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Preliminary Volcano-Hazard Assessment for Redoubt Volcano, Alaska Preliminary Volcano-Hazard Assessment for Redoubt Volcano, Alaska

Redoubt Volcano is a stratovolcano located within a few hundred kilometers of more than half of the population of Alaska. This volcano has erupted explosively at least six times since historical observations began in 1778. The most recent eruption occurred in 1989-90 and similar eruptions can be expected in the future. The early part of the 1989-90 eruption was characterized by explosive...
Authors
Christopher F. Waythomas, Joseph M. Dorava, Thomas P. Miller, Christina A. Neal, Robert G. McGimsey

Living with a restless caldera: Long Valley, California Living with a restless caldera: Long Valley, California

No abstract available.
Authors
David P. Hill, Roy A. Bailey, Michael L. Sorey, James W. Hendley, Peter H. Stauffer

Magmatic processes that generated the rhyolite of Glass Mountain, Medicine Lake volcano, N. California Magmatic processes that generated the rhyolite of Glass Mountain, Medicine Lake volcano, N. California

Glass Mountain consists of a 1 km3, compositionally zoned rhyolite to dacite glass flow containing magmatic inclusions and xenoliths of underlying shallow crust. Mixing of magmas produced by fractional crystallization of andesite and crustal melting generated the rhyolite of Glass Mountain. Melting experiments were carried out on basaltic andesite and andesite magmatic inclusions at 100...
Authors
Timothy L. Grove, Julie Donnelly-Nolan, T. Housh

Lahars of Mount Pinatubo, Philippines Lahars of Mount Pinatubo, Philippines

On June 15, 1991, Mount Pinatubo in the Philippines exploded in the second largest volcanic eruption on Earth this century. This eruption deposited more than 1 cubic mile (5 cubic kilometers) of volcanic ash and rock fragments on the volcano's slopes. Within hours, heavy rains began to wash this material down into the surrounding lowlands in giant, fast-moving mudflows called lahars. In...
Authors
Christopher G. Newhall, Peter H. Stauffer, James W. Hendley

Depositional processes in large-scale debris-flow experiments Depositional processes in large-scale debris-flow experiments

This study examines the depositional process and characteristics of deposits of large‐scale experimental debris flows (to 15 m3) composed of mixtures of gravel (to 32 mm), sand, and mud. The experiments were performed using a 95‐m‐long, 2‐m‐wide debris‐flow flume that slopes 31°. Following release, experimental debris flows invariably developed numerous shallow (∼ 10 cm deep) surges...
Authors
J. J. Major

Imaging the crustal magma sources beneath Mauna Loa and Kilauea volcanoes, Hawaii Imaging the crustal magma sources beneath Mauna Loa and Kilauea volcanoes, Hawaii

Three-dimensional seismic P-wave traveltime tomography is used to image the magma sources beneath Mauna Loa and Kilauea volcanoes, Hawaii. High-velocity bodies (>6.4 km/s) in the upper 9 km of the crust beneath the summits and rift zones of the volcanoes correlate with zones of high magnetic intensities and are interpreted as solidified gabbro-ultramafic cumulates from which the surface...
Authors
Paul G. Okubo, Harley M. Benz, Bernard A. Chouet

Volcanic ash - danger to aircraft in the north Pacific Volcanic ash - danger to aircraft in the north Pacific

The world's busy air traffic corridors pass over hundreds of volcanoes capable of sudden, explosive eruptions. In the United States alone, aircraft carry many thousands of passengers and millions of dollars of cargo over volcanoes each day. Volcanic ash can be a serious hazard to aviation even thousands of miles from an eruption. Airborne ash can diminish visibility, damage flight...
Authors
Christina A. Neal, Thomas J. Casadevall, Thomas P. Miller, James W. Hendley, Peter H. Stauffer

The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines

The second-largest volcanic eruption of this century, and by far the largest eruption to affect a densely populated area, occurred at Mount Pinatubo in the Philippines on June 15, 1991. The eruption produced high-speed avalanches of hot ash and gas, giant mudflows, and a cloud of volcanic ash hundreds of miles across. The impacts of the eruption continue to this day.
Authors
Christopher G. Newhall, James W. Hendley, Peter H. Stauffer

Volcano and earthquake hazards in the Crater Lake region, Oregon Volcano and earthquake hazards in the Crater Lake region, Oregon

Crater Lake lies in a basin, or caldera, formed by collapse of the Cascade volcano known as Mount Mazama during a violent, climactic eruption about 7,700 years ago. This event dramatically changed the character of the volcano so that many potential types of future events have no precedent there. This potentially active volcanic center is contained within Crater Lake National Park...
Authors
Charles R. Bacon, Larry G. Mastin, Kevin M. Scott, Manuel Nathenson

Comparative ultrastructure of two closely related thalassiosira species: Thalassiosira vulnifica (gombos) fenner and T. fasciculata Harwood et Maruyama Comparative ultrastructure of two closely related thalassiosira species: Thalassiosira vulnifica (gombos) fenner and T. fasciculata Harwood et Maruyama

The distinctive morphology and relatively short geological range (3.25 to 2.5 Ma) of Thalassiosira vulniflca (Gombos) Fenner make it especially useful for Pliocene biostratigraphic studies in the Antarctic region. Thalassiosira fasciculata Harwood et Maruyama has a geological range (4.5 to 0.75 Ma) that overlaps that of T. vulnifica and it resembles this taxon in possessing prominent...
Authors
Albert D. Mahood, John A. Barron

Characteristics of debris flows of noneruptive origin on Mount Shasta, northern California Characteristics of debris flows of noneruptive origin on Mount Shasta, northern California

Studies of Mount Shasta indicate that eruptive activity has occurred, on the average, once every 800 years. Debris flows and deposits of non- eruptive origin, in addition to those associated with eruptive activity (lava flows, pyroclastic flows, and ash fall), inundate the fans and channels and can endanger people or property on the flanks of the mountain. This study evaluates the source...
Authors
James C. Blodgett, Karen R. Poeschel, Waite R. Osterkamp

A preliminary survey of the broadband seismic wavefield at Puu Oo, the active vent of Kilauea volcano, Hawaii A preliminary survey of the broadband seismic wavefield at Puu Oo, the active vent of Kilauea volcano, Hawaii

The seismic wavefield near an active volcanic vent consists of superimposed signals in a wide range of frequency bands from sources inside and outside the volcano. To characterize the broadband wavefield near Puu Oo, we deployed a profile of three three-component broadband sensors in a 200 m long line about 1.5 km WSW of the active vent. During this period, Puu Oo maintained a constant...
Authors
D. Seidl, M. Hellweg, P. Okubo, H. Rademacher
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