Publications
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U.S. Geological Survey Karst Interest Group: proceedings, St Petersburg, Florida February 13-16, 2001 U.S. Geological Survey Karst Interest Group: proceedings, St Petersburg, Florida February 13-16, 2001
Karst and similar landscapes are found in a wide range of biogeographic classes. In the U.S. for example, Everglades, Mammoth Cave, and Hawaii Volcanoes National Parks have little in common - except karst or pseudokarst, and a cultural past (even though these are very different). This diversity of geologic settings makes karst difficult to categorize and work with when designing a...
Authors
Eve L. Kuniansky
TES premapping data: Slab ice and snow flurries in the Martian north polar night TES premapping data: Slab ice and snow flurries in the Martian north polar night
In the 1970s, Mariner and Viking spacecraft observations of the north polar region of Mars revealed polar brightness temperatures that were significantly below the expected kinetic temperatures for CO2 sublimation. For the past few decades, the scientific community has speculated as to the nature of these Martian polar cold spots. Thermal Emission Spectrometer (TES) thermal spectral data...
Authors
Timothy N. Titus, Hugh H. Kieffer, Kevin F. Mullins, Phillip R. Christensen
Wildfire-related debris-flow initiation processes, Storm King Mountain, Colorado Wildfire-related debris-flow initiation processes, Storm King Mountain, Colorado
A torrential rainstorm on September 1, 1994 at the recently burned hillslopes of Storm King Mountain, CO, resulted in the generation of debris flows from every burned drainage basin. Maps (1:5000 scale) of bedrock and surficial materials and of the debris-flow paths, coupled with a 10-m Digital Elevation Model (DEM) of topography, are used to evaluate the processes that generated fire...
Authors
S.H. Cannon, R. M. Kirkham, M. Parise
TES mapping of Mars' north seasonal cap TES mapping of Mars' north seasonal cap
The Mars Global Surveyor thermal emission spectrometer has made observations of Mars' north polar region for nearly a full martian year. Measurements of bolometric emission and reflectance, as well as brightness temperatures in specific bands synthesized from thermal radiance spectra, are used to track the behavior of surface and atmospheric temperatures, the distribution of condensed...
Authors
Hugh H. Kieffer, Timothy N. Titus
Density model of the Cascadia subduction zone Density model of the Cascadia subduction zone
The main goal of this work is to construct self-consistent density models along two profiles crossing the northern and central Cascadia subduction zone that have been comprehensively studied on the basis of geological, geophysical, etc. data.
Authors
T.V. Romanyuk, Walter D. Mooney, R.J. Blakely
Volcano collapse promoted by hydrothermal alteration and edifice shape, Mount Rainier, Washington Volcano collapse promoted by hydrothermal alteration and edifice shape, Mount Rainier, Washington
Catastrophic collapses of steep volcano flanks threaten many populated regions, and understanding factors that promote collapse could save lives and property. Large collapses of hydrothermally altered parts of Mount Rainier have generated far-traveled debris flows; future flows would threaten densely populated parts of the Puget Sound region. We evaluate edifice collapse hazards at Mount...
Authors
M.E. Reid, T. W. Sisson, D.L. Brien
Huge, CO2-charged debris-flow deposits and tectonic sagging in the northern plains of Mars Huge, CO2-charged debris-flow deposits and tectonic sagging in the northern plains of Mars
The northern plains of Mars contain a vast deposit, covering one-sixth of the planet, that apparently resulted in extensive lithospheric deformation. The center of the deposit may be as much as 2–3 km thick. The deposit has lobate margins consistent with the flow of fluidized debris for hundreds to thousands of kilometers derived from highland and high-plains sources. The deposit surface...
Authors
K. L. Tanaka, W.B. Banerdt, J.S. Kargel, N. Hoffman
Thermal thickness and evolution of Precambrian lithosphere: A global study Thermal thickness and evolution of Precambrian lithosphere: A global study
The thermal thickness of Precambrian lithosphere is modeled and compared with estimates from seismic tomography and xenolith data. We use the steady state thermal conductivity equation with the same geothermal constraints for all of the Precambrian cratons (except Antarctica) to calculate the temperature distribution in the stable continental lithosphere. The modeling is based on the...
Authors
I.M. Artemieva, Walter D. Mooney
Catastrophic debris flows transformed from landslides in volcanic terrains : mobility, hazard assessment and mitigation strategies Catastrophic debris flows transformed from landslides in volcanic terrains : mobility, hazard assessment and mitigation strategies
Communities in lowlands near volcanoes are vulnerable to significant volcanic flow hazards in addition to those associated directly with eruptions. The largest such risk is from debris flows beginning as volcanic landslides, with the potential to travel over 100 kilometers. Stratovolcanic edifices commonly are hydrothermal aquifers composed of unstable, altered rock forming steep slopes...
Authors
Kevin M. Scott, Jose Luis Macias, Jose Antonio Naranjo, Sergio Rodriguez, John P. McGeehin
Hydrologic data for Long Valley Caldera, Mono County, California, 1994-96 Hydrologic data for Long Valley Caldera, Mono County, California, 1994-96
Hydrologic data were collected during 1994-96 as part of the U.S. Geological Survey's long-term Volcanic Hazards Monitoring Program of the Long Valley Caldera, Mono County, California, and the Long Valley Hydrologic Advisory Committee monitoring program. Hydrologic data collected include continuous record of ground-water levels in 4 wells; instantaneous measurements of ground-water...
Authors
James F. Howle, Christopher D. Farrar
High-resolution seismic reflection/refraction images near the outer margin of the Chesapeake Bay impact crater, York-James Peninsula, southeastern Virginia High-resolution seismic reflection/refraction images near the outer margin of the Chesapeake Bay impact crater, York-James Peninsula, southeastern Virginia
Powars and Bruce (1999) showed that the Chesapeake Bay region of southeastern Virginia was the site of an asteroid or comet impact during the late Eocene, approximately 35 million years ago (Fig. 1). Initial borehole and marine seismic-reflection data revealed a 90-km-diameter impact structure, referred to as the Chesapeake Bay Impact Crater (CBIC), that lies buried beneath the southern...
Authors
R. D. Catchings, D.E. Saulter, D.S. Powars, M. R. Goldman, J.A. Dingler, G. S. Gohn, J.S. Schindler, G.H. Johnson