Publications
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Density structure of the island of Hawai’i and the implications for gravity-driven motion of the south flank of Kilauea volcano Density structure of the island of Hawai’i and the implications for gravity-driven motion of the south flank of Kilauea volcano
The discovery that large landslides dissected the Hawaiian islands, scattering debris over thousands of square kilometers of seafloor, changed our ideas of island growth and evolution. The evidence is consistent with catastrophic flank collapse during volcano growth, and draws our focus to the currently active island of Hawai’i, the volcanoes Mauna Loa and Kīlauea, and particularly to...
Authors
Roger P. Denlinger, Ashton F. Flinders
Evolution in eruptive style of the 2018 eruption of Veniaminof volcano, Alaska, reflected in groundmass textures and remote sensing Evolution in eruptive style of the 2018 eruption of Veniaminof volcano, Alaska, reflected in groundmass textures and remote sensing
Variable eruptive style and explosivity is common in basaltic to basaltic andesite volcanoes but can have uncertain origins. Veniaminof volcano in the Alaska-Aleutian arc is a frequently active open-vent center, regularly producing Strombolian eruptions and small lava flows from an intracaldera cone within an intracaldera ice cap. The September–December 2018 eruption of Veniaminof...
Authors
Matthew W. Loewen, Hannah R. Dietterich, Nathan Graham, Pavel Izbekof
Influence of permafrost type and site history on losses of permafrost carbon after thaw Influence of permafrost type and site history on losses of permafrost carbon after thaw
We quantified permafrost peat plateau and post-thaw carbon (C) stocks across a chronosequence in Interior Alaska to evaluate the amount of C lost with thaw. Macrofossil reconstructions revealed three stratigraphic layers of peat: (1) a base layer of fen/marsh peat, (2) peat from a forested peat plateau (with permafrost) and, (3) collapse-scar bog peat (at sites where permafrost thaw has...
Authors
Kristen L. Manies, Miriam C. Jones, Mark Waldrop, Mary-Catherine Leewis, Christopher C. Fuller, Robert S. Cornman, Kristen Hoefke
Fitting jet noise similarity spectra to volcano infrasound data Fitting jet noise similarity spectra to volcano infrasound data
Infrasound (low-frequency acoustic waves) has proven useful to detect and characterize subaerial volcanic activity, but understanding the infrasonic source during sustained eruptions is still an area of active research. Preliminary comparison between acoustic eruption spectra and the jet noise similarity spectra suggests that volcanoes can produce an infrasonic form of jet noise from...
Authors
Julia Gestrich, David Fee, Robin Matoza, John J. Lyons, Mario Ruiz
A 40-year story of river sediment at Mount St. Helens A 40-year story of river sediment at Mount St. Helens
The 1980 eruption of Mount St. Helens in Washington State unleashed one of the largest debris avalanches (landslide) in recorded history. The debris avalanche deposited 3.3 billion cubic yards of material into the upper North Fork Toutle River watershed and obstructed the Columbia River shipping channel downstream. From the eruption on May 18, 1980, to September 30, 2018, the Toutle...
Authors
Mark A. Uhrich, Kurt R. Spicer, Adam R. Mosbrucker, Dennis R. Saunders, Tami S. Christianson
A new analysis of caldera unrest through the integration of geophysical data and FEM modeling: The Long Valley caldera case study A new analysis of caldera unrest through the integration of geophysical data and FEM modeling: The Long Valley caldera case study
The Long Valley Caldera, located at the eastern edge of the Sierra Nevada range in California, has been in a state of unrest since the late 1970s. Seismic, gravity and geodetic data strongly suggest that the source of unrest is an intrusion beneath the caldera resurgent dome. However, it is not clear yet if the main contribution to the deformation comes from pulses of ascending high...
