The Land This Is a View of the City of Concord Taken About 1930. Note
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3.6 Geology, Soils, and Seismicity
3.6 Geology, Soils, and Seismicity ENVIRONMENTAL SETTING PHYSICAL SETTING Geology The city of Emeryville is situated within the Coast Ranges geomorphic province of California. The Coast Ranges is the largest of the state’s geomorphic provinces extending approximately 400 miles from the Klamath Mountains (near northern Humboldt County) to the Santa Ynez River in Santa Barbara County. The province lies between the Pacific Ocean and the Great Valley (Sacramento and San Joaquin valleys) provinces and is characterized by a series of northwest trending mountain ridges and valleys, running generally parallel to the San Andreas Fault zone. These mountain ridges and valleys have been formed by tectonic forces that compressed ancient sedimentary deposits over the course of millions of years. The San Francisco Bay is located in a broad depression in the Franciscan bedrock resulting from an east-west expansion between the San Andreas and the Hayward fault systems. The bedrock surface can be found at elevations of 200 to 2,000 feet below mean sea level across the Bay Area. Sedimentary deposits that overlie the Franciscan bedrock originated from millions of years of erosion, deposition, and changes in sea level. Geologists categorize these sedimentary deposits into geologic formations based on the period of deposition and material type, as described below for the San Francisco Bay region. • The Alameda Formation is the deepest and oldest of these sedimentary deposits and consists of a mixture of clay, silt, sand, gravel, and some shells with predominantly silt and clay sediments surrounding discontinuous layers of sand and gravel. Members of this formation include Yerba Buena Mud (also named Old Bay Mud), and the San Antonio/Merrit/Posey Member, and Young Bay Mud (RWQCB, 2008). -
Geology and Soils
Environmental Checklist and Analysis – Geology and Soils 1 3.6 GEOLOGY AND SOILS Less Than Potentially Less Than Significant No GEOLOGY AND SOILS – Would the Project: Significant Significant with Impact Impact Impact Mitigation a) Expose people or structures to potential substantial adverse effects, including the risk of loss, injury, or death involving: i) Rupture of a known earthquake fault, as delineated on the most recent Alquist-Priolo Earthquake Fault Zoning Map issued by the State Geologist for the area or based on other substantial evidence of a known fault? Refer to Division of Mines and Geology Special Publication 42. ii) Strong seismic ground shaking? iii) Seismic-related ground failure, including liquefaction? iv) Landslides? b) Result in substantial soil erosion or the loss of topsoil? c) Be located on a geologic unit or soil that is unstable, or that would become unstable as a result of the Project, and potentially result in on- or off-site landslide, lateral spreading, subsidence, liquefaction or collapse? d) Be located on expansive soil, as defined in Table 18-1-B of the Uniform Building Code (1994), creating substantial risks to life or property? e) Have soils incapable of adequately supporting the use of septic tanks or alternative waste water disposal systems where sewers are not available for the disposal of waste water? 2 3.6.1 Environmental Setting 3 Regional Setting 4 The Project site lies within the Coast Range Geomorphic Province of California, a 5 region with independent and discontinuous northwest-trending mountain ranges, ridges, 6 and intervening valleys (California Geological Survey [CGS] 2002). -
Fault-Rupture Hazard Zones in California
SPECIAL PUBLICATION 42 Interim Revision 2007 FAULT-RUPTURE HAZARD ZONES IN CALIFORNIA Alquist-Priolo Earthquake Fault Zoning Act 1 with Index to Earthquake Fault Zones Maps 1 Name changed from Special Studies Zones January 1, 1994 DEPARTMENT OF CONSERVATION California Geological Survey STATE OF CALIFORNIA ARNOLD SCHWARZENEGGER GOVERNOR THE RESOURCES AGENCY DEPARTMENT OF CONSERVATION MIKE CHRISMAN BRIDGETT LUTHER SECRETARY FOR RESOURCES DIRECTOR CALIFORNIA GEOLOGICAL SURVEY JOHN G. PARRISH, PH.D. STATE GEOLOGIST SPECIAL PUBLICATION 42 FAULT-RUPTURE HAZARD ZONES IN CALIFORNIA Alquist-Priolo Earthquake Fault Zoning Act With Index to Earthquake