Paper No. 16-6
Presentation Time: 9:15 AM-9:30 AM
EVANS, Stephen G. and COUTURE, Réjean, Geol Survey of Canada, 601 Booth Street, Ottawa, ON K1A 0E8, Canada,

As David Varnes noted, sagging rock slopes are common in mountain landscapes. A challenge to landslide specialists lies in the evaluation of the catastrophic potential of such slopes. The 1965 Hope Slide involved the total movement of about 48 x 106 m3 of rock from the slopes of Johnson Peak which had undergone significant gravitational deformation in postglacial time, including a large prehistoric rock avalanche which occurred at the site ca. 10,000 y. B.P. Pre-1965 aerial photographs show a series of linear trenches near the headscarp of the 1965 event and similar manifestations of slope deformation to the southeast of the landslide. Trenches recently dug into these features have allowed a reconstruction of the deformation history of the failed slope during the Holocene. Trench stratigraphy shows that deformation of the trench fill has been not been episodic but more of a gradual process. A previously published analysis of seismograph records from January 9, 1965 suggested that the Hope Slide event probably occurred as two rock avalanches separated by about 3 hours. The first, involving the failure of the headscarp of the prehistoric rock avalanche, was controlled mainly by gouge filled lithologic contacts between felsite sheets, dipping less than the slope inclination, and greenstone, which dips at or a little steeper than the slope. Debuttressing of the upper slope by the first slide event led to a complex detachment along steeply dipping joints within the greenstone three hours later. With the resolution of the seismic events recorded at the time of the rockslide, no seismic or hydrometeorological trigger is discernible for the 1965 events. It is suggested that progressive long-term deformation of the slopes of the southwest flanks of Johnson Peak caused the stability of the slope to deteriorate to a point where the 1965 events occurred. Thus we conclude that the Hope Slide was a catastrophic termination of very long term non-episodic mountain slope deformation.

2002 Denver Annual Meeting (October 27-30, 2002)
Session No. 16
Case Studies in Landslide Problem Solving, Landslide Monitoring, and Alarm Methodology: In Honor of David J. Varnes
Colorado Convention Center: A101/103
8:00 AM-12:00 PM, Sunday, October 27, 2002

© Copyright 2002 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.