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Widespread loess-like deposit in the Martian northern lowlands identifies Middle Amazonian climate change Widespread loess-like deposit in the Martian northern lowlands identifies Middle Amazonian climate change

Consistently mappable units critical to distinguishing the style and interplay of geologic processes through time are sparse in the Martian lowlands. This study identifies a previously unmapped Middle Amazonian (ca. 1 Ga) unit (Middle Amazonian lowland unit, mAl) that postdates the Late Hesperian and Early Amazonian lowland plains by >2 b.y. The unit is regionally defined by subtle...
Authors
James A. Skinner, Kenneth L. Tanaka, Thomas Platz

Relation of landslides triggered by the Kiholo Bay earthquake to modeled ground motion Relation of landslides triggered by the Kiholo Bay earthquake to modeled ground motion

The 2006 Kiholo Bay, Hawaii, earthquake triggered high concentrations of rock falls and slides in the steep canyons of the Kohala Mountains along the north coast of Hawaii. Within these mountains and canyons a complex distribution of landslides was triggered by the earthquake shaking. In parts of the area, landslides were preferentially located on east‐facing slopes, whereas in other...
Authors
Edwin L. Harp, Stephen H. Hartzell, Randall W. Jibson, L. Ramirez-Guzman, Robert G. Schmitt

The 17 May 2012 M4.8 earthquake near Timpson, East Texas: An event possibly triggered by fluid injection The 17 May 2012 M4.8 earthquake near Timpson, East Texas: An event possibly triggered by fluid injection

This study summarizes our investigation of the 17 May 2012 MW-RMT4.8 earthquake near Timpson, Texas, the largest earthquake recorded historically in eastern Texas. To identify preshocks and aftershocks of the 17 May event we examined the arrivals recorded at Nacogdoches (NATX) 30 km from the 17 May epicenter, at nearby USArray Transportable Array stations, and at eight temporary stations...
Authors
Cliff Frohlich, William L. Ellsworth, Wesley Brown, Michael Brunt, James Luetgert, Tim G. MacDonald, Steven Walters

Empirical models for predicting volumes of sediment deposited by debris flows and sediment-laden floods in the transverse ranges of southern California Empirical models for predicting volumes of sediment deposited by debris flows and sediment-laden floods in the transverse ranges of southern California

Debris flows and sediment-laden floods in the Transverse Ranges of southern California pose severe hazards to nearby communities and infrastructure. Frequent wildfires denude hillslopes and increase the likelihood of these hazardous events. Debris-retention basins protect communities and infrastructure from the impacts of debris flows and sediment-laden floods and also provide critical...
Authors
Joseph E. Gartner, Susan H. Cannon, Paul M Santi

The rock abrasion record at Gale Crater: Mars Science Laboratory results from Bradbury Landing to Rocknest The rock abrasion record at Gale Crater: Mars Science Laboratory results from Bradbury Landing to Rocknest

Ventifacts, rocks abraded by wind-borne particles, are found in Gale Crater, Mars. In the eastward drive from “Bradbury Landing” to “Rocknest,” they account for about half of the float and outcrop seen by Curiosity's cameras. Many are faceted and exhibit abrasion textures found at a range of scales, from submillimeter lineations to centimeter-scale facets, scallops, flutes, and grooves...
Authors
N.T. Bridges, F.J. Calef, B.W. Hallett, Kenneth E. Herkenhoff, N.L. Lanza, S. Le Mouélic, C.E. Newman, D.L. Blaney, de Pablo, G.A. Kocurek, Y. Langevin, K.W. Lewis, N. Mangold, S. Maurice, P.-Y. Meslin, P. Pinet, N.O. Renno, CM.S. Rice, M.E. Richardson, V. Sautter, R.S. Sletten, R. C. Wiens, R.A. Yingst

Thermal measurements of dark and bright surface features on Vesta as derived from Dawn/VIR Thermal measurements of dark and bright surface features on Vesta as derived from Dawn/VIR

