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The Breckenridge landslide

From National Research Council Canada

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DOIResolve DOI: https://doi.org/10.4224/20337956
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FormatText, Technical Report
Physical description11 p.
Abstract
In 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 of Canada
Series
  • Internal Report (National Research Council of Canada. Division of Building Research), no. DBR-IR-316.
LanguageEnglish
Peer reviewedNo
NRC numberNRC-IRC-7498
NPARC number20337956
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Record identifierd2eb493e-645f-4e0a-a895-500165703a06
Record created2012-07-19
Record modified2023-02-02
Date modified: