By Albert E. Roberts Open-File Report 81-260 This Report Is Preliminary
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Geology and Ground-Water Features of the Edison-Maricopa Area Kern County, California
Geology and Ground-Water Features of the Edison-Maricopa Area Kern County, California By P. R. WOOD and R. H. DALE GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1656 Prepared in cooperation with the California Department of Heater Resources UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library catalog card for tbis publication appears on page following tbe index. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract______________-_______----_-_._________________________ 1 Introduction._________________________________-----_------_-______ 3 The water probiem-________--------------------------------__- 3 Purpose of the investigation.___________________________________ 4 Scope and methods of study.___________________________________ 5 Location and general features of the area_________________________ 6 Previous investigations.________________________________________ 8 Acknowledgments. ____________________________________________ 9 Well-numbering system._______________________________________ 9 Geography ___________________________________________________ 11 Climate.__-________________-____-__------_-----_---_-_-_----_ 11 Physiography_..__________________-__-__-_-_-___-_---_-----_-_- 14 General features_________________________________________ 14 Sierra Nevada___________________________________________ 15 Tehachapi Mountains..---.________________________________ -
3D Geologic Modeling of the Southern San Joaquin Basin for the Westcarb Kimberlina Demonstration Project- a Status Report
LLNL-TR-412487 3D Geologic Modeling of the Southern San Joaquin Basin for the Westcarb Kimberlina Demonstration Project- A Status Report J. Wagoner April 24, 2009 Disclaimer This document was prepared as an account of work sponsored by an agency of the United States government. Neither the United States government nor Lawrence Livermore National Security, LLC, nor any of their employees makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States government or Lawrence Livermore National Security, LLC. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States government or Lawrence Livermore National Security, LLC, and shall not be used for advertising or product endorsement purposes. This work performed under the auspices of the U.S. Department of Energy by Lawrence Livermore National Laboratory under Contract DE-AC52-07NA27344. 3D Geologic Modeling of the Southern San Joaquin Basin for the Westcarb Kimberlina Demonstration Project- A Status Report Wagoner, Jeffrey L. Lawrence Livermore National Laboratory Atmospheric, Earth and Energy Division P.O. Box 808, Livermore, CA 94551 ABSTRACT The objective of the Westcarb Kimberlina pilot project is to safely inject 250,000 t CO2/yr for four years into the deep subsurface at the Clean Energy Systems (CES) Kimberlina power plant in southern San Joaquin Valley, California. -
Structural Evolution of the Russell Ranch Oil Field and Vicinity, Southern Coast Ranges, California
AN ABSTRACT OF THE THESIS OF Barbara B. Nevins for the degree of Master of Science in Geology presented on December 14, 1982 Title: STRUCTURAL EVOLUTION OF THE RUSSELL RANCH OIL FIELD AND VICINITY, SOUTHERN COAST RANCES-(ALIFORN Abstract approved: Signature redacted for privacy. ' D. Robert(SA Yeats The Russell Ranch oil field is located in the southern Coast Rangeswest ofBakersfield, California. Detailed subsurface mapping shows that a northwest-oriented right-lateral wrench-fault system was active from possibly latest Oligocene to Pliocene time. The effects of Quaternary thrusting were superimposed on, and in- fluenced by, structures associated with the older wrench tectonic regime. The right-lateral shear system produced a complex pattern of right-stepping en echelon folds, dip-slip faults with normal separation, and strike-slip faults with both normal and reverse separation. Deformation along the wrench system began