Publications
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The relative effectiveness of empirical and physical models for simulating the dense undercurrent of pyroclastic flows under different emplacement conditions The relative effectiveness of empirical and physical models for simulating the dense undercurrent of pyroclastic flows under different emplacement conditions
High concentration pyroclastic density currents (PDCs) are hot avalanches of volcanic rock and gas and are among the most destructive volcanic hazards due to their speed and mobility. Mitigating the risk associated with these flows depends upon accurate forecasting of possible impacted areas, often using empirical or physical models. TITAN2D, VolcFlow, LAHARZ, and ΔH/L or energy cone...
Authors
Sarah E. Ogburn, Eliza S Calder
Database for geologic maps of pyroclastic-flow and related deposits of the 1980 eruptions of Mount St. Helens, Washington Database for geologic maps of pyroclastic-flow and related deposits of the 1980 eruptions of Mount St. Helens, Washington
This publication releases digital versions of the geologic maps in U.S. Geological Survey Miscellaneous Investigations Map 1950 (USGS I-1950), “Geologic maps of pyroclastic-flow and related deposits of the 1980 eruptions of Mount St. Helens, Washington” (Kuntz, Rowley, and MacLeod, 1990) (https://pubs.er.usgs.gov/publication/i1950). The 1980 Mount St. Helens eruptions on May 18, May 25...
Authors
Andrew J. Furze, Joseph A. Bard, Joel Robinson, David W. Ramsey, Mel A. Kuntz, Peter D. Rowley, Norman S. MacLeod
Probing magma reservoirs to improve volcano forecasts Probing magma reservoirs to improve volcano forecasts
When it comes to forecasting eruptions, volcano observatories rely mostly on real-time signals from earthquakes, ground deformation, and gas discharge, combined with probabilistic assessments based on past behavior [Sparks and Cashman, 2017]. There is comparatively less reliance on geophysical and petrological understanding of subsurface magma reservoirs.
Authors
Jacob B. Lowenstern, Thomas W. Sisson, Shaul Hurwitz
The Volcano Disaster Assistance Program—Helping to save lives worldwide for more than 30 years The Volcano Disaster Assistance Program—Helping to save lives worldwide for more than 30 years
What do you do when a sleeping volcano roars back to life? For more than three decades, countries around the world have called upon the U.S. Geological Survey’s (USGS) Volcano Disaster Assistance Program (VDAP) to contribute expertise and equipment in times of crisis. Co-funded by the USGS and the U.S. Agency for International Development’s Office of U.S. Foreign Disaster Assistance...
Authors
Jacob B. Lowenstern, David W. Ramsey
Volcanic unrest at Mauna Loa, Earth's largest active volcano Volcanic unrest at Mauna Loa, Earth's largest active volcano
Mauna Loa is showing persistent signs of volcanic unrest. Since 2014, increased seismicity and deformation indicate that Mauna Loa, the volcano that dominates more than half of the island of Hawaiʻi, may be building toward its first eruption since 1984. Thousands of residents and key infrastructure are potentially at risk from lava flows, so a critical question is whether the volcano...
Authors
Weston Thelen, Asta Mikijus, Christina A. Neal
Seismic evidence for a possible deep crustal hot zone beneath Southwest Washington Seismic evidence for a possible deep crustal hot zone beneath Southwest Washington
Crustal pathways connecting deep sources of melt and the active volcanoes they supply are poorly understood. Beneath Mounts St. Helens, Adams, and Rainier these pathways connect subduction-induced ascending melts to shallow magma reservoirs. Petrogenetic modeling predicts that when these melts are emplaced as a succession of sills into the lower crust they generate deep crustal hot zones...
Authors
Ashton F. Flinders, Yang Shen
Kīlauea summit eruption—Lava returns to Halemaʻumaʻu Kīlauea summit eruption—Lava returns to Halemaʻumaʻu
In March 2008, a new volcanic vent opened within Halemaʻumaʻu, a crater at the summit of Kīlauea Volcano in Hawaiʻi Volcanoes National Park on the Island of Hawaiʻi. This new vent is one of two ongoing eruptions on the volcano. The other is on Kīlauea’s East Rift Zone, where vents have been erupting nearly nonstop since 1983. The duration of these simultaneous summit and rift zone...
