Publications
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Non-perturbational surface-wave inversion: A Dix-type relation for surface waves Non-perturbational surface-wave inversion: A Dix-type relation for surface waves
We extend the approach underlying the well-known Dix equation in reflection seismology to surface waves. Within the context of surface wave inversion, the Dix-type relation we derive for surface waves allows accurate depth profiles of shear-wave velocity to be constructed directly from phase velocity data, in contrast to perturbational methods. The depth profiles can subsequently be used...
Authors
Matthew M. Haney, Victor C. Tsai
Lahars at Cotopaxi and Tungurahua Volcanoes, Ecuador: Highlights from stratigraphy and observational records and related downstream hazards Lahars at Cotopaxi and Tungurahua Volcanoes, Ecuador: Highlights from stratigraphy and observational records and related downstream hazards
Lahars are volcanic debris flows that are dubbed primary when triggered by eruptive activity or secondary when triggered by other factors such as heavy rainfall after eruptive activity has waned. Variation in time and space of the proportion of sediment to water within a lahar dictates lahar flow phase and the resultant sedimentary character of deposits. Characteristics of source...
Authors
Patricia A Mothes, James W. Vallance
Episodic deflation-inflation events at Kīlauea Volcano and implications for the shallow magma system Episodic deflation-inflation events at Kīlauea Volcano and implications for the shallow magma system
Episodic variations in magma pressures and flow rates at Kīlauea Volcano, defined by a characteristic temporal evolution and termed deflation-inflation (DI) events, have been observed since at least the 1990s. DI events consist of transient, days-long deflations and subsequent reinflations of the summit region, accompanied since 2008 by fluctuations in the surface height of Kīlauea's...
Authors
Kyle R. Anderson, Michael P. Poland, Jessica H. Johnson, Asta Miklius
Ice-clad volcanoes Ice-clad volcanoes
An icy volcano even if called extinct or dormant may be active at depth. Magma creeps up, crystallizes, releases gas. After decades or millennia the pressure from magmatic gas exceeds the resistance of overlying rock and the volcano erupts. Repeated eruptions build a cone that pokes one or two kilometers or more above its surroundings - a point of cool climate supporting glaciers. Ice...
Authors
Richard B. Waitt, B.R. Edwards, Andrew G. Fountain
Reticulite‐producing fountains from ring fractures in Kīlauea Caldera ca. 1500 CE Reticulite‐producing fountains from ring fractures in Kīlauea Caldera ca. 1500 CE
A widely dispersed reticulite bed occurs close to the base of the Keanakākoʻi Tephra at Kīlauea Volcano. It can be divided into six subunits in the northern sector of the volcano; the reticulite also occurs in the southern sector, but outcrops are sparse owing to penecontemporaneous erosion and burial. Multilobate isopachs for each subunit and the total deposit suggest that multiple...
Authors
Michael May, Rebecca J. Carey, Don Swanson, Bruce F. Houghton
Using SO2 camera imagery and seismicity to examine degassing and gas accumulation at Kīlauea Volcano, May 2010 Using SO2 camera imagery and seismicity to examine degassing and gas accumulation at Kīlauea Volcano, May 2010
SO2 camera measurements at Kīlauea Volcano, Hawaii, in May of 2010 captured two occurrences of lava lake rise and fall within the Halema'um'au Crater summit vent. During high lava stands we observed diminished SO2 emission rates and decreased seismic tremor. Similar events at Kīlauea have been described as the result of sporadic degassing following gas accumulation beneath a mostly...
