Type of Services Current Conditions Soils, Geology, and Geologic Hazards Envision San José 2040 General Plan Update
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1180 Main Street Project, Cultural Resources Inventory and Evaluation Report, Redwood City, San Mateo County, California
1180 Main Street Project, Cultural Resources Inventory and Evaluation Report, Redwood City, San Mateo County, California Prepared for: Premia Capital, LLC 801 Hamilton Street Redwood City, CA Prepared by: Stantec Consulting Services, Inc. January 18, 2019 1180 MAIN STREET PROJECT, CULTURAL RESOURCES INVENTORY AND EVALUATION REPORT, REDWOOD CITY, SAN MATEO COUNTY, CALIFORNIA This document entitled 1180 Main Street Project, Cultural Resources Inventory and Evaluation Report, Redwood City, San Mateo County, California was prepared by Stantec Inc. (“Stantec”) for the account of Premia Capital, LLC (the “Client”). Any reliance on this document by any third party is strictly prohibited. The material in it reflects Stantec’s professional judgment in light of the scope, schedule and other limitations stated in the document and in the contract between Stantec and the Client. The opinions in the document are based on conditions and information existing at the time the document was published and do not take into account any subsequent changes. In preparing the document, Stantec did not verify information supplied to it by others. Any use which a third party makes of this document is the responsibility of such third party. Such third party agrees that Stantec shall not be responsible for costs or damages of any kind, if any, suffered by it or any other third party as a result of decisions made or actions taken based on this document. Prepared by (signature) Joanne Grant, Archaeologist, MA, RPA Reviewed by (signature) John A. Nadolski, M.A. Approved -
5.4.5 Geological Hazards
Section 5.4.5: Risk Assessment – Geological Hazards 5.4.5 Geological Hazards The following section provides the hazard profile (hazard description, location, extent, previous occurrences and losses, probability of future occurrences, and impact of climate change) and vulnerability assessment for the geological hazards in Sussex County. 2016 Plan Update Changes The hazard profile has been significantly enhanced to include a detailed hazard description, location, extent, previous occurrences, probability of future occurrence, and potential change in climate and its impacts on the geological hazards is discussed. The geological hazards is now located in Section 5 of the plan update. It includes landslide, land subsidence and sinkholes, all of which were profiled separately in the 2011 HMP. New and updated figures from federal and state agencies are incorporated. U.S. 2010 Census data was incorporated, where appropriate. Previous occurrences were updated with events that occurred between 2008 and 2015. A vulnerability assessment was conducted for the geological hazards and it now directly follows the hazard profile. 5.4.5.1 Profile Hazard Description Geological hazards are any geological or hydrological processes that pose a threat to humans and natural properties. Every year, severe natural events destroy infrastructure and cause injuries and deaths. Geologic hazards may include volcanic eruptions and other geothermal related features, earthquakes, landslides and other slope failures, mudflows, sinkhole collapses, snow avalanches, flooding, glacial surges and outburst floods, tsunamis, and shoreline movements. For the purpose of this HMP update, only landslides and land subsidence/sinkholes will be discussed in the Geological Hazard profile. Landslides According to the U.S. -
Diocese of San Jose 2020 Directory
