Strand Ranch Integrated Banking Project FEIR
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Newsletter of the Biological Survey of Canada
Newsletter of the Biological Survey of Canada Vol. 40(1) Summer 2021 The Newsletter of the BSC is published twice a year by the In this issue Biological Survey of Canada, an incorporated not-for-profit From the editor’s desk............2 group devoted to promoting biodiversity science in Canada. Membership..........................3 President’s report...................4 BSC Facebook & Twitter...........5 Reminder: 2021 AGM Contributing to the BSC The Annual General Meeting will be held on June 23, 2021 Newsletter............................5 Reminder: 2021 AGM..............6 Request for specimens: ........6 Feature Articles: Student Corner 1. City Nature Challenge Bioblitz Shawn Abraham: New Student 2021-The view from 53.5 °N, Liaison for the BSC..........................7 by Greg Pohl......................14 Mayflies (mainlyHexagenia sp., Ephemeroptera: Ephemeridae): an 2. Arthropod Survey at Fort Ellice, MB important food source for adult by Robert E. Wrigley & colleagues walleye in NW Ontario lakes, by A. ................................................18 Ricker-Held & D.Beresford................8 Project Updates New book on Staphylinids published Student Corner by J. Klimaszewski & colleagues......11 New Student Liaison: Assessment of Chironomidae (Dip- Shawn Abraham .............................7 tera) of Far Northern Ontario by A. Namayandeh & D. Beresford.......11 Mayflies (mainlyHexagenia sp., Ephemerop- New Project tera: Ephemeridae): an important food source Help GloWorm document the distribu- for adult walleye in NW Ontario lakes, tion & status of native earthworms in by A. Ricker-Held & D.Beresford................8 Canada, by H.Proctor & colleagues...12 Feature Articles 1. City Nature Challenge Bioblitz Tales from the Field: Take me to the River, by Todd Lawton ............................26 2021-The view from 53.5 °N, by Greg Pohl..............................14 2. -
Table of Contents Page
BIOLOGICAL RECONNAISSANCE SURVEY FOR WOODVILLE PUBLIC UTILITY DISTRICT’S WATER WELL REPLACEMENT PROJECT ( NEAR WOODVILLE, TULARE COUNTY, CALIFORNIA ) Prepared for Woodville Public Utility District P.O. Box 4567 16716 Avenue 168 Woodville, CA 93258 (559) 686-9649 September 2019 Prepared by HALSTEAD & ASSOCIATES Environmental / Biological Consultants 296 Burgan Avenue, Clovis, CA 93611 Office (559) 298-2334; Mobile (559) 970-2875 Fax (559) 322-0769; [email protected] Table of Contents Page 1. Summary ..............................................................................................................................1 2. Background ..........................................................................................................................2 3. Project Location ...................................................................................................................2 4. Project Description...............................................................................................................2 5. Project Site Description .......................................................................................................2 6. Regulatory Overview ...........................................................................................................3 7. Survey Methods ...................................................................................................................7 8. Wildlife Resources in the Project Area ................................................................................8 -
Internal Deformation of the Southern Sierra Nevada Microplate Associated with Foundering Lower Lithosphere, California
