'Debris flows' presentation slideshows

Mass Movements: Flows

Mass Movements: Flows. Semester Schedule. 28-Oct Creep Processes 31-Oct No Class 4-Nov Style/Activity/Distribution 7-Nov Type: Slides 9-Nov FIELD TRIP 11-Nov Type: Flow 14-Nov Type: Topple and Rockfall 18-Nov Causes: Earthquakes and Overloading

766 views • 54 slides

Burn Area Emergency Response

631 views • 51 slides

Brian McInerney

Brian McInerney. National Weather Service. Hydrologist. AMS Presentation on BAER. October 29th, 2009. What is BAER?. Burn Area Emergency Response. Mud Flow, Debris Flow, Landslide. Mud Flow is filled with clays, silt, and other fine grained debris

554 views • 36 slides

Late-Breaking Gravel (Mt. Hood, Hwy 35 debris flows of 2006 and 1998)

Late-Breaking Gravel (Mt. Hood, Hwy 35 debris flows of 2006 and 1998). By Andrew Unscrupulously complied from: http://www.fhwa.dot.gov/engineering/hydraulics/pubs/mthod/mthood.cfm#09 http://vulcan.wr.usgs.gov/Volcanoes/Hood/RiverDrainages/framework.html

355 views • 25 slides

Appalachian Debris Flows: The Need to Increase Awareness and Preparedness

Appalachian Debris Flows: The Need to Increase Awareness and Preparedness. Steve Keighton Science and Operations Officer NOAA/NWS Blacksburg, VA Presented at the 2010 ER Flash Flood Workshop June 2-4, 2010. Acknowledgements. Larry Lee and WFO GSP (sharing presentations and local policy)

406 views • 25 slides

High mobility of subaqueous debris flows and the lubricating layer model

418 views • 24 slides

Causes of Flooding are i) climatic ii) terrestrial processes iii) human activity

Causes of Flooding are i) climatic ii) terrestrial processes iii) human activity. CASE STUDY: Quebrada San Julian Drainage Basin Vargas coastal region, Venezuela Dec 1999. Acknowledgements: serc.carleton.edu/files/NAGTWorkshops/health04/MarinPoster.ppt

426 views • 23 slides

Temporal and spatial changes of evolving and coalescing lahars at Semeru, Indonesia

Geolsoc 09, Oamuru. Temporal and spatial changes of evolving and coalescing lahars at Semeru, Indonesia. E. E. Doyle 1 , S. J. Cronin 1 , S. E. Cole 1 , J. -C. Thouret 2 . emmadoyle79@gmail.com 1 Inst. Natural Resources, Massey University, Private Bag 11 222, Palmerston North

305 views • 23 slides

Lithosphere: Mass Movements

659 views • 22 slides

Incident & Resource Management D.H.S. Workshop on Emergency Management:

326 views • 20 slides

Part 7

Part 7. DEBRIS FLOW MITIGATION TECHNIQUES. Check Dams. Check dams are commonly employed to arrest channel downcutting and store sediment. These can also be employed to create flatter surfaces and retard development of destructive snouts on rapidly moving debris flows.

350 views • 18 slides

Some Great Satellite Images

293 views • 15 slides

344 views • 14 slides

Comparative Emergency Management

Comparative Emergency Management. Session 7 Slide Deck. Session Objectives. Understand the difference between a hazard and a disaster, and the various methods of categorizing hazards Discuss the Natural Hazard Category Discuss the Technological Hazard Category

385 views • 13 slides

Shasta/Lava Beds/Lassen

Shasta/Lava Beds/Lassen. The Cascade Volcanoes. Caused by subduction Explorer, Juan de Fuca, and Gorda = oceanic plates North American = continental plate. Mt. Shasta. prominent landmark at an elevation of 4,317 meters (14,162 feet)

245 views • 13 slides

341 views • 12 slides

Mount Rainier

Mount Rainier. The Mountain. Location. Latitude:46.87 N Longitude:121.758 W. Mt. Rainer, Washington. Elevation. Towers 8,000 ft. Mount Rainier is a stratovolcano / composite. 4,392 meters. (14,411 feet ). History and Hazards. Of Mount Rainier.

643 views • 11 slides

Effects of Tectonic Activity

Effects of Tectonic Activity. Volcanic Effects. Lava: buries whatever is in its path Pyroclastic Clouds: burn, bury or asphyxiate everything in their path Ash: various sizes falling back to Earth; finer stuff getting up into atmosphere; lethal to plants, animals, and people.

213 views • 7 slides

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