Publications
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Volcano seismology, hazards assessment Volcano seismology, hazards assessment
The last few years have seen several impressive examples of seismic monitoring at volcanoes to provide warnings that have saved lives and property. Changes in the rates and character of volcanic earthquakes provided precursory signs to explosive eruptions of moderate size at Redoubt volcano (Alaska), Mount Unzen (Japan), Mount Spurr (Alaska), and Rabaul caldera (Papua New Guinea), as...
Authors
J. Mori
Thermodynamics of gas and steam-blast eruptions Thermodynamics of gas and steam-blast eruptions
Eruptions of gas or steam and non-juvenile debris are common in volcanic and hydrothermal areas. From reports of non-juvenile eruptions or eruptive sequences world-wide, at least three types (or end-members) can be identified: (1) those involving rock and liquid water initially at boiling-point temperatures (‘boiling-point eruptions’); (2) those powered by gas (primarily water vapor) at...
Authors
L.G. Mastin
Episode 49 of the Pu'u 'Ō'ō-Kūpaianaha eruption of Kilauea volcano-breakdown of a steady-state eruptive era Episode 49 of the Pu'u 'Ō'ō-Kūpaianaha eruption of Kilauea volcano-breakdown of a steady-state eruptive era
The Pu'u 'O'o-Kupaianaha eruption (1983-present) is the longest lived rift eruption of either Kilauea or neighboring Mauna Loa in recorded history. The initial fissure opening in January 1983 was followed by three years of episodic fire fountaining at the Pu'u 'O'o vent on Kilauea's east rift zone ∼19km from the summit (episodes 4–47). These spectacular events gave way in July 1986 to...
Authors
M. T. Mangan, C. C. Heliker, T. N. Mattox, J. P. Kauahikaua, Rosalind Tuthill Helz
Giant blocks in the South Kona landslide, Hawaii Giant blocks in the South Kona landslide, Hawaii
A large field of blocky sea-floor hills, up to 10 km long and 500 m high, are gigantic slide blocks derived from the west flank of Mauna Loa volcano on the island of Hawaii. These megablocks are embedded in the toe of the South Kona landslide, which extends ∼80 km seaward from the present coastline to depths of nearly 5 km. A 10–15-km-wide belt of numerous, smaller, 1–3-km-long slide...
Authors
J.G. Moore, W.B. Bryan, M.H. Beeson, W. R. Normark
Forest-killing diffuse CO2 emission at Mammoth Mountain as a sign of magmatic unrest Forest-killing diffuse CO2 emission at Mammoth Mountain as a sign of magmatic unrest
Mammoth Mountain, in the western United States, is a large dacitic volcano with a long history of volcanism that began 200 kyr ago and produced phreatic eruptions as recently as 500 ± 200 yr BP. Seismicity, ground deformation and changes in fumarole gas composition suggested an episode of shallow dyke intrusion in 1989–90. Areas of dying forest and incidents of near asphyxia in confined...
Authors
C. D. Farrar, M.L. Sorey, William C. Evans, J. F. Howle, B.D. Kerr, B. M. Kennedy, C.-Y. King, J. R. Southon
Is Glacier Peak a dangerous volcano? Is Glacier Peak a dangerous volcano?
No abstract available
Authors
L.G. Mastin, R. B. Waitt
Bench mark descriptions and photographs for global positioning system (GPS) stations in the vicinity of Mt. Shasta and Medicine Lake, California Bench mark descriptions and photographs for global positioning system (GPS) stations in the vicinity of Mt. Shasta and Medicine Lake, California
No abstract available.
Authors
K.M. Yamashita, D.E. Wieprecht
Volcano hazards from Mount Rainier, Washington Volcano hazards from Mount Rainier, Washington
Mount Rainier—at 4393 meters (14,410 feet) the highest peak in the Cascade Range—is a dormant volcano whose load of glacier ice exceeds that of any other mountain in the conterminous United States. This tremendous mass of rock and ice, in combination with great topographic relief, poses a variety of geologic hazards, both during inevitable future eruptions and during the intervening...
Authors
R. Hoblitt, J. S. Walder, C. L. Driedger, K. M. Scott, P. T. Pringle, J.W. Vallance
Radiocarbon ages of pre-bomb clams and the hard-water effect in Lakes Michigan and Huron Radiocarbon ages of pre-bomb clams and the hard-water effect in Lakes Michigan and Huron
Five radiocarbon ages, all determined by accelerator mass spectrometry, have been obtained for two pre-bomb bivalves from Lake Michigan and one from Lake Huron. After correcting those ages for the fractionation of14C in calcite and for the radioactively inert CO2 in the atmosphere, we find residual ages, caused by the hard water effect, of about 250 years for Lake Michigan and 440 years...
Authors
David K. Rea, Steven M. Colman
Geological mapping of biological habitats on Georges Bank and Stellwaen Bank, Gulf of Maine region Geological mapping of biological habitats on Georges Bank and Stellwaen Bank, Gulf of Maine region
No abstract available.
Authors
Page C. Valentine, Eric A. Schmuck
Velocities of southern Basin and Range xenoliths: Insights on the nature of lower crustal reflectivity and composition Velocities of southern Basin and Range xenoliths: Insights on the nature of lower crustal reflectivity and composition
To reconcile differences between the assessments of crustal composition in the southern Basin and Range province on the basis of seismic refraction and reflection data and lower-crustal xenoliths, we measured velocities of xenoliths from the Cima volcanic field in southern California. Lower-crustal samples studied included gabbro, microgabbro, and pyroxenite. We find that the mafic...
Authors
Thomas E. Parsons, Nikolas I. Christensen, Howard G. Wilshire