Publications
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Landslide-dammed lake at Tangjiashan, Sichuan province, China (triggered by the Wenchuan Earthquake, May 12, 2008): Risk assessment, mitigation strategy, and lessons learned Landslide-dammed lake at Tangjiashan, Sichuan province, China (triggered by the Wenchuan Earthquake, May 12, 2008): Risk assessment, mitigation strategy, and lessons learned
Landslides and rock avalanches triggered by the 2008 Wenchuan Earthquake produced 257 landslide dams, mainly situated along the eastern boundary of the Qinghai-Tibet Plateau where rivers descend approximately 3,000 m into the Sichuan Basin. The largest of these dams blocked the Tongkou River (a tributary of the Fujiang River) at Tangjiashan. The blockage, consisting of 2.04 × 107 m3 of...
Authors
P. Cui, C. Dang, J. Zhuang, Y. You, X. Chen, Kevin M. Scott
Hydrogen isotope investigation of amphibole and biotite phenocrysts in silicic magmas erupted at Lassen Volcanic Center, California Hydrogen isotope investigation of amphibole and biotite phenocrysts in silicic magmas erupted at Lassen Volcanic Center, California
Hydrogen isotope ratio, water content and Fe3 +/Fe2 + in coexisting amphibole and biotite phenocrysts in volcanic rocks can provide insight into shallow pre- and syn-eruptive magmatic processes such as vesiculation, and lava drainback with mixing into less devolatilized magma that erupts later in a volcanic sequence. We studied four ~ 35 ka and younger eruption sequences (i.e. Kings...
Authors
S.J. Underwood, T.C. Feeley, M.A. Clynne
Surface heat flow and CO2 emissions within the Ohaaki hydrothermal field, Taupo Volcanic Zone, New Zealand Surface heat flow and CO2 emissions within the Ohaaki hydrothermal field, Taupo Volcanic Zone, New Zealand
Carbon dioxide emissions and heat flow have been determined from the Ohaaki hydrothermal field, Taupo Volcanic Zone (TVZ), New Zealand following 20 a of production (116 MWe). Soil CO2 degassing was quantified with 2663 CO2 flux measurements using the accumulation chamber method, and 2563 soil temperatures were measured and converted to equivalent heat flow (W m−2) using published soil...
Authors
C. Rissmann, B. Christenson, Cynthia A. Werner, M. Leybourne, J. Cole, D. Gravley
Water and heat transport in boreal soils: Implications for soil response to climate change Water and heat transport in boreal soils: Implications for soil response to climate change
Soil water content strongly affects permafrost dynamics by changing the soil thermal properties. However, the movement of liquid water, which plays an important role in the heat transport of temperate soils, has been under-represented in boreal studies. Two different heat transport models with and without convective heat transport were compared to measurements of soil temperatures in...
Authors
Zhaosheng Fan, Jennifer W. Harden, G.C. Winston, Jonathan A. O’Donnell, Jason C. Neff, Tingjun Zhang, Hugo Veldhuis, C.I. Czimczik
‘Measurement of Clay Surface Areas by Polyvinylpyrrolidone (PVP) Sorption: A New Method for Quantifying Illite and Smectite Abundance’ ‘Measurement of Clay Surface Areas by Polyvinylpyrrolidone (PVP) Sorption: A New Method for Quantifying Illite and Smectite Abundance’
No abstract available.
Authors
Alex E. Blum, Lopaka Lee, Dennis D. Eberl
Vulnerability of high-latitude soil organic carbon in North America to disturbance Vulnerability of high-latitude soil organic carbon in North America to disturbance
This synthesis addresses the vulnerability of the North American high-latitude soil organic carbon (SOC) pool to climate change. Disturbances caused by climate warming in arctic, subarctic, and boreal environments can result in significant redistribution of C among major reservoirs with potential global impacts. We divide the current northern high-latitude SOC pools into (1) near-surface...
