Publications
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Cycles of explosive and effusive eruptions at Kīlauea Volcano, Hawai‘i
The subaerial eruptive activity at Kīlauea Volcano (Hawai‘i) for the past 2500 yr can be divided into 3 dominantly effusive and 2 dominantly explosive periods, each lasting several centuries. The prevailing style of eruption for 60% of this time was explosive, manifested by repeated phreatic and phreatomagmatic activity in a deep summit caldera. During dominantly explosive periods, the magma suppl
Authors
Don Swanson, Timothy R. Rose, Adonara E Mucek, Michael O. Garcia, Richard S. Fiske, Larry G. Mastin
Brittle deformation and slope failure at the North Menan Butte tuff cone, Eastern Snake River Plain, Idaho
The manifestation of brittle deformation within inactive slumps along the North Menan Butte, a basaltic tuff cone in the Eastern Snake River Plain, is investigated through field and laboratory studies. Microstructural observations indicate that brittle strain is localized along deformation bands, a class of structural discontinuity that is predominant within moderate to high-porosity, clastic sedi
Authors
Chris H. Okubo
Intraplate seismic hazard: evidence for distributed strain and implications for seismic hazard
No abstract available.
Authors
Susan E. Hough
Surface‐wave Green’s tensors in the near field
We demonstrate the connection between theoretical expressions for the correlation of ambient noise Rayleigh and Love waves and the exact surface‐wave Green’s tensors for a point force. The surface‐wave Green’s tensors are well known in the far‐field limit. On the other hand, the imaginary part of the exact Green’s tensors, including near‐field effects, arises in correlation techniques such as the
Authors
Matthew M. Haney, Hisashi Nakahara
Modeling the effects of source and path heterogeneity on ground motions of great earthquakes on the Cascadia Subduction Zone Using 3D simulations
We ran finite‐difference earthquake simulations for great subduction zone earthquakes in Cascadia to model the effects of source and path heterogeneity for the purpose of improving strong‐motion predictions. We developed a rupture model for large subduction zone earthquakes based on a k−2 slip spectrum and scale‐dependent rise times by representing the slip distribution as the sum of normal modes
Authors
Andrew Delorey, Arthur Frankel, Pengcheng Liu, William J. Stephenson
1964 Great Alaska Earthquake: a photographic tour of Anchorage, Alaska
On March 27, 1964, at 5:36 p.m., a magnitude 9.2 earthquake, the largest recorded earthquake in U.S. history, struck southcentral Alaska (fig. 1). The Great Alaska Earthquake (also known as the Good Friday Earthquake) occurred at a pivotal time in the history of earth science, and helped lead to the acceptance of plate tectonic theory (Cox, 1973; Brocher and others, 2014). All large subduction zon
Authors
Evan E. Thoms, Peter J. Haeussler, Rebecca Anderson, Robert G. McGimsey
Evaluating a slope-stability model for shallow rain-induced landslides using gage and satellite data
Improving prediction of landslide early warning systems requires accurate estimation of the conditions that trigger slope failures. This study tested a slope-stability model for shallow rainfall-induced landslides by utilizing rainfall information from gauge and satellite records. We used the TRIGRS model (Transient Rainfall Infiltration and Grid-based Regional Slope-stability analysis) for simula
Authors
S. Yatheendradas, D. Kirschbaum, Rex L. Baum, Jonathan W. Godt
Evolution of wear and friction along experimental faults
We investigate the evolution of wear and friction along experimental faults composed of solid rock blocks. This evolution is analyzed through shear experiments along five rock types, and the experiments were conducted in a rotary apparatus at slip velocities of 0.002–0.97 m/s, slip distances from a few millimeters to tens of meters, and normal stress of 0.25–6.9 MPa. The wear and friction measurem
Authors
Yeval Boneh, Jefferson C. Chang, David A. Lockner, Zeev Reches
HiRISE observations of Recurring Slope Lineae (RSL) during southern summer on Mars
Recurring Slope Lineae (RSL) are active features on Mars that might require flowing water. Most examples observed through 2011 formed on steep, equator-facing slopes in the southern mid-latitudes. They form and grow during warm seasons and fade and often completely disappear during colder seasons, but recur over multiple Mars years. They are recognizable by their incremental growth, relatively low
Authors
Lujendra Ojha, Alfred McEwen, Colin M. Dundas, Shane Byrne, Sarah Mattson, James Wray, Marion Masse, Ethan Schaefer
ChemCam results from the Shaler Outcrop in Gale Crater, Mars
The "Shaler" outcrop in Gale crater is approximately 0.7 m thick and >20 m long, and exhibits multiple well-exposed platy and cross-stratified facies [1] interpreted to be primarily fluvial sandstone deposits. The outcrop is a part of the upper Glenelg member in the Yellowknife Bay (YKB) stratigraphic section [2]. Curiosity first encountered the "Shaler" outcrop on sol 121 of the mission, and retu
Authors
Ryan Bradley Anderson, L. Edgar, J.C. Bridges, A. Williams, J. Williams, A. Ollila, O. Forni, N. Mangold, N. Lanza, V. Sautter, S. Gupta, D. Blaney, B. Clark, G. Clegg, G. Dromart, O. Gasnault, J. Lasue, S. Le Mouélic, Richard Léveillé, E. Lewin, K. Lewis, S. Maurice, Marion Nachon, H. Newsom, D. Vaniman, R. C. Wiens
Determining grain characteristics in the Shaler Outcrop with ChemCam Remote Micro-Imager mosaics
Analysis of grain size distribution from RMI mosaics (Curiosity) are used to better define variations in grain size and facies in the Shaler outcrop.
Authors
A. J. Williams, J. M. Williams, R.B. Anderson, L.A. Edgar, H. Newsom, S. Le Mouélic, M. Minitti, R. Wiens, S. Maurice
Characterizing the primary material sources and dominant erosional processes for post-fire debris-flow initiation in a headwater basin using multi-temporal terrestrial laser scanning data
Wildfire dramatically alters the hydrologic response of a watershed such that even modest rainstorms can produce hazardous debris flows. Relative to shallow landslides, the primary sources of material and dominant erosional processes that contribute to post-fire debris-flow initiation are poorly constrained. Improving our understanding of how and where material is eroded from a watershed during a
Authors
Dennis M. Staley, Thad A. Waslewicz, Jason W. Kean