GEOLOGY of SAN FRANCISCO, CALIFORNIA United States of America

Total Page:16

File Type:pdf, Size:1020Kb

GEOLOGY of SAN FRANCISCO, CALIFORNIA United States of America San Francisco Pacific Ocean San Francisco Bay GEOLOGY OF SAN FRANCISCO, CALIFORNIA United States of America Geology of the Cities of the World Series Association Engineering Geologists Geology of Cities of the World Series Geology of San Francisco, California, United States of America Issued to registrants at the 61st Annual Meeting of the Association of Environmental & Engineering Geologists and 13th International Association of Environmental & Engineering Geologists Congress in San Francisco, CA – September 16 through 22, 2018. Editors: Kenneth A. Johnson, PhD, CEG, PE WSP USA, San Francisco, CA Greg W. Bartow, CHg, CEG California State Parks, Sacramento, CA Contributing Authors: John Baldwin, Greg W. Bartow, Peter Dartnell, George Ford, Jeffrey A. Gilman, Robert Givler, Sally Goodin, Russell W. Graymer, H. Gary Greene, Kenneth A. Johnson, Samuel Y. Johnson, Darrell Klingman, Keith L. Knudsen, William Lettis, William E. Motzer, Dorinda Shipman, Lori A. Simpson, Philip J. Stuecheli, and Raymond Sullivan. It is hard to be unaware of the earth in San Francisco (Wahrhaftig, 1984). A generous grant from the AEG Foundation, Robert F. Legget Fund, helped make this publication possible. Founded in 1993, the Robert F. Legget Fund of the AEG foundation supports publications and public outreach in engineering geology and environmental geology that serve as information resources for the professional practitioner, students, faculty, and the public. The fund also supports education about the interactions between the works of mankind and the geologic environment. Cover Plate: European Space Agency i Table of Contents PREFACE v ABSTRACT 1 INTRODUCTION 1 Geographic Setting . 1 Climate . 6 History and Founding . 6 Native Americans . 6 European Founding of San Francisco . 7 Gold Rush and Its Impact to San Francisco . 11 Between the Gold Rush and the 1906 Earthquake . 13 Quarries in San Francisco . 16 1906 Earthquake . 19 Rebuilding after the 1906 Earthquake and Fire . 23 Panama-Pacific International Exposition . 24 World War II: Military Base Expansion . 24 Post-WWII High-Rise Building Boom: The Manhattanization of San Francisco . 25 San Francisco in the Future: Major New Transit Projects on the Horizon . 25 GEOLOGY AND GEOLOGIC HISTORY 30 Overview of the Geology of the San Francisco Bay Region . 30 Introduction: The Road to Accretion . 30 Geologic Overview of the San Francisco Bay Region . 33 Geology of San Francisco . 41 San Francisco Basement Complex Rocks . 41 Geologic Structures in San Francisco . 51 Tertiary Overlap Sequences . 51 Quaternary Deposits in San Francisco . 52 San Francisco’s Offshore Geology . 58 Geologic History of San Francisco . 61 Rocks Passing Through . 61 Rocks From Somewhere Else . 62 Neogene Paleogeography . 64 GEOTECHNICAL AND ENGINEERING GEOLOGY CHARACTERISTICS OF GEOLOGIC UNITS 67 Artificial Fill . 67 Eolian Deposits and Dune Sands . 67 Young Bay Mud . 68 Colma Foundation . 68 Index Properties . 68 Hydraulic Conductivity . 68 General Engineering Practice . 69 Yerba Buena Mud (Old Bay Deposits) . 69 Index Properties . 69 Relative Density and Consistency . 69 Hydraulic Conductivity . 69 Franciscan Complex Rocks . 69 Quarries . 70 ii Rock Falls and Slope Stability . 70 GEOLOGIC ASPECTS OF NATURAL HAZARDS 70 Earthquake Hazards . 70 San Andreas Fault . 71 Hayward–Rodgers Creek Fault . 78 San Gregorio Fault . 79 Calaveras Fault . 80 Faults of San Francisco . 81 Liquefaction and Lateral Spreading . 82 WATER RESOURCES 84 San Francisco’s Water Supply . 84 Early Years . 84 Post Gold Rush . 84 Search for a Sierra Source . 84 Sunset Well Field . 86 Hetch Hetchy Regional Water System . 87 Water System Improvement Program . 87 Auxiliary Water Supply System . 90 Diversification of Water Supplies . 92 Local Groundwater . 92 Non-Potable Water . 92 Recycled Water . 92 San Francisco Creeks and Lakes . 93 Lobos Creek . 93 Mountain Lake . 93 Lake Merced . 93 Vista Grande Drainage Basin Improvement Project . 95 Groundwater . 95 Westside Groundwater Basin . 95 Lobos Groundwater Basin . 102 Marina Groundwater Basin . 102 Visitacion Valley Groundwater Basin . 103 Downtown Groundwater Basin . 103 Islais Valley Groundwater Basin . 105 South San Francisco Groundwater Basin . 105 ENVIRONMENTAL CONCERNS 106 Regulatory Setting . 106 GeoTracker . 106 Maher Ordinance . 106 Hunters Point Naval Shipyard . 108 Cleanup Program at the Shipyard . ..
