Natural Hazards
Publications
Exposure of an early to middle Noachian valley network in three dimensions on Mars
We document a set of channels in a section of the Martian cratered highlands located between crustal massifs northeast of Hellas Planitia that are visible in cross section and planview >200 m below the surface. The morphometry and spatial distribution of the outcrops provide concrete geological evidence of a dynamic aqueous system in a...
Skinner, James A.; Fortezzo, Corey M.; Mouginis-Mark, Peter J.
Geologic map of Jezero crater and the Nili Planum region, Mars
The cratered highlands located northwest of Isidis Planitia have been recognized as one of the best preserved Noachian landscapes currently exposed on Mars; the area hosts a record of diverse surface processes, diagenesis, and aqueous alteration. This region has consistently been considered a high priority for landed-mission exploration and...
Sun, Vivian Z.; Stack, Kathryn M. Planetary cave exploration progresses
Planetary caves have been identified on the Moon and on Mars, and are likely to occur across the Solar System. They present a new frontier for planetary science, subsurface astrobiology, geology and human exploration. The fourth in a series of scientific meetings focusing on the science and exploration of planetary caves brought together 55...
Titus, Timothy N.; Phillips-Lander, C. M.; Boston, P. J.; Wynne, J. J.; Kerber, L. Generalizing the inversion‐based PSHA source model for an interconnected fault system
This article represents a step toward generalizing and simplifying the procedure for constructing an inversion‐based seismic hazard source model for an interconnected fault system, including the specification of adjustable segmentation constraints. A very simple example is used to maximize understandability and to counter the notion that an...
Field, Edward H.; Milner, Kevin R.; Page, Morgan T. Earthquake early warning in Aotearoa New Zealand: A survey of public perspectives to guide warning system development
Earthquake early warning (EEW) can be used to detect earthquakes and provide advanced notification of strong shaking, allowing pre-emptive actions to be taken that not only benefit infrastructure but reduce injuries and fatalities. Currently Aotearoa New Zealand does not have a nationwide EEW system, so a survey of the public was undertaken to...
Becker, Julia S.; Potter, Sally H.; Vinnel, Lauren; Nakayachi, Kazuya; McBride, Sara; Johnston, David A. Detection and assessment of a large and potentially‐tsunamigenic periglacial landslide in Barry Arm, Alaska
The retreat of glaciers in response to global warming has the potential to trigger landslides in glaciated regions around the globe. Landslides that enter fjords or lakes can cause tsunamis, which endanger people and infrastructure far from the landslide itself. Here we document the ongoing movement of an unstable slope (total volume of 455...
Dai, Chunli; Higman, Bretwood; Lynett, Patrick J.; Jacquemart, Mylène; Howat, Ian; Liljedahl, Anna K.; Dufresne, Anja; Freymueller, Jeffery T.; Geertsema, Marten; Jones, Melissa Ward; Haeussler, Peter Evaluation of seismic hazard models with fragile geologic features
We provide an overview of a 2019 workshop on the use of fragile geologic features (FGFs) to evaluate seismic hazard models. FGFs have been scarcely utilized in the evaluation of seismic hazard models, despite nearly 30 yr having passed since the first recognition of their potential value. Recently, several studies have begun to focus on the...
Stirling, Mark W.; Oskin, Mike; Arrowsmith, J. Ramon; Rood, Anna H.; Goulet, Christine A.; Grant Ludwig, Lisa; King, Tamarah; Kottke, Albert; Lozos, Julian C.; Madugo, Chris L M; McPhillips, Devin; Rood, Dylan; Sleep, Norman; Wittich, Christine Injection‐induced earthquakes near Milan, Kansas, controlled by Karstic Networks
Induced earthquakes from waste disposal operations in otherwise tectonically stable regions significantly increases seismic hazard. It remains unclear why injections induce large earthquakes on non‐optimally oriented faults kilometers below the injection horizon, particularly since fluids are not injected under pressure, but rather poured, into...
Joubert, Charlene; Sohrabi, Reza; Rubinstein, Justin; Jansen, Gunnar; Miller, Stephen A Localized fault-zone dilatancy and surface inelasticity of the 2019 Ridgecrest earthquakes
Earthquakes produce a spectrum of elastic and inelastic deformation processes that are reflected across various length and time scales. While elasticity has long dominated research assumptions in active tectonics, increasing interest has focused on the inelastic characteristics of earthquakes, particularly those of the surface fault rupture zone...
Barnhart, William D.; Gold, Ryan D.; Hollingsworth, James Identifying the greatest earthquakes of the past 2000 years at the Nehalem River Estuary, Northern Oregon Coast, USA
We infer a history of three great megathrust earthquakes during the past 2000 years at the Nehalem River estuary based on the lateral extent of sharp (≤3 mm) peat-mud stratigraphic contacts in cores and outcrops, coseismic subsidence as interpreted from fossil diatom assemblages and reconstructed with foraminiferal assemblages using a Bayesian...
Nelson, Alan R.; Hawkes, Andrea D.; Sawai, Yuki; Engelhart, Simon E.; Witter, Robert C.; Grant-Walter, Wendy C.; Bradley, Lee-Ann; Dura, Tina; Cahill, Niamh; Horton, Benajamin P. VS30 and Dominant Site Frequency (fd) as Provisional Station ML Corrections (dML) in California
New seismic stations added to a regional seismic network cannot be used to calculate local magnitude (ML">MLML) until a revised regionwide amplitude decay function is developed. Each station must record a minimum number of local and regional earthquakes that meet specific amplitude requirements prior to recalibration of the amplitude decay...
Yong, Alan; Cochran, Elizabeth S.; Andrews, Jennifer; Hudson, Kenneth; Antony Martin; Yu, Ellen; Herrick, Julie A; Dozal, Jessica Selecting three components of ground motions from Conditional Spectra for multiple stripe analyses
For complex structures where the seismic response depends appreciably on the vertical (V) component of ground motion (GM) (e.g., base-isolated buildings, long-span bridges, dams, nuclear power plants), incremental dynamic analysis (IDA) is commonly utilized to estimate seismic risk, where the V components of GM are selected and scaled based on the...
Kwong, Neal (Simon) S; Jaiswal, Kishor; Luco, Nicolas; Baker, J.W.