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Yucca Mountain (1)
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New York
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Adirondack Mountains (1)
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Ohio
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Erie County Ohio (1)
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Ottawa County Ohio (1)
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Virginia
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Pulaski County Virginia (1)
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West Virginia
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Greenbrier County West Virginia (1)
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Mercer County West Virginia (1)
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Pocahontas County West Virginia (2)
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commodities
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petroleum
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natural gas (1)
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fossils
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burrows (3)
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ichnofossils
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Nereites (1)
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Skolithos (2)
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Teichichnus (1)
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Invertebrata
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Porifera
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geologic age
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Cenozoic
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Paleozoic
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Cambrian
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Upper Cambrian
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Carboniferous
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Mississippian
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Lower Mississippian
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Kinderhookian (1)
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Price Formation (4)
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Upper Mississippian
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Greenbrier Limestone (1)
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Devonian
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Middle Devonian
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Columbus Limestone (1)
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Eifelian (1)
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Ordovician (1)
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Primary terms
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Atlantic Ocean
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North Atlantic
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Gulf of Mexico
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Mississippi Canyon (1)
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Cenozoic
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Quaternary (1)
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geophysical methods (1)
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government agencies (1)
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heat flow (1)
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ichnofossils
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Cruziana (3)
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Diplocraterion (1)
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Nereites (1)
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Skolithos (2)
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Teichichnus (1)
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Invertebrata
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Cnidaria (1)
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Porifera
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Stromatoporoidea (1)
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museums (1)
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North America
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Appalachians
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Appalachian Plateau (1)
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Central Appalachians (2)
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Great Lakes region (1)
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Saint Lawrence Lowlands (1)
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ocean floors (1)
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paleoecology (1)
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paleontology (3)
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Paleozoic
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Cambrian
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Upper Cambrian
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Potsdam Sandstone (1)
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Carboniferous
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Mississippian
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Lower Mississippian
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Kinderhookian (1)
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Price Formation (4)
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Upper Mississippian
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Greenbrier Limestone (1)
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Devonian
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Middle Devonian
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Columbus Limestone (1)
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Eifelian (1)
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Ordovician (1)
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petroleum
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natural gas (1)
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pollution (1)
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sea-level changes (3)
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sedimentary rocks
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clastic rocks
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conglomerate (2)
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sandstone (2)
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shale (2)
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siltstone (1)
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sedimentary structures
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bedding plane irregularities (1)
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biogenic structures
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bioherms (1)
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bioturbation (1)
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planar bedding structures
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cross-bedding (1)
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sedimentation (5)
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stratigraphy (5)
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structural geology (1)
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tectonics (1)
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United States
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Nevada
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Nye County Nevada
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Yucca Mountain (1)
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New York
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Adirondack Mountains (1)
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Ohio
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Erie County Ohio (1)
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Ottawa County Ohio (1)
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Virginia
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Pulaski County Virginia (1)
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West Virginia
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Greenbrier County West Virginia (1)
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Mercer County West Virginia (1)
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Pocahontas County West Virginia (2)
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waste disposal (1)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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conglomerate (2)
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sandstone (2)
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shale (2)
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siltstone (1)
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sedimentary structures
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burrows (3)
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sedimentary structures
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bedding plane irregularities (1)
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biogenic structures
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bioherms (1)
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bioturbation (1)
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planar bedding structures
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cross-bedding (1)
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striations (1)
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Evaluation of hydrocarbon broaching after subsurface containment failure, Gulf of Mexico
2-24: Interference Structure, Gulf of Mexico, U.S.A.
Expectations of geological science: Yucca Mountain site characterization, Nevada
Abstract The U.S. Department of Energy (DOE) has brought data, analyses, and conclusions on landscape stability and denudation rates from the Yucca Mountain site characterization program to the U.S. Nuclear Regulatory Commission (NRC) for evaluation. In the United States the NRC must license a geologic repository to dispose of spent nuclear reactor fuel and high-level radioactive wastes from military reprocessing through phases of construction, operation, and closure. The DOE reported rates of hillslope denudation at Yucca Mountain, valley incision in bedrock over the repository block, and alluvial stream incision on the major drainage system in the area. These data were presented in combination with a regulatory compliance argument that concluded extreme erosion had not occurred during the Quaternary Period and that erosion would not jeopardize performance of a geologic repository system over the next 10,000 years, if located there. The NRC defined “extreme erosion” and the duration of the Quaternary Period in a qualitative regulatory context as one of 24 “potentially adverse conditions” (NRC, 1991) to be evaluated during site characterization. The DOE made a compliance argument using the NRC’s regulatory requirement, supplemented by qualitative definitions from internal NRC guidance. The NRC was critical of the DOE’s technical documentation and compliance argument because (1) the erosion assessment used time-averaged denudation rates, (2) erosion rates for the most recent 10,000 to 100,000 years of the Quaternary Period were not provided, and (3) multiple dating methods were not used to establish age of the surficial landforms examined. The DOE encountered several difficulties interpreting the regulation and its administrative record, framing a compliance argument, and documenting the data, analyses, and conclusions from a field study program. Among these, (1) the DOE misinterpreted the regulation and its administrative record by primarily relying on extant written guidance to explain how the NRC staff interpreted their regulation; (2) the DOE had no knowledge of how the NRC would evaluate a limited and specific compliance argument against their regulation; (3) the DOE’s technical documentation, in retrospect, was not robust enough to meet the NRC’s expectations of high confidence in conclusions accompanied by low uncertainty; and (4) the NRC’s comments implied expectations for geochronologic accuracy and degree of resolution that may be considered beyond the state of the practice.
Trace fossils and bioturbation in peritidal facies of the Potsdam-Theresa formations (Cambrian-Ordovician), Northwest Adirondacks
Repository for Devonian-Mississippian trace fossil figured specimens
Trace fossils from the Early Mississippian Price Delta, Southeast West Virginia
Multivariate analyses of trace fossil distribution from an Early Mississippian oxygen-deficient basin, Central Appalachians
Trace fossils indicating estuarine deposystems for the Devonian-Mississippian Cloyd Conglomerate Member, Price Formation, Central Appalachians
Comment and Reply on “Sedimentary response to Mississippian tectonic activity at the east end of the 38th Parallel fracture zone”: COMMENT
Kelleys Island: Giant glacial grooves and Devonian shelf carbonates in north-central Ohio
Abstract Kelleys Island is the easternmost of the Lake Erie Islands group, located north of Marblehead Peninsula and Sandusky, Ohio, (Fig. 1) on the Kelleys Island 7½-minute Quadrangle. Access to the Island is provided by the Newman Boat Lines which operates a ferry from Marblehead (April through November) and from Sandusky (June through Labor Day). Throughout the year, the Island is also served by Island Arilines from Port Clinton Municipal Airport. On the Island, transportation is available in the form of rental bicycles, golf carts, or private cars ferried from the mainland.