Fault Zones Maps by WILLIAM A. BRYANT and EARL W. HART Geologists Interim Revision 2007 California Department of Conservation California Geological Survey 801 K Street, MS 12-31 Sacramento, California 95814 PREFACE The purpose of the Alquist-Priolo Earthquake Fault Zoning Act is to regulate development near active faults so as to mitigate the hazard of surface fault rupture. This report summarizes the various responsibilities under the Act and details the actions taken by the State Geologist and his staff to implement the Act. This is the eleventh revision of Special Publication 42, which was first issued in December 1973 as an “Index to Maps of Special Studies Zones.” A text was added in 1975 and subsequent revisions were made in 1976, 1977, 1980, 1985, 1988, 1990, 1992, 1994, and 1997. The 2007 revision is an interim version, available in electronic format only, that has been updated to reflect changes in the index map and listing of additional affected cities. In response to requests from various users of Alquist-Priolo maps and reports, several digital products are now available, including digital raster graphic (pdf) and Geographic Information System (GIS) files of the Earthquake Fault Zones maps, and digital files of Fault Evaluation Reports and site reports submitted to the California Geological Survey in compliance with the Alquist-Priolo Act (see Appendix E). -
4.8 Geology, Soils, and Geohazards
4. Environmental Setting, Impacts, Standard Conditions of Approval, and Mitigation Measures 4.8 Geology, Soils, and Geohazards This section describes geologic and seismic conditions in the project vicinity to provide relevant background information of the physical characteristics of the project site with respect to soils and potential geologic hazards. The following information is compiled from geologic maps and reports available from the City of Oakland, the California Geological Survey (CGS; formerly California Division of Mines and Geology), the ABAG, two geotechnical reports prepared by Geomatrix in 2008, and a third geotechnical report prepared by AMEC Geomatrix in 2009. This section identifies any potentially significant geologic impacts and, if necessary, appropriate mitigation measures or standard conditions of approval. Pursuant to the City’s amendment to the Oakland General Plan (City of Oakland, 2005), as well as Section 15358(b) of the CEQA Guidelines, mitigation measures are proposed only to address physical impacts that may result from the project. 4.8.1 Environmental Setting The project site is situated within the Coast Ranges geomorphic province of California. The Coast Ranges is the largest of the state’s geomorphic provinces extending approximately 400 miles from the Klamath Mountains (near northern Humboldt County) to the Santa Ynez River in Santa Barbara County. The province lies between the Pacific Ocean and the Great Valley (Sacramento and San Joaquin valleys) provinces and is characterized by a series of northwest trending mountain ridges and valleys, running generally parallel to the San Andreas Fault zone. These mountain ridges and valleys have been formed by tectonic forces that compressed ancient sedimentary deposits over the course of millions of years. -
WMH Corporation, Inc. April 29, 2014 50 West San Fernando Street, Suite 950 Project No.: 2013-105-WCB San Jose, CA 95113
WMH Corporation, Inc. April 29, 2014 50 West San Fernando Street, Suite 950 Project No.: 2013-105-WCB San Jose, CA 95113 Attention: Mr. Tim Lee Subject: Surface Fault Rupture Displacement Hazard (SFRDH) Analysis for Bridge Structures Widening of Walnut Creek Bridges – Bridge Numbers: 28-0240L/R (CC-4-13.4) (within Alquist-Priolo Earthquake Fault Zone) I-680/SR-4 Interchange Project - Phase 3 (SR-4 Widening), Contra Costa County, California Dear Mr. Tim Lee: As requested, we are providing this memorandum for the “Surface Fault Rupture Displacement Hazard (SFRDH)” analysis for the widening of Walnut Creek Bridges that are part of the “I- 680/SR-4 Interchange Project – Phase 3 (SR-4 Widening)” (Phase 3 Project). SUMMARY Caltrans bridges 28-0240L/R are located approximately 2 miles north of downtown Concord, Contra Costa County (CC-4-13.4; Plate 1). The bridges are within the Alquist-Priolo Earthquake Fault Zone (EFZ) for the Concord fault (Plate 