The Breckenridge Landslide

Download
  1. (PDF, 785 KB)
DOIResolve DOI: http://doi.org/10.4224/20337956
AuthorSearch for: ; Search for: ; Search for:
TypeTechnical Report
Series titleInternal Report (National Research Council Canada. Division of Building Research); no. DBR-IR-316
Physical description11 p.
AbstractIn April 1963, a small earthflow involving about 30,000 cu yd of clay took place on the side of a deep ravine near Breckenridge Station, approximately 15 miles northwest of Ottawa. The Soil Mechanics Section of the Division of Building Research is conducting an investigation of the landslide, including stability analyses in terms of both total and effective stresses. This report presents the results obtained thus far in the investigation.
Publication date
PublisherNational Research Council Canada
LanguageEnglish
AffiliationNational Research Council Canada
Peer reviewedNo
NRC numberNRC-IRC-7498
NPARC number20337956
Export citationExport as RIS
Report a correctionReport a correction
Record identifierd2eb493e-645f-4e0a-a895-500165703a06
Record created2012-07-19
Record modified2017-06-29
Bookmark and share
  • Share this page with Facebook (Opens in a new window)
  • Share this page with Twitter (Opens in a new window)
  • Share this page with Google+ (Opens in a new window)
  • Share this page with Delicious (Opens in a new window)