Geodynamics and Consequences of Lithospheric Removal in the Sierra Nevada, California themed issue Internal deformation of the southern Sierra Nevada microplate associated with foundering lower lithosphere, California Jeffrey Unruh1, Egill Hauksson2, and Craig H. Jones3 1Lettis Consultants International, Inc., 1981 North Broadway, Suite 330, Walnut Creek, California 94596, USA 2Seismological Laboratory, California Institute of Technology, Pasadena, California 91125, USA 3Department of Geological Sciences and CIRES (Cooperative Institute for Research in Environmental Sciences), CB 399, University of Colorado Boulder, Boulder, Colorado 80309-0399, USA ABSTRACT here represents westward encroachment of Sierra Nevada east of the Isabella anomaly. The dextral shear into the microplate from the seismicity represents internal deformation of the Quaternary faulting and background eastern California shear zone and southern Sierra Nevada microplate, a large area of central seismicity in the southern Sierra Nevada Walker Lane belt. The strain rotation may and northern California that moves ~13 mm/yr microplate are concentrated east and south refl ect the presence of local stresses associated to the northwest relative to stable North Amer- of the Isabella anomaly, a high-velocity body with relaxation of subsidence in the vicinity ica as an independent and nominally rigid block in the upper mantle interpreted to be lower of the Isabella anomaly. Westward propaga- (Argus and Gordon, 1991, 2001). At the latitude Sierra lithosphere that is foundering into the tion of foundering lithosphere, with spatially of the Isabella anomaly, the majority of micro- astheno sphere. We analyzed seismicity in this associated patterns of upper crustal deforma- plate translation is accommodated by mixed region to evaluate patterns of upper crustal tion similar to those documented herein, can strike-slip and normal faulting in the southern deformation above and adjacent to the Isa- account for observed late Cenozoic time- and Walker Lane belt (Fig. -
Catálogo Taxonómico-Geográfico De Los Coleópteros De La Familia Meloidae De México
Graellsia, 63(2): 165-258 (2007) CATÁLOGO TAXONÓMICO-GEOGRÁFICO DE LOS COLEÓPTEROS DE LA FAMILIA MELOIDAE DE MÉXICO M. García-París1, D. Buckley1,3 y G. Parra-Olea2 RESUMEN Se presenta un catálogo taxonómico de los representantes mexicanos de la familia Meloidae que incluye un listado revisado de sinonimias, localidades típicas y registros geográficos publicados de cada una de las especies. La fauna mexicana incluye en la actualidad 255 especies vivientes y una fósil, distribuidas en 21 géneros de las subfami- lias Meloinae, Nemognathinae y Tetraonycinae. En el último catálogo general, Black- welder (1945) recogió la presencia en México de 160 especies de esta familia, casi 100 especies menos de las que se conocen en la actualidad y sin embargo, la cifra actual pare- ce encontrarse aún lejos de la real, ya que existen muchas especies ampliamente distri- buidas al norte de la frontera con los Estados Unidos cuya presencia es muy probable en territorio mexicano. En cuanto a la taxonomía y nomenclatura de las especies, en este catálogo se propo- ne el uso de los nombres Epicauta dugesi Werner, 1957 y Tegrodera erosa extincta Beauregard, 1890; se incluyen tres sinonimias nuevas de Nemognatha chrysomeloides (Linnaeus, 1763) (N. atra Beauregard, 1890; N. pallidicollis Beauregard, 1890 y N. vio- lacea Beauregard, 1890) y otra de E. dugesi (Epicauta tamara Adams & Selander, 1979); se designa lectotipo para Lytta koltzei var. minor Haag-Rutenberg, 1880 con el propósito de solucionar el problema taxonómico generado tras la designación inválida de lectotipo de L. k. var. cyanescens; y finalmente se consideran como especies posible- mente a excluir del listado de Meloidae de México a Cissites maculata (Swederus, 1787) y Tetraonyx (Tetraonyx) bimaculatus (Klug, 1825). -
Marilyn P. Maccabe, Editor U.S. Geological Survey 345 Middlefield
EARTHQUAKE HAZARDS REDUCTION PROGRAM PROJECT SUMMARIES - 1979-80 Marilyn P. MacCabe, Editor U.S. Geological Survey 345 Middlefield Road Menlo Park, California 94025 Open-File Report 81-41 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey standards Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS CONTENTS Introduction ........................... 1 Highlights of Major Accomplishments .................. 2 Earthquake Hazards ....................... 2 Earthquake Prediction ...................... 5 Global Seismology ........................ 7 Induced Seismicity ........................ 9 Project Summaries .......................... 10 Earthquake Hazards Studies .................... 10 Earthquake potential ..................... 10 Tectonic framework, Quaternary geology, and active faults . 10 California ...................... 10 Western U.S. (excluding California) ........... 21 Eastern U.S. ..................... 31 National ...................... 34 Earthquake recurrence and age dating .............. 35 Earthquake effects ...................... 41 Ground Motion .............. ....... 41 Ground failure ...................... 51 Surface faulting ..................... 54 Post-earthquake studies .................. 55 Earthquake losses ...................... 55 Transfer of Research Findings ................. 56 Earthquake Prediction Studies ................... 57 Location of areas where large earthquake are most likely to occur . 57 Syntheses of seismicity, -
