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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. -
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. -
U. S. Department of the Interior U. S. Geological Survey
U. S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Estimates of ultimate recovery of oil from California's giant fields (> 100 million barrels), 1923-1995 by Marilyn E. Tennyson1 Open-File Report 98-513-A 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. !U. S. Geological Survey MS 939 Box 25046 DFC Denver, CO 80225 1998 INTRODUCTION In 1995, an assessment of the petroleum resources of the United States, including both discovered and undiscovered oil and gas as well as unconventional resources, was completed by the U. S. Geological Survey (Gautier and others, 1995; U. S. Geological Survey National Oil and Gas Resource Assessment Team, 1995). On the basis of observed growth patterns in estimated sizes of oil and gas fields in the Nation, compiled by the Energy Information Administration for the period 1977 to 1991, the assessment team concluded that growth of reserves in already-discovered oil accumulations would account for far more future production than would petroleum in fields yet to be discovered. The volume of oil and gas that a newly discovered field is estimated to contain is often significantly smaller than the amount the field actually produces after it has been fully developed and secondary recovery techniques have been applied. A widely assumed model holds that a field grows rapidly in the first decade or two after discovery and then grows at a generally decreasing rate, eventually reaching an "ultimate" volume. -
United States Department of the Interior Bureau of Land Management Bakersfield Field Office
United States Department of the Interior Bureau of Land Management Bakersfield Field Office Environmental Assessment Vintage Production LLC. Mount Poso; Six APDs for Wells Sarrett Fee 1113LVH, 1114TVH, 1115LVH & 1116FVH and Matthew Fee 1107LVH & 1108LVH DOI-BLM-CA-C060-2016-0004-EA Programmatic Project #828 Chapter 1. Purpose and Need PURPOSE AND NEED Bureau of Land Management (BLM) proposes to approve six (6) Applications for Permit to Drill (APDs) submitted by Vintage Production California LLC. (Vintage) to drill 6 new oil wells: Sarrett Fee 1113LVH, 1114TVH, 1115LVH & 1116FVH and Matthew Fee 1107LVH & 1108LVH on Vintage’s federal mineral lease (CAS019301C) in Section 4, T27S, R28E, MDBM. This project is sited on private land owned by Vintage, containing BLM administered subsurface minerals within the Mount Poso Oil Field. The proposed project is located northeast of Bakersfield, California, in Kern County. The proposed well pad sites are accessed by a series of unpaved roads off Famoso Road. The drilling of 6 new wells would require the expansion of current well pads onto previously disturbed and undisturbed locations. Vintage would also install fourteen (14) power poles, eleven (11) anchors, and six (6) new flowlines that total 4,900 feet. In addition, the project would require construction of permanent access roads. Estimated surface disturbance for the proposed project is 2.993 acres, which would total 6.144 acres of compensation as required by the BLM Bakersfield Field Office 2001 Oil and Gas Programmatic Biological Opinion. The purpose of the proposed action is to provide Vintage with the authority to drill 6 new oil wells and associated facilities to produce its federal mineral lease (CAS019301C) and to supply energy resources to the American public. -
By Albert E. Roberts Open-File Report 81-260 This Report Is Preliminary
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY PHOSPHATIC ROCK LOCALITIES IN CALIFORNIA by Albert E. Roberts Open-File Report 81-260 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Introduction California, a leading agricultural state, needs an ever increasing amount of phosphorus, an essential element for plant growth, to improve crop yields. Current requirements for phosphorus are met by imports or as by products from other industry, such as phosphoric acid from Searles Lake brines. Marine phosphatic-rocks are distributed throughout the world with a stratigraphic range of Pre-Cambrian to Quaternary age. Marine phosphatic- rocks in California are presently known in sedimentary sequences that range from Ordovician to Quaternary; however, no significant economic deposits have yet been developed. Current geologic information indicates the highest potential is in the widespread phc>sphatic-rocks in formations of Miocene age. Stratigraphic units in which the principal deposits occur are the Santos Shale Member of the Temblor Formation (Lower Miocene) in the Temblor Range; Sandholdt Member of the Monterey Formation (Middle Miocene) in the Santa Lucia and La Panza Ranges; and phosphatic members of the Santa Margarita Formation (Upper Miocene) in the Sierra Madre and San Rafael Mountains. This preliminary map was compiled as a part of the U.S. Geological Survey's program to evaluate the phosphate resources of the United States. This map was prepared to summarize known localities and provide planning for future onsite field studies; to identify phosphate-bearing lands relative to federal leasing programs; and to encourage field examination and reporting of additional phosphate information by other researchers. -
Jefferson Vasconcellos
Copyright By Jefferson Vasconcellos 2016 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 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. -
United States Department of the Interior Bureau of Land Management Bakersfield Field Office
United States Department of the Interior Bureau of Land Management Bakersfield Field Office Environmental Assessment California Resources Production Corporation Mount Poso; One APD for Glide 1009V DOI-BLM-CA-C060-2019-0125-EA Programmatic Project #71 Chapter 1. Purpose and Need PURPOSE AND NEED Bureau of Land Management (BLM) proposes to approve one (1) Applications for Permit to Drill (APDs) submitted by California Resources Production Corporation (CRPC) to drill Well Glide 1009V on federal mineral leases CACA053785 located in Section 15, T27S, R28E, MDBM. The proposed project would occur on private lands containing subsurface minerals administered by the BLM in the Mount Poso Oilfield. The proposed new well is primarily staked on an existing, previously disturbed location. Access for the proposed well pad location is by existing dirt roadways located on the north and southwest side of the proposed pad. Grading and leveling of the project area will impact a small area of habitat, resulting in an estimated 0.01 acres of permanent disturbance and 0.08 acres of temporary disturbance. In addition, three new power poles will be installed on previously disturbed surfaces, as well as an associated new 3- inch production line of approximately 298-feet long that will tie into the Glide-Security Header 2. The pipeline will be installed on previously disturbed surfaces. Therefore, no new disturbance will result from power poles or flowline installation. Estimated disturbance for the project is 0.090 acres, requiring a total of 0.118 acres of compensation to meet conditions of the 2017 Oil and Gas Programmatic Biological Opinion (08ESMF00-2016-F-0683). -
Depositional Environment of the Basal Etchegoin Formation
Copyright By Carol Leigh Beahm 2015 Depositional Environment of the Basal Etchegoin Formation within the Poso Creek Oil Field, Kern County, California A Thesis By Carol Beahm Submitted to the Department of Geological Sciences, California State University Bakersfield In partial fulfillment of the requirements of the degree of Masters of Geology Fall 2015 Depositional Environment of the Basal Etchegoin Formation within the Poso Creek Oil Field, Kern County, California By Carol Beahm This thesis has been accepted on behalf of the Department of Geological Science by the members of the supervisory committee: ' ' Dr. Janice Gillespie Committee Chair J Committee Kenneth Frost, Linn Energy Committee Member Acknowledgements I owe much to Linn Energy (formerly Berry Petroleum) for allowing me the use of their data, resources, and time for the completion of this paper. In particular, I would like to thank my Asset Manager, Greg Wagner, for not becoming entirely too impatient during the course of time spent on this project and for encouraging me and directing me all the way through. I would also like to thank Ken Frost for acting as a geologic mentor and thesis advisor for these many years. I would like to thank my professors Jan Gillespie and Rob Negrini. Not only for serving as committee members, but for being my advisors and mentors for over a decade now and for giving me much of the geologic knowledge I have today. The Well Repository at CSUB provided the core data necessary for this project. This is a wonderful source for any local geologic study. And a special dedication to my family.