during de- position of the late Oligocene-earlv Miocene Soda Lake Shale and Painted Rock Sandstone members of the Vaqueros Formation, pro- duciu elongate en echelon submarine troughs and highs. Northerly trending growth faults of early Miocene age caused thickening of the late Saucesian-early Relizian Saltos Shale Member of the MontereyFormation and mayhave initiated growth of the Russell Ranch anticline. Northeast- to northwest-trending normal faults and northwest-trending strike-slipfaults ofthe Russell fault system were active during deposition of a sequence tentatively correlated with the Branch Canyon Sandstone and Santa Margarita Formation of middle and late Miocene age. Strike-slip faulting produced a complex interleaving of fault slices and juxtaposed slices of contrasting lithologies and orientations. Subsequent minor movement along the wrench system folded the base of the Morales Formation, of PJ.iocene-Pleistocene age, into elongate en echelon folds. -
Abies Bracteata Revised 2011 1 Abies Bracteata (D. Don) Poit
Lead Forest: Los Padres National Forest Forest Service Endemic: No Abies bracteata (D. Don) Poit. (bristlecone fir) Known Potential Synonym: Abies venusta (Douglas ex Hook.) K. Koch; Pinus bracteata D. Don; Pinus venusta Douglas ex Hook (Tropicos 2011). Table 1. Legal or Protection Status (CNDDB 2011, CNPS 2011, and Other Sources). Federal Listing Status; State Heritage Rank California Rare Other Lists Listing Status Plant Rank None; None G2/S2.3 1B.3 USFS Sensitive Plant description: Abies bracteata (Pinaceae) (Fig. 1) is a perennial monoecious plant with trunks longer than 55 m and less than 1.3 m wide. The branches are more-or-less drooping, and the bark is thin. The twigs are glabrous, and the buds are 1-2.5 cm long, sharp-pointed, and non- resinous. The leaves are less than 6 cm long, are dark green, faintly grooved on their upper surfaces, and have tips that are sharply spiny. Seed cones are less than 9 cm long with stalks that are under15 mm long. The cones have bracts that are spreading, exserted, and that are 1.5–4.5 cm long with a slender spine at the apex. Taxonomy: Abies bracteata is a fir species and a member of the pine family (Pinaceae). Out of the fir species growing in North America (Griffin and Critchfield 1976), Abies bracteata has the smallest range and is the least abundant. Identification: Many features of A. bracteata can be used to distinguish this species from other conifers, including the sharp-tipped needles, thin bark, club-shaped crown, non-resinous buds, and exserted spine tipped bracts (Gymnosperms Database 2010). -
Official Program
Catch the Energy Wave!! 2015 Pacific Section AAPG Joint Annual Meeting May 3-5, 2015 Oxnard, CA Official Program CONTENTS Convention Schedule……………………………………………....…………....…………..……….... 02 Sponsors……..…………………………………………………………..…………….…………….…… 05 Letter from the PSAAPG President, John Williams……………………………………..………. 06 Letter from the Convention Chair, Joan Barminski………………..…………….…………….… 07 Officers and Convention Committee Pacific Section AAPG Officers………………………………………….….………….....……. 08 Coast Geological Society Officers…………………………………….……...……..………… 08 2015 Convention Committee…...…………………...…………………………………………. 08 Exhibitors…………………………………………………………………………………………….……. 09 General Information……………………………………………...……………………..………...…..... 12 The Area – Activities, Food, Fun……..………………………………..………..……………... 14 Speaker and Judge Information……………………………………………………………….. 19 Highlights…………………………………………………..………………………………..……………. 20 Breakfasts – Luncheons – Receptions……….……………..………..………..……….…….. 20 Student Q&A – Visiting Professional Geoscientists…………………..………..…………….. 23 Guest Events…………………......………….……………………………………………………...…… 24 Dinner Cruise……..………….……………………………………………………………...………...… 24 Geology Field Trips……..………….……………………………………………………………...…… 25 Teachers Workshop…….….……………………………..…..……………………….…………. 29 Short Courses….…………………….……………………..…..……………………….…………. 30 Technical Program – Oral Sessions – Monday, May 4..………………………………………. 33 Technical Program – Poster Sessions– Monday, May 4….……………………………………. 49 Technical Program – Oral Sessions– Tuesday, May 5..……………….……………………….. 59 Technical -