Authors
Guido Grosse, Jennifer W. Harden, Merritt Turetsky, A. David McGuire, Philip Camill, Charles Tarnocai, Steve Frolking, Edward A.G. Schuur, Torre Jorgenson, Sergei Marchenko, Vladimir Romanovsky, Kimberly P. Wickland, Nancy French, Mark P. Waldrop, Laura L. Bourgeau-Chavez, Robert G. Striegl
The role of dyking and fault control in the rapid onset of eruption at Chaitén Volcano, Chile The role of dyking and fault control in the rapid onset of eruption at Chaitén Volcano, Chile
Rhyolite is the most viscous of liquid magmas, so it was surprising that on 2 May 2008 at Chaitén Volcano, located in Chile’s southern Andean volcanic zone, rhyolitic magma migrated from more than 5 km depth in less than 4 hours and erupted explosively with only two days of detected precursory seismic activity. The last major rhyolite eruption before that at Chaitén was the largest...
Authors
Charles W. Wicks, J. Carlos de la Llera, Luis E. Lara, Jacob B. Lowenstern
Thermal mapping of Hawaiian volcanoes with ASTER satellite data Thermal mapping of Hawaiian volcanoes with ASTER satellite data
Thermal mapping of volcanoes is important to determine baseline thermal behavior in order to judge future thermal activity that may precede an eruption. We used cloud-free kinetic temperature images from the ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) sensor obtained between 2000 and 2010 to produce thermal maps for all five subaerial volcanoes in Hawaii that...
Authors
Matthew R. Patrick, Coral-Nadine Witzke
Columbia River Estuary ecosystem classification—Concept and application Columbia River Estuary ecosystem classification—Concept and application
This document describes the concept, organization, and application of a hierarchical ecosystem classification that integrates saline and tidal freshwater reaches of estuaries in order to characterize the ecosystems of large flood plain rivers that are strongly influenced by riverine and estuarine hydrology. We illustrate the classification by applying it to the Columbia River estuary...
Authors
Charles A. Simenstad, Jennifer L. Burke, Jim E. O'Connor, Charles Cannon, Danelle W. Heatwole, Mary F. Ramirez, Ian R. Waite, Timothy D. Counihan, Krista L. Jones
Channel change and bed-material transport in the Umpqua River basin, Oregon Channel change and bed-material transport in the Umpqua River basin, Oregon
The Umpqua River drains 12,103 square kilometers of western Oregon; with headwaters in the Cascade Range, the river flows through portions of the Klamath Mountains and Oregon Coast Range before entering the Pacific Ocean. Above the head of tide, the Umpqua River, along with its major tributaries, the North and South Umpqua Rivers, flows on a mixed bedrock and alluvium bed, alternating...
Authors
J. Rose Wallick, Jim E. O'Connor, Scott Anderson, Mackenzie K. Keith, Charles Cannon, John C. Risley
Flood-frequency analyses from paleoflood investigations for Spring, Rapid, Boxelder, and Elk Creeks, Black Hills, western South Dakota Flood-frequency analyses from paleoflood investigations for Spring, Rapid, Boxelder, and Elk Creeks, Black Hills, western South Dakota
Flood-frequency analyses for the Black Hills area are important because of severe flooding of June 9-10, 1972, that was caused by a large mesoscale convective system and caused at least 238 deaths. Many 1972 peak flows are high outliers (by factors of 10 or more) in observed records that date to the early 1900s. An efficient means of reducing uncertainties for flood recurrence is to...
Authors
Tessa M. Harden, Jim E. O'Connor, Daniel G. Driscoll, John F. Stamm
Earthquakes in Hawai‘i—an underappreciated but serious hazard Earthquakes in Hawai‘i—an underappreciated but serious hazard
The State of Hawaii has a history of damaging earthquakes. Earthquakes in the State are primarily the result of active volcanism and related geologic processes. It is not a question of "if" a devastating quake will strike Hawai‘i but rather "when." Tsunamis generated by both distant and local quakes are also an associated threat and have caused many deaths in the State. The U.S...
Authors
Paul G. Okubo, Jennifer S. Nakata