Publications
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Geology of the Selk crater region on Titan from Cassini VIMS observations Geology of the Selk crater region on Titan from Cassini VIMS observations
Observations of Titan obtained by the Cassini Visual and Infrared Mapping Spectrometer (VIMS) have revealed Selk crater, a geologically young, bright-rimmed, impact crater located ???800. km north-northwest of the Huygens landing site. The crater rim-crest diameter is ???90. km; its floor diameter is ???60. km. A central pit/peak, 20-30. km in diameter, is seen; the ratio of the size of...
Authors
J.M. Soderblom, R. H. Brown, L.A. Soderblom, J. W. Barnes, R. Jaumann, Stéphane Le Mouélic, Christophe Sotin, K. Stephan, K. H. Baines, B. J. Buratti, R. N. Clark, P. D. Nicholson
Saturn's icy satellites investigated by Cassini-VIMS. II. Results at the end of nominal mission Saturn's icy satellites investigated by Cassini-VIMS. II. Results at the end of nominal mission
We report the detailed analysis of the spectrophotometric properties of Saturn's icy satellites as derived by full-disk observations obtained by visual and infrared mapping spectrometer (VIMS) experiment aboard Cassini. In this paper, we have extended the coverage until the end of the Cassini's nominal mission (June 1st 2008), while a previous paper (Filacchione, G., and 28 colleagues...
Authors
G. Filacchione, F. Capaccioni, R. N. Clark, J.N. Cuzzi, D. P. Cruikshank, A. Coradini, P. Cerroni, P. D. Nicholson, T. B. McCord, R. H. Brown, B. J. Buratti, F. Tosi, R.M. Nelson, R. Jaumann, K. Stephan
The architecture of the Cassini division The architecture of the Cassini division
The Cassini Division in Saturn's rings contains a series of eight named gaps, three of which contain dense ringlets. Observations of stellar occultations by the Visual and Infrared Mapping Spectrometer onboard the Cassini spacecraft have yielded 40 accurate and precise measurements of the radial position of the edges of all of these gaps and ringlets. These data reveal suggestive...
Authors
M.M. Hedman, P. D. Nicholson, K. H. Baines, B. J. Buratti, Christophe Sotin, R. N. Clark, R. H. Brown, R.G. French, E.A. Marouf
Questa Baseline and Pre-mining Ground-Water Quality Investigation, 7. A Pictorial Record of Chemical Weathering, Erosional Processes, and Potential Debris-flow Hazards in Scar Areas Developed on Hydrothermally Altered Rocks Questa Baseline and Pre-mining Ground-Water Quality Investigation, 7. A Pictorial Record of Chemical Weathering, Erosional Processes, and Potential Debris-flow Hazards in Scar Areas Developed on Hydrothermally Altered Rocks
Erosional scar areas developed along the lower Red River basin, New Mexico, reveal a complex natural history of mineralizing processes, rapid chemical weathering, and intense physical erosion during periodic outbursts of destructive, storm-induced runoff events. The scar areas are prominent erosional features with craggy headwalls and steep, denuded slopes. The largest scar areas...
Authors
Geoffrey S. Plumlee, Steve Ludington, Kirk R. Vincent, Philip L. Verplanck, Jonathan S. Caine, K. Eric Livo
Sample collection of ash and burned soils from the October 2007 southern California Wildfires Sample collection of ash and burned soils from the October 2007 southern California Wildfires
Between November 2 through 9, 2007 scientists from the U.S. Geological Survey (USGS) collected samples of ash and burned soils from 28 sites in six areas burned as a result of the Southern California wildfires of October 2007, including the Harris, Witch, Santiago, Ammo, Canyon, and Grass Valley Fires. The primary goal of this sampling and analysis effort was to understand how...
Authors
Todd M. Hoefen, Raymond F. Kokaly, Deborah A. Martin, Carlton J. Rochester, Geoffrey S. Plumlee, Greg Mendez, Eric G. Reichard, Robert N. Fisher
Materials characterization of dusts generated by the collapse of the World Trade Center Materials characterization of dusts generated by the collapse of the World Trade Center
The major inorganic components of the dusts generated from the collapse of the World Trade Center buildings on September 11, 2001 were concrete materials, gypsum, and man-made vitreous fibers. These components were likely derived from lightweight Portland cement concrete floors, gypsum wallboard, and spray-on fireproofing and ceiling tiles, respectively. All of the 36 samples collected...
