Publications
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Evidence from the AD 2000 Izu islands earthquake swarm that stressing rate governs seismicity Evidence from the AD 2000 Izu islands earthquake swarm that stressing rate governs seismicity
Magma intrusions and eruptions commonly produce abrupt changes in seismicity far from magma conduits1,2,3,4 that cannot be associated with the diffusion of pore fluids or heat5. Such ‘swarm’ seismicity also migrates with time, and often exhibits a ‘dog-bone’-shaped distribution3,4,6,7,8,9. The largest earthquakes in swarms produce aftershocks that obey an Omori-type (exponential)...
Authors
Shingi Toda, Ross S. Stein, Takeshi Sagiya
Animation of the Holocene evolution of the southern Washington and northern Oregon shelf and coast Animation of the Holocene evolution of the southern Washington and northern Oregon shelf and coast
No abstract available.
Authors
VeAnn A. Cross, David C. Twichell
Basis and methods of NASA airborne topographic mapper lidar surveys for coastal studies Basis and methods of NASA airborne topographic mapper lidar surveys for coastal studies
This paper provides an overview of the basic principles of airborne laser altimetry for surveys of coastal topography, and describes the methods used in the acquisition and processing of NASA Airborne Topographic Mapper (ATM) surveys that cover much of the conterminous US coastline. This form of remote sensing, also known as "topographic lidar", has undergone extremely rapid development...
Authors
John Brock, C. Wayne Wright, Asbury H. Sallenger, William B. Krabill, Robert N. Swift
Genesis of the Doğankuzu and Mortaş Bauxite deposits, Taurides, Turkey: separation of Al, Fe, and Mn and implications for passive margin metallogeny Genesis of the Doğankuzu and Mortaş Bauxite deposits, Taurides, Turkey: separation of Al, Fe, and Mn and implications for passive margin metallogeny
The Taurides region of Turkey is host to a number of important bauxite, Al-rich laterite, and Mn deposits. The most important bauxite deposits, Doğankuzu and Mortaş, are karst-related, unconformity-type deposits in Upper Cretaceous limestone. The bottom contact of the bauxite ore is undulatory, and bauxite fills depressions and sinkholes in the footwall limestone, whereas its top surface...
Authors
Huseyin Ozturk, James R. Hein, Nurullah Hanilci
Interpreting the earthquake source of the Wabash Valley seismic zone (Illinois, Indiana, and Kentucky) from seismic-reflection, gravity, and magnetic-intensity data Interpreting the earthquake source of the Wabash Valley seismic zone (Illinois, Indiana, and Kentucky) from seismic-reflection, gravity, and magnetic-intensity data
Reprocessing of seismic-reflection data reveals new images of upper- to middle-crustal structures beneath the Wabash Valley seismic zone, located north of the New Madrid seismic zone within the seismically active southern Illinois basin. Four intersecting deep seismic profiles (243 km total) indicate an anomalous, 5–10-km-wide zone of dipping reflections and diffractions below the...
Authors
John H. McBride, Thomas G. Hildenbrand, William J. Stephenson, Christopher J. Potter
Emergency assessment of potential debris-flow peak discharges, Missionary Ridge fire, Colorado Emergency assessment of potential debris-flow peak discharges, Missionary Ridge fire, Colorado
These maps present the results of assessments of peak discharges that can potentially be generated by debris flows issuing from the basins burned by the Missionary Ridge fire of June 9 through July 14, 2002, near Durango, Colorado. The maps are based on a regression model for debris-flow peak discharge normalized by average storm intensity as a function of basin gradient and burned...
Authors
Susan H. Cannon, Alan H. Rea, J. Andrew Gleason, Stephen P. Garcia
Hawaiian Volcano Observatory summary 101: Part 1, seismic data, January to December 2001 Hawaiian Volcano Observatory summary 101: Part 1, seismic data, January to December 2001
The Hawaiian Volcano Observatory (HVO) summary presents seismic data gathered during the year and a chronological narrative describing the volcanic events. The seismic summary is offered without interpretation as a source of preliminary data. It is complete in the sense that all data for events of M>1.5 routinely gathered by the Observatory are included. The emphasis in collection of...
Authors
Jennifer S. Nakata, C. Heliker
Topographic map of Mars M 25M RKN Topographic map of Mars M 25M RKN
NOTES ON BASE This map is based on data from the Mars Orbiter Laser Altimeter (MOLA) (Smith and others, 2001), an instrument on NASA's Mars Global Surveyor (MGS) spacecraft (Albee and others, 2001). The image used for the base of this map represents more than 600 million measurements gathered between 1999 and 2001, adjusted for consistency (Neumann and others, 2001, 2002) and converted...
Authors
Water Resources Division U.S. Geological Survey
Color-coded contour map of Mars M 25M RKN Color-coded contour map of Mars M 25M RKN
NOTES ON BASE This map is based on data from the Mars Orbiter Laser Altimeter (MOLA) (Smith and others, 2001), an instrument on NASA's Mars Global Surveyor (MGS) spacecraft (Albee and others, 2001). The image used for the base of this map represents more than 600 million measurements gathered between 1999 and 2001, adjusted for consistency (Neumann and others, 2001, 2002) and converted...
Authors
Water Resources Division U.S. Geological Survey
Mars Geodesy/Cartography Working Group recommendations on Mars cartographic constants and coordinate systems Mars Geodesy/Cartography Working Group recommendations on Mars cartographic constants and coordinate systems
NASA's Mars Geodesy/Cartography Working Group (MGCWG), established in 1998 and chaired since 2000 by one of us (TCD), consists of leading researchers in planetary geodesy and cartography at such diverse institutions as JPL, NASA Ames and Goddard Centers, Purdue and Ohio State Universities, Malin Space Science Systems, the German Center for Aerospace Research DLR, and the US Geological...
Authors
T. C. Duxbury, Randolph L. Kirk, Brent A. Archinal, G.A. Neumann