Publications
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Toward a comprehensive areal model of earthquake-induced landslides Toward a comprehensive areal model of earthquake-induced landslides
This paper provides a review of regional-scale modeling of earthquake-induced landslide hazard with respect to the needs for disaster risk reduction and sustainable development. Based on this review, it sets out important research themes and suggests computing with words (CW), a methodology that includes fuzzy logic systems, as a fruitful modeling methodology for addressing many of these...
Authors
S.B. Miles, D. K. Keefer
Preliminary investigation of some large landslides triggered by the 2008 Wenchuan earthquake, Sichuan Province, China Preliminary investigation of some large landslides triggered by the 2008 Wenchuan earthquake, Sichuan Province, China
The M s 8.0 Wenchuan earthquake or "Great Sichuan Earthquake" occurred at 14:28 p.m. local time on 12 May 2008 in Sichuan Province, China. Damage by earthquake-induced landslides was an important part of the total earthquake damage. This report presents preliminary observations on the Hongyan Resort slide located southwest of the main epicenter, shallow mountain surface failures in...
Authors
F. Wang, Q. Cheng, L. Highland, M. Miyajima, Hongfang Wang, C. Yan
Developing framework to constrain the geometry of the seismic rupture plane on subduction interfaces a priori - A probabilistic approach Developing framework to constrain the geometry of the seismic rupture plane on subduction interfaces a priori - A probabilistic approach
A key step in many earthquake source inversions requires knowledge of the geometry of the fault surface on which the earthquake occurred. Our knowledge of this surface is often uncertain, however, and as a result fault geometry misinterpretation can map into significant error in the final temporal and spatial slip patterns of these inversions. Relying solely on an initial hypocentre and...
Authors
G.P. Hayes, D.J. Wald
In situ measurements of contributions to the global electrical circuit by a thunderstorm in southeastern Brazil In situ measurements of contributions to the global electrical circuit by a thunderstorm in southeastern Brazil
The global electrical circuit, which maintains a potential of about 280??kV between the earth and the ionosphere, is thought to be driven mainly by thunderstorms and lightning. However, very few in situ measurements of electrical current above thunderstorms have been successfully obtained. In this paper, we present dc to very low frequency electric fields and atmospheric conductivity...
Authors
J.N. Thomas, R.H. Holzworth, M.P. McCarthy
Submarine landslide as the source for the October 11, 1918 Mona Passage tsunami: Observations and modeling Submarine landslide as the source for the October 11, 1918 Mona Passage tsunami: Observations and modeling
The October 11, 1918 ML 7.5 earthquake in the Mona Passage between Hispaniola and Puerto Rico generated a local tsunami that claimed approximately 100 lives along the western coast of Puerto Rico. The area affected by this tsunami is now significantly more populated. Newly acquired high-resolution bathymetry and seismic reflection lines in the Mona Passage show a fresh submarine...
Authors
A.M. López-Venegas, Uri S. ten Brink, Eric L. Geist
A landslide in Tertiary marine shale with superheated fumaroles, Coast Ranges, California A landslide in Tertiary marine shale with superheated fumaroles, Coast Ranges, California
In August 2004, a National Forest fire crew extinguished a 1.2 ha fire in a wilderness area ~40 km northeast of Santa Barbara, California. Examination revealed that the fire originated on a landslide dotted with superheated fumaroles. A 4 m borehole punched near the hottest (262 °C) fumarole had a maximum temperature of 307 °C. Temperatures in this borehole have been decreasing by ~0.1...
Authors
Robert H. Mariner, Scott A. Minor, A. King, J.R. Boles, Karl S. Kellogg, William C. Evans, Gary Landis, A.G. Hunt, Christy B. Till
Deciphering landslide behavior using large-scale flume experiments Deciphering landslide behavior using large-scale flume experiments
Landslides can be triggered by a variety of hydrologic events and they can exhibit a wide range of movement dynamics. Effective prediction requires understanding these diverse behaviors. Precise evaluation in the field is difficult; as an alternative we performed a series of landslide initiation experiments in the large-scale, USGS debris-flow flume. We systematically investigated the...
Authors
Mark E. Reid, Richard M. Iverson, Neal R. Iverson, Richard G. LaHusen, Dianne L. Brien, Matthew Logan
The Landslide Handbook - A Guide to Understanding Landslides The Landslide Handbook - A Guide to Understanding Landslides
This handbook is intended to be a resource for people affected by landslides to acquire further knowledge, especially about the conditions that are unique to their neighborhoods and communities. Considerable literature and research are available concerning landslides, but unfortunately little of it is synthesized and integrated to address the geographically unique geologic and climatic...
Authors
Lynn M. Highland, Peter Bobrowsky
Landslides Mapped from LIDAR Imagery, Kitsap County, Washington Landslides Mapped from LIDAR Imagery, Kitsap County, Washington
Landslides are a recurring problem on hillslopes throughout the Puget Lowland, Washington, but can be difficult to identify in the densely forested terrain. However, digital terrain models of the bare-earth surface derived from LIght Detection And Ranging (LIDAR) data express topographic details sufficiently well to identify landslides. Landslides and escarpments were mapped using LIDAR...
Authors
Jonathan P. McKenna, David J. Lidke, Jeffrey A. Coe
Earthquakes generated from bedding plane-parallel reverse faults above an active wedge thrust, Seattle fault zone Earthquakes generated from bedding plane-parallel reverse faults above an active wedge thrust, Seattle fault zone
A key question in earthquake hazard analysis is whether individual faults within fault zones represent independent seismic sources. For the Seattle fault zone, an upper plate structure within the Cascadia convergent margin, evaluating seismic hazard requires understanding how north-side-up, bedding-plane reverse faults, which generate late Holocene fault scarps, interact with the north...
Authors
Harvey Kelsey, Brian L. Sherrod, Alan R. Nelson, Thomas M. Brocher
What can we learn from the Wells, NV earthquake sequence about seismic hazard in the intermountain west? What can we learn from the Wells, NV earthquake sequence about seismic hazard in the intermountain west?
The February 21, 2008 Wells, NV earthquake (M 6) was felt throughout eastern Nevada, southern Idaho, and western Utah. The town of Wells sustained significant damage to unreinforced masonry buildings. The earthquake occurred in a region of low seismic hazard with little seismicity, low geodetic strain rates, and few mapped faults. The peak horizontal ground acceleration predicted by the...
Authors
M.D. Petersen, K.L. Pankow, G. P. Biasi, M. Meremonte
Rapid exposure and loss estimates for the May 12, 2008 Mw 7.9 Wenchuan earthquake provided by the U.S. Geological Survey's PAGER system Rapid exposure and loss estimates for the May 12, 2008 Mw 7.9 Wenchuan earthquake provided by the U.S. Geological Survey's PAGER system
One half-hour after the May 12th Mw 7.9 Wenchuan, China earthquake, the U.S. Geological Survey’s Prompt Assessment of Global Earthquakes for Response (PAGER) system distributed an automatically generated alert stating that 1.2 million people were exposed to severe-to-extreme shaking (Modified Mercalli Intensity VIII or greater). It was immediately clear that a large-scale disaster had...
Authors
P.S. Earle, D.J. Wald, T.I. Allen, K. S. Jaiswal, K.A. Porter, M.G. Hearne