Geomorphic Constraints on the Evolution of the Kern Gorge, Southern Sierra Nevada
Geomorphic constraints on the evolution of the Kern Gorge, southern Sierra Nevada, California By Blake C. Foreshee A Thesis Submitted to the Department of Geological Sciences, California State University Bakersfield In Partial Fulfillment for the Degree of Masters of Geology Summer 2017 Copyright By Blake C. Foreshee 2017 Geom(Jrpbh; Con:!tlrainls on lb t- E,·ulut1oo or4.1 1¢ F<c1·n Go•·ge, Southern Sien-a Nevada, Caljfornia By Blake Foreshee Thi10 thesis has bt!eo a&<:ept.ed uo behalf or UlC Dcp;:u·tmcnl of Geological Sciences by their supervisor}' t:OII'imi u;ee: ~v~---- Dr. W1lh<~m C. Krugh A sst~ Ian t. Prn rr.s ~or of Gr.ology, Cfl lit"orn [a St>lt e lJ n i \' er~ity, Haker;;fie:u Commi:tcc Chclir' Pmfc.<Sod :~.:' Univmity, lli<ke,ftdd Ur. Acl<~m ~ u :\ s ~ i st<mt l'rofessor of Geology, Cal ifumla SWt.tl Un iVCl'Si t~r. Ra l<ersfi el d ACKNOWLEDGEMENTS I want to thank, first and foremost, my advisor and committee chair Dr. William C. Krugh for guiding and mentoring me through this thesis project. Thank you for leading me through an intriguing investigation of the Sierra Nevada and for expressing passion and enthusiasm throughout the duration of this work. I am grateful for my committee members Dr. Adam Guo and Dr. Anthony Rathburnfor providing constructive support and feedback during this project. Thank you Dr. Greg Wilkerson for taking time out of your schedule to go into the field and show me around the lower Kern River. -
Air Photo Lineaments, Southern Sierra Nevada, California
DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Air photo lineaments, southern Sierra Nevada, California by Donald C. Ross1 Open-File Report 89-365 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, firm, or product names is for descriptive purposes only and does not imply endorsement by the U. S. Government. 'Menlo Park, California 1989 CONTENTS Page Introduction .................................................................................................................................... i Discussion .................................................................................................................................... 2 Air photo lineaments along known faults.............................................................................. 2 San Andreas and Garlock faults................................................................................. 2 Kern Canyon-Breckenridge-White Wolf fault zone.................................................. 2 Durmc>c>d fault?.........7...:............... 2 Pinyon Peak fault....................................................................................................... 4 Jawbone fault............................................................................................................. 4 Sierra Nevada fault.................................................................................................... 4 Kern River fault........................................................................................................ -
North Bay Vital Signs
North Bay Vital Signs An Integrated Ecosystem-Climate Monitoring Framework for Sonoma County Lisa Micheli (Pepperwood) and Deanne DiPietro (Point Blue Conservation Science) Co-chairs, North Bay Climate Adaptation Initiative (NBCAI) Science Working Group A report prepared for Community Foundation Sonoma County December 2013 A product of the North Bay Climate Adaptation Initiative www.northbayclimate.org NBCAI’s North Bay Vital Signs December 2013 North Bay Vital Signs: an Integrated Ecosystem-Climate Monitoring Framework for Sonoma County Lisa Micheli (Pepperwood) and Deanne DiPietro (Point Blue Conservation Science) Co-chairs, North Bay Climate Adaptation Initiative (NBCAI) Science Working Group A report prepared for Community Foundation Sonoma County, December 2013 1. Executive Summary This report summarizes the North Bay Climate Adaptation Initiative (NBCAI)’s progress towards designing and implementing a Sonoma County-wide network capable of detecting local changes in climate and biodiversity, and of feeding into regional, state and national networks designed to support natural resource management decision- making at multiple scales. The strategy outlined here advances the following NBCAI Vital Signs objectives. o To maximize the input of advising technical experts on an indicator framework o To utilize protected lands as potential “hubs” of an integrated climate-biota monitoring network o To establish a sustainable, long-term set of combined climate-hydrology-biology measuring stations o To define data structure, collection protocols, stewardship, statistics, sharing, and reporting needed to regularly assess the status of key climate-ecosystem indicators o To explore the appropriate role of citizen scientists o To assess the feasibility of monitoring implementation recommendations with voluntarily participating conservation land managers NBCAI’s science working group has accomplished the following first steps towards these objectives, as described in more detail in this report. -
21St Century Dam Design — Advances and Adaptations
United States Society on Dams 21st Century Dam Design — Advances and Adaptations 31st Annual USSD Conference San Diego, California, April 11-15, 2011 CONTENTS Plenary Session Managing Multiple Priorities: Raising a Dam, Operating a Reservoir, and Coordinating a System of Projects ............................1 Kelly Rodgers and Gerald E. Reed III, San Diego County Water Authority; Rosalva Morales and Yana Balotsky, City of San Diego; Thomas O. Keller, GEI Consultants, Inc.; and Kevin N. Davis, Black & Veatch Corporation Partnering with Project Stakeholders at the San Vicente Dam Raise...........3 Thomas C. Haid, Parsons/Black & Veatch JV; Gerald E. Reed III, Vic Bianes and Kelly Rodgers, San Diego County Water Authority; and William A. Corn, Shimmick Construction Company Managing Unexpected Endangered Species Issues on Bid-Ready Projects........5 Anita M. Hayworth, Dudek; Mary Putnam, San Diego County Water Authority; and Douglas Gettinger, Jeffrey D. Priest and Paul M. Lemons, Dudek Planning and Cost Reduction Considerations for RCC Dam Construction........7 Adam Zagorski, Shimmick/Obayashi JV; and Mike Pauletto, M. Pauletto and Associates Ten Years After the World Commission on Dams Report: Where Are We?........9 Manoshree Sundaram, Federal Energy Regulatory Commission Australian Risk Approach for Assessment of Dams ...................11 M. Barker, GHD The Relative Health of the Dams and Reservoirs Market ................13 Del A. Shannon, ASI Constructors, Inc. Design of the Dams of the Panama Canal Expansion ..................15 Lelio Mejia, John Roadifer and Mike Forrest, URS Corporation; and Antonio Abrego and Maximiliano De Puy, Autoridad del Canal de Panama Concrete Dams: Advances in Analysis Myponga Dam Stability Evaluation: Modeling Stress Relaxation for Arch Dams Using Linear Finite Element Analysis ..........................17 Scott L. -
Late Cenozoic Structure and Tectonics of the Southern Sierra Nevada–San Joaquin Basin Transition, California
Research Paper GEOSPHERE Late Cenozoic structure and tectonics of the southern Sierra Nevada–San Joaquin Basin transition, California GEOSPHERE, v. 15, no. 4 Jason Saleeby and Zorka Saleeby Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA https://doi.org/10.1130/GES02052.1 ■ ABSTRACT the San Joaquin Basin is widely known for its Neogene deep-marine condi- 17 figures; 3 tables; 1 set of supplemental files tions that produced prolific hydrocarbon reserves (Hoots et al., 1954). Rarely This paper presents a new synthesis for the late Cenozoic tectonic, paleogeo- in the literature are the late Cenozoic geologic features of these two adjacent CORRESPONDENCE: [email protected] graphic, and geomorphologic evolution of the southern Sierra Nevada and adja- regions discussed in any depth together. The late Cenozoic features of these cent eastern San Joaquin Basin. The southern Sierra Nevada and San Joaquin Ba- two regions speak to a number of significant issues in tectonics and geomor- CITATION: Saleeby, J., and Saleeby, Z., 2019, Late Cenozoic structure and tectonics of the southern Si- sin contrast sharply, with the former constituting high-relief basement exposures phology. These include: (1) the Earth’s surface responses to geologically rapid erra Nevada–San Joaquin Basin transition, Califor- and the latter constituting a Neogene marine basin with superposed low-relief changes in the distribution of mantle lithosphere loads; (2) the stability of nia: Geosphere, v. 15, no. 4, p. 1164–1205, https:// uplifts actively forming along its margins. Nevertheless, we show that Neogene cover strata–basement transition zones and the time scales over which pro- doi .org /10.1130 /GES02052.1. -
