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Three short videos by the Yellowstone Volcano Observatory Three short videos by the Yellowstone Volcano Observatory

This is a collection of videos of unscripted interviews with Jake Lowenstern, who is the Scientist in Charge of the Yellowstone Volcano Observatory (YVO). YVO was created as a partnership among the U.S. Geological Survey (USGS), Yellowstone National Park, and University of Utah to strengthen the long-term monitoring of volcanic and earthquake unrest in the Yellowstone National Park...
Authors
Stephen Wessells, Jake Lowenstern, Dina Venezky

Precision leveling and geodetic GPS observations performed on Surtsey between 1967 and 2002 Precision leveling and geodetic GPS observations performed on Surtsey between 1967 and 2002

The load on the crust from the ~ 0.8 km3 of eruptive products of the Surtsey eruption is expected to lead to subsidence of the Surtsey island by sagging of the lithosphere, compaction of material, and slumping of the volcanic edifice. Immediately after the eruption ended in the summer of 1967 a levelling line was established across the island to monitor this expected subsidence. The line
Authors
Erik Sturkell, P. Einarsson, Halldor Geirsson, E. Tryggvason, James G. Moore, Rosa Olafsdottir

Deep low-frequency earthquakes in tremor localize to the plate interface in multiple subduction zones Deep low-frequency earthquakes in tremor localize to the plate interface in multiple subduction zones

Deep tremor under Shikoku, Japan, consists primarily, and perhaps entirely, of swarms of low-frequency earthquakes (LFEs) that occur as shear slip on the plate interface. Although tremor is observed at other plate boundaries, the lack of cataloged low-frequency earthquakes has precluded a similar conclusion about tremor in those locales. We use a network autocorrelation approach to...
Authors
Justin R. Brown, Gregory C. Beroza, Satoshi Ide, David R. Shelly, Kazuaki Ohta, Susan Y. Schwartz, Wolfgang Rabbel, M. Thorwart, Honn Kao

Mapping products of Titan's surface Mapping products of Titan's surface

Remote sensing instruments aboard the Cassini spacecraft have been observed the surface of Titan globally in the infrared and radar wavelength ranges as well as locally by the Huygens instruments revealing a wealth of new morphological features indicating a geologically active surface. We present a summary of mapping products of Titan's surface derived from data of the remote sensing...
Authors
Katrin Stephan, Ralf Jaumann, Erich Karkoschka, Jason W. Barnes, Martin G. Tomasko, Elizabeth P. Turtle, Lucille Le Corre, Mirjam Langhans, Stephane Le Mouelic, Ralf D. Lorenz, Jason Perry

Ice and water on Newberry Volcano, central Oregon Ice and water on Newberry Volcano, central Oregon

Newberry Volcano in central Oregon is dry over much of its vast area, except for the lakes in the caldera and the single creek that drains them. Despite the lack of obvious glacial striations and well-formed glacial moraines, evidence indicates that Newberry was glaciated. Meter-sized foreign blocks, commonly with smoothed shapes, are found on cinder cones as far as 7 km from the caldera...
Authors
Julie M. Donnelly-Nolan, Robert A. Jensen

Multiple dendrochronological responses to the eruption of Cinder Cone, Lassen Volcanic National Park, California Multiple dendrochronological responses to the eruption of Cinder Cone, Lassen Volcanic National Park, California

Two dendrochronological properties – ring width and ring chemistry – were investigated in trees near Cinder Cone in Lassen Volcanic National Park, northeastern California, for the purpose of re-evaluating the date of its eruption. Cinder Cone is thought to have erupted in AD 1666 based on ring-width evidence, but interpreting ring-width changes alone is not straightforward because many...
Authors
P.R. Sheppard, M.H. Ort, K.C. Anderson, M.A. Clynne, E.M. May

Elements of an improved model of debris-flow motion Elements of an improved model of debris-flow motion

A new depth-averaged model of debris-flow motion describes simultaneous evolution of flow velocity and depth, solid and fluid volume fractions, and pore-fluid pressure. Non-hydrostatic pore-fluid pressure is produced by dilatancy, a state-dependent property that links the depth-averaged shear rate and volumetric strain rate of the granular phase. Pore-pressure changes caused by shearing...
Authors
R.M. Iverson

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

Overview of the magnetic properties experiments on the Mars Exploration Rovers Overview of the magnetic properties experiments on the Mars Exploration Rovers

The Mars Exploration Rovers have accumulated airborne dust on different types of permanent magnets. Images of these magnets document the dynamics of dust capture and removal over time. The strongly magnetic subset of airborne dust appears dark brown to black in Panoramic Camera (Pancam) images, while the weakly magnetic one is bright red. Images returned by the Microscopic Imager reveal...
Authors
M.B. Madsen, W. Goetz, P. Bertelsen, C.S. Binau, F. Folkmann, H.P. Gunnlaugsson, J.I. Hjollum, S.F. Hviid, J. Jensen, K.M. Kinch, K. Leer, D.E. Madsen, J. Merrison, M. Olsen, H.M. Arneson, J.F. Bell, Ralf Gellert, Kenneth E. Herkenhoff, J. R. Johnson, M. J. Johnson, G. Klingelhofer, E. McCartney, D. W. Ming, R.V. Morris, J.B. Proton, D. Rodionov, M. Sims, S. W. Squyres, T. Wdowiak, A. S. Yen

Improved prediction and tracking of volcanic ash clouds Improved prediction and tracking of volcanic ash clouds

During the past 30 years, more than 100 airplanes have inadvertently flown through clouds of volcanic ash from erupting volcanoes. Such encounters have caused millions of dollars in damage to the aircraft and have endangered the lives of tens of thousands of passengers. In a few severe cases, total engine failure resulted when ash was ingested into turbines and coating turbine blades...
Authors
Larry G. Mastin, Peter Webley

A guide to differences between stochastic point-source and stochastic finite-fault simulations A guide to differences between stochastic point-source and stochastic finite-fault simulations

Why do stochastic point-source and finite-fault simulation models not agree on the predicted ground motions for moderate earthquakes at large distances? This question was posed by Ken Campbell, who attempted to reproduce the Atkinson and Boore (2006) ground-motion prediction equations for eastern North America using the stochastic point-source program SMSIM (Boore, 2005) in place of the...
Authors
G. M. Atkinson, K. Assatourians, D.M. Boore, K. Campbell, D. Motazedian
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