Recommended publications
  • Ovarian Development of the Mud Crab Scylla Paramamosain in a Tropical Mangrove Swamps, Thailand
    Available Online JOURNAL OF SCIENTIFIC RESEARCH Publications J. Sci. Res. 2 (2), 380-389 (2010) www.banglajol.info/index.php/JSR Ovarian Development of the Mud Crab Scylla paramamosain in a Tropical Mangrove Swamps, Thailand M. S. Islam1, K. Kodama2, and H. Kurokura3 1Department of Aquaculture and Fisheries, Jessore Science and Technology University, Jessore- 7407, Bangladesh 2Marine Science Institute, The University of Texas at Austin, Channel View Drive, Port Aransas, Texas 78373, USA 3Laboratory of Global Fisheries Science, Department of Global Agricultural Sciences, The University of Tokyo, Bunkyo, Tokyo 113-8657, Japan Received 15 October 2009, accepted in revised form 21 March 2010 Abstract The present study describes the ovarian development stages of the mud crab, Scylla paramamosain from Pak Phanang mangrove swamps, Thailand. Samples were taken from local fishermen between June 2006 and December 2007. Ovarian development was determined based on both morphological appearance and histological observation. Ovarian development was classified into five stages: proliferation (stage I), previtellogenesis (II), primary vitellogenesis (III), secondary vitellogenesis (IV) and tertiary vitellogenesis (V). The formation of vacuolated globules is the initiation of primary vitellogenesis and primary growth. The follicle cells were found around the periphery of the lobes, among the groups of oogonia and oocytes. The follicle cells were hardly visible at the secondary and tertiary vitellogenesis stages. Yolk granules occurred in the primary vitellogenesis stage and are first initiated in the inner part of the oocytes, then gradually concentrated to the periphery of the cytoplasm. The study revealed that the initiation of vitellogenesis could be identified by external observation of the ovary but could not indicate precisely.
    [Show full text]
  • New Empirical Relationships Among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement
    Bulletin of the Seismological Society of America, Vol. 84, No. 4, pp. 974-1002, August 1994 New Empirical Relationships among Magnitude, Rupture Length, Rupture Width, Rupture Area, and Surface Displacement by Donald L. Wells and Kevin J. Coppersmith Abstract Source parameters for historical earthquakes worldwide are com­ piled to develop a series of empirical relationships among moment magnitude (M), surface rupture length, subsurface rupture length, downdip rupture width, rupture area, and maximum and average displacement per event. The resulting data base is a significant update of previous compilations and includes the ad­ ditional source parameters of seismic moment, moment magnitude, subsurface rupture length, downdip rupture width, and average surface displacement. Each source parameter is classified as reliable or unreliable, based on our evaluation of the accuracy of individual values. Only the reliable source parameters are used in the final analyses. In comparing source parameters, we note the fol­ lowing trends: (1) Generally, the length of rupture at the surface is equal to 75% of the subsurface rupture length; however, the ratio of surface rupture length to subsurface rupture length increases with magnitude; (2) the average surface dis­ placement per event is about one-half the maximum surface displacement per event; and (3) the average subsurface displacement on the fault plane is less than the maximum surface displacement but more than the average surface dis­ placement. Thus, for most earthquakes in this data base, slip on the fault plane at seismogenic depths is manifested by similar displacements at the surface. Log-linear regressions between earthquake magnitude and surface rupture length, subsurface rupture length, and rupture area are especially well correlated, show­ ing standard deviations of 0.25 to 0.35 magnitude units.