Cuyama Valley Groundwater Basin (3-13) Boundary Modification Request
CUYAMA VALLEY GROUNDWATER BASIN (3-13) BOUNDARY MODIFICATION REQUEST TECHNICAL MEMORANDUM April 3, 2018 Prepared for GRAPEVINE CAPITAL MANAGEMENT April 3, 2018 CLEATH-HARRIS GEOLOGISTS 71 Zaca Lane, Suite 140 San Luis Obispo, California 93401 (805) 543-1413 TABLE OF CONTENTS SECTION PAGE INTRODUCTION………………………………………………………………………………….1 DESCRIPTION OF PROPOSED BOUNDARY MODIFICATION (§ 344.6)…………….……...3 Overview of Request for Boundary Modification (§ 344.6(a))……………………………..……...3 Category of Proposed Boundary Modification (§ 344.6(a)(1))…………………………………….3 Identification of all Affected Basins or Subbasins (§ 344.6(a)(2))………………………………….3 Proposed name for each new subbasin (§ 344.6 (a)(3)…….…………….…………………………4 GENERAL INFORMATION (§344.10)…………………………………………………………...5 Description of lateral basin boundaries and definable bottom (§ 344.10(a))……………………….5 Graphical Map of lateral basin boundaries (§344.10 (b)).………………………………………….5 HYDROGEOLOGIC CONCEPTUAL MODEL (§ 344.12)……………………………………….6 Principal Aquifers and Regional Aquitard (§ 344.12(1))…………………………………………..6 Lateral Boundaries (§ 344.12(2))……………………………………………………………….......8 Geologic Features Impacting Groundwater Flow (§ 344.12(2)(A,B,C))…………………………...9 Key Surface Water Bodies and Significant Recharge Sources (§ 344.12(2)(D))…………………12 Recharge and Discharge Areas (§ 344.12(3)) …………………………………………………….12 Definable Bottom of the Basin (§ 344.12(4))……………………………………………………..13 TECHNICAL INFORMATION FOR SCIENTIFIC MODIFICATION (§ 344.14)……………...14 Qualified Map (§ 344.14(a)(1))…………………………………………………………………...14 Technical -
Analysis of Competing Hypotheses for the Tectonic Evolution of the Bakersfield Arch
ANALYSIS OF COMPETING HYPOTHESES FOR THE TECTONIC EVOLUTION OF THE BAKERSFIELD ARCH by Jefferson Vasconcellos A Thesis Submitted to the Department of Geology California State University Bakersfield In Partial Fulfillment for the Degree of Masters of Petroleum Geology Winter 2016 Copyright By Jefferson Vasconcellos 2016 ANALYSIS OF COMPETING HYPOTHESES FOR THE TECTONIC EVOLUTION OF THE BAKERSFIELD ARCH By Jefferson Vasconcellos This thesis has been accepted on behalf of the Department of Geology by their supervisory committee: ' uf~i::;e,~¥&'f: . Professor of Geology Committee Chair Robert Negrini, PhD Professor of Geology Dirk Baron, PhD Department Chair, Professor of Geology ABSTRACT The widespread presence of Neogene and Quaternary units in the southeastern San Joaquin Valley provide evidence for the tectonic evolution of the Bakersfield Arch, an area of major oil production in California. The purpose of this study is to test two different age hypotheses for the uplift of the Arch: middle Miocene and late Quaternary. Electric log correlations of stratigraphic marker units were used to create isochore maps of sedimentary packages of various ages across the Arch. These data indicate that changes in horizontal distribution and thickness of stratigraphic units across the Arch are influenced by two distinct uplift events in the area: 1) during middle to late Miocene time and 2) latest Miocene (post-Etchegoin Formation deposition) to Pleistocene time. Future work incorporating more detailed correlation of individual chert markers within the Monterey Formation would more closely define the exact timing of the earlier episode of uplift in the area. Age diagnostic data are insufficient to determine the time of onset of the later period of uplift. -
27-Prothero Et Al (Sharktooth Pmag).P65