2). The Walnut Creek Bridges straddle the mapped Main Trace of the Concord fault. The mapped East Trace of the Concord fault is located approximately 230 meters (755 feet) east of the Main Trace. The Concord fault is capable of moderate displacements, but the probability of off-fault displacements decreases rapidly with increasing distance from the fault. We expect moderate displacements to occur along the Main Trace of the Concord fault within the bridge footprint. Conservatively, we have assumed that all of the potential slip will occur along the Main Trace of the fault. The potential off-fault horizontal displacements within the bridge footprint are; 0.22 meters (8.7 inches) deterministically and 0.57 meter (22.4 inches) probabilistically. -
Initial Study / Mitigated Negative Declaration City of Concord Concord Village Residential Project
INITIAL STUDY / MITIGATED NEGATIVE DECLARATION CITY OF CONCORD CONCORD VILLAGE RESIDENTIAL PROJECT JANUARY 2017 LEAD AGENCY: City of Concord, Planning Division 1950 Parkside Drive Concord, CA 94519 (925) 671-3152 www.cityofconcord.org INITIAL STUDY / MITIGATED NEGATIVE DECLARATION CITY OF CONCORD CONCORD VILLAGE RESIDENTIAL PROJECT JANUARY 2017 LEAD AGENCY: City of Concord, Planning Division 1950 Parkside Drive Concord, CA 94519 (925) 671-3152 www.cityofconcord.org PREPARED BY: Analytical Environmental Services 1801 7th Street, Suite 100 Sacramento, CA 95811 (916) 447-3479 www.analyticalcorp.com Section 1.0 Introduction Table Contents SECTION 1.0 – INTRODUCTION ................................................................................ 1-3 1.1 Purpose of Study ....................................................................................................................... 1-4 1.2 Environmental Factors Potentially Affected ............................................................................... 1-4 1.3 Significance Determination ........................................................................................................ 1-5 SECTION 2.0 – PROJECT DESCRIPTION ................................................................. 2-1 2.1 Location and Existing Setting .................................................................................................... 2-1 2.2 Project Description ..................................................................................................................... 2-7 2.3 -
Database of Potential Sources for Earthquakes Larger Than Magnitude 6 in Northern California
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY DATABASE OF POTENTIAL SOURCES FOR EARTHQUAKES LARGER THAN MAGNITUDE 6 IN NORTHERN CALIFORNIA By The Working Group on Northern California Earthquake Potential Open-File Report 96-705 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American stratigraphic code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1996 Working Group on Northern California Earthquake Potential William Bakun U.S. Geological Survey Edward Bortugno California Office of Emergency Services William Bryant California Division of Mines & Geology Gary Carver Humboldt State University Kevin Coppersmith Geomatrix N. T. Hall Geomatrix James Hengesh Dames & Moore Angela Jayko U.S. Geological Survey Keith Kelson William Lettis Associates Kenneth Lajoie U.S. Geological Survey William R. Lettis William Lettis Associates James Lienkaemper* U.S. Geological Survey Michael Lisowski Hawaiian Volcano Observatory Patricia McCrory U.S. Geological Survey Mark Murray Stanford University David Oppenheimer U.S. Geological Survey William D. Page Pacific Gas & Electric Co. Mark Petersen California Division of Mines & Geology Carol S. Prentice U.S. Geological Survey William Prescott U.S. Geological Survey Thomas Sawyer William Lettis Associates David P. Schwartz* U.S. Geological Survey Jeff Unruh William Lettis Associates Dave Wagner California Division of Mines & Geology -
Documents Pertaining to the Adjudication of Private Land Claims in California, Circa 1852-1904