    [Show full text]
  • Section 3.4 Biological Resources 3.4- Biological Resources
    SECTION 3.4 BIOLOGICAL RESOURCES 3.4- BIOLOGICAL RESOURCES 3.4 BIOLOGICAL RESOURCES This section discusses the existing sensitive biological resources of the San Francisco Bay Estuary (the Estuary) that could be affected by project-related construction and locally increased levels of boating use, identifies potential impacts to those resources, and recommends mitigation strategies to reduce or eliminate those impacts. The Initial Study for this project identified potentially significant impacts on shorebirds and rafting waterbirds, marine mammals (harbor seals), and wetlands habitats and species. The potential for spread of invasive species also was identified as a possible impact. 3.4.1 BIOLOGICAL RESOURCES SETTING HABITATS WITHIN AND AROUND SAN FRANCISCO ESTUARY The vegetation and wildlife of bayland environments varies among geographic subregions in the bay (Figure 3.4-1), and also with the predominant land uses: urban (commercial, residential, industrial/port), urban/wildland interface, rural, and agricultural. For the purposes of discussion of biological resources, the Estuary is divided into Suisun Bay, San Pablo Bay, Central San Francisco Bay, and South San Francisco Bay (See Figure 3.4-2). The general landscape structure of the Estuary’s vegetation and habitats within the geographic scope of the WT is described below. URBAN SHORELINES Urban shorelines in the San Francisco Estuary are generally formed by artificial fill and structures armored with revetments, seawalls, rip-rap, pilings, and other structures. Waterways and embayments adjacent to urban shores are often dredged. With some important exceptions, tidal wetland vegetation and habitats adjacent to urban shores are often formed on steep slopes, and are relatively recently formed (historic infilled sediment) in narrow strips.
    [Show full text]
  • Glossary Glossary
    Glossary Glossary Albedo A measure of an object’s reflectivity. A pure white reflecting surface has an albedo of 1.0 (100%). A pitch-black, nonreflecting surface has an albedo of 0.0. The Moon is a fairly dark object with a combined albedo of 0.07 (reflecting 7% of the sunlight that falls upon it). The albedo range of the lunar maria is between 0.05 and 0.08. The brighter highlands have an albedo range from 0.09 to 0.15. Anorthosite Rocks rich in the mineral feldspar, making up much of the Moon’s bright highland regions. Aperture The diameter of a telescope’s objective lens or primary mirror. Apogee The point in the Moon’s orbit where it is furthest from the Earth. At apogee, the Moon can reach a maximum distance of 406,700 km from the Earth. Apollo The manned lunar program of the United States. Between July 1969 and December 1972, six Apollo missions landed on the Moon, allowing a total of 12 astronauts to explore its surface. Asteroid A minor planet. A large solid body of rock in orbit around the Sun. Banded crater A crater that displays dusky linear tracts on its inner walls and/or floor. 250 Basalt A dark, fine-grained volcanic rock, low in silicon, with a low viscosity. Basaltic material fills many of the Moon’s major basins, especially on the near side. Glossary Basin A very large circular impact structure (usually comprising multiple concentric rings) that usually displays some degree of flooding with lava. The largest and most conspicuous lava- flooded basins on the Moon are found on the near side, and most are filled to their outer edges with mare basalts.
    [Show full text]
  • Sediment Transport in the San Francisco Bay Coastal System: an Overview
    Marine Geology 345 (2013) 3–17 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Sediment transport in the San Francisco Bay Coastal System: An overview Patrick L. Barnard a,⁎, David H. Schoellhamer b,c, Bruce E. Jaffe a, Lester J. McKee d a U.S. Geological Survey, Pacific Coastal and Marine Science Center, Santa Cruz, CA, USA b U.S. Geological Survey, California Water Science Center, Sacramento, CA, USA c University of California, Davis, USA d San Francisco Estuary Institute, Richmond, CA, USA article info abstract Article history: The papers in this special issue feature state-of-the-art approaches to understanding the physical processes Received 29 March 2012 related to sediment transport and geomorphology of complex coastal–estuarine systems. Here we focus on Received in revised form 9 April 2013 the San Francisco Bay Coastal System, extending from the lower San Joaquin–Sacramento Delta, through the Accepted 13 April 2013 Bay, and along the adjacent outer Pacific Coast. San Francisco Bay is an urbanized estuary that is impacted by Available online 20 April 2013 numerous anthropogenic activities common to many large estuaries, including a mining legacy, channel dredging, aggregate mining, reservoirs, freshwater diversion, watershed modifications, urban run-off, ship traffic, exotic Keywords: sediment transport species introductions, land reclamation, and wetland restoration. The Golden Gate strait is the sole inlet 9 3 estuaries connecting the Bay to the Pacific Ocean, and serves as the conduit for a tidal flow of ~8 × 10 m /day, in addition circulation to the transport of mud, sand, biogenic material, nutrients, and pollutants.