Diocese of San Jose 2020 Directory 1150 North First Street, Suite 100 San Jose, California 95112 Phone (408) 983-0100 www.dsj.org updated 10/8/2020 1 2 Table of Contents Diocese Page 5 Chancery Office Page 15 Deaneries Page 29 Churches Page 43 Schools Page 163 Clergy & Religious Page 169 Organizations Page 205 Appendix 1 Page A-1 Appendix 2 Page A-15 3 4 Pope Francis Bishop of Rome Jorge Mario Bergoglio was born in Buenos Aires, Argentina's capital city, on December 17, 1936. He studied and received a master's degree in chemistry at the University of Buenos Aires, but later decided to become a Jesuit priest and studied at the Jesuit seminary of Villa Devoto. He studied liberal arts in Santiago, Chile, and in 1960 earned a degree in philosophy from the Catholic University of Buenos Aires. Between 1964 and 1965 he was a teacher of literature and psychology at Inmaculada High School in the province of Santa Fe, and in 1966 he taught the same courses at the prestigious Colegio del Salvador in Buenos Aires. In 1967, he returned to his theological studies and was ordained a priest on December 13, 1969. After his perpetual profession as a Jesuit in 1973, he became master of novices at the Seminary of Villa Barilari in San Miguel. Later that same year, he was elected superior of the Jesuit province of Argentina and Uruguay. In 1980, he returned to San Miguel as a teacher at the Jesuit school, a job rarely taken by a former provincial superior. -
Coastal and Other Hazards (Se)
Goleta General Plan /Coastal Land Use Plan 5.0 Safety Element CHAPTER 5.0 SAFETY ELEMENT: COASTAL AND OTHER HAZARDS (SE) 5.1 INTRODUCTION General Plan Law Requirements [GP] The Safety Element is one of seven general Safety Element Policies plan elements mandated by state law. The SE 1: Safety in General scope of the Safety Element is specified in SE 2: Bluff Erosion and Retreat Section 65302 (g) of the California SE 3: Beach Erosion and Shoreline Hazards SE 4: Seismic and Seismically Induced Hazards Government Code as follows: SE 5: Soil and Slope Stability Hazards SE 6: Flood Hazards The general plan shall include a safety SE 7: Urban and Wildland Fire Hazards element for the protection of the SE 8: Oil and Gas Industry Hazards community from any unreasonable SE 9: Airport-Related Hazards. SE 10: Hazardous Materials and Facilities risks associated with the effects of SE 11: Emergency Preparedness seismically induced surface rupture, ground shaking, ground failure, tsunami, seiche, and dam failure; slope instability leading to mudslides and landslides; subsidence and other geologic hazards known to the legislative body; flooding; and wild land and urban fires. The safety element shall include mapping of known seismic and other geologic hazards. It shall also address evacuation routes, peak-load water supply requirements, and minimum road widths and clearances around structures, as those items relate to identified fire and geologic hazards. Coastal hazards such as bluff retreat and shoreline erosion are also addressed in this element, as are hazards associated with oil and gas production, processing, and transport. California Coastal Act Requirements [CP] The California Coastal Act (Coastal Act) requires new development to be sited and designed to minimize risks, ensure stability and structural integrity, and neither create nor contribute significantly to erosion or require the construction of new shoreline protective devices that would substantially alter natural landforms along coastal bluffs and cliffs. -
BAER) Assessment Specialist Report, Phase 2 – GEOLOGIC HAZARDS
Burned Area Emergency Response (BAER) Assessment Specialist Report, Phase 2 – GEOLOGIC HAZARDS Thomas Fire, Los Padres National Forest January 2018 Allen King – Geologist, Los Padres NF (retired) Dennis Veich – Forest Geologist, Shasta-Trinity NF Fire-damaged Tree near Chismahoo Mountain “When rain starts to fall, people in higher risk basins should be prepared to evacuate. Do not remain in, near or below burned areas at the base of canyons, even during light rain. Stay away from small streams that could become raging rivers in the blink of an eye. If the forecast calls for heavy rains through the night, homes may not be safe places if they are located in or near drainage areas and within a mile of the mountain front. Roads can suddenly become blocked with mud and debris, and can wash out at stream crossings. It is important to pay strong attention to warnings from local emergency responders and weather advisories.” -Sue Cannon, USGS Landslide Hazards Program, 2003 INTRODUCTION The Thomas Fire started on December 4, 2017, near the Thomas Aquinas College (east end of Sulphur Mountain), Ventura County, California. The fire is still considered to be active and as of January 12th, 2018, it is estimated to have burned 281,900 acres and is 92% contained. Approximately 181,300 acres within the burn area are National Forest lands (~64%); 98,200 acres are private (~35%); and 2,400 acres (~1%) are a combination of state and county properties. Although tremendous down-slope/down-drainage resources and values and lives are recognized and kept in mind during our analysis, this report addresses the effects of the Thomas Fire and the associated Values At Risk (VARs) ONLY on Forest Service lands, since the other lands are being evaluated by teams of Cal Fire scientists and other agencies. -
