NH51B:
The Oso Disaster and Other New Perspectives on High-Mobility Landslides and Debris Flows I Poster

Session ID#: 5571

Friday, 19 December 2014: 8:00 AM-12:20 PM
Poster Hall (Moscone_South)
Chairs:  Scott W McCoy, University of Nevada Reno, Department of Geological Sciences and Engineering, Reno, United States and Mark E Reid, USGS, Volcano Science Center, Moffett Field, United States
Primary Convener:  Scott W McCoy, University of Nevada Reno, Department of Geological Sciences and Engineering, Reno, United States
Co-conveners:  Richard M Iverson, USGS, Vancouver, WA, United States and Mark E Reid, USGS, Volcano Science Center, Moffett Field, United States
OSPA Liaison:  Scott W McCoy, University of Nevada Reno, Department of Geological Sciences and Engineering, Reno, United States
Co-Sponsor(s):
  • EP - Earth and Planetary Surface Processes
  • V - Volcanology, Geochemistry and Petrology
Index Terms:

1810 Debris flow and landslides [HYDROLOGY]
1824 Geomorphology: general [HYDROLOGY]
4314 Mathematical and computer modeling [NATURAL HAZARDS]
4315 Monitoring, forecasting, prediction [NATURAL HAZARDS]
Virtual Option?: No

Abstracts Submitted to this Session:

 
NH51B-3846
The Effect of Debris-Flow Composition on Runout Distance (6734)
Tjalling de Haas1, Lisanne Braat2, Jasper Leuven3, Ivar Lokhorst3 and Maarten G Kleinhans1, (1)Utrecht University, Physical Geography, Utrecht, Netherlands, (2)California Institute of Technology, Division of Geological and Planetary Sciences, Pasadena, CA, United States, (3)Utrecht University, Utrecht, Netherlands
 
NH51B-3847
High-Speed Granular Chute Flows (31616)
Jim McElwaine, WSL Institute for Snow & Avalanche Research, Davos Dorf, Switzerland
 
NH51B-3848
Pre-2014 mudslides at Oso revealed by InSAR and multi-source DEM analysis (19799)
Jin Woo Kim1, Zhong Lu1 and Feifei Qu2, (1)Southern Methodist University, Roy M. Huffington Department of Earth Sciences, Dallas, TX, United States, (2)Southern Methodist University, Dallas, TX, United States
 
NH51B-3849
Forecasting Inundation from Debris Flows That Grow By Entraining Sediment (7008)
Mark E Reid1, Jeffrey A. Coe2 and Dianne L Brien1, (1)USGS, Volcano Science Center, Moffett Field, United States, (2)USGS Geologic Hazards Science Center, Golden, United States
 
NH51B-3851
A Laboratory Investigation of the Controls on the High Mobility of Hillslope Debris Flows (9166)
Brian W McArdell1 and Marcel Hürlimann1,2, (1)WSL Swiss Federal Institute for Forest, Snow and Landscape Research, Birmensdorf, Switzerland, (2)Barcelona Tech, Department of Geotechnical Engineering and Geosciences, Barcelona, Spain
 
NH51B-3852
Can the flow dynamics of debris flows be identified from seismic data? (20238)
Jason W Kean, U.S. Geological Survey, Landslide Hazards Program, Golden, CO, United States, Jeffrey A. Coe, USGS, Geologic Hazards Science Center, Golden, CO, United States, Joel Smith, U.S. Geological Survey, Denver, CO, United States, Velio Coviello, CNR - IRPI, Torino, Italy and Scott W McCoy, University of Nevada Reno, Department of Geological Sciences and Engineering, Reno, United States
 
NH51B-3853
The Time-Frequency Signatures of Advanced Seismic Signals Generated by Debris Flows (20310)
Chung-Ray Chu1, Ching-Jer Huang2, Ching-ren Lin3, Chau-chang Wang1, Ban-Yuan Kuo3 and Hsiao-Yuan Yin4, (1)Institute of Undersea Technology, National Sun Yat-sen University, Kaohsiung, Taiwan, (2)National Cheng Kung University, Department of Hydraulic and Ocean Engineering, Tainan, Taiwan, (3)Institute of Earth Sciences Academia Sinica, Taipei, Taiwan, (4)Soil and Water Conservation Bureau, Council of Agriculture, Nantou, Taiwan
 
NH51B-3854
Persistence of Episodic Extreme Events: Sustained Colluvial Contributions of Fine Sediment to Vermont Rivers Post-Irene (22284)
Evan Dethier1, Frank J Magilligan2, Carl E Renshaw3 and David Sinclair2, (1)Dartmouth College, Department of Earth Sciences, Hanover, United States, (2)Dartmouth College, Hanover, NH, United States, (3)Dartmouth College, Earth Sciences, Hanover, NH, United States
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