    [Show full text]
  • Geodetic Constraints on San Francisco Bay Area Fault Slip Rates and Potential Seismogenic Asperities on the Partially Creeping Hayward Fault Eileen L
    Masthead Logo Smith ScholarWorks Geosciences: Faculty Publications Geosciences 3-2012 Geodetic Constraints on San Francisco Bay Area Fault Slip Rates and Potential Seismogenic Asperities on the Partially Creeping Hayward Fault Eileen L. Evans Harvard University John P. Loveless Harvard University, [email protected] Brendan J. Meade Harvard University Follow this and additional works at: https://scholarworks.smith.edu/geo_facpubs Part of the Geology Commons Recommended Citation Evans, Eileen L.; Loveless, John P.; and Meade, Brendan J., "Geodetic Constraints on San Francisco Bay Area Fault Slip Rates and Potential Seismogenic Asperities on the Partially Creeping Hayward Fault" (2012). Geosciences: Faculty Publications, Smith College, Northampton, MA. https://scholarworks.smith.edu/geo_facpubs/21 This Article has been accepted for inclusion in Geosciences: Faculty Publications by an authorized administrator of Smith ScholarWorks. For more information, please contact [email protected] JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117, B03410, doi:10.1029/2011JB008398, 2012 Geodetic constraints on San Francisco Bay Area fault slip rates and potential seismogenic asperities on the partially creeping Hayward fault Eileen L. Evans,1 John P. Loveless,1,2 and Brendan J. Meade1 Received 28 March 2011; revised 17 November 2011; accepted 31 January 2012; published 31 March 2012. [1] The Hayward fault in the San Francisco Bay Area (SFBA) is sometimes considered unusual among continental faults for exhibiting significant aseismic creep during the interseismic phase of the seismic cycle while also generating sufficient elastic strain to produce major earthquakes. Imaging the spatial variation in interseismic fault creep on the Hayward fault is complicated because of the interseismic strain accumulation associated with nearby faults in the SFBA, where the relative motion between the Pacific plate and the Sierra block is partitioned across closely spaced subparallel faults.
    [Show full text]
  • Regional Oral History Off Ice University of California the Bancroft Library Berkeley, California
    Regional Oral History Off ice University of California The Bancroft Library Berkeley, California Richard B. Gump COMPOSER, ARTIST, AND PRESIDENT OF GUMP'S, SAN FRANCISCO An Interview Conducted by Suzanne B. Riess in 1987 Copyright @ 1989 by The Regents of the University of California Since 1954 the Regional Oral History Office has been interviewing leading participants in or well-placed witnesses to major events in the development of Northern California, the West,and the Nation. Oral history is a modern research technique involving an interviewee and an informed interviewer in spontaneous conversation. The taped record is transcribed, lightly edited for continuity and clarity, and reviewed by the interviewee. The resulting manuscript is typed in final form, indexed, bound with photographs and illustrative materials, and placed in The Bancroft Library at the University of California, Berkeley, and other research collections for scholarly use. Because it is primary material, oral history is not intended to present the final, verified, or complete narrative of events. It is a spoken account, offered by the interviewee in response to questioning, and as such it is reflective, partisan, deeply involved, and irreplaceable. All uses of this manuscript are covered by a legal agreement between the University of California and Richard B. Gump dated 7 March 1988. The manuscript is thereby made available for research purposes. All literary rights in the manuscript, including the right to publish, are reserved to The Bancroft Library of the University of California, Berkeley. No part of the manuscript may be quoted for publication without the written permission of the Director of The Bancroft Library of the University of California, Berkeley.
