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Species at Risk on Department of Defense Installations
Species at Risk on Department of Defense Installations Revised Report and Documentation Prepared for: Department of Defense U.S. Fish and Wildlife Service Submitted by: January 2004 Species at Risk on Department of Defense Installations: Revised Report and Documentation CONTENTS 1.0 Executive Summary..........................................................................................iii 2.0 Introduction – Project Description................................................................. 1 3.0 Methods ................................................................................................................ 3 3.1 NatureServe Data................................................................................................ 3 3.2 DOD Installations............................................................................................... 5 3.3 Species at Risk .................................................................................................... 6 4.0 Results................................................................................................................... 8 4.1 Nationwide Assessment of Species at Risk on DOD Installations..................... 8 4.2 Assessment of Species at Risk by Military Service.......................................... 13 4.3 Assessment of Species at Risk on Installations ................................................ 15 5.0 Conclusion and Management Recommendations.................................... 22 6.0 Future Directions............................................................................................. -
References and Appendices
References Ainley, D.G., S.G. Allen, and L.B. Spear. 1995. Off- Arnold, R.A. 1983. Ecological studies on six endan- shore occurrence patterns of marbled murrelets gered butterflies (Lepidoptera: Lycaenidae): in central California. In: C.J. Ralph, G.L. Hunt island biogeography, patch dynamics, and the Jr., M.G. Raphael, and J.F. Piatt, technical edi- design of habitat preserves. University of Cali- tors. Ecology and Conservation of the Marbled fornia Publications in Entomology 99: 1–161. Murrelet. USDA Forest Service, General Techni- Atwood, J.L. 1993. California gnatcatchers and coastal cal Report PSW-152; 361–369. sage scrub: the biological basis for endangered Allen, C.R., R.S. Lutz, S. Demairais. 1995. Red im- species listing. In: J.E. Keeley, editor. Interface ported fire ant impacts on Northern Bobwhite between ecology and land development in Cali- populations. Ecological Applications 5: 632-638. fornia. Southern California Academy of Sciences, Allen, E.B., P.E. Padgett, A. Bytnerowicz, and R.A. Los Angeles; 149–169. Minnich. 1999. Nitrogen deposition effects on Atwood, J.L., P. Bloom, D. Murphy, R. Fisher, T. Scott, coastal sage vegetation of southern California. In T. Smith, R. Wills, P. Zedler. 1996. Principles of A. Bytnerowicz, M.J. Arbaugh, and S. Schilling, reserve design and species conservation for the tech. coords. Proceedings of the international sym- southern Orange County NCCP (Draft of Oc- posium on air pollution and climate change effects tober 21, 1996). Unpublished manuscript. on forest ecosystems, February 5–9, 1996, River- Austin, M. 1903. The Land of Little Rain. University side, CA. -
Region of the San Andreas Fault, Western Transverse Ranges, California
Thrust-Induced Collapse of Mountains— An Example from the “Big Bend” Region of the San Andreas Fault, Western Transverse Ranges, California By Karl S. Kellogg Scientific Investigations Report 2004–5206 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Reston, Virginia: 2004 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. iii Contents Abstract ……………………………………………………………………………………… 1 Introduction …………………………………………………………………………………… 1 Geology of the Mount Pinos and Frazier Mountain Region …………………………………… 3 Fracturing of Crystalline Rocks in the Hanging Wall of Thrusts ……………………………… 5 Worldwide Examples of Gravitational Collapse ……………………………………………… 6 A Spreading Model for Mount Pinos and Frazier Mountain ………………………………… 6 Conclusions …………………………………………………………………………………… 8 Acknowledgments …………………………………………………………………………… 8 References …………………………………………………………………………………… 8 Illustrations 1. Regional geologic map of the western Transverse Ranges of southern California …………………………………………………………………………… 2 2. Simplified geologic map of the Mount Pinos-Frazier Mountain region …………… 2 3. View looking southeast across the San Andreas rift valley toward Frazier Mountain …………………………………………………………………… 3 4. View to the northwest of Mount Pinos, the rift valley (Cuddy Valley) of the San Andreas fault, and the trace of the Lockwood Valley fault ……………… 3 5. -
Saltillo, Coahuila a 25 De Agosto De 2020 Programa De Maestría En
Saltillo, Coahuila a 25 de agosto de 2020 Programa de Maestría en Ciencias en Agroplasticultura Coordinación de Posgrado P R E S E N T E Por este conducto nos permitimos informar a esta coordinación que, el documento de tesis preparado por ANTONNY URIEL VILLEGAS CHAVEZ titulado "Estudio de la diversidad genética de plantassilvestres de Guayule ( Parthenium argentatum Gray) mediante marcadores ITS” el cual fue presentado el día de hoy 25 de agosto de 20 20, ha sido modificado de acuerdo a las observaciones, comentarios y sugerencias, realizadas por el Comité Evaluador asignado. Por tal motivo, avalamos que el documento corresponde a la versión final del documento de tesis. Atentamente, SINODALES ________ ___________________________ __________________________________ Dra. Ileana Vera Reyes Dra. Mona Kassem Presidente Secretario ______________________________ Dr. Gerardo Hernandez Vera Vocal Vo. Bo. de los Asesores __________ ___ _ _ __________ _________ _______________ __________ _________ __ Dra. Ana Margarita Rodríguez Hernández Dr. Marco Antonio Castillo Campohermoso CENTRO DE INVESTIGACIÓN EN QUÍMICA APLICADA Programa de Maestría en Ciencias en Agroplasticultura TESIS Estudio de la diversidad genética de plantas silvestres de Guayule (Parthenium argentatum Gray) mediante marcadores ITS Presentada por: ANTONNY URIEL VILLEGAS CHAVEZ Para obtener el grado de: Maestro en Ciencias en Agroplasticultura Asesorada por: Dra. Ana Margarita Rodríguez Hernández Dr. Marco Antonio Castillo Campohermoso SINODALES ________________________ _____________________ Dra. Ileana Vera Reyes Dra. Mona Kassem Presidente Secretario _______________________________ Dr. Gerardo Hernández Vera Vocal Saltillo, Coahuila Agosto, 2020 CENTRO DE INVESTIGACIÓN EN QUÍMICA APLICADA Programa de Maestría en Ciencias en Agroplasticultura TESIS Estudio de la diversidad genética de plantas silvestres de Guayule (Parthenium argentatum Gray) mediante marcadores ITS Presentada por: ANTONNY URIEL VILLEGAS CHAVEZ Para obtener el grado de: Maestro en Ciencias en Agroplasticultura Asesorado por: Dra. -
Phylogenies and Secondary Chemistry in Arnica (Asteraceae)
Digital Comprehensive Summaries of Uppsala Dissertations from the Faculty of Science and Technology 392 Phylogenies and Secondary Chemistry in Arnica (Asteraceae) CATARINA EKENÄS ACTA UNIVERSITATIS UPSALIENSIS ISSN 1651-6214 UPPSALA ISBN 978-91-554-7092-0 2008 urn:nbn:se:uu:diva-8459 !"# $ % !& '((" !()(( * * * + , - . , / , '((", + 0 1# 2, # , 34', 56 , , 70 46"84!855&86(4'8(, - 1# 2 . * 9 10-2 . * . # 9 , * * 1 ! " #! !$ 2 1 2 .8 # * * :# 77 1%&'(2 . !6 '3, + . .8 ) / , ; < * . * ** # , * * * , 09 * . # * * 33 * != , 0- # 9 * * 1, , * 2 . * , 0 * * * * * . * , $ * 0- * % # , # 8 * * * * * * $8> # . * * !' , * * . ** , ? . 0- , +,- # # 7-0 -0 :+' 9 +# $8> ./0) . ) 1 ) 2 * 3) ) .456(7 ) , @ / '((" 700 !=5!8='!& 70 46"84!855&86(4'8( ) ))) 8"&54 1 );; ,/,; A B ) ))) 8"&542 List of Papers This thesis is based on the following papers, which are referred to in the text by their Roman numerals: I Ekenäs, C., B. G. Baldwin, and K. Andreasen. 2007. A molecular phylogenetic -
Active Tectonics at Wheeler Ridge, Southern San Joaquin Valley, California
Active tectonics at Wheeler Ridge, southern San Joaquin Valley, California E. A. Keller* Environmental Studies Program and Department of Geological Sciences, University of California, Santa Barbara, California 93106 R. L. Zepeda 1342 Grove Street, Alameda, California 94501 T. K. Rockwell Department of Geological Sciences, San Diego State University, San Diego, California 91282 T. L. Ku Department of Earth Sciences, University of Southern California, Los Angeles, California 90089-0740 W. S. Dinklage Department of Geological Sciences, University of California, Santa Barbara, California 93106 ABSTRACT INTRODUCTION where geomorphic surfaces are folded over the anticlinal axis (Zepeda et al., 1986). In addition, Wheeler Ridge is an east-west–trending Buried reverse faults associated with actively the 1952 Kern County earthquake was centered anticline that is actively deforming on the up- deforming folds are known to produce large earth- below Wheeler Ridge, but not on the Wheeler per plate of the Pleito–Wheeler Ridge thrust- quakes. Several recent, large California earth- Ridge thrust fault; therefore the potential earth- fault system. Holocene and late Pleistocene de- quakes are examples: M = 6.7, Northridge, 1994; quake hazard in the area is clear. formation is demonstrated at the eastern end M = 6.1, Whittier Narrows, 1987; MS = 6.4, The primary goals of the research at Wheeler of the anticline where Salt Creek crosses the Coalinga, 1983, and MS = 7.7, Kern County, Ridge are (1) to characterize the tectonic geomor- anticlinal axis. Uplift, tilting, and faulting, as- 1952. Detailed investigations of folding associ- phology; (2) to develop the Pleistocene chronol- sociated with the eastward growth of the anti- ated with concealed reverse faults are therefore ogy; and (3) to test the hypothesis that climatic cline, are documented by geomorphic surfaces necessary in order to better understand earthquake perturbations are responsible for most Pleistocene that are higher and older to the west. -
A Checklist of Vascular Plants Endemic to California
Humboldt State University Digital Commons @ Humboldt State University Botanical Studies Open Educational Resources and Data 3-2020 A Checklist of Vascular Plants Endemic to California James P. Smith Jr Humboldt State University, [email protected] Follow this and additional works at: https://digitalcommons.humboldt.edu/botany_jps Part of the Botany Commons Recommended Citation Smith, James P. Jr, "A Checklist of Vascular Plants Endemic to California" (2020). Botanical Studies. 42. https://digitalcommons.humboldt.edu/botany_jps/42 This Flora of California is brought to you for free and open access by the Open Educational Resources and Data at Digital Commons @ Humboldt State University. It has been accepted for inclusion in Botanical Studies by an authorized administrator of Digital Commons @ Humboldt State University. For more information, please contact [email protected]. A LIST OF THE VASCULAR PLANTS ENDEMIC TO CALIFORNIA Compiled By James P. Smith, Jr. Professor Emeritus of Botany Department of Biological Sciences Humboldt State University Arcata, California 13 February 2020 CONTENTS Willis Jepson (1923-1925) recognized that the assemblage of plants that characterized our flora excludes the desert province of southwest California Introduction. 1 and extends beyond its political boundaries to include An Overview. 2 southwestern Oregon, a small portion of western Endemic Genera . 2 Nevada, and the northern portion of Baja California, Almost Endemic Genera . 3 Mexico. This expanded region became known as the California Floristic Province (CFP). Keep in mind that List of Endemic Plants . 4 not all plants endemic to California lie within the CFP Plants Endemic to a Single County or Island 24 and others that are endemic to the CFP are not County and Channel Island Abbreviations . -
Transverse Ranges - Wikipedia, the Free Encyclopedia
San Gabriel Mountains - Field Trip http://www.csun.edu/science/geoscience/fieldtrips/san-gabriel-mts/index.html Sourcebook Home Biology Chemistry Physics Geoscience Reference Search CSUN San Gabriel Mountains - Field Trip Science Teaching Series Geography & Topography The Sourcebook for Teaching Science Hands-On Physics Activities Tour - The route of the field trip Hands-On Chemistry Activities GPS Activity HIstory of the San Gabriels Photos of field trip Internet Resources Geology of the San Gabriel Mountains I. Developing Scientific Literacy 1 - Building a Scientific Vocabulary Plate Tectonics, Faults, Earthquakes 2 - Developing Science Reading Skills 3 - Developing Science Writing Skills Rocks, Minerals, Geological Features 4 - Science, Technology & Society Big Tujunga Canyon Faults of Southern California II. Developing Scientific Reasoning Gneiss | Schist | Granite | Quartz 5 - Employing Scientific Methods 6 - Developing Scientific Reasoning Ecology of the San Gabriel Mountains 7 - Thinking Critically & Misconceptions Plant communities III. Developing Scientific Animal communities Understanding Fire in the San Gabriel Mountains 8 - Organizing Science Information Human impact 9 - Graphic Oganizers for Science 10 - Learning Science with Analogies 11 - Improving Memory in Science Meteorology, Climate & Weather 12 - Structure and Function in Science 13 - Games for Learning Science Inversion Layer Los Angeles air pollution. Åir Now - EPA reports. IV. Developing Scientific Problem Climate Solving Southern Calfirornia Climate 14 - Science Word Problems United States Air Quality blog 15 - Geometric Principles in Science 16 - Visualizing Problems in Science 1 of 2 7/14/08 12:56 PM San Gabriel Mountains - Field Trip http://www.csun.edu/science/geoscience/fieldtrips/san-gabriel-mts/index.html 17 - Dimensional Analysis Astronomy 18 - Stoichiometry 100 inch Mount Wilson telescope V. -
Insights from Lowtemperature Thermochronometry Into
TECTONICS, VOL. 32, 1602–1622, doi:10.1002/2013TC003377, 2013 Insights from low-temperature thermochronometry into transpressional deformation and crustal exhumation along the San Andreas fault in the western Transverse Ranges, California Nathan A. Niemi,1 Jamie T. Buscher,2 James A. Spotila,3 Martha A. House,4 and Shari A. Kelley 5 Received 21 May 2013; revised 21 October 2013; accepted 28 October 2013; published 20 December 2013. [1] The San Emigdio Mountains are an example of an archetypical, transpressional structural system, bounded to the south by the San Andreas strike-slip fault, and to the north by the active Wheeler Ridge thrust. Apatite (U-Th)/He and apatite and zircon fission track ages were obtained along transects across the range and from wells in and to the north of the range. Apatite (U-Th)/He ages are 4–6 Ma adjacent to the San Andreas fault, and both (U-Th)/He and fission track ages grow older with distance to the north from the San Andreas. The young ages north of the San Andreas fault contrast with early Miocene (U-Th)/He ages from Mount Pinos on the south side of the fault. Restoration of sample paleodepths in the San Emigdio Mountains using a regional unconformity at the base of the Eocene Tejon Formation indicates that the San Emigdio Mountains represent a crustal fragment that has been exhumed more than 5 km along the San Andreas fault since late Miocene time. Marked differences in the timing and rate of exhumation between the northern and southern sides of the San Andreas fault are difficult to reconcile with existing structural models of the western Transverse Ranges as a thin-skinned thrust system. -
Los Padres National Forest Tamarisk Removal Draft Environmental
Draft Environmental Impact United States Department of Agriculture Statement Forest Service Los Padres National Forest June 2016 Tamarisk Removal Project Los Padres National Forest Kern, Los Angeles, Monterey, San Luis Obispo, Santa Barbara and Ventura Counties, California In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877- 8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD- 3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. -
Signature Redacted for Privacy. Robeqs. Yeats
AN ABSTRACT OF THE DISSERTATION OF Barbara Jean Ellis for the degree of Doctor of Philosophy in Geology presented on May 12, 1994, Title: Changing Tectonic Regimes in the Southern Salinian Block: Extension, Strike-Slip Faulting. Compression and Rotation in the Cuyama Valley, Ca1ifornia ,.Signature redacted forprivacy. Abstract approved: RobeqS.Yeats During the Cenozoic, tectonics in the Cuyama basin of the southeastern Salinian block changed from extension to strike-slip faulting to compression and rotation. During the Oligocene-early Miocene, the Cuyama basin was adjacent to the southern Mojave region and part of that extensional tectonic regime. Many present-day reverse faults have an extensional history. At -P23 Ma, strike-slip faulting began, and the Cuyama basin was part of a zone of distributed shear between the North American and Pacific plates. The Russell fault, which is the oldest documented right-lateral fault in the region, began movement at -P23 Ma which continued until 4 Ma. Tracing its 29 km of slip south of the Big Pine fault is problematic.It may connect with the Blue Rock fault below the Cuyama Badlands, and then correlate with the Clemens Well-Fenner-San Francisquito fault segments, another early strand of the San Andreas fault system to the south. An associated left-lateral fault is proposed to underlie the southeast Caliente Range. The Cox normal fault, which was active during deposition of the Saltos Shale member of the Monterey Formation, is another structure associated with the early right-lateral shear. Compressional tectonics have occurred more recently. The Caliente Range is moving south on the Whiterock and Morales thrusts; the Sierra Madre is moving north on the South Cuyama and Ozena faults. -
Inventoried Roadless Areas and Wilderness Evaluations
Introduction and Evaluation Process Summary Inventoried Roadless Areas and Wilderness Evaluations For reader convenience, all wilderness evaluation documents are compiled here, including duplicate sections that are also found in the Draft Environmental Impact Statement, Appendix D Inventoried Roadless Areas. Introduction and Evaluation Process Summary Inventoried Roadless Areas Proposed Wilderness by and Wilderness Evaluations Alternative Introduction and Evaluation Process Summary Roadless areas refer to substