Publications
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Magma mixing and high fountaining during the 1959 Kīlauea Iki eruption, Hawai‘i Magma mixing and high fountaining during the 1959 Kīlauea Iki eruption, Hawai‘i
The 1959 Kīlauea Iki eruption provides a unique opportunity to investigate the process of shallow magma mixing, its impact on the magmatic volatile budget and its role in triggering and driving episodes of Hawaiian fountaining. Melt inclusions hosted by olivine record a continuous decrease in H2O concentration through the 17 episodes of the eruption, while CO2 concentrations correlate...
Authors
I. Sides, M. Edmonds, J. Maclennan, Bruce F. Houghton, Don Swanson, M.J. Steele-MacInnis
Multi-scale observations of the variability of magmatic CO2 emissions, Mammoth Mountain, CA, USA Multi-scale observations of the variability of magmatic CO2 emissions, Mammoth Mountain, CA, USA
One of the primary indicators of volcanic unrest at Mammoth Mountain is diffuse emission of magmatic CO2, which can effectively track this unrest if its variability in space and time and relationship to near-surface meteorological and hydrologic phenomena versus those occurring at depth beneath the mountain are understood. In June–October 2013, we conducted accumulation chamber soil CO2...
Authors
Jennifer L. Lewicki, George E. Hilley
Holocene sea surface temperature and sea ice extent in the Okhotsk and Bering Seas Holocene sea surface temperature and sea ice extent in the Okhotsk and Bering Seas
Accurate prediction of future climate requires an understanding of the mechanisms of the Holocene climate; however, the driving forces, mechanisms, and processes of climate change in the Holocene associated with different time scales remain unclear. We investigated the drivers of Holocene sea surface temperature (SST) and sea ice extent in the North Pacific Ocean, and the Okhotsk and...
Authors
Naomi Harada, Kota Katsuki, Mitsuhiro Nakagawa, Akiko Matsumoto, Osamu Seki, Jason A. Addison, Bruce P. Finney, Miyako Sato
What caused terrestrial dust loading and climate downturns between A.D. 533 and 540? What caused terrestrial dust loading and climate downturns between A.D. 533 and 540?
Sn-rich particles, Ni-rich particles, and cosmic spherules are found together at four discrete stratigraphic levels within the 362-360 m depth interval of the Greenland Ice Sheet Project 2 (GISP2) ice core (72.6°N, 38.5°W, elevation: 3203 m). Using a previously derived calendar-year time scale, these particles span a time of increased dust loading of Earth's atmosphere between A.D. 533...
Authors
Dallas H. Abbott, Dee Breger, Pierre E. Biscaye, John A. Barron, Robert A. Juhl, Patrick McCafferty
Interagency collaboration on an active volcano: A case study at Hawai‘i Volcanoes National Park Interagency collaboration on an active volcano: A case study at Hawai‘i Volcanoes National Park
Hawai‘i Volcanoes National Park (HAVO) includes two active Hawai‘i shield volcanoes – Mauna Loa, the largest active volcano on earth that most recently erupted for three weeks in 1984, and Kīlauea, which has been erupting continuously for more than 31 years. Unlike the steep-sided volcanoes around the rim of the Pacific Ocean, all Hawaiian volcanoes have gentle-sloped flanks that result...
Authors
James P. Kauahikaua, Cindy Orlando
Time-averaged discharge rate of subaerial lava at Kīlauea Volcano, Hawai‘i, measured from TanDEM-X interferometry: Implications for magma supply and storage during 2011-2013 Time-averaged discharge rate of subaerial lava at Kīlauea Volcano, Hawai‘i, measured from TanDEM-X interferometry: Implications for magma supply and storage during 2011-2013
Differencing digital elevation models (DEMs) derived from TerraSAR add-on for Digital Elevation Measurements (TanDEM-X) synthetic aperture radar imagery provides a measurement of elevation change over time. On the East Rift Zone (EZR) of Kīlauea Volcano, Hawai‘i, the effusion of lava causes changes in topography. When these elevation changes are summed over the area of an active lava...
