Publications
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Mars Exploration Program 2007 Phoenix landing site selection and characteristics Mars Exploration Program 2007 Phoenix landing site selection and characteristics
To ensure a successful touchdown and subsequent surface operations, the Mars Exploration Program 2007 Phoenix Lander must land within 65° to 72° north latitude, at an elevation less than −3.5 km. The landing site must have relatively low wind velocities and rock and slope distributions similar to or more benign than those found at the Viking Lander 2 site. Also, the site must have a soil...
Authors
R. Arvidson, D. Adams, G. Bonfiglio, P. Christensen, S. Cull, Matthew P. Golombek, J. Guinn, E. Guinness, T. Heet, Randolph L. Kirk, A. Knudson, M. Malin, M. Mellon, Alfred S. McEwen, A. Mushkin, T. Parker, F. Seelos, K. Seelos, P. Smith, D. Spencer, T. Stein, L. Tamppari
Evaluation of CAMEL - comprehensive areal model of earthquake-induced landslides Evaluation of CAMEL - comprehensive areal model of earthquake-induced landslides
A new comprehensive areal model of earthquake-induced landslides (CAMEL) has been developed to assist in planning decisions related to disaster risk reduction. CAMEL provides an integrated framework for modeling all types of earthquake-induced landslides using fuzzy logic systems and geographic information systems. CAMEL is designed to facilitate quantitative and qualitative...
Authors
S.B. Miles, D. K. Keefer
Martian mud volcanism: Terrestrial analogs and implications for formational scenarios Martian mud volcanism: Terrestrial analogs and implications for formational scenarios
The geology of Mars and the stratigraphic characteristics of its uppermost crust (mega-regolith) suggest that some of the pervasively-occurring pitted cones, mounds, and flows may have formed through processes akin to terrestrial mud volcanism. A comparison of terrestrial mud volcanism suggests that equivalent Martian processes likely required discrete sedimentary depocenters, volatile...
Authors
James A. Skinner, A. Mazzini
Assessment of the UV camera sulfur dioxide retrieval for point source plumes Assessment of the UV camera sulfur dioxide retrieval for point source plumes
Digital cameras, sensitive to specific regions of the ultra-violet (UV) spectrum, have been employed for quantifying sulfur dioxide (SO2) emissions in recent years. The instruments make use of the selective absorption of UV light by SO2 molecules to determine pathlength concentration. Many monitoring advantages are gained by using this technique, but the accuracy and limitations have not...
Authors
M.P. Dalton, I.M. Watson, P.A. Nadeau, C. Werner, W. Morrow, J.M. Shannon
Geomorphology, stability and mobility of the Currituck slide Geomorphology, stability and mobility of the Currituck slide
Over the last 100,000??years, the U.S. Atlantic continental margin has experienced various types of mass movements some of which are believed to have taken place at times of low sea level. At one of these times of low sea level a significant trigger caused a major submarine mass movement off the coast of Virginia: the Currituck slide which is believed to have taken place between 24 and...
Authors
J. Locat, H. Lee, Uri S. ten Brink, D. Twichell, E. Geist, M. Sansoucy
Uplift and magma intrusion at Long Valley caldera from InSAR and gravity measurements Uplift and magma intrusion at Long Valley caldera from InSAR and gravity measurements
The Long Valley caldera (California) formed ~760,000 yr ago following the massive eruption of the Bishop Tuff. Postcaldera volcanism in the Long Valley volcanic field includes lava domes as young as 650 yr. The recent geological unrest is characterized by uplift of the resurgent dome in the central section of the caldera (75 cm in the past 33 yr) and earthquake activity followed by...
Authors
Pietro Tizzani, Maurizio Battaglia, Giovanni Zeni, Simone Atzori, Paolo Berardino, Riccardo Lanari
Reassessment of probabilistic seismic hazard in the Marmara region Reassessment of probabilistic seismic hazard in the Marmara region
In 1999, the eastern coastline of the Marmara region (Turkey) witnessed increased seismic activity on the North Anatolian fault (NAF) system with two damaging earthquakes (M 7.4 Kocaeli and M 7.2 D??zce) that occurred almost three months apart. These events have reduced stress on the western segment of the NAF where it continues under the Marmara Sea. The undersea fault segments have...
Authors
Erol Kalkan, Polat Gulkan, Nazan Yilmaz, Mehmet Çelebi
Morphology of late Quaternary submarine landslides along the U.S. Atlantic continental margin Morphology of late Quaternary submarine landslides along the U.S. Atlantic continental margin
The nearly complete coverage of the U.S. Atlantic continental slope and rise by multibeam bathymetry and backscatter imagery provides an opportunity to reevaluate the distribution of submarine landslides along the margin and reassess the controls on their formation. Landslides can be divided into two categories based on their source areas: those sourced in submarine canyons and those...
Authors
D.C. Twichell, J.D. Chaytor, Uri S. ten Brink, B. Buczkowski
Postshield stage transitional volcanism on Mahukona Volcano, Hawaii Postshield stage transitional volcanism on Mahukona Volcano, Hawaii
Age spectra from 40Ar/39Ar incremental heating experiments yield ages of 298 ± 25ka and 310 ± 31ka for transitional composition lavas from two cones on submarine Mahukona Volcano, Hawaii. These ages are younger than the inferred end of the tholeiitic shield stage and indicate that the volcano had entered the postshield alkalic stage before going extinct. Previously reported elevated...
Authors
D.A. Clague, A.T. Calvert
Revised Dst and the epicycles of magnetic disturbance: 1958-2007 Revised Dst and the epicycles of magnetic disturbance: 1958-2007
A revised version of the storm-time disturbance index Dst is calculated using hourly-mean magnetic-observatory data from four standard observatories and collected over the years 1958-2007. The calculation algorithm is a revision of that established by Sugiura et al., and which is now used by the Kyoto World Data Center for routine production of Dst. The most important new development is...
Authors
J.J. Love, J.L. Gannon
Non-double-couple mechanisms of microearthquakes induced by hydraulic fracturing Non-double-couple mechanisms of microearthquakes induced by hydraulic fracturing
We have inverted polarity and amplitude information of representative microearthquakes to investigate source mechanisms of seismicity induced by hydraulic fracturing in the Carthage Cotton Valley, east Texas, gas field. With vertical arrays of four and eight three-component geophones in two monitoring wells, respectively, we were able to reliably determine source mechanisms of the...
Authors
J. Sileny, D.P. Hill, Leo Eisner, F.H. Cornet
Toward a comprehensive areal model of earthquake-induced landslides Toward a comprehensive areal model of earthquake-induced landslides
This paper provides a review of regional-scale modeling of earthquake-induced landslide hazard with respect to the needs for disaster risk reduction and sustainable development. Based on this review, it sets out important research themes and suggests computing with words (CW), a methodology that includes fuzzy logic systems, as a fruitful modeling methodology for addressing many of these...
Authors
S.B. Miles, D. K. Keefer