Seismic Design Guidelines Appendix B: Geotechnical
Mandatory Retrofit Program for Non-Ductile Concrete Buildings And Pre-Northridge Steel Moment Frame Buildings Ordinance 17-1011 SEISMIC DESIGN GUIDELINES APPENDIX B ISSUED NOVEMBER 8, 2019 REVISED SEPTEMBER 25, 2020 APPENDIX B: GEOTECHNICAL / GEOLOGICAL REPORT REQUIREMENTS 1.0 INTRODUCTION ASCE 41 geotechnical/geological report requirements for seismic evaluation and retrofit design varies greatly based on the amount of as-built information obtained and type of existing foundation system. The following document is intended to help clarify geotechnical / geological requirements of Ordinance 17-1011 for Non-Ductile Concrete and Pre-Northridge Steel Moment Frames. It is noted that all geotechnical / geological reports shall be signed and stamped by a California licensed Geotechnical Engineer and by a California licensed Geologist (if applicable). 2.0 SEISMIC SITE HAZARD The following frequently asked questions and answers are intended to clarify the scope and requirements of the seismic site hazard requirements of Ordinance 17-1011. 2.1 When is a site-specific seismic hazard determination required? A site-specific seismic hazard procedure is required when: a. The building is located on Site Class E soils and the mapped BSE-2N Sxs>2.0 or b. The building is located on Site Class F soils, unless Ss<0.20. In addition, a site-specific hazard is required to scale records when performing a non- linear dynamic time-history analysis. [Ref. ASCE 41 Section 2.4]. 2.2 When scaling a suite of acceleration records, is there a required or preferred scaling method? A site-specific response spectra shall be developed per ASCE 41 Section 2.4.2.1 requirements. -
Identification and Mitigation of Geologic Hazards
AIPGprofessional geologists in all specialties of the science Identification and Mitigation of Geologic Hazards An important and practical application of and because earthquakes geology is identifying hazardous natural are of such a scale that phenomena and isolating their causes in they can affect several order to safeguard communities. According communities si-multane- to the USGS, the average economic toll ously, the risk to human life from natural hazards in the United States is is obvious.2 The largest approximately $52 billion per year, while recorded earthquake to hit the average annual death toll is approxi- the North American conti- mately 200.1 The primary causes are nent had a magnitude of earthquakes, landslides, and flooding, but 9.2, which occurred on other events, such as subsidence, volcanic March 27, 1964 in eruptions, and exposure to radon or asbes- Anchorage, Alaska. It dev- tos, also pose considerable danger. astated the town and sur- Awareness of the potential hazards that rounding area, and could persist in areas under consideration for be felt over an area of half Figure 2. Volcano Zones both private and community development a million square miles.2 is critical, and so geological consultants Land-slides caused most of the average global temperature by 2 and engineers are called in to survey land the damage, while a 30-foot high tsunami degrees Fahrenheit for 2 years.3 development sites and assist building con- generated by an underwater quake leveled tractors in designing structures that will coastal villages around the Gulf of Alaska, The role of geologists in mitigating such stand the test of time. -
Salt and Nutrient Management Plan Santa Clara Subbasin This Page Is Intentionally Left Blank REVISED FINAL SALT and NUTRIENT MANAGEMENT PLAN: SANTA CLARA SUBBASIN