Authors
Michael P. Poland
A depth-averaged debris-flow model that includes the effects of evolving dilatancy. I. Physical basis A depth-averaged debris-flow model that includes the effects of evolving dilatancy. I. Physical basis
To simulate debris-flow behaviour from initiation to deposition, we derive a depth-averaged, two-phase model that combines concepts of critical-state soil mechanics, grain-flow mechanics and fluid mechanics. The model's balance equations describe coupled evolution of the solid volume fraction, m, basal pore-fluid pressure, flow thickness and two components of flow velocity. Basal...
Authors
Richard M. Iverson, David L. George
The geology and geochemistry of Isla Floreana, Galápagos: A different type of late-stage ocean island volcanism The geology and geochemistry of Isla Floreana, Galápagos: A different type of late-stage ocean island volcanism
Isla Floreana, the southernmost volcano in the Galápagos Archipelago, has erupted a diverse suite of alkaline basalts continually since 1.5 Ma. Because these basalts have different compositions than xenoliths and older lavas from the deep submarine sector of the volcano, Floreana is interpreted as being in a rejuvenescent or late-stage phase of volcanism. Most lavas contain xenoliths, or...
Authors
Karen S. Harpp, Dennis J. Geist, Alison M. Koleszar, Branden Christensen, John J. Lyons, Melissa Sabga, Nathan Rollins
Contrasting volcanism in Hawaiʻi and the Galápagos Contrasting volcanism in Hawaiʻi and the Galápagos
The archipelagos of Hawai‘i and the Galápagos originated at mantle hotspots, yet the volcanoes that make up the island chains differ in most respects. Some of the most important differences include the dynamics of magma supply, characteristics of magma storage and transport, morphology, and compositional and structural evolution. Of particular significance in the Galápagos is the lack of...
Authors
Michael P. Poland, Karen S. Harpp, Eric Mittelstaedt, Noemi d’Ozouville, David W. Graham
Sulfur isotope fractionation between fluid and andesitic melt: An experimental study Sulfur isotope fractionation between fluid and andesitic melt: An experimental study
Glasses produced from decompression experiments conducted by Fiege et al. (2014a) were used to investigate the fractionation of sulfur isotopes between fluid and andesitic melt upon magma degassing. Starting materials were synthetic glasses with a composition close to a Krakatau dacitic andesite. The glasses contained 4.55–7.95 wt% H2O, ∼140 to 2700 ppm sulfur (S), and 0–1000 ppm...
Authors
Adrian Fiege, Francois Holtz, Nobumichi Shimizu, Charlie Mandeville, Harald Behrens, Jaayke L. Knipping
Hydrothermal monitoring in a quiescent volcanic arc: Cascade Range, northwestern United States Hydrothermal monitoring in a quiescent volcanic arc: Cascade Range, northwestern United States
Ongoing (1996–present) volcanic unrest near South Sister, Oregon, is accompanied by a striking set of hydrothermal anomalies, including elevated temperatures, elevated major ion concentrations, and 3He/4He ratios as large as 8.6 RA in slightly thermal springs. These observations prompted the US Geological Survey to begin a systematic hydrothermal-monitoring effort encompassing 25 sites...
Authors
Steven E. Ingebritsen, N. G. Randolph-Flagg, Katrina D. Gelwick, Elizabeth A. Lundstrom, Ilana M. Crankshaw, Anna M. Murveit, M.E. Schmidt, Deborah Bergfeld, Kurt R. Spicer, David S. Tucker, Robert H. Mariner, William C. Evans
Publications of the Volcano Hazards Program 2012 Publications of the Volcano Hazards Program 2012
The Volcano Hazards Program of the U.S. Geological Survey (USGS) is part of the Geologic Hazards Assessments subactivity, as funded by Congressional appropriation. Investigations are carried out by the USGS and with cooperators at the Alaska Division of Geological and Geophysical Surveys, University of Alaska Fairbanks Geophysical Institute, University of Hawaii Manoa and Hilo...
Authors
Manuel Nathenson