The Breckenridge Landslide

  1. (PDF, 685 KB)
DOIResolve DOI:
AuthorSearch for: ; Search for: ; Search for:
TypeTechnical Report
Series titleInternal Report, Division of Building Research, National Research Council Canada; Volume 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
AffiliationNRC Institute for Research in Construction; National Research Council Canada
Peer reviewedNo
NRC number7498
NPARC number20337956
Export citationExport as RIS
Report a correctionReport a correction
Record identifierd2eb493e-645f-4e0a-a895-500165703a06
Record created2012-07-19
Record modified2016-10-03
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)