NOVEMBER 2014 Salt and Nutrient Management Plan Santa Clara Subbasin This page is intentionally left blank REVISED FINAL SALT AND NUTRIENT MANAGEMENT PLAN: SANTA CLARA SUBBASIN Originally posted online in November, 2014; Revised in June 2016 to add San Francisco Bay Regional Water Quality Control Board comments and Santa Clara Valley Water District responses ACKNOWLEDGMENTS PREPARED BY: Thomas Mohr, P.G., H.G. Senior Hydrogeologist UNDER THE DIRECTION OF: James Fielder Chief Operating Officer, Water Utility Enterprise Garth Hall Deputy Operating Officer Water Supply Division Behzad Ahmadi Unit Manager,Groundwater (retired) CONTRIBUTORS: Chanie Abuye, Civil Engineer Randy Behrens, Geologist Ellen Fostersmith, Geologist (retired) Ardy Ghoreishi, Engineering Technician Robert Siegfried, Soil Scientist (retired) Miguel Silva, Associate Civil Engineer Xiaoyong Zhan, Civil Engineer GRAPHICS DESIGN: Benjamin Apollo BOARD OF DIRECTORS: John L. Varela, District 1 Barbara Keegan, District 2 (Chair) Richard Santos, District 3 Linda J. LeZotte, District 4 Nai Hsueh, District 5 Tony Estremera, District 6 Gary Kremen, District 7 TABLE OF CONTENTS Page ACRONYMS ....................................................................................................................... x EXECUTIVE SUMMARY ............................................................................................................ 1 CHAPTER 1: INTRODUCTION AND BACKGROUND .............................................................. 5 1.1 Introduction .............................................................................................................. -
Geologic Hazards
Geologic Hazards CVEN 3698 Engineering Geology Definitions • A geologic hazard is one of several types of adverse geologic conditions capable of causing damage or loss of property and life (Wikipedia) • A geologic hazard shall mean a geologic condition or geologic process which poses a significant threat to health, life, limb, or property. (BC Land Use Department) • A geologic constraint shall mean a geologic condition which does not pose a significant threat to life or limb, but which can cause intolerable damage to structures (BC Land Use Department) • A geologic hazard is a natural geologic event that can endanger human lives and threaten human property. Earthquakes, geomagnetic storms, landslides, sinkholes, tsunamis, and volcanoes are all types of geologic hazards. The U.S. Geological Survey (USGS) provides real-time hazard information on earthquakes, landslides, geo-magnetics, and volcanoes, as well as background information on all the types of hazards. http://geohazards.cr.usgs.gov Counties and Municipalities in Colorado regulate geologic Hazards in four different ways • Master and Land Use Plans for land use patterns and development • Zoning Regulations • 1041 Regulations where hazardous areas are identified • Land Use or Subdivision Codes https://www.bouldercounty.org/departments/land-use/ http://coloradogeologicalsurvey.org/ https://assets.bouldercounty.org/wp-content/uploads/2017/06/cesare- geologic-hazard-study-boulder-county-20170331.pdf Front Range Geologic Hazards Field Trip: http://coloradogeologicalsurvey.org/wp-content/uploads/2013/08/6.pdf Two Types • Hazards associated with particular earth materials. Examples include swelling soils and rocks, toxic minerals (asbestos, acid drainage) and toxic gases (radon gas). • Hazards associated with earth processes (earthquakes, volcanoes, landslides, avalanches, rock slides and rock falls, soil creep, subsidence, floods, frost heave, coastal hazards). -
Southern Santa Cruz Mountains
33 3. Field Trip to Lexington Reservoir and Loma Prieta Peak Area in the Southern Santa Cruz Mountains Trip Highlights: San Andreas Rift Valley, Quaternary faults, Stay in the right lane and exit onto Alma Bridge Road. Follow landslide deposits, Franciscan Complex, serpentinite, stream Alma Bridge Road across Lexington Reservoir Dam and turn terrace deposits, Lomitas Fault, Sargent Fault, Cretaceous fos- right into the boat dock parking area about 0.6 mile (1 km) sils, deep-sea fan deposits, conglomerate from the exit on Highway 17 north. A Santa Clara County Parks day-use parking pass is required to park in the paved lot. This field trip examines faults, landslides, rocks, and The park day use pass is $5. Vehicles can be left here for the geologic features in the vicinity of the San Andreas Fault and day to allow car pooling (the park is patrolled, but as always, other