Authors
Janet L. Babb, Stephen M. Wessells, Christina A. Neal
238U–230Th–226Ra–210Pb–210Po disequilibria constraints on magma generation, ascent, and degassing during the ongoing eruption of Kīlauea 238U–230Th–226Ra–210Pb–210Po disequilibria constraints on magma generation, ascent, and degassing during the ongoing eruption of Kīlauea
The timescales of magma genesis, ascent, storage and degassing at Kīlauea volcano, Hawai‘i are addressed by measuring 238U-series radionuclide abundances in lava and tephra erupted between 1982 and 2008. Most analyzed samples represent lavas erupted by steady effusion from Pu‘u ‘Ō‘ō and Kūpahianaha from 1983 to 2008. Also included are samples erupted at the summit in April 1982 and March...
Authors
Guillaume Girard, Mark K. Reagan, Kenneth W. W. Sims, Carl Thornber, Christopher L. Waters, Erin H. Phillips
2015 Volcanic activity in Alaska—Summary of events and response of the Alaska Volcano Observatory 2015 Volcanic activity in Alaska—Summary of events and response of the Alaska Volcano Observatory
The Alaska Volcano Observatory (AVO) responded to eruptions, volcanic unrest or suspected unrest, and seismic events at 14 volcanic centers in Alaska during 2015. The most notable volcanic activity consisted of continuing intermittent ash eruptions from Cleveland and Shishaldin volcanoes in the Aleutian Islands. Two eruptive episodes, at Veniaminof and Pavlof, on the Alaska Peninsula...
Authors
James P. Dixon, Cheryl E. Cameron, Alexandra M. Iezzi, Kristi L. Wallace
Semipermanent GPS (SPGPS) as a volcano monitoring tool: Rationale, method, and applications Semipermanent GPS (SPGPS) as a volcano monitoring tool: Rationale, method, and applications
Semipermanent GPS (SPGPS) is an alternative to conventional campaign or survey-mode GPS (SGPS) and to continuous GPS (CGPS) that offers several advantages for monitoring ground deformation. Unlike CGPS installations, SPGPS stations can be deployed quickly in response to changing volcanic conditions or earthquake activity such as a swarm or aftershock sequence. SPGPS networks can be more...
Authors
Daniel Dzurisin, Michael Lisowski, Charles W. Wicks
2014 volcanic activity in Alaska: Summary of events and response of the Alaska Volcano Observatory 2014 volcanic activity in Alaska: Summary of events and response of the Alaska Volcano Observatory
The Alaska Volcano Observatory (AVO) responded to eruptions, possible eruptions, volcanic unrest or suspected unrest, and seismic events at 18 volcanic centers in Alaska during 2014. The most notable volcanic activity consisted of intermittent ash eruptions from long-active Cleveland and Shishaldin Volcanoes in the Aleutian Islands, and two eruptive episodes at Pavlof Volcano on the...
Authors
Cheryl E. Cameron, James P. Dixon, Christina A. Neal, Christopher F. Waythomas, Janet R. Schaefer, Robert G. McGimsey
Plateaus and sinuous ridges as the fingerprints of lava flow inflation in the Eastern Tharsis Plains of Mars Plateaus and sinuous ridges as the fingerprints of lava flow inflation in the Eastern Tharsis Plains of Mars
The Tharsis Montes rift aprons are composed of outpourings of lava from chaotic terrains to the northeast and southwest flank of each volcano. Sinuous and branching channel networks that are present on the rift aprons suggest the possibility of fluvial processes in their development, or erosion by rapidly emplaced lavas, but the style of lava flow emplacement throughout rift apron...
Authors
Jacob E. Bleacher, Tim R. Orr, Andrew P. de Wet, James R. Zimbelman, Christopher W. Hamilton, W. Brent Garry, Larry S. Crumpler, David A. Williams