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Rhyolite themobarometry and the shallowing of the magma reservoir, Coso volcanic field, California Rhyolite themobarometry and the shallowing of the magma reservoir, Coso volcanic field, California

The compositionally bimodal Pleistocene Coso volcanic field is located at the western margin of the Basin and Range province ∼60 km north of the Garlock fault. Thirty-nine nearly aphyric high-silica rhyolite domes were emplaced in the past million years: one at 1 Ma from a transient magma reservoir, one at ∼0·6 Ma, and the rest since ∼0·3 Ma. Over the past 0·6 My, the depth from which...
Authors
C.R. Manley, Charles R. Bacon

Preliminary volcano-hazard assessment for Aniakchak Volcano, Alaska Preliminary volcano-hazard assessment for Aniakchak Volcano, Alaska

Aniakchak is an active volcano located on the Alaska Peninsula 670 kilometers southwest of Anchorage. The volcano consists of a dramatic, 10-kilometer-diameter, 0.5 to 1.0-kilometer-deep caldera that formed during a catastrophic eruption 3,500 years ago. Since then, at least a dozen separate vents within the caldera have erupted, often explosively, to produce lava flows and widespread...
Authors
Christina A. Neal, Robert G. McGimsey, Thomas P. Miller, James R. Riehle, Christopher F. Waythomas

A numerical program for steady-state flow of magma-gas mixtures through vertical eruptive conduits A numerical program for steady-state flow of magma-gas mixtures through vertical eruptive conduits

This report presents a model that calculates flow properties (pressure, vesicularity, and some 35 other parameters) as a function of vertical position within a volcanic conduit during a steady-state eruption. The model idealizes the magma-gas mixture as a single homogeneousfluid and calculates gas exsolution under the assumption of equilibrium conditions. These are the same assumptions...
Authors
Larry G. Mastin, Mark S. Ghiorso

Preliminary volcano-hazard assessment for the Katmai volcanic cluster, Alaska Preliminary volcano-hazard assessment for the Katmai volcanic cluster, Alaska

The world’s largest volcanic eruption of the 20th century broke out at Novarupta (fig. 1) in June 1912, filling with hot ash what came to be called the Valley of Ten Thousand Smokes and spreading downwind more fallout than all other historical Alaskan eruptions combined. Although almost all the magma vented at Novarupta, most of it had been stored beneath Mount Katmai 10 km away, which...
Authors
Judy Fierstein, Wes Hildreth

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
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