    [Show full text]
  • Bodega Bay Field Trip Guide
    ESP/ERS 30 World Ecosystem and Geography Davis-Bodega Bay Sacramento Valley - Coastal Ranges & Valleys - Coastline Introduction This trip follows a westward transect from Davis across the low coastal mountain ranges to the coast. A. Plant Communities 1. Central Valley Grassland (now primarily agricultural fields and orchards) 2. Oak Savannas and Oak Woodlands 3. Chaparral and a chaparral variant with Gray Pine 4. A variety of Riparian habitats 5. Mixed Evergreen Forest 6. Redwood Forest 7. North Coastal Scrub and Prairie 8. Coastal Beach, Marsh, and Tidal Communities B. Environmental Factors Climatic zones you will encounter include the somewhat “continental” climate of the Sacramento Valley, characterized by cool, wet winters with frequent winter fog (a result of cold air subsidence off the Sierras and entrapment in the Valley by the Coast Ranges), and long, dry, hot summers. Even more continental climates are characteristic of regions much further inland, e.g., Ohio. Really extreme continental climates occur in Central Asia and Siberia. Continental climates are so called because as you move inland away from the ocean, the moderating effect of the ocean on temperature leads to more extremes inland. The Coast Ranges are characterized by somewhat less extreme, but still highly variable, conditions of temperature and precipitation as they are in a zone of transition between the more Continental climate of the Valley and the highly Maritime climate of the Coast. The climate along the Coast is dominated by the cool waters of the Pacific Ocean and the California Current which flows south along this part of our coast. The ocean acts as a buffer and greatly reduces the extremes in temperature characteristic of the Sacramento Valley but also increases the amount of moisture in the air, increasing relative humidity.
    [Show full text]
  • AQ Conformity Amended PBA 2040 Supplemental Report Mar.2018
    TRANSPORTATION-AIR QUALITY CONFORMITY ANALYSIS FINAL SUPPLEMENTAL REPORT Metropolitan Transportation Commission Association of Bay Area Governments MARCH 2018 Metropolitan Transportation Commission Jake Mackenzie, Chair Dorene M. Giacopini Julie Pierce Sonoma County and Cities U.S. Department of Transportation Association of Bay Area Governments Scott Haggerty, Vice Chair Federal D. Glover Alameda County Contra Costa County Bijan Sartipi California State Alicia C. Aguirre Anne W. Halsted Transportation Agency Cities of San Mateo County San Francisco Bay Conservation and Development Commission Libby Schaaf Tom Azumbrado Oakland Mayor’s Appointee U.S. Department of Housing Nick Josefowitz and Urban Development San Francisco Mayor’s Appointee Warren Slocum San Mateo County Jeannie Bruins Jane Kim Cities of Santa Clara County City and County of San Francisco James P. Spering Solano County and Cities Damon Connolly Sam Liccardo Marin County and Cities San Jose Mayor’s Appointee Amy R. Worth Cities of Contra Costa County Dave Cortese Alfredo Pedroza Santa Clara County Napa County and Cities Carol Dutra-Vernaci Cities of Alameda County Association of Bay Area Governments Supervisor David Rabbit Supervisor David Cortese Councilmember Pradeep Gupta ABAG President Santa Clara City of South San Francisco / County of Sonoma San Mateo Supervisor Erin Hannigan Mayor Greg Scharff Solano Mayor Liz Gibbons ABAG Vice President City of Campbell / Santa Clara City of Palo Alto Representatives From Mayor Len Augustine Cities in Each County City of Vacaville
    [Show full text]
  • Park Report Part 1
    Alcatraz Island Golden Gate National Recreation Area Physical History PRE-EUROPEAN (Pre-1776) Before Europeans settled in San Francisco, the area was inhabited by Native American groups including the Miwok, in the area north of San Francisco Bay (today’s Marin County), and the Ohlone, in the area south of San Francisco Bay (today’s San Francisco peninsula). Then, as today, Alcatraz had a harsh environment –strong winds, fog, a lack of a fresh water source (other than rain or fog), rocky terrain –and there was only sparse vegetation, mainly grasses. These conditions were not conducive to living on the island. These groups may have used the island for a fishing station or they may have visited it to gather seabird eggs since the island did provide a suitable habitat for colonies of seabirds. However, the Miwok and Ohlone do not appear to have lived on Alcatraz or to have visibly altered its landscape, and no prehistoric archeological sites have been identified on the island. (Thomson 1979: 2, Delgado et al. 1991: 8, and Hart 1996: 4). SPANISH AND MEXICAN PERIOD (1776-1846) Early Spanish explorers into Alta California encountered the San Francisco Bay and its islands. (Jose Francisco Ortega saw the bay during his scouting for Gaspar de Portola’s 1769 expedition, and Pedro Fages described the three major islands –Angel, Alcatraz, and Yerba Buena –in his journal from the subsequent 1772 expedition.) However, the first Europeans to record their visit to Alcatraz were aboard the Spanish ship San Carlos, commanded by Juan Manuel de Ayala that sailed through the Golden Gate and anchored off Angel Island in August 1775.
