Skip to main content
U.S. flag

An official website of the United States government

Publications

Filter Total Items: 3085

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

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

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

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

Tsunami generation by pyroclastic flow during the 3500-year B.P. caldera-forming eruption of Aniakchak Volcano, Alaska Tsunami generation by pyroclastic flow during the 3500-year B.P. caldera-forming eruption of Aniakchak Volcano, Alaska

A discontinuous pumiceous sand, a few centimeters to tens of centimeters thick, is located up to 15 m above mean high tide within Holocene peat along the northern Bristol Bay coastline of Alaska. The bed consists of fine-to-coarse, poorly to moderately well-sorted, pumice-bearing sand near the top of a 2-m-thick peat sequence. The sand bed contains rip-up clasts of peat and tephra and is...
Authors
Christopher F. Waythomas, Christina A. Neal

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
Was this page helpful?