faults in the central Santa Cruz Mountains in the vicinity take valuables with you). of both Lexington Reservoir and Loma Prieta Peak (fig. 3-1). Detailed geologic maps, cross sections, and descriptions The field trip begins at Lexington Reservoir Dam at the boat featuring bedrock geology, faults, and landslide information dock parking area. To get to Lexington Reservoir Dam, take useful for this field-trip area are available on-line at theUSGS Highway 17 south (toward Santa Cruz). Highway 17 enters San Francisco Bay Region Geology website [http://sfgeo. Los Gatos Creek Canyon about 3 miles (5 km) south of the wr.usgs.gov/]. McLaughlin and others (2001) have produced intersection of highways 85 and 17. -
Critical Habitat Designation Stress to Obtain Essential Nutrients Or Currently Aware of Any Federal Lands Water
Monday, October 16, 2000 Part II Department of the Interior Fish and Wildlife Service 50 CFR Part 17 Endangered and Threatened Wildlife and Plants; Proposed Designation of Critical Habitat for the Bay Checkerspot Butterfly (Euphydryas editha bayensis); Proposed Rule VerDate 11<MAY>2000 18:45 Oct 13, 2000 Jkt 194001 PO 00000 Frm 00001 Fmt 4717 Sfmt 4717 E:\FR\FM\16OCP2.SGM pfrm02 PsN: 16OCP2 61218 Federal Register / Vol. 65, No. 200 / Monday, October 16, 2000 / Proposed Rules DEPARTMENT OF THE INTERIOR (3) You may hand-deliver comments threatened bay checkerspot as occurring to our Sacramento Fish and Wildlife in San Francisco Bay area counties, Fish and Wildlife Service Office, U.S. Fish and Wildlife Service, notably the Counties of San Mateo and 2800 Cottage Way, Suite W 2605, Santa Clara. 50 CFR Part 17 Sacramento, California 95825. The bay checkerspot formerly Public Hearing: We will hold the occurred around San Francisco Bay, RIN 1018±AH61 Newark hearing at the Hilton Newark/ from Twin Peaks and San Bruno Endangered and Threatened Wildlife Fremont, 39900 Balentine Drive, Mountain (west of the Bay) and Contra and Plants; Proposed Designation of Newark, California. Costa County (east of the Bay) south Critical Habitat for the Bay Document Availability: Comments through Santa Clara County. Before the Checkerspot Butterfly (Euphydryas and materials received, as well as introduction of invasive Eurasian editha bayensis) supporting documentation used in the grasses and other weeds in the 1700s, its preparation of this proposed rule, will distribution may have been wider AGENCY: Fish and Wildlife Service, be available for public inspection, by (Service 1998). -
Geologic Hazards
3 | GEOLOGIC HAZARDS 3.1 | OVERVIEW Primary hazards Most, though not all, of the geologic hazards that present the threat of devastation to life and property are the direct or indirect result of ground movement due to earthquakes (see below). The primary, or direct, earthquake hazards are surface-fault rupture and ground shaking. Secondary hazards, associated with ground shaking, include several forms of ground failure and inundation. (Inundation hazards, which may or may not be associated with earthquakes, are discussed in Chapter 6, “Flooding Hazards.”) Ground failure is the permanent deformation of the ground due to its loss of strength or failure of the underlying materials during earthquake shaking, and includes liquefaction, landslides, mudslides, differential settlement and subsidence. The likelihood of occurrence of these secondary earthquake effects (with the exception of inundation) is generally high. The main geologic hazards include: ● Fault rupture or displacement: a sudden shifting of the ground along the trace of an earthquake fault; usually, but not always, occurs at the time of an earthquake, and is associated with stronger quakes. PROTECT OAKLAND ● Ground shaking: movement of the ground caused by the passage of seismic waves through the earth’s outer crust during an earthquake; it typically is strongest near the earthquake fault. Ground shaking is the most noticeable phenomenon of seismic activity and the one people associate most closely with earthquakes; it also represents the major hazard from an earthquake, in the form of damage to structures. The intensity of ground shaking at a particular site is affected by the characteristics of the earthquake, distance from the fault, and the characteristics of the underlying soil.