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Identifying hazards associated with lava deltas Identifying hazards associated with lava deltas

Lava deltas, formed where lava enters the ocean and builds a shelf of new land extending from the coastline, represent a significant local hazard, especially on populated ocean island volcanoes. Such structures are unstable and prone to collapse—events that are often accompanied by small explosions that can deposit boulders and cobbles hundreds of meters inland. Explosions that coincide...
Authors
Michael P. Poland, Tim R. Orr

Database for the geologic map of upper Eocene to Holocene volcanic and related rocks in the Cascade Range, Washington Database for the geologic map of upper Eocene to Holocene volcanic and related rocks in the Cascade Range, Washington

This geospatial database for a geologic map of the Cascades Range in Washington state is one of a series of maps that shows Cascade Range geology by fitting published and unpublished mapping into a province-wide scheme of lithostratigraphic units. Geologic maps of the Eocene to Holocene Cascade Range in California and Oregon complete the series, providing a comprehensive geologic map of...
Authors
Andrew D. Barron, David W. Ramsey, James G. Smith

Uncertainty estimates in broadband seismometer sensitivities using microseisms Uncertainty estimates in broadband seismometer sensitivities using microseisms

The midband sensitivity of a seismic instrument is one of the fundamental parameters used in published station metadata. Any errors in this value can compromise amplitude estimates in otherwise high-quality data. To estimate an upper bound in the uncertainty of the midband sensitivity for modern broadband instruments, we compare daily microseism (4- to 8-s period) amplitude ratios...
Authors
Adam T. Ringler, Tyler L. Storm, Lind S. Gee, Charles R. Hutt, David C. Wilson

Comparative mineral chemistry and textures of SAFOD fault gouge and damage-zone rocks Comparative mineral chemistry and textures of SAFOD fault gouge and damage-zone rocks

Creep in the San Andreas Fault Observatory at Depth (SAFOD) drillhole is localized to two foliated gouges, the central deforming zone (CDZ) and southwest deforming zone (SDZ). The gouges consist of porphyroclasts of serpentinite and sedimentary rock dispersed in a foliated matrix of Mg-smectite clays that formed as a result of shearing-enhanced reactions between the serpentinite and
Authors
Diane E. Moore

Using surface creep rate to infer fraction locked for sections of the San Andreas fault system in northern California from alignment array and GPS data Using surface creep rate to infer fraction locked for sections of the San Andreas fault system in northern California from alignment array and GPS data

Surface creep rate, observed along five branches of the dextral San Andreas fault system in northern California, varies considerably from one section to the next, indicating that so too may the depth at which the faults are locked. We model locking on 29 fault sections using each section’s mean long‐term creep rate and the consensus values of fault width and geologic slip rate. Surface...
Authors
James J. Lienkaemper, Forrest S. McFarland, Robert W. Simpson, S. John Caskey

Ball-and-socket tectonic rotation during the 2013 Mw7.7 Balochistan earthquake Ball-and-socket tectonic rotation during the 2013 Mw7.7 Balochistan earthquake

The September 2013 Mw7.7 Balochistan earthquake ruptured a ∼200-km-long segment of the curved Hoshab fault in southern Pakistan with 10±0.2 m of peak sinistral and ∼1.7±0.8 m of dip slip. This rupture is unusual because the fault dips 60±15° towards the focus of a small circle centered in northwest Pakistan, and, despite a 30° increase in obliquity along strike, the ratios of strike and...
Authors
William D. Barnhart, Gavin P. Hayes, Richard W. Briggs, Ryan D. Gold, R. Bilham

Potential postwildfire debris-flow hazards: a prewildfire evaluation for the Sandia and Manzano Mountains and surrounding areas, central New Mexico Potential postwildfire debris-flow hazards: a prewildfire evaluation for the Sandia and Manzano Mountains and surrounding areas, central New Mexico

Wildfire can drastically increase the probability of debris flows, a potentially hazardous and destructive form of mass wasting, in landscapes that have otherwise been stable throughout recent history. Although there is no way to know the exact location, extent, and severity of wildfire, or the subsequent rainfall intensity and duration before it happens, probabilities of fire and debris...
Authors
Anne C. Tillery, Jessica R. Haas, Lara W. Miller, Joe H. Scott, Matthew P. Thompson

Rapid mapping of ultrafine fault zone topography with structure from motion Rapid mapping of ultrafine fault zone topography with structure from motion

Structure from Motion (SfM) generates high-resolution topography and coregistered texture (color) from an unstructured set of overlapping photographs taken from varying viewpoints, overcoming many of the cost, time, and logistical limitations of Light Detection and Ranging (LiDAR) and other topographic surveying methods. This paper provides the first investigation of SfM as a tool for...
Authors
Kendra Johnson, Edwin Nissen, Srikanth Saripalli, J. Ramon Arrowsmith, Patrick McGarey, Katherine M. Scharer, Patrick Williams, Kimberly Blisniuk

Dynamics of the Yellowstone hydrothermal system Dynamics of the Yellowstone hydrothermal system

The Yellowstone Plateau Volcanic Field is characterized by extensive seismicity, episodes of uplift and subsidence, and a hydrothermal system that comprises more than 10,000 thermal features, including geysers, fumaroles, mud pots, thermal springs, and hydrothermal explosion craters. The diverse chemical and isotopic compositions of waters and gases derive from mantle, crustal, and...
Authors
Shaul Hurwitz, Jacob B. Lowenstern

Interannual observations and quantification of summertime H2O ice deposition on the Martian CO2 ice south polar cap Interannual observations and quantification of summertime H2O ice deposition on the Martian CO2 ice south polar cap

The spectral signature of water ice was observed on Martian south polar cap in 2004 by the Observatoire pour l'Mineralogie, l'Eau les Glaces et l'Activite (OMEGA) ( Bibring et al., 2004). Three years later, the OMEGA instrument was used to discover water ice deposited during southern summer on the polar cap ( Langevin et al., 2007). However, temporal and spatial variations of these water...
Authors
Adrian J. Brown, Sylvain Piqueux, Timothy N. Titus

Chemical complexity and source of the White River Ash, Alaska and Yukon Chemical complexity and source of the White River Ash, Alaska and Yukon

The White River Ash, a prominent stratigraphic marker bed in Alaska (USA) and Yukon (Canada), consists of multiple compositional units belonging to two geochemical groups. The compositional units are characterized using multiple criteria, with combined glass and ilmenite compositions being the best discriminators. Two compositional units compose the northern group (WRA-Na and WRA-Nb)...
Authors
S.J. Preece, Robert G. McGimsey, J.A. Westgate, N.J.G. Pearce, W.K. Hartmann, W.T. Perkins

Laboratory generated M -6 earthquakes Laboratory generated M -6 earthquakes

We consider whether mm-scale earthquake-like seismic events generated in laboratory experiments are consistent with our understanding of the physics of larger earthquakes. This work focuses on a population of 48 very small shocks that are foreshocks and aftershocks of stick–slip events occurring on a 2.0 m by 0.4 m simulated strike-slip fault cut through a large granite sample. Unlike...
Authors
Gregory C. McLaskey, Brian D. Kilgore, David A. Lockner, Nicholas M. Beeler
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