Publications
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Deep magmatic structures of Hawaiian volcanoes, imaged by three-dimensional gravity models Deep magmatic structures of Hawaiian volcanoes, imaged by three-dimensional gravity models
A simplified three-dimensional model for the island of Hawai'i, based on 3300 gravity measurements, provides new insights on magma pathways within the basaltic volcanoes. Gravity anomalies define dense cumulates and intrusions beneath the summits and known rift zones of every volcano. Linear gravity anomalies project southeast from Kohala and Mauna Kea summits and south from Hualālai...
Authors
J. Kauahikaua, T. Hildenbrand, M. Webring
Magma storage and mixing conditions for the 1953-1974 eruption of Southwest Trident volcano, Katmai National Park, Alaska Magma storage and mixing conditions for the 1953-1974 eruption of Southwest Trident volcano, Katmai National Park, Alaska
Between 1953 and 1974, approximately 0.5 km3 of andesite and dacite erupted from a new vent on the southwest flank of Trident volcano in Katmai National Park, Alaska, forming an edifice now known as Southwest (or New) Trident. Field, analytical, and experimental evidence shows that the eruption commenced soon after mixing of dacite and andesite magmas at shallow crustal levels. Four lava...
Authors
Michelle L. Coombs, John C. Eichelberger, Malcom J. Rutherford
A model for the magmatic-hydrothermal system at Mount Rainier, Washington, from seismic and geochemical observations A model for the magmatic-hydrothermal system at Mount Rainier, Washington, from seismic and geochemical observations
Mount Rainier is one of the most seismically active volcanoes in the Cascade Range, with an average of one to two high-frequency volcano-tectonic (or VT) earthquakes occurring directly beneath the summit in a given month. Despite this level of seismicity, little is known about its cause. The VT earthquakes occur at a steady rate in several clusters below the inferred base of the...
Authors
S.C. Moran, D. R. Zimbelman, S. D. Malone
Late Pleistocene granodiorite beneath Crater Lake caldera, Oregon, dated by ion microprobe Late Pleistocene granodiorite beneath Crater Lake caldera, Oregon, dated by ion microprobe
Variably melted granodiorite blocks ejected during the Holocene caldera-forming eruption of Mount Mazama were plucked from the walls of the climactic magma chamber at ∼5 km depth. Ion-microprobe U-Pb dating of zircons from two unmelted granodiorite blocks with SHRIMP RG (sensitive high-resolution ion microprobe–reverse geometry) gives a nominal 238U/206Pb age of100+78−80100−80+78 ka...
Authors
C. R. Bacon, H.M. Persing, J. L. Wooden, T. R. Ireland
Carbon cycling in boreal wetlands: A comparison of three approaches Carbon cycling in boreal wetlands: A comparison of three approaches
Three independent methods were used to measure net ecosystem production (NEP) in four wetlands near Thompson, Manitoba, Canada. The first method calculated NEP by subtracting heterotrophic respiration from net primary productivity, using both measurements and estimates derived from the literature. The second method used radiocarbon data from cores to derive long-term NEP averaged over...
Authors
Susan E. Trumbore, Jill Bubier, Jennifer W. Harden, Patrick M. Crill
Gas and Isotope Geochemistry of 81 Steam Samples from Wells in The Geysers Geothermal Field, Sonoma and Lake Counties, California Gas and Isotope Geochemistry of 81 Steam Samples from Wells in The Geysers Geothermal Field, Sonoma and Lake Counties, California
The Geysers geothermal field in northern California, with about 2000-MW electrical capacity, is the largest geothermal field in the world. Despite its importance as a resource and as an example of a vapor-dominated reservoir, very few complete geochemical analyses of the steam have been published (Allen and Day, 1927; Truesdell and others, 1987). This report presents data from 90 steam...
Authors
Jacob B. Lowenstern, Cathy J. Janik, Lynne Fahlquist, Linda S. Johnson
Gas-driven filter pressing in magmas Gas-driven filter pressing in magmas
Most silicic and some mafic magmas expand via second boiling if they crystallize at depths of about 10 km or less. The buildup of gas pressure due to second boiling can be relieved by expulsion of melt out of the region of crystallization, and this process of gas-driven filter pressing assists the crystallization differentiation of magmas. For gas-driven filter pressing to be effective...
Authors
Thomas W. Sisson, Charles R. Bacon
Late Quaternary slip rate and seismic hazards of the West Klamath Lake fault zone near Crater Lake, Oregon Cascades Late Quaternary slip rate and seismic hazards of the West Klamath Lake fault zone near Crater Lake, Oregon Cascades
Crater Lake caldera is at the north end of the Klamath graben, where this N10°W-trending major Basin and Range structure impinges upon the north-south–trending High Cascades volcanic arc. East-facing normal faults, typically 10–15 km long, form the West Klamath Lake fault zone, which bounds the graben on its west side. The fault zone terminates on the south near the epicentral area of...
Authors
C. R. Bacon, M. A. Lanphere, D.E. Champion
Proceedings of the Workshop on Present and Future Directions in Volcano-Hazard Assessment; Menlo Park, California, September 23-24, 1998 Proceedings of the Workshop on Present and Future Directions in Volcano-Hazard Assessment; Menlo Park, California, September 23-24, 1998
No abstract available.
Authors
C. R. Bacon, Thomas C. Hanks, W. E. Scott
Magma migration and resupply during the 1974 summit eruptions of Kilauea Volcano, Hawaii Magma migration and resupply during the 1974 summit eruptions of Kilauea Volcano, Hawaii
The purpose of this paper is to present a complete account of contrasting yet related eruptions, thus filling a gap in the published narratives of recent activity of Kilauea; and to examine their significance within a broader context of regional magmatic and eruptive dynamics. We have gained a historical perspective and can view these three eruptions within a multidecade context of the...
Authors
John P. Lockwood, Robert I. Tilling, Robin T. Holcomb, Fred W. Klein, Arnold T. Okamura, Donald W. Peterson
Volcano hazards in the Mount Jefferson region, Oregon Volcano hazards in the Mount Jefferson region, Oregon
Mount Jefferson is a prominent feature of the landscape seen from highways east and west of the Cascades. Mount Jefferson (one of thirteen major volcanic centers in the Cascade Range) has erupted repeatedly for hundreds of thousands of years, with its last eruptive episode during the last major glaciation which culminated about 15,000 years ago. Geologic evidence shows that Mount...
Authors
Joseph S. Walder, Cynthia A. Gardner, Richard M. Conrey, Bruce J. Fisher, Steven P. Schilling
The Puelche volcanic field: Extensive Pleistocene rhyolite lava flows in the Andes of central Chile The Puelche volcanic field: Extensive Pleistocene rhyolite lava flows in the Andes of central Chile
A remote volcanic field in the rugged headwaters of the Río Puelche and Río Invernada (35.8°S) constitutes the largest cluster of Quaternary rhyolite lava flows yet identified in the Andean Southern Volcanic Zone. The Puelche Volcanic Field belongs to an intra-arc belt of silicic magmatic centers that extends, at least, 140 km north-south and lies well east of the volcanic front but...
Authors
Wes Hildreth, J. Fierstein, E. Godoy, Robert E. Drake, B. Singer