http://oac.cdlib.org/findaid/ark:/13030/hb109nb422 Online items available Finding Aid to the Documents Pertaining to the Adjudication of Private Land Claims in California, circa 1852-1904 Finding Aid written by Michelle Morton and Marie Salta, with assistance from Dean C. Rowan and Randal Brandt The Bancroft Library University of California, Berkeley Berkeley, California, 94720-6000 Phone: (510) 642-6481 Fax: (510) 642-7589 Email: [email protected] URL: http://bancroft.berkeley.edu/ © 2008, 2013 The Regents of the University of California. All rights reserved. Finding Aid to the Documents BANC MSS Land Case Files 1852-1892BANC MSS C-A 300 FILM 1 Pertaining to the Adjudication of Private Land Claims in Cali... Finding Aid to the Documents Pertaining to the Adjudication of Private Land Claims in California, circa 1852-1904 Collection Number: BANC MSS Land Case Files The Bancroft Library University of California, Berkeley Berkeley, California Finding Aid Written By: Michelle Morton and Marie Salta, with assistance from Dean C. Rowan and Randal Brandt. Date Completed: March 2008 © 2008, 2013 The Regents of the University of California. All rights reserved. Collection Summary Collection Title: Documents pertaining to the adjudication of private land claims in California Date (inclusive): circa 1852-1904 Collection Number: BANC MSS Land Case Files 1852-1892 Microfilm: BANC MSS C-A 300 FILM Creators : United States. District Court (California) Extent: Number of containers: 857 Cases. 876 Portfolios. 6 volumes (linear feet: Approximately 75)Microfilm: 200 reels10 digital objects (1494 images) Repository: The Bancroft Library University of California, Berkeley Berkeley, California, 94720-6000 Phone: (510) 642-6481 Fax: (510) 642-7589 Email: [email protected] URL: http://bancroft.berkeley.edu/ Abstract: In 1851 the U.S. -
Quaternary Fault and Fold Database of the United States
Jump to Navigation Quaternary Fault and Fold Database of the United States As of January 12, 2017, the USGS maintains a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. For the most up-to-date information, please refer to the interactive fault map. Concord fault, Ygnacio Valley section (Class A) No. 38c Last Review Date: 1998-08-18 Compiled in cooperation with the California Geological Survey citation for this record: Bryant, W.A., and Cluett, S.E., compilers, 1998, Fault number 38c, Concord fault, Ygnacio Valley section, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, https://earthquakes.usgs.gov/hazards/qfaults, accessed 12/14/2020 03:11 PM. Synopsis General: Holocene active dextral strike-slip fault. Fault is characterized by aseismic creep at a rate of 3.0–3.5 mm/yr (Galehouse, 1999 #5500). Several site-specific studies in compliance with the Alquist-Priolo Act have documented the location and approximate time of the most recent faulting (Wills and Hart, 1992 #5340; 1992 #5341). Detailed studies at Galindo Creek yielded a preliminary slip-rate of 3.7±2.0 mm/yr (Borchardt, 1998 #5334). Sections: This fault has 3 sections. Sharp (1973 #508) defined Sections: This fault has 3 sections. Sharp (1973 #508) defined three segments based on differences in geomorphic expression and amount of fault creep. Due to reconnaissance nature of his report, Sharp's segments are herein considered as sections. Name General: Concord fault was first mapped and named by Poland comments (1935 #5337) based on groundwater data. -
Explanatory Text to Accompany the Fault Activity Map of California
An Explanatory Text to Accompany the Fault Activity Map of California Scale 1:750,000 ARNOLD SCHWARZENEGGER, Governor LESTER A. SNOW, Secretary BRIDGETT LUTHER, Director JOHN G. PARRISH, Ph.D., State Geologist STATE OF CALIFORNIA THE NATURAL RESOURCES AGENCY DEPARTMENT OF CONSERVATION CALIFORNIA GEOLOGICAL SURVEY CALIFORNIA GEOLOGICAL SURVEY JOHN G. PARRISH, Ph.D. STATE GEOLOGIST Copyright © 2010 by the California Department of Conservation, California Geological Survey. All rights reserved. No part of this publication may be reproduced without written consent of the California Geological Survey. The Department of Conservation makes no warranties as to the suitability of this product for any given purpose. An Explanatory Text to Accompany the Fault Activity Map of California Scale 1:750,000 Compilation and Interpretation by CHARLES W. JENNINGS and WILLIAM A. BRYANT Digital Preparation by Milind Patel, Ellen Sander, Jim Thompson, Barbra Wanish, and Milton Fonseca 2010 Suggested citation: Jennings, C.W., and Bryant, W.A., 2010, Fault activity map of California: California Geological Survey Geologic Data Map