    [Show full text]
  • The EERI Oral History Series
    CONNECTIONS The EERI Oral History Series Robert E. Wallace CONNECTIONS The EERI Oral History Series Robert E. Wallace Stanley Scott, Interviewer Earthquake Engineering Research Institute Editor: Gail Hynes Shea, Albany, CA ([email protected]) Cover and book design: Laura H. Moger, Moorpark, CA Copyright ©1999 by the Earthquake Engineering Research Institute and the Regents of the University of California. All rights reserved. All literary rights in the manuscript, including the right to publish, are reserved to the Earthquake Engineering Research Institute and the Bancroft Library of the University of California at Berkeley. No part may be reproduced, quoted, or transmitted in any form without the written permission of the executive director of the Earthquake Engi- neering Research Institute or the Director of the Bancroft Library of the University of California at Berkeley. Requests for permission to quote for publication should include identification of the specific passages to be quoted, anticipated use of the passages, and identification of the user. The opinions expressed in this publication are those of the oral history subject and do not necessarily reflect the opinions or policies of the Earthquake Engineering Research Institute or the University of California. Published by the Earthquake Engineering Research Institute 499 14th Street, Suite 320 Oakland, CA 94612-1934 Tel: (510) 451-0905 Fax: (510) 451-5411 E-Mail: [email protected] Web site: http://www.eeri.org EERI Publication No.: OHS-6 ISBN 0-943198-99-2 Library of Congress Cataloging-in-Publication Data Wallace, R. E. (Robert Earl), 1916- Robert E. Wallace / Stanley Scott, interviewer. p. cm – (Connections: the EERI oral history series ; 7) (EERI publication ; no.
    [Show full text]
  • Warm Springs Extension Title VI Equity Analysis and Public Participation Report
    Warm Springs Extension Title VI Equity Analysis and Public Participation Report May 7, 2015 Prepared jointly by CDM Smith and the San Francisco Bay Area Rapid Transit District, Office of Civil Rights 1 Table of Contents Executive Summary 3 Section 1: Introduction 6 Section 2: Project Description 7 Section 3: Methodology 14 Section 4: Service Analysis Findings 23 Section 5: Fare Analysis Findings 27 Appendix A: 2011 Warm Springs Survey 33 Appendix B: Proposed Service Options Description 36 Public Participation Report 4 1 2 Warm Springs Extension Title VI Equity Analysis and Public Participation Report Executive Summary In June 2011, staff completed a Title VI Analysis for the Warm Springs Extension Project (Project). Per the Federal Transit Administration (FTA) Title VI Circular (Circular) 4702.1B, Title VI Requirements and Guidelines for Federal Transit Administration Recipients (October 1, 2012), the District is required to conduct a Title VI Service and Fare Equity Analysis (Title VI Equity Analysis) for the Project's proposed service and fare plan six months prior to revenue service. Accordingly, staff completed an updated Title VI Equity Analysis for the Project’s service and fare plan, which evaluates whether the Project’s proposed service and fare will have a disparate impact on minority populations or a disproportionate burden on low-income populations based on the District’s Disparate Impact and Disproportionate Burden Policy (DI/DB Policy) adopted by the Board on July 11, 2013 and FTA approved Title VI service and fare methodologies. Discussion: The Warm Springs Extension will add 5.4-miles of new track from the existing Fremont Station south to a new station in the Warm Springs district of the City of Fremont, extending BART’s service in southern Alameda County.
    [Show full text]