Remote sensing data acquired during Dawn’s orbital mission at Vesta showed several local concentrations of high-albedo (bright) and low-albedo (dark) material units, in addition to spectrally distinct meteorite impact ejecta. The thermal behavior of such areas seen at local scale (1-10 km) is related to physical properties that can provide information about the origin of those materials...
Authors
Federico Tosi, Maria Teresa Capria, De Sanctis, J.-Ph. Combe, F. Zambon, A. Nathues, S.E. Schröder, J.-Y. Li, E. Palomba, A. Longobardo, D.T. Blewett, B.W. Denevi, E. Palmer, F. Capaccioni, E. Ammannito, Timothy N. Titus, D.W. Mittlefehldt, J.M. Sunshine, C.T. Russell, C.A. Raymond, Dawn/VIR Team

Geologic and physiographic controls on bed-material yield, transport, and channel morphology for alluvial and bedrock rivers, western Oregon Geologic and physiographic controls on bed-material yield, transport, and channel morphology for alluvial and bedrock rivers, western Oregon

The rivers of western Oregon have diverse forms and characteristics, with channel substrates ranging from continuous alluvial gravel to bare bedrock. Analysis of several measurable morphologic attributes of 24 valley reaches on 17 rivers provides a basis for comparing nonalluvial and alluvial channels. Key differences are that alluvial reaches have greater bar area, greater migration...
Authors
James E. O'Connor, Joseph F. Mangano, Scott A. Anderson, J. Rose Wallick, Krista L. Jones, Mackenzie K. Keith

Continuous monitoring of Hawaiian volcanoes with thermal cameras Continuous monitoring of Hawaiian volcanoes with thermal cameras

Continuously operating thermal cameras are becoming more common around the world for volcano monitoring, and offer distinct advantages over conventional visual webcams for observing volcanic activity. Thermal cameras can sometimes “see” through volcanic fume that obscures views to visual webcams and the naked eye, and often provide a much clearer view of the extent of high temperature...
Authors
Matthew R. Patrick, Tim R. Orr, Loren Antolik, Robert Lopaka Lee, Kevan P. Kamibayashi

Geodetic constraints on the 2014 M 6.0 South Napa earthquake Geodetic constraints on the 2014 M 6.0 South Napa earthquake

On 24 August 2014, the M 6.0 South Napa earthquake shook much of the San Francisco Bay area, leading to significant damage in the Napa Valley. The earthquake occurred in the vicinity of the West Napa fault (122.313° W, 38.22° N, 11.3 km), a mapped structure located between the Rodger’s Creek and Green Valley faults, with nearly pure right‐lateral strike‐slip motion (strike 157°, dip 77°...
Authors
William D. Barnhart, Jessica R. Murray, S H Yun, Jerry L. Svarc, SV Samsonov, EJ Fielding, Benjamin A. Brooks, Pietro Milillo

High-resolution digital elevation model of Mount St. Helens crater and upper North Fork Toutle River basin, Washington, based on an airborne lidar survey of September 2009 High-resolution digital elevation model of Mount St. Helens crater and upper North Fork Toutle River basin, Washington, based on an airborne lidar survey of September 2009

The lateral blast, debris avalanche, and lahars of the May 18th, 1980, eruption of Mount St. Helens, Washington, dramatically altered the surrounding landscape. Lava domes were extruded during the subsequent eruptive periods of 1980–1986 and 2004–2008. More than three decades after the emplacement of the 1980 debris avalanche, high sediment production persists in the North Fork Toutle...
Authors
Adam R. Mosbrucker

Science during crisis: the application of social science during major environmental crises Science during crisis: the application of social science during major environmental crises

Historical and contemporary experience suggests that science plays an increasingly critical role in governmental and institutional responses to major environmental crises. Recent examples include major western wildfires (2009), the Deepwater Horizon oil spill (2010), the Fukushima nuclear accident (2011), and Hurricane Sandy (2012). The application of science during such crises has...
Authors
Gary Machlis, Kris Ludwig

A depth-averaged debris-flow model that includes the effects of evolving dilatancy: II. Numerical predictions and experimental tests. A depth-averaged debris-flow model that includes the effects of evolving dilatancy: II. Numerical predictions and experimental tests.

We evaluate a new depth-averaged mathematical model that is designed to simulate all stages of debris-flow motion, from initiation to deposition. A companion paper shows how the model’s five governing equations describe simultaneous evolution of flow thickness, solid volume fraction, basal pore-fluid pressure, and two components of flow momentum. Each equation contains a source term that
Authors
David L. George, Richard M. Iverson
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