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Landslides in the San Francisco Bay area (SFBA) of California

Dates

Start Date
2009

Summary

Landslides in the San Francisco Bay area (SFBA) of California impact people, infrastructure, and the environment, and are commonly induced by intense or prolonged rainfall associated with strong winter storms. Both shallow (<3 meter) and deep (≥3 meter) landslides can occur. Typically, shallow landslides occur as a result of high-intensity precipitation when the ground is already nearly saturated with water from previous storms. These types of events typically occur during the height of the rainy season, from December through February. Deep-seated landslides can also initiate or renew movement during these times but are also often triggered during the spring months (March through May), when water from rainfall has had a chance to make [...]

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Buckeye_Debris_Flow_Source_DBrien_2023_IMG_0917.JPG
“2023 landslide source area for long-runout debris flow on San Bruno Mountain”
thumbnail 5.64 MB image/jpeg

Purpose

The U.S. Geological Survey, in cooperation with local and state government organizations, operates several shallow landslide monitoring sites in the SFBA for research purposes. The goal of this research is to identify thresholds for widespread shallow landsliding and related high-mobility debris flows based on in-situ soil moisture conditions. This information is being used to develop landslide warning criteria with the National Weather Service.
2023 landslide source area for long-runout debris flow on San Bruno Mountain
2023 landslide source area for long-runout debris flow on San Bruno Mountain

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  • USGS Data Release Products

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