Authors
Gregory P. Meeker, Stephen J. Sutley, Isabelle Brownfield, Heather Lowers, Amy M. Bern, Gregg A. Swayze, Todd M. Hoefen, Geoffrey S. Plumlee, Roger N. Clark, Carol A. Gent
Inorganic chemical composition and chemical reactivity of settled dust generated by the World Trade Center building collapse Inorganic chemical composition and chemical reactivity of settled dust generated by the World Trade Center building collapse
Samples of dust deposited around lower Manhattan by the September 11, 2001, World Trade Center (WTC) collapse have inorganic chemical compositions that result in part from the variable chemical contributions of concrete, gypsum wallboard, glass fibers, window glass, and other materials contained in the buildings. The dust deposits were also modified chemically by variable interactions...
Authors
Geoffrey S. Plumlee, Philip L. Hageman, Paul J. Lamothe, Thomas L. Ziegler, Gregory P. Meeker, Peter M. Theodorakos, Isabelle Brownfield, Monique G. Adams, Gregg A. Swayze, Todd M. Hoefen, Joseph E. Taggart, Roger N. Clark, S. Wilson, Stephen J. Sutley
Environmental mapping of the World Trade Center area with imaging spectroscopy after the September 11, 2001 attack Environmental mapping of the World Trade Center area with imaging spectroscopy after the September 11, 2001 attack
The Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) was flown over the World Trade Center area on September 16, 18, 22, and 23, 2001. The data were used to map the WTC debris plume and its contents, including the spectral signatures of asbestiform minerals. Samples were collected and used as ground truth for the AVARIS mapping. A number of thermal hot spots were observed with...
Authors
Roger N. Clark, Gregg A. Swayze, Todd M. Hoefen, Robert O. Green, Keith E. Livo, Gregory P. Meeker, Stephen J. Sutley, Geoffrey S. Plumlee, Betina Pavri, Charles M. Sarture, Joe Boardman, Isabelle Brownfield, Laurie C. Morath
Fast forward modeling of Titan's infrared spectra to invert VIMS/Cassini hyperspectral images Fast forward modeling of Titan's infrared spectra to invert VIMS/Cassini hyperspectral images
The surface of Titan, the largest icy moon of Saturn, is veiled by a very thick and hazy atmosphere. The Visual and Infrared Mapping Spectrometer onboard the Cassini spacecraft, in orbit around Saturn since July 2004, conduct an intensive survey of Titan with the objective to understand the complex nature of the atmosphere and surface of the mysterious moon and the way they interact...
Authors
S. Rodriguez, Stéphane Le Mouélic, P. Rannou, J. #NAME? Combe, L.L. Corre, G. Tobie, J. W. Barnes, Christophe Sotin, R. H. Brown, K. H. Baines, B. J. Buratti, R. N. Clark, P. D. Nicholson
Discovery of jarosite within the Mawrth Vallis region of Mars: Implications for the geologic history of the region Discovery of jarosite within the Mawrth Vallis region of Mars: Implications for the geologic history of the region
Analysis of visible to near infrared reflectance data from the MRO CRISM hyperspectral imager has revealed the presence of an ovoid-shaped landform, approximately 3 by 5 km in size, within the layered terrains surrounding the Mawrth Vallis outflow channel. This feature has spectral absorption features consistent with the presence of the ferric sulfate mineral jarosite, specifically a K...
Authors
W. H. Farrand, T.D. Glotch, J. W. Rice, J.A. Hurowitz, G.A. Swayze
A synthesis of Martian aqueous mineralogy after 1 Mars year of observations from the Mars Reconnaissance Orbiter A synthesis of Martian aqueous mineralogy after 1 Mars year of observations from the Mars Reconnaissance Orbiter
Martian aqueous mineral deposits have been examined and characterized using data acquired during Mars Reconnaissance Orbiter's (MRO) primary science phase, including Compact Reconnaissance Imaging Spectrometer for Mars hyperspectral images covering the 0.4-3.9 ??m wavelength range, coordinated with higher-spatial resolution HiRISE and Context Imager images. MRO's new high-resolution...
Authors
S.L. Murchie, J.F. Mustard, B.L. Ehlmann, R.E. Milliken, J.L. Bishop, N.K. McKeown, E.Z. Noe Dobrea, F.P. Seelos, D.L. Buczkowski, S.M. Wiseman, R. E. Arvidson, J.J. Wray, G. Swayze, R. N. Clark, D.J. Des Marais, A. S. McEwen, J.-P. Bibring
Characterizing canopy biochemistry from imaging spectroscopy and its application to ecosystem studies Characterizing canopy biochemistry from imaging spectroscopy and its application to ecosystem studies
For two decades, remotely sensed data from imaging spectrometers have been used to estimate non-pigment biochemical constituents of vegetation, including water, nitrogen, cellulose, and lignin. This interest has been motivated by the important role that these substances play in physiological processes such as photosynthesis, their relationships with ecosystem processes such as litter...
Authors
R.F. Kokaly, Gregory P. Asner, S.V. Ollinger, M.E. Martin, C.A. Wessman