No. 6, map scale 1:750,000. ARNOLD SCHWARZENEGGER, Governor LESTER A. SNOW, Secretary BRIDGETT LUTHER, Director JOHN G. PARRISH, Ph.D., State Geologist STATE OF CALIFORNIA THE NATURAL RESOURCES AGENCY DEPARTMENT OF CONSERVATION CALIFORNIA GEOLOGICAL SURVEY An Explanatory Text to Accompany the Fault Activity Map of California INTRODUCTION data for states adjacent to California (http://earthquake.usgs.gov/hazards/qfaults/). The The 2010 edition of the FAULT ACTIVTY MAP aligned seismicity and locations of Quaternary OF CALIFORNIA was prepared in recognition of the th volcanoes are not shown on the 2010 Fault Activity 150 Anniversary of the California Geological Map. -
3.7 Geological and Seismic Hazards
3.7 Geological and Seismic Hazards This section describes geologic and seismic conditions in the Hillcrest Station Area Specific Plan Planning Area (referred to throughout this section as “Planning Area”) to provide relevant background information of the physical characteristics of the Planning Area with respect to geologic hazards, soils, and seismic conditions. The following information is compiled from geologic maps and reports available from Contra Costa County, City of Antioch, the California Geological Survey (CGS; formerly California Divisions of Mines and Geology), the U.S. Geographical Survey (USGS), the United States Department of Agriculture (USDA) Natural Resources Conservation Service (NRCS), and the Association of Bay Area Governments (ABAG). ENVIRONMENTAL SETTING PHYSICAL SETTING Topography The Planning Area is located in northeastern Contra Costa County, on the northern flank of Mount Diablo at the southern edge of the Pittsburg-Antioch Plain. The Pittsburg-Antioch Plain is an alluvial plain that slopes gently north away from the base of the foothills of Mount Diablo to the tidal marshes of the Sacramento-San Joaquin Delta. The northern half of the alluvial plain is dominated by salt water marshes; the southern half is underlain by alluvial materials eroded from the Diablo Range to the south. With the exception of two hills adjacent to Highway 4 (SR 4), the Planning Area is a shallow valley bisected by East Antioch Creek, which meanders in a northwest direction across the site and empties into the San Joaquin River approximately 1.5 miles northwest of the site. The topography of the Planning Area varies from gentle slopes of 2-3 percent on the valley floor to 15-30 percent slopes on the hilly areas in the southeast. -
Page 1 of 145 P&O Committee Meeting March 2, 2015
MEETING OF THE BOARD OF DIRECTORS OF THE MUNICIPAL WATER DISTRICT OF ORANGE COUNTY Jointly with the PLANNING & OPERATIONS COMMITTEE March 2, 2015, 8:30 a.m. MWDOC Conference Room 101 P&O Committee: Staff: R. Hunter, K. Seckel, R. Bell, Director Osborne, Chair H. De La Torre, P. Meszaros, J. Berg Director Barbre Director Hinman Ex Officio Member: L. Dick MWDOC Committee meetings are noticed and held as joint meetings of the Committee and the entire Board of Directors and all members of the Board of Directors may attend and participate in the discussion. Each Committee has designated Committee members, and other members of the Board are designated alternate committee members. If less than a quorum of the full Board is in attendance, the Board meeting will be adjourned for lack of a quorum and the meeting will proceed as a meeting of the Committee with those Committee members and alternate members in attendance acting as the Committee. PUBLIC COMMENTS - Public comments on agenda items and items under the jurisdiction of the Committee should be made at this time. ITEMS RECEIVED TOO LATE TO BE AGENDIZED - Determine there is a need to take immediate action on item(s) and that the need for action came to the attention of the District subsequent to the posting of the Agenda. (Requires a unanimous vote of the Committee) ITEMS DISTRIBUTED TO THE BOARD LESS THAN 72 HOURS PRIOR TO MEETING -- Pursuant to Government Code section 54957.5, non-exempt public records that relate to open session agenda items and are distributed to a majority of the Board less than seventy-two (72) hours prior to the meeting will be available for public inspection in the lobby of the District’s business office located at 18700 Ward Street, Fountain Valley, California 92708, during regular business hours.