| Cordilleran Section - 101st Annual Meeting (April 29–May 1, 2005) | |
| Paper No. 2-10 | |
| Presentation Time: 11:20 AM-11:40 AM | ||
RESTORATION OF DECLINING LAKE LEVELS IN THE WESTSIDE GROUNDWATER BASIN, SAN FRANCISCO AND SAN MATEO COUNTIES, CALIFORNIA | ||
|
BARTOW, Greg, San Francisco Public Utilities Commission, 1145 Market Street, Suite 401, San Francisco, CA 94103, gbartow@sfwater.org. Lake Merced is popular urban fishing and boating lake located in the southwest corner of the City of San Francisco and within the Westside Groundwater Basin. The 1.2 km2 fresh water lake is a surface expression of the shallow groundwater table. Lake levels dropped 4.5 meters, beginning in the mid-1980's, partially related to groundwater pumping, as well as the historic diversion of surface water tributaries. The Westside Groundwater Basin underlies portions of San Mateo County (73 km2) and the City and County of San Francisco (31 km2). Total groundwater pumping for municipal and irrigation purposes averages about 1.5x106 m3 /year. The Westside Basin provides up to 50% of the drinking water for 200,000 residents in northern San Mateo County. In San Francisco, groundwater is currently only pumped for non-potable purposes, primarily irrigation. However, additional municipal pumping is planned. Geologic investigations have resulted in a conceptual geologic model that is being used to 1) begin restoring declining lake levels, 2) develop additional groundwater resources in San Francisco and 3) develop a conjunctive use program in the San Mateo County portion of the Westside Basin. | ||
|
Cordilleran Section - 101st Annual Meeting (April 29–May 1, 2005)
General Information for this Meeting | ||
| Session No. 2 Groundwater and Surface Water Interactions: Hydrogeology and Water Quality in the San Francisco Bay Region Fairmont Hotel: Gold 7:55 AM-12:00 PM, Friday, April 29, 2005 Geological Society of America Abstracts with Programs, Vol. 37, No. 4, p. 36 | ||
© Copyright 2005 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. | ||