Authors
Patricia A Nadeau, Cynthia A. Werner, Gregory P. Waite, Simon A Carn, Ian D Brewer, Tamar Elias, Andrew Sutton, Christoph Kern
An ignimbrite caldera from the bottom up: Exhumed floor and fill of the resurgent Bonanza caldera, Southern Rocky Mountain volcanic field, Colorado An ignimbrite caldera from the bottom up: Exhumed floor and fill of the resurgent Bonanza caldera, Southern Rocky Mountain volcanic field, Colorado
Among large ignimbrites, the Bonanza Tuff and its source caldera in the Southern Rocky Mountain volcanic field display diverse depositional and structural features that provide special insights concerning eruptive processes and caldera development. In contrast to the nested loci for successive ignimbrite eruptions at many large multicyclic calderas elsewhere, Bonanza caldera is an...
Authors
Peter W. Lipman, Matthew J. Zimmerer, William C. McIntosh
The 2008 phreatomagmatic eruption of Okmok volcano, Aleutian Islands, Alaska: Chronology, deposits, and landform changes The 2008 phreatomagmatic eruption of Okmok volcano, Aleutian Islands, Alaska: Chronology, deposits, and landform changes
Okmok volcano, Aleutian Islands, Alaska, explosively erupted over a five-week period between July 12 and August 23, 2008. The eruption was predominantly phreatomagmatic, producing fine-grained tephra that covered most of northeastern Umnak Island. The eruption had a maximum Volcanic Explosivity Index (VEI) of 4, with eruption column heights up to 16 km during the opening phase. Several...
Authors
Jessica Larsen, Christina A. Neal, Janet R. Schaefer, Max Kaufman, Zhong Lu
The Yellowstone “hot spot” track results from migrating basin-range extension The Yellowstone “hot spot” track results from migrating basin-range extension
Whether the volcanism of the Columbia River Plateau, eastern Snake River Plain, and Yellowstone (western U.S.) is related to a mantle plume or to plate tectonic processes is a long-standing controversy. There are many geological mismatches with the basic plume model as well as logical flaws, such as citing data postulated to require a deep-mantle origin in support of an “upper-mantle...
Authors
Gillian R. Foulger, Robert L. Christiansen, Don L. Anderson
Chronology and ecology of late Pleistocene megafauna in the northern Willamette Valley, Oregon Chronology and ecology of late Pleistocene megafauna in the northern Willamette Valley, Oregon
Since the mid-19th century, western Oregon's Willamette Valley has been a source of remains from a wide variety of extinct megafauna. Few of these have been previously described or dated, but new chronologic and isotopic analyses in conjunction with updated evaluations of stratigraphic context provide substantial new information on the species present, timing of losses, and...
Authors
Daniel M. Gilmour, Virginia L. Butler, James E. O'Connor, Edward Byrd Davis, Brendan J. Culleton, Douglas J. Kennett, Gregory W. L. Hodgins
A sinuous tumulus over an active lava tube at Kīlauea Volcano: evolution, analogs, and hazard forecasts A sinuous tumulus over an active lava tube at Kīlauea Volcano: evolution, analogs, and hazard forecasts
Inflation of narrow tube-fed basaltic lava flows (tens of meters across), such as those confined by topography, can be focused predominantly along the roof of a lava tube. This can lead to the development of an unusually long tumulus, its shape matching the sinuosity of the underlying lava tube. Such a situation occurred during Kīlauea Volcano's (Hawai'i, USA) ongoing East Rift Zone...
Authors
Tim R. Orr, Jacob E. Bleacher, Matthew R. Patrick, Kelly M. Wooten
Database compilation for the geologic map of the San Francisco volcanic field, north-central Arizona Database compilation for the geologic map of the San Francisco volcanic field, north-central Arizona
The main component of this publication is a geologic map database prepared using geographic information system (GIS) applications. The geodatabase of geologic points, lines, and polygons was produced as a compilation from five adjoining map sections originally published as printed maps in 1987 (see references in metadata). Four of the sections (U.S. Geological Survey Miscellaneous Field...
Authors
Joseph A. Bard, David W. Ramsey, Edward W. Wolfe, George E. Ulrich, Christopher G. Newhall, Richard B. Moore, Norman G. Bailey, Richard F. Holm