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Preliminary assessment of channel stability and bed-material transport along Hunter Creek, southwestern Oregon Preliminary assessment of channel stability and bed-material transport along Hunter Creek, southwestern Oregon

This preliminary assessment of (1) bed-material transport in the Hunter Creek basin, (2) historical changes in channel condition, and (3) supplementary data needed to inform permitting decisions regarding instream gravel extraction revealed the following: Along the lower 12.4 km (kilometers) of Hunter Creek from its confluence with the Little South Fork Hunter Creek to its mouth, the...
Authors
Krista L. Jones, J. Rose Wallick, Jim E. O'Connor, Mackenzie K. Keith, Joseph F. Mangano, John C. Risley

Improved earthquake monitoring in the central and eastern United States in support of seismic assessments for critical facilities Improved earthquake monitoring in the central and eastern United States in support of seismic assessments for critical facilities

Evaluation of seismic monitoring capabilities in the central and eastern United States for critical facilities - including nuclear powerplants - focused on specific improvements to understand better the seismic hazards in the region. The report is not an assessment of seismic safety at nuclear plants. To accomplish the evaluation and to provide suggestions for improvements using funding...
Authors
William S. Leith, Harley M. Benz, Robert B. Herrmann

Albuquerque Seismological Laboratory--50 years of global seismology Albuquerque Seismological Laboratory--50 years of global seismology

The U.S. Geological Survey Albuquerque Seismological Laboratory is about 15 miles southeast of Albuquerque on the Pueblo of Isleta, adjacent to Kirtland Air Force Base. The Albuquerque Seismological Laboratory supports the Global Seismographic Network Program and the Advanced National Seismic System through the installation, operation, and maintenance of seismic stations around the world...
Authors
C. R. Hutt, Jon Peterson, Lind Gee, John Derr, Adam Ringler, David Wilson

Earthquakes in Mississippi and vicinity 1811-2010 Earthquakes in Mississippi and vicinity 1811-2010

This map summarizes two centuries of earthquake activity in Mississippi. Work on the Mississippi map was done in collaboration with the Mississippi Department of Environmental Quality, Office of Geology. The earthquake data plotted on the map are from several sources: the Mississippi Department of Environmental Quality, the Center for Earthquake Research and Information, the National...
Authors
Richard L. Dart, Michael B. E. Bograd

Earthquakes in Arkansas and vicinity 1699-2010 Earthquakes in Arkansas and vicinity 1699-2010

This map summarizes approximately 300 years of earthquake activity in Arkansas. It is one in a series of similar State earthquake history maps. Work on the Arkansas map was done in collaboration with the Arkansas Geological Survey. The earthquake data plotted on the map are from several sources: the Arkansas Geological Survey, the Center for Earthquake Research and Information, the...
Authors
Richard L. Dart, Scott M. Ausbrooks

Spatially explicit shallow landslide susceptibility mapping over large areas Spatially explicit shallow landslide susceptibility mapping over large areas

Recent advances in downscaling climate model precipitation predictions now yield spatially explicit patterns of rainfall that could be used to estimate shallow landslide susceptibility over large areas. In California, the United States Geological Survey is exploring community emergency response to the possible effects of a very large simulated storm event and to do so it has generated...
Authors
Dino Bellugi, William E. Dietrich, Jonathan D. Stock, Jim McKean, Brian Kazian, Paul Hargrove

A two-phase debris-flow model that includes coupled evolution of volume fractions, granular dilatancy, and pore-fluid pressure A two-phase debris-flow model that includes coupled evolution of volume fractions, granular dilatancy, and pore-fluid pressure

Pore-fluid pressure plays a crucial role in debris flows because it counteracts normal stresses at grain contacts and thereby reduces intergranular friction. Pore-pressure feedback accompanying debris deformation is particularly important during the onset of debrisflow motion, when it can dramatically influence the balance of forces governing downslope acceleration. We consider further...
Authors
David L. George, Richard M. Iverson

Three‐dimensional model for the crust and upper mantle in the Barents Sea region Three‐dimensional model for the crust and upper mantle in the Barents Sea region

The Barents Sea and its surroundings is an epicontinental region which previously has been difficult to access, partly because of its remote Arctic location (Figure 1) and partly because the region has been politically sensitive. Now, however, this region, and in particular its western parts, has been very well surveyed with a variety of geophysical studies, motivated in part by...
Authors
H. Bangum, O. Ritzmann, N. Maercklin, J.I. Faleide, Walter D. Mooney, Shane T. Detweiler

Small explosion from new vent at Kilauea’s summit Small explosion from new vent at Kilauea’s summit

At 0258 Hawaii‐Aleutian Standard Time (HST) on 19 March 2008, a small explosion scattered altered and fresh lithic debris across a 40‐hectare area at the summit of Kilauea volcano. This explosion, the first recorded there since 1924, issued from a vent about 35 meters wide along the east wall of Halema'uma'u Crater. Ballistic fragments—the largest measuring nearly 1 meter across—were...
Authors
David C. Wilson, Tamar Elias, Tim R. Orr, Matthew R. Patrick, Jeff Sutton, Don Swanson

Mars atmospheric surface interactions and the CO2 cycle Mars atmospheric surface interactions and the CO2 cycle

Mars' northern and southern seasonal polar caps are formed during their respective autumn and winter seasons both by condensation of atmospheric carbon dioxide (CO2) directly onto the surface, and through atmospheric precipitation in the form of CO2 snow. During the polar spring and summer, the seasonal ice sublimes, returning CO2 to the atmosphere. Roughly 25% of the atmosphere, which...
Authors
Timothy N. Titus, Anthony Colaprete

Coseismic slip distribution of the February 27, 2010 Mw 8.9 Maule, Chile earthquake Coseismic slip distribution of the February 27, 2010 Mw 8.9 Maule, Chile earthquake

[1] Static offsets produced by the February 27, 2010 Mw = 8.8 Maule, Chile earthquake as measured by GPS and InSAR constrain coseismic slip along a section of the Andean megathrust of dimensions 650 km (in length) × 180 km (in width). GPS data have been collected from both campaign and continuous sites sampling both the near-field and far field. ALOS/PALSAR data from several ascending...
Authors
Fred F. Pollitz, Ben Brooks, Xiaopeng Tong, Michael G. Bevis, James H. Foster, Roland Burgmann
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