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Hydrothermal systems of the Cascade Range, north-central Oregon Hydrothermal systems of the Cascade Range, north-central Oregon

Quaternary volcanoes of the Cascade Range form a 1,200- kilometer-long arc that extends from southern British Columbia to northern California. The section of the Cascade Range volcanic arc in central Oregon is characterized by relatively high Quaternary volcanic extrusion rates and hot-spring discharge rates. Stableisotope data and measurements of hot-spring heat discharge indicate that...
Authors
S. E. Ingebritsen, Robert H. Mariner, David R. Sherrod

The role of magmas in the formation of hydrothermal ore deposits The role of magmas in the formation of hydrothermal ore deposits

Magmatic fluids, both vapour and hypersaline liquid, are a primary source of many components in hydrothermal ore deposits formed in volcanic arcs. These components, including metals and their ligands, become concentrated in magmas in various ways from various sources, including subducted oceanic crust. Leaching of rocks also contributes components to the hydrothermal fluid—a process...
Authors
Jeffrey W. Hedenquist, Jacob B. Lowenstern

The 1989-1990 eruption of Redoubt Volcano, Alaska: impacts on aircraft operations The 1989-1990 eruption of Redoubt Volcano, Alaska: impacts on aircraft operations

The December 1989–June 1990 eruption of Redoubt Volcano affected commercial and military air operations in the vicinity of Anchorage, Alaska. These effects were due to the direct impact of volcanic ash on jet aircraft, as well as to the rerouting and cancellations of flight operations owing to eruptive activity. Between December and February, five commercial jetliners were damaged from...
Authors
T. J. Casadevall

Hornblende-melt trace-element partitioning measured by ion microprobe Hornblende-melt trace-element partitioning measured by ion microprobe

Trace-element abundances were measured in situ by ion microprobe in five samples of hornblende and melt ranging from basaltic andesite to high-silica rhyolite. Except for one sample, for which quench overgrowth or disequilibrium is suspected, the abundance ratios show systematic inter-element and inter-sample variations, and probably approach true partition coefficients. Apparent...
Authors
T. W. Sisson

Correlation of gold in siliceous sinters with 3He 4He in hot spring waters of Yellowstone National Park Correlation of gold in siliceous sinters with 3He 4He in hot spring waters of Yellowstone National Park

Opaline sinter samples collected at Yellowstone National Park (YNP) were analyzed for gold by neutron activation and for other trace elements by the inductively coupled plasma optical emission spectroscopy (ICP-OES) method. No correlation was found between Au and As, Sb, or total Fe in the sinters, although the sample containing the highest Au also contains the highest Sb. There also was...
Authors
R.O. Fournier, B. M. Kennedy, M. Aoki, J. M. Thompson

Increased pressure from rising bubbles as a mechanism for remotely triggered seismicity Increased pressure from rising bubbles as a mechanism for remotely triggered seismicity

Aftershocks of large earthquakes tend to occur close to the main rupture zone, and can be used to constrain its dimensions. But following the 1992 Landers earthquake (magnitude M(w) = 7.3) in southern California, many aftershocks were reported in areas remote from the mainshock. Intriguingly, this remote seismicity occurred in small clusters near active volcanic and geothermal systems...
Authors
A. T. Linde, I. S. Sacks, M.J.S. Johnston, D.P. Hill, R.G. Bilham

Eruptive history and petrology of Mount Drum volcano, Wrangell Mountains, Alaska Eruptive history and petrology of Mount Drum volcano, Wrangell Mountains, Alaska

Mount Drum is one of the youngest volcanoes in the subduction-related Wrangell volcanic field (80x200 km) of southcentral Alaska. It lies at the northwest end of a series of large, andesite-dominated shield volcanoes that show a northwesterly progression of age from 26 Ma near the Alaska-Yukon border to about 0.2 Ma at Mount Drum. The volcano was constructed between 750 and 250 ka during...
Authors
D.H. Richter, E. J. Moll-Stalcup, T. P. Miller, M. A. Lanphere, G. B. Dalrymple, R. L. Smith

Late Quaternary normal faulting of the Hat Creek basalt, northern California Late Quaternary normal faulting of the Hat Creek basalt, northern California

The Hat Creek fault is a major, young, north-striking, normal fault along the western boundary of extensional Basin and Range deformation in the Lessen region of northeastern California. Volcanic rocks of Quaternary and late Pliocene age are displaced a total of >500 m down to the west along west-facing, en echelon scarps now retreated to ∼35° slopes. Fresh, young scarps as much as 30 m...
Authors
L.I.P. Muffler, M.A. Clynne, D.E. Champion

Chemistry of spring and well waters on Kilauea Volcano, Hawaii, and vicinity Chemistry of spring and well waters on Kilauea Volcano, Hawaii, and vicinity

Published and new data for chemical and isotopic samples from wells and springs on Kilauea Volcano and vicinity are presented. These data are used to understand processes that determine the chemistry of dilute meteoric water, mixtures with sea water, and thermal water. Data for well and spring samples of non-thermal water indicate that mixing with sea water and dissolution of rock from...
Authors
Cathy J. Janik, Manuel Nathenson, M. A. Scholl
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