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Votes:0 Features that may Indicate Catastrophic Landslide Movement Before (Photo by J. Kostelecky, 1987) After (Photo by D.P. Schwert, North Dakota State University, 1988) "Landslides have a maximum speed of about 17 miles per hour," stated the lead geologist for the City of Anaheim, Mark McLarty with Eberhart and Stone, Inc., to a group of landslide victims -- as if we all could somehow easily drive away from our impending doom at 60 miles per hour. But what if the unsuspecting homeowner doesn't sleep in his car, with his family at his side? What to do and look for during and immediately after heavy rains Areas that are generally prone to landslide hazards: On existing old landslides. On or at the base of slopes. In or at the base of minor drainage hollows. At the base or top of an old fill slope Read More Go to Site
Votes:0 The webpage you are looking for has moved. Please change your bookmarks. The new location is http://landslides.usgs.gov/hwy50/ In 10 seconds you will be taken there. 04/12/05, Lyn Topinka, Cascades Volcano Observatory. Read More Go to Site
Votes:0 This page has moved. You will be automatically redirected to its new location in 5 seconds. If you aren't forwarded to the new page, click here Read More Go to Site
Votes:0 [ Interior Watershed Assessment Procedure Guidebook Table of Contents ] Appendix 5. Definition of unstable slopes and those with a potential for mass wasting The potential for slopes to experience landsliding is determined by terrain (surficial geology) mapping, and the subsequent interpretation of the terrain mapping information into slope stability classes using, as defining criteria, slope angle, materials and landforms, material texture, active geomorphological processes, and soil drainage. Terrain maps provide information about the distribution and characteristics of surficial materials, landforms, and geological processes in an area. The terrain classification system used for mapping in British Columbia is defined in Howes and Kenk (1988). The Resources Inventory Committee (1994) pro Read More Go to Site
Votes:0 My name is Marco Amanti and I am a geologist. I am a member of Italian Geological Survey and I often go to work on landslide sites. On this page I want to show you some of the landslides I met during the last 10 years. Photos of Italian landslides Photos of Campania mudflows (5 - 6 May 1998) Photos of mudflows of S. Felice a Cancello (CE) (5 - 6 May 1998) Updated February 1 st , 2001 Sign Guestbook View Guestbook Well, till now persons visited this page! Congratulation, you are one of them! If you want to contact me please e-mail me at molla@geocities.com Read More Go to Site
Votes:0 Kelso Landslide A:hover {color: #FFFF00} This page has resources relating to the Kelso, WA slide and slides in general. Photo Highlights Japanese Landslide Video (3.4mb): Live Mt. Saint Helens Volcano Cam Add this page to your favorites menu View these other nwgeoscience.com pages: Oregon Dunes Photo index If anybody has any quality digital photos, send them to me , and I will post them...eventually. Links This takes you to a page to other websites of interest to this area. Student and Professional Geologic Reports April 2001 Geological Society of America Abstract on the method of determining if movement is occurring; first developed with these projects. Winter 2000 PSU report Acrobat version of the presentation given to the Kelso City council by the members of this project. The total move Read More Go to Site
Votes:0 Landslides in BC The Hope slide, 18 kilometres east of Hope, was one of the largest slides in Canadian history. The southwestern slope of Johnson Peak, collapsed on January 9, 1965, spreading 47 million cubic metres of debris, 85 metres thick, over a 3 kilometre stretch of the Hope-Princeton highway. The slide occurred in an unpopulated area in early morning hours and resulted in four deaths (photo courtesy of the Ministry of Environment, Lands and Parks). What do we mean by the word "landslide"? Landslide is a general term used to describe the down-slope movement of soil, rock and organic materials under the influence of gravity. It also describes the landform that results. British Columbia's steep, mountainous terrain, its complex geology, its high precipitation, both as rain a Read More Go to Site
Votes:0 Streams, Landslides, Logging, Roads and Rain The heavy rains of early Feb 1996, washed more than just new logs into our streams. Here are some reports on what happpened. Silver Creek on the McKenzie Background for the following 3 reports from PCFFA Post-Storm Aerial Reconnaissance of the Middle Oregon Cascades and Middle Coast Range AERIAL LANDSLIDE SURVEY OF MAPLETON RANGER DISTRICT FOLLOWING RAINSTORM OF FEBRUARY, 1996 February 14, 1996 NEW STUDY: NORTHWEST LOGGING ROAD CONSTRUCTION OUTPACES STREETS, HIGHWAYS For a detailed explanation of what happened in the Upper McKenzie Drainage, ie Blue River area, read about the Andrews Forest Flood of 1996 This wasn't an isolated event. There was more destruction in British Columbia and Idaho: Clayoquot Sound, BC Landslides Heavy Rain Causes Exten Read More Go to Site
Votes:0 SLOPE DESIGN Developed by Helen Connolly, now maintained by David Toll (d.g.toll@durham.ac.uk) Please reference: Connolly H. (1997) World Wide Web Pages for Slope Design , MEng final year project report, School of Engineering: University of Durham, pp 43. INTRODUCTION INTRODUCTION
TO SLOPES INTRODUCTION
TO SLOPE INSTABILITY SLOPE STABILITY
ANALYSIS REMEDIAL
AND CORRECTIVE MEASURES FOR FAILING SLOPES SLOPES
IN THE REAL WORLD- SOME CASE STUDIES SAMPLE
SLOPE STABILITY PROBLEMS FEEDBACK
ON THIS SITE To Top Of Page Read More Go to Site
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