4.6 Geologic and Seismic Hazards
METROPOLITAN BAKERSFIELD METROPOLITAN BAKERSFIELD GENERAL PLAN UPDATE EIR 4.6 GEOLOGIC AND SEISMIC HAZARDS The purpose of this Section is to describe the geologic and seismic setting of the Bakersfield Metropolitan area, identify potential impacts associated with implementation of the General Plan Update, reference General Plan goals, policies, and standards, and, where necessary, recommends mitigation measures to reduce the significance of impacts. The issues addressed in this section include risks associated with: faults, strong seismic ground shaking, seismic related ground failure such as liquefaction, landslides, and unstable geologic units and/or soils. ENVIRONMENTAL SETTING GEOLOGY Geologic Structure The Metropolitan Bakersfield area is a part of the Great Valley Geomorphic Province of California which is an alluvial plain, about 50 miles wide and 400 miles long, between the Coast Ranges and Sierra Nevada. The Great Valley is drained by the Sacramento and San Joaquin rivers, which join and enter San Francisco Bay. The southern part of the Great Valley is the San Joaquin Valley. The Valley is a northwesterly trending trough (geocycline) filled with immense thickness of sediments (estimated at 40,000 feet at the axis) deposited from surrounding mountains. Streams flowing westerly from the Sierra Nevada have eroded and deposited materials into the trough, forming alluvial fans at the surface. The largest of these in the Plan area is the Kern River fan, covering about 300 square miles of the valley and made up of sand, silt and clay deposits. The Kern River flood plain is incised into the upper part of the fan, north of downtown Bakersfield, and spread out across the broad, flat lower fan to the southwest. -
2011 SCEC Report Implementing a Statewide Community Fault Model in Coordination with UCERF3 and the USGS/CGS Q-Fault Database
2011 SCEC Report Implementing a Statewide Community Fault Model in coordination with UCERF3 and the USGS/CGS Q-fault database Principal Investigator: John H. Shaw Professor of Structural & Economic Geology Harvard University Dept. of Earth & Planetary Sciences 20 Oxford St., Cambridge, MA 02138 [email protected] //(617) 495-8008 co-Investigator: Andreas Plesch (Harvard) Proposal Categories: A: Data gathering and products Primary Focus Area: USR Primary Discipline Group: Geology Science Objectives: C, A4, A3 Summary In the past year, we developed new, substantially enhanced versions of the SCEC Community Fault (CFM) and Statewide Community Fault (SCFM) Models in collaboration with Craig Nicholson (UCSB). The models were improved by updating fault representations using more precise fault traces and relocated seismicity, with an emphasis on refining fault geometry and segmentation along the San Andreas and San Jacinto fault systems. We also developed more than 70 new fault representations in northern California. These new models are currently being evaluated by the SCEC community and will serve as a basis for the Uniform California Earthquake Rupture Forecast (UCERF 3) working group efforts. Finally, we developed a new nomenclature system for the CFM that is more informative and consistent with the USGS Qfault database, enabling users to access and combine fault information more readily. Updates to the SCEC CFM (southern California) The SCEC Community Fault Model (CFM 4.0) includes more than 150 fault representations in southern California that are based on surface exposures, seismicity, seismic reflection profiles, well data, and other types of information. At the outset of the effort to develop the CFM, the fault trace map of Jennings (1994) was chosen as the primary database for defining surface fault traces, due to its widespread use in hazard assessment efforts.