Authors
Fabio Pulvirenti, Francesca Silverii, Maurizio Battaglia
Geodetic constraints on a 25-year magmatic inflation episode near Three Sisters, central Oregon Geodetic constraints on a 25-year magmatic inflation episode near Three Sisters, central Oregon
Crustal inflation near the Three Sisters volcanic center documented since the mid-1990s has persisted for more than two decades. We update past analyses of the event through 2020 by simultaneously inverting InSAR interferograms, GPS time series, and leveling data for time-dependent volcanic deformation source parameters. We explore several source models to estimate how the deformation...
Authors
Michael Lisowski, Robert McCaffrey, Charles Wicks, Daniel Dzurisin
Five-year management plan for establishing and operating NVEWS—The National Volcano Early Warning System Five-year management plan for establishing and operating NVEWS—The National Volcano Early Warning System
On March 12, 2019, Congress passed the John D. Dingell, Jr., Conservation, Management, and Recreation Act (Public Law 116–9; 133 Stat. 580), in which Title V, §5001 (43 U.S.C. 31k) authorized the establishment of the National Volcano Early Warning and Monitoring System (NVEWS) within the U.S. Geological Survey (USGS). Conceived by the USGS Volcano Hazards Program in 2005, NVEWS is...
Authors
Peter F. Cervelli, Charlie Mandeville, Victoria F. Avery, Aleeza Wilkins
Evaluating lava flow propagation models with a case study from the 2018 eruption of Kīlauea Volcano, Hawai'i Evaluating lava flow propagation models with a case study from the 2018 eruption of Kīlauea Volcano, Hawai'i
The 2018 lower East Rift Zone (LERZ) eruption of Kīlauea, Hawai’i, provides an excellent natural laboratory with which to test models of lava flow propagation. During early stages of eruption crises, the most useful lava flow propagation equations utilize readily determined parameters and require fewer a priori assumptions about future behavior of the flow. Here, we leverage the numerous
Authors
Rebecca deGraffenried, Julia E. Hammer, Hannah R. Dietterich, Ryan L. Perroy, Matthew R. Patrick, Thomas Shea
High-speed lava flow infrasound from Kīlauea’s fissure 8 and its utility in monitoring effusion rate High-speed lava flow infrasound from Kīlauea’s fissure 8 and its utility in monitoring effusion rate
The 2018 eruption of Kīlauea Volcano produced large and destructive lava flows from the fissure 8 (Ahu ‘aila ‘au) vent with flow velocities up to 17 m s−1, highly variable effusion rates over both short (minutes) and long (hours) time scales, and a proximal channel or spillway that displayed flow features similar to open channel flow in river systems. Monitoring such dynamic vent and...
Authors
John J. Lyons, Hannah R. Dietterich, Matthew R. Patrick, David Fee
Rayleigh-wave ellipticity in weakly heterogeneous layered media Rayleigh-wave ellipticity in weakly heterogeneous layered media
We derive approximate expressions for the ellipticity (i.e. horizontal-to-vertical or vertical-to-horizontal ratio) of Rayleigh waves propagating in a layered medium. The approximation is based on the generalized energy equation for Rayleigh waves, which has been used previously to obtain perturbational results for ellipticity. For a medium with weakly heterogeneous layers, we obtain an
Authors
Matthew M. Haney, Victor C. Tsai
Arc versus river: The geology of the Columbia River Gorge Arc versus river: The geology of the Columbia River Gorge
The Columbia River Gorge is the Columbia River’s long-held yet evolving passage through the volcanic arc of the Cascade Range. The globally unique setting of a continental-scale river bisecting an active volcanic arc at the leading edge of a major plate boundary creates a remarkable setting where dynamic volcanic and tectonic processes interact with diverse and energetic fluvial...
Authors
Jim E. O'Connor, Ray Wells, Scott E.K. Bennett, Charles M. Cannon, Lydia M. Staisch, James L Anderson, Anthony Francis Pivarunas, Gabriel Wells Gordon, Richard J. Blakely, Mark E. Stelten, Russell C. Evarts