Lucas et al., eds., 2008, Neogene Mammals. New Mexico Museum of Natural History and Science Bulletin 44. 357 MAGNETIC STRATIGRAPHY OF THE EARLY TO MIDDLE MIOCENE OLCESE SAND AND ROUND MOUNTAIN SILT, KERN COUNTY, CALIFORNIA DONALD R. PROTHERO1, FRANCISCO SANCHEZ1 AND LISA L. DENKE2 1 Dept. Geology, Occidental College, Los Angeles, CA 90041; 2 T.J. Cross Engineers, Inc., 200 New Stine Road, Suite 270, Bakersfield, CA 93309 Abstract—The Olcese Sand and Round Mountain Silt, northeast of Bakersfield, California, are famous for their marine fossils, especially for the vertebrates from the Sharktooth Hill bone bed. Their ages are thought to be early to middle Miocene. Magnetic samples were taken from the 70-m thick Nickel Cliff section of the Olcese Sand, and from two sections spanning 70 m of the Round Mountain Siltstone: one at Ernst Ranch and the other along Poso Creek-Round Mountain Road. The samples were demagnetized with both alternating field and thermal demagne- tization, and produced stable remanence that passed a reversal test. The Olcese Sand is mostly normal in polarity, except for short reversed magnetozones at the middle and top of the section. Based on strontium-isotope ages ranging from 16.9-17.6 Ma, Relizian benthic foraminifera, and a fission-track date of 15.7 ± 1.7 Ma, we correlate the upper member of the Olcese Sand with Chrons C5Cn2-C5Cn3 (16.1-16.6 Ma), or latest early Miocene. Most of the Round Mountain Silt is reversed in polarity except for the very base of the section, and a short normal magnetozone in the upper third. -
GEOLOGICAL SURVEY PROFESSIONAL PAPER 1245 Historical Surface Deformation Near Oildale, California
GEOLOGICAL SURVEY PROFESSIONAL PAPER 1245 Historical Surface Deformation near Oildale, California By ROBERT 0. CASTLE, JACK P. CHURCH, ROBERT F. YERKES, and JOHN C. MANNING GEOLOGICAL SURVEY PROFESSIONAL PAPER 1245 A description and analysis of continuing surface movements recognized along the east edge of the southern San Joaquin Valley UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Castle, Robert 0. Historical surface deformation near Oildale, California (Geological Survey Professional Paper 1245) Includes bibliographical references. Supt. of Docs, no.: I 19.16:1245. 1. Subsidences (Earth movements) California Oildale Region. I. Castle, Robert 0. II. Series: United States. Geological Survey. Professional Paper 1245. QE600.3.U6H57 1983 551.3 83-600205 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Page Abstract 1 Probable nature of the surface deformation Cont. Introduction 1 Development and general characteristics of the Kern Acknowledgments 1 River, Kern Front, Poso Creek, Mount Poso, and Geologic framework 2 Fruitvale oil fields - 15 Historical surface movements 3 Differential subsidence 30 Faulting 33 Faulting 3 Height changes 9 Surface movements attributable to tectonic activity 35 Height changes 35 Probable nature of the surface deformation 12 Surface deformation attributable to ground-water with Faulting 35 drawals 14 Conclusion 36 Subsidence 14 Supplemental data: An appraisal of compaction-induced subsid Faulting 15 ence in the central Bakersfield area 36 Surface movements attributable to oil-field operations 15 References cited 40 ILLUSTRATIONS PLATE 1. -
The Purpose of This Paper Is to Present The
D R Paso Robles Groundwater Basin Water Banking Feasibility Study A Description of Water Banking Alternatives F San Luis Obispo County Flood Control And Water Conservation District Date: June 2007 Project No: 064030 T PASO ROBLES GROUNDWATER BASIN WATER BANKING FEASIBILITY STUDY DESCRIPTION OF WATER BANKING ALTERNATIVES Introduction The Paso Robles Groundwater Basin (Basin) located in northern San Luis Obispo County (County) is one of the largest groundwater basins in the County (Figure 1). The Coastal Branch of the California State Water Project (SWP) enters the County and the Central Coast just east of the Basin near the town of Shandon and continues southwest across the Basin. These two features along with the County’s unused allocation of SWP water led local water leaders to want to explore the feasibility of banking water in the Basin for the D benefit of County residents. This Description of Water Banking Alternatives summarizes information used to develop the water banking alternatives that are to be evaluated in the Paso Robles Groundwater Basin Water Banking Feasibility Study (Feasibility Study) and provides members of the Groundwater Banking Subcommittee (GBSC), Water Resources Advisory Committee (WRAC), Shandon Advisory Committee (SAC), and other interested parties an R opportunity to review and comment on the alternatives prior to completing the technical analysis. This work was completed by the project team, which was lead by GEI Consultants, Inc. with hydrogeologic support by Fugro West and Cleath & Associates. Project Background The Water Banking Feasibility Study for the Paso Robles Groundwater Basin is being led by the San Luis Obispo County Flood Control and Water Conservation District (District) A in coordination with the GBSC of the WRAC. -
Salt/Nutrient Management Plan for Paso Robles Groundwater Basin
Salt/Nutrient Management Plan for the Paso Robles Groundwater Basin MAY 2015 Salt/Nutrient Management Plan for the Paso Robles Groundwater Basin Final Report Prepared by: May 2015 Paso Robles Salt / Nutrient Management Plan Table of Contents This page intentionally left blank. May 2015 Paso Robles Salt / Nutrient Management Plan Table of Contents Table of Contents Executive Summary .............................................................................................................. ES-1 ES-1 Introduction ........................................................................................................ ES-1 ES-2 Outreach ............................................................................................................. ES-2 ES-3 Basin Characterization ...................................................................................... ES-3 ES-4 Existing and Foreseeable Salt and Nutrient Sources ..................................... ES-6 ES-5 Assimilative Capacity and Anti-Degradation Analysis ................................. ES-11 ES-6 Implementation Measures, Goals & Objectives ............................................ ES-13 ES-7 Salt and Nutrient Groundwater Quality Monitoring Program ....................... ES-16 Chapter 1 Introduction ........................................................................................................... 1-1 1.1 Regulatory Framework ............................................................................................ 1-1 1.2 Purpose of the SNMP ............................................................................................ -
Special Joint Meeting of Cuyama Basin Groundwater Sustainability Agency Board of Directors and the Standing Advisory Committee
Special Joint Meeting of Cuyama Basin Groundwater Sustainability Agency Board of Directors and the Standing Advisory Committee Board of Directors Derek Yurosek Chairperson, Cuyama Basin Water District Paul Chounet Cuyama Community Services District Lynn Compton Vice Chairperson, County of San Luis Obispo George Cappello Cuyama Basin Water District Das Williams Santa Barbara County Water Agency Byron Albano Cuyama Basin Water District Cory Bantilan Santa Barbara County Water Agency Jane Wooster Cuyama Basin Water District Glenn Shephard County of Ventura Tom Bracken Cuyama Basin Water District David Couch County of Kern Standing Advisory Committee Roberta Jaffe Chairperson Brenton Kelly Vice Chair Brad DeBranch Louise Draucker Jake Furstenfeld Mike Post Joe Haslett Agenda March 7, 2018 NOTE: The Special Joint meeting of the Cuyama Basin Groundwater Sustainability Agency Board and Standing Advisory Committee will begin at 2 pm. Public workshops are expected to begin at approximately 4 pm in English, and 6:30 pm in Spanish. The workshops are for the benefit of interested members of the public and will continue in the event Board or Committee members depart and there is no longer a quorum, and one or both of those meetings are adjourned. Workshop materials will be provided at the meetings. Agenda for a meeting of the Cuyama Basin Groundwater Sustainability Agency Board of Directors and Standing Advisory Committee to be held on Wednesday, March 7, 2018 at 2:00 PM, at the Cuyama Valley Family Resource Center, 4689 CA- 166, New Cuyama, CA 93254. To hear the session live call (888) 222-0475 Code 6375195#. The order in which agenda items are discussed may be changed to accommodate scheduling or other needs of the Board or Committee, the public, or meeting participants.