| Paper No. 16-7 | ||
| Presentation Time: 9:30 AM-9:45 AM | ||
| USE OF DETAILED MAPPING AND MONITORING OF A LANDSLIDE TO PERMIT SAFE OCCUPATION OF SURROUNDING RESIDENCES: AN EXAMPLE IN SAN LEANDRO, CALIFORNIA | ||
|
SCHULZ, William H., Central Region Geologic Hazards Team, United States Geol Survey, Denver Federal Center, P.O. Box 25046, MS-966, Denver, CO 80225-0046, wschulz@usgs.gov and COTTON, William R., Cotton, Shires & Assoc, Inc, 330 Village Ln, Los Gatos, CA 95030-7218 A 60,000 m3 translational landslide occurred in San Leandro, California during the El Niņo winter of 1997/98, forcing evacuation of eight homes. Careful investigation and monitoring permitted safe reoccupation of homes and construction of cost-effective control measures. Detailed engineering geologic mapping and observations made in boreholes and trenches indicated that the landslide was a new failure that occurred on a cutslope in gabbro bedrock. The gabbro was highly fractured and sheared due to its position within the Hayward fault zone. The landslide occurred on approximately February 7, 1998 and moved at a nearly constant maximum rate of 0.4 m/day during the nine days thereafter. Initial displacement slowed, then quickly stopped, soon after heavy rains ceased. Slide movement typically recurred with each significant rainfall event. Monitoring of slope inclinometers indicated that the basal rupture surface occurred from 9 to 15 m below the ground surface. The local groundwater table was identified within a small portion (less than a few percent) of the landslide body a few days after initial failure and dropped beneath it within ten days. Increased pore-water pressures in fractures and pre-existing shear zones through which the rupture surface propagated apparently triggered the failure. The landslide posed a significant hazard to residents situated below from catastrophic failure onto the homes, rockfall/slide off the toe, or rupture through utilities and/or residential foundations. Earthwork and monitoring measures implemented during the fall of 1998 permitted relatively safe occupation of homes during the winter of 1998/99. Removal of slide debris from the head, placement of buttress fill on the toe, improvement of surface drainage and construction of rockfall-protection fences reduced the danger of renewed movement. Installation and bi-weekly monitoring of inclinometers, groundwater wells and topographic survey monuments enabled us to predict reactivation of the landslide and issue appropriate warnings. Long-term control measures implemented during 2000/01 permitted safe, permanent occupation of six of the eight homes. These measures consisted primarily of construction of tied-back, shear-pin retaining walls, surface-drainage improvements and horizontal subdrains. | ||
|
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. | ||