Wes Hildreth (Former Employee)
Science and Products
Filter Total Items: 70
Complex proximal deposition during the Plinian eruptions of 1912 at Novarupta, Alaska Complex proximal deposition during the Plinian eruptions of 1912 at Novarupta, Alaska
Proximal (
Authors
Bruce Houghton, C. Wilson, J. Fierstein, W. Hildreth
Rear-arc vs. arc-front volcanoes in the Katmai reach of the Alaska Peninsula: A critical appraisal of across-arc compositional variation Rear-arc vs. arc-front volcanoes in the Katmai reach of the Alaska Peninsula: A critical appraisal of across-arc compositional variation
Physical and compositional data and K-Ar ages are reported for 14 rear-arc volcanoes that lic 11-22 km behind the narrowly linear volcanic front defined by the Mount Katmai-to-Devils Desk chain on the Alaska Peninsula. One is a 30-km3 stratocone (Mount Griggs; 51-63% SiO2) active intermittently from 292 ka to Holocene. The others are monogenetic cones, domes, lava flows, plugs, and maars...
Authors
W. Hildreth, J. Fierstein, D. Siems, J. R. Budahn, J. Ruiz
Rhyodacites of Kulshan caldera, North Cascades of Washington: Postcaldera lavas that span the Jaramillo Rhyodacites of Kulshan caldera, North Cascades of Washington: Postcaldera lavas that span the Jaramillo
Kulshan caldera (4.5×8 km), at the northeast foot of Mount Baker, is filled with rhyodacite ignimbrite (1.15 Ma) and postcaldera lavas and is only the third Quaternary caldera identified in the Cascade arc. A gravity traverse across the caldera yields a steep-sided, symmetrical, complete Bouguer anomaly of −16 mGal centered over the caldera. Density considerations suggest that the...
Authors
W. Hildreth, M. Lanphere, D.E. Champion, J. Fierstein
Geochronology and eruptive history of the Katmai volcanic cluster, Alaska Peninsula Geochronology and eruptive history of the Katmai volcanic cluster, Alaska Peninsula
In the Katmai district of the Alaska Peninsula, K–Ar and 40Ar/39Ar ages have been determined for a dozen andesite–dacite stratocones on the arc front and for 11 rear-arc volcanoes, 10 of which are monogenetic. Tied to mapping and stratigraphic studies, our dating emphasized proximal basal lavas that rest on basement rocks, in order to estimate ages of inception of each polygenetic cone...
Authors
Wes Hildreth, Marvin Lanphere, Judy Fierstein
Eruptive history and geochronology of the Mount Baker volcanic field, Washington Eruptive history and geochronology of the Mount Baker volcanic field, Washington
Mount Baker, a steaming, ice-mantled, andesitic stratovolcano, is the most conspicuous component of a multivent Quaternary volcanic field active almost continuously since 1.3 Ma. More than 70 packages of lava flows and ~110 dikes have been mapped, ???500 samples chemically analyzed, and ~80 K-Ar and 40Ar/39Ar ages determined. Principal components are (1) the ignimbrite-filled Kulshan...
Authors
W. Hildreth, J. Fierstein, M. Lanphere
New osmium isotope evidence for intracrustal recycling of crustal domains with discrete ages New osmium isotope evidence for intracrustal recycling of crustal domains with discrete ages
New 187Os/188Os ratios of Quaternary Mount Adams volcanic rocks from the Cascade arc in southern Washington vary by >300% (187Os/188Os = 0.165-0.564) and fall into high (>0.319) and low (0.166 to 0.281) groups of 187Os/188Os ratios that are substantially more radiogenic than mantle values. These Os isotope compositions and groupings are interpreted to reflect recycling of discrete...
Authors
G.L. Hart, C.M. Johnson, W. Hildreth, S.B. Shirey
Magma storage prior to the 1912 eruption at Novarupta, Alaska Magma storage prior to the 1912 eruption at Novarupta, Alaska
New analytical and experimental data constrain the storage and equilibration conditions of the magmas erupted in 1912 from Novarupta in the 20th century's largest volcanic event. Phase relations at H2O+CO2 fluid saturation were determined for an andesite (58.7 wt% SiO2) and a dacite (67.7 wt%) from the compositional extremes of intermediate magmas erupted. The phase assemblages, matrix...
Authors
J.E. Hammer, M.J. Rutherford, W. Hildreth
Bacon receives 1999 Bowen Award Bacon receives 1999 Bowen Award
Charles R. Bacon received the 1999 Bowen Award, presented by the Volcanology Geochemistry, and Petrology Section during the 1999 AGU Fall Meeting.
Authors
Wes Hildreth, Charles Bacon
Katmai volcanic cluster and the great eruption of 1912 Katmai volcanic cluster and the great eruption of 1912
In June 1912, the world's largest twentieth century eruption broke out through flat-lying sedimentary rocks of Jurassic age near the base of Trident volcano on the Alaska Peninsula. The 60 h ash-flow and Plinian eruptive sequence excavated and subsequently backfilled with ejecta a flaring funnel-shaped vent since called Novarupta. The vent is adjacent to a cluster of late Quaternary...
Authors
W. Hildreth, J. Fierstein
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 Drake, B. Singer
Hybrid fall deposits in the Bishop Tuff, California: A novel pyroclastic depositional mechanism Hybrid fall deposits in the Bishop Tuff, California: A novel pyroclastic depositional mechanism
Hybrid fall deposits in the Bishop Tuff show features common to both archetypal fall and surge deposits. Like normal-fall deposits, they have an overall plane-parallel bedding and flat-lying pumice clasts but also, like surge deposits, they show variable development of cross-bedding, some crystal and pumice sorting, and some rounding of pumice clasts. All variations exist from normal...
Authors
C. Wilson, W. Hildreth
The age and constitution of Cerro Campanario, a mafic stratovolcano in the Andes of central Chile The age and constitution of Cerro Campanario, a mafic stratovolcano in the Andes of central Chile
Cerro Campanario, a towering landmark on the continental divide near Paso Pehuenche, is a glacially eroded remnant of a mafic stratovolcano that is much younger than previously supposed. Consisting of fairly uniform basaltic andesite, rich in olivine and plagioclase, the 10-15 km3 edifice grew rapidly near the end of the middle Pleistocene, about 150-160 ka, as indicated by 40Ar/39Ar and...
Authors
Wes Hildreth, B. Singer, E. Godoy, F. Munizaga
Non-USGS Publications**
Hildreth, W., 1976, Death Valley Geology: Death Valley Natural History Association, Furnace Creek, CA, 64 p.
Ewart, A., Hildreth, W., and Carmichael, I.S. E., 1975, Quaternary acid magma in New Zealand: Contributions to Mineralogy and Petrology, v. 51, p. 1–27.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Filter Total Items: 70
Complex proximal deposition during the Plinian eruptions of 1912 at Novarupta, Alaska Complex proximal deposition during the Plinian eruptions of 1912 at Novarupta, Alaska
Proximal (
Authors
Bruce Houghton, C. Wilson, J. Fierstein, W. Hildreth
Rear-arc vs. arc-front volcanoes in the Katmai reach of the Alaska Peninsula: A critical appraisal of across-arc compositional variation Rear-arc vs. arc-front volcanoes in the Katmai reach of the Alaska Peninsula: A critical appraisal of across-arc compositional variation
Physical and compositional data and K-Ar ages are reported for 14 rear-arc volcanoes that lic 11-22 km behind the narrowly linear volcanic front defined by the Mount Katmai-to-Devils Desk chain on the Alaska Peninsula. One is a 30-km3 stratocone (Mount Griggs; 51-63% SiO2) active intermittently from 292 ka to Holocene. The others are monogenetic cones, domes, lava flows, plugs, and maars...
Authors
W. Hildreth, J. Fierstein, D. Siems, J. R. Budahn, J. Ruiz
Rhyodacites of Kulshan caldera, North Cascades of Washington: Postcaldera lavas that span the Jaramillo Rhyodacites of Kulshan caldera, North Cascades of Washington: Postcaldera lavas that span the Jaramillo
Kulshan caldera (4.5×8 km), at the northeast foot of Mount Baker, is filled with rhyodacite ignimbrite (1.15 Ma) and postcaldera lavas and is only the third Quaternary caldera identified in the Cascade arc. A gravity traverse across the caldera yields a steep-sided, symmetrical, complete Bouguer anomaly of −16 mGal centered over the caldera. Density considerations suggest that the...
Authors
W. Hildreth, M. Lanphere, D.E. Champion, J. Fierstein
Geochronology and eruptive history of the Katmai volcanic cluster, Alaska Peninsula Geochronology and eruptive history of the Katmai volcanic cluster, Alaska Peninsula
In the Katmai district of the Alaska Peninsula, K–Ar and 40Ar/39Ar ages have been determined for a dozen andesite–dacite stratocones on the arc front and for 11 rear-arc volcanoes, 10 of which are monogenetic. Tied to mapping and stratigraphic studies, our dating emphasized proximal basal lavas that rest on basement rocks, in order to estimate ages of inception of each polygenetic cone...
Authors
Wes Hildreth, Marvin Lanphere, Judy Fierstein
Eruptive history and geochronology of the Mount Baker volcanic field, Washington Eruptive history and geochronology of the Mount Baker volcanic field, Washington
Mount Baker, a steaming, ice-mantled, andesitic stratovolcano, is the most conspicuous component of a multivent Quaternary volcanic field active almost continuously since 1.3 Ma. More than 70 packages of lava flows and ~110 dikes have been mapped, ???500 samples chemically analyzed, and ~80 K-Ar and 40Ar/39Ar ages determined. Principal components are (1) the ignimbrite-filled Kulshan...
Authors
W. Hildreth, J. Fierstein, M. Lanphere
New osmium isotope evidence for intracrustal recycling of crustal domains with discrete ages New osmium isotope evidence for intracrustal recycling of crustal domains with discrete ages
New 187Os/188Os ratios of Quaternary Mount Adams volcanic rocks from the Cascade arc in southern Washington vary by >300% (187Os/188Os = 0.165-0.564) and fall into high (>0.319) and low (0.166 to 0.281) groups of 187Os/188Os ratios that are substantially more radiogenic than mantle values. These Os isotope compositions and groupings are interpreted to reflect recycling of discrete...
Authors
G.L. Hart, C.M. Johnson, W. Hildreth, S.B. Shirey
Magma storage prior to the 1912 eruption at Novarupta, Alaska Magma storage prior to the 1912 eruption at Novarupta, Alaska
New analytical and experimental data constrain the storage and equilibration conditions of the magmas erupted in 1912 from Novarupta in the 20th century's largest volcanic event. Phase relations at H2O+CO2 fluid saturation were determined for an andesite (58.7 wt% SiO2) and a dacite (67.7 wt%) from the compositional extremes of intermediate magmas erupted. The phase assemblages, matrix...
Authors
J.E. Hammer, M.J. Rutherford, W. Hildreth
Bacon receives 1999 Bowen Award Bacon receives 1999 Bowen Award
Charles R. Bacon received the 1999 Bowen Award, presented by the Volcanology Geochemistry, and Petrology Section during the 1999 AGU Fall Meeting.
Authors
Wes Hildreth, Charles Bacon
Katmai volcanic cluster and the great eruption of 1912 Katmai volcanic cluster and the great eruption of 1912
In June 1912, the world's largest twentieth century eruption broke out through flat-lying sedimentary rocks of Jurassic age near the base of Trident volcano on the Alaska Peninsula. The 60 h ash-flow and Plinian eruptive sequence excavated and subsequently backfilled with ejecta a flaring funnel-shaped vent since called Novarupta. The vent is adjacent to a cluster of late Quaternary...
Authors
W. Hildreth, J. Fierstein
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 Drake, B. Singer
Hybrid fall deposits in the Bishop Tuff, California: A novel pyroclastic depositional mechanism Hybrid fall deposits in the Bishop Tuff, California: A novel pyroclastic depositional mechanism
Hybrid fall deposits in the Bishop Tuff show features common to both archetypal fall and surge deposits. Like normal-fall deposits, they have an overall plane-parallel bedding and flat-lying pumice clasts but also, like surge deposits, they show variable development of cross-bedding, some crystal and pumice sorting, and some rounding of pumice clasts. All variations exist from normal...
Authors
C. Wilson, W. Hildreth
The age and constitution of Cerro Campanario, a mafic stratovolcano in the Andes of central Chile The age and constitution of Cerro Campanario, a mafic stratovolcano in the Andes of central Chile
Cerro Campanario, a towering landmark on the continental divide near Paso Pehuenche, is a glacially eroded remnant of a mafic stratovolcano that is much younger than previously supposed. Consisting of fairly uniform basaltic andesite, rich in olivine and plagioclase, the 10-15 km3 edifice grew rapidly near the end of the middle Pleistocene, about 150-160 ka, as indicated by 40Ar/39Ar and...
Authors
Wes Hildreth, B. Singer, E. Godoy, F. Munizaga
Non-USGS Publications**
Hildreth, W., 1976, Death Valley Geology: Death Valley Natural History Association, Furnace Creek, CA, 64 p.
Ewart, A., Hildreth, W., and Carmichael, I.S. E., 1975, Quaternary acid magma in New Zealand: Contributions to Mineralogy and Petrology, v. 51, p. 1–27.
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government