Publications
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Origin, extent, and thickness of quaternary geologic units in the Willamette Valley, Oregon Origin, extent, and thickness of quaternary geologic units in the Willamette Valley, Oregon
Stratigraphic and chronologic information collected for Quaternary deposits in the Willamette Valley, Oregon, provides a revised stratigraphic framework that serves as a basis for a 1:250,000-scale map, as well as for thickness estimates of widespread Quaternary geologic units. We have mapped 11 separate Quaternary units that are differentiated on the basis of stratigraphic, topographic...
Authors
Jim E. O'Connor, Andrei M. Sarna-Wojcicki, Karl C. Wozniak, Danial J. Polette, Robert J. Fleck
The Quaternary and Pliocene Yellowstone Plateau volcanic field of Wyoming, Idaho, and Montana The Quaternary and Pliocene Yellowstone Plateau volcanic field of Wyoming, Idaho, and Montana
This region of Yellowstone National Park has been the active focus of one of the Earth's largest magmatic systems for more than 2 million years. The resulting volcanism has been characterized by the eruption of voluminous rhyolites and subordinate basalts but virtually no lavas of intermediate composition. The magmatic system at depth remains active and drives the massive hydrothermal...
Authors
Robert L. Christiansen
Volcano hazards in the Three Sisters region, Oregon Volcano hazards in the Three Sisters region, Oregon
Three Sisters is one of three potentially active volcanic centers that lie close to rapidly growing communities and resort areas in Central Oregon. Two types of volcanoes exist in the Three Sisters region and each poses distinct hazards to people and property. South Sister, Middle Sister, and Broken Top, major composite volcanoes clustered near the center of the region, have erupted...
Authors
William E. Scott, R.M. Iverson, S. P. Schilling, B.J. Fisher
Bathymetry and selected perspective views of Crater Lake, Oregon Bathymetry and selected perspective views of Crater Lake, Oregon
No abstract available
Authors
J.V. Gardner, Peter Dartnell, Laurent Hellequin, C. R. Bacon, L. A. Mayer, M.W. Buktenica
Geologic studies in Alaska by the U.S. Geological Survey, 1999 Geologic studies in Alaska by the U.S. Geological Survey, 1999
The collection of nine papers that follow continue the series of U.S. Geological Survey (USGS) investigative reports in Alaska under the broad umbrella of the geologic sciences. The series presents new and sometimes preliminary findings that are of interest to earth scientists in academia, government, and industry; to land and resource managers; and to the general public. Reports...
Progress made in understanding Mount Rainier's hazards Progress made in understanding Mount Rainier's hazards
At 4392 m high, glacier-clad Mount Rainier dominates the skyline of the southern Puget Sound region and is the centerpiece of Mount Rainier National Park. About 2.5 million people of the greater Seattle-Tacoma metropolitan area can see Mount Rainier on clear days, and 150,000 live in areas swept by lahars and floods that emanated from the volcano during the last 6,000 years (Figure 1)...
Authors
T. W. Sisson, J.W. Vallance, P. T. Pringle
Distributed shear of subglacial till due to Coulomb slip Distributed shear of subglacial till due to Coulomb slip
In most models of the flow of glaciers on till beds, it has been assumed that till behaves as a viscoplastic fluid, despite contradictory evidence from laboratory studies. In accord with this assumption, displacement profiles measured in subglacial till have been fitted with viscoplastic models by estimating the stress distribution. Here we present a model that illustrates how observed
Authors
Neal R. Iverson, Richard M. Iverson
Lahar hazards at Mombacho Volcano, Nicaragua Lahar hazards at Mombacho Volcano, Nicaragua
Mombacho volcano, at 1,350 meters, is situated on the shores of Lake Nicaragua and about 12 kilometers south of Granada, a city of about 90,000 inhabitants. Many more people live a few kilometers southeast of Granada in 'las Isletas de Granada and the nearby 'Peninsula de Aseses. These areas are formed of deposits of a large debris avalanche (a fast moving avalanche of rock and debris)...
Authors
J.W. Vallance, S. P. Schilling, G. Devoli
Lahar hazards at Agua volcano, Guatemala Lahar hazards at Agua volcano, Guatemala
At 3760 m, Agua volcano towers more than 3500 m above the Pacific coastal plain to the south and 2000 m above the Guatemalan highlands to the north. The volcano is within 5 to 10 kilometers (km) of Antigua, Guatemala and several other large towns situated on its northern apron. These towns have a combined population of nearly 100,000. It is within about 20 km of Escuintla (population, ca...
Authors
S. P. Schilling, J.W. Vallance, O. Matias, M.M. Howell
Volcano-hazard zonation for San Vicente volcano, El Salvador Volcano-hazard zonation for San Vicente volcano, El Salvador
San Vicente volcano, also known as Chichontepec, is one of many volcanoes along the volcanic arc in El Salvador. This composite volcano, located about 50 kilometers east of the capital city San Salvador, has a volume of about 130 cubic kilometers, rises to an altitude of about 2180 meters, and towers above major communities such as San Vicente, Tepetitan, Guadalupe, Zacatecoluca, and...
Authors
J. J. Major, S. P. Schilling, C.R. Pullinger, C.D. Escobar, M.M. Howell
A simple calculator of ballistic trajectories for blocks ejected during volcanic eruptions A simple calculator of ballistic trajectories for blocks ejected during volcanic eruptions
During the past century, numerous observers have described the violent ejection of large blocks and bombs from volcanoes during volcanic explosions. Minakami (1942) mapped the locations of blocks ejected from Asama Volcano during explosions in 1937. He developed a mathematical expression relating initial velocity and trajectory angle of ejected blocks to the ejection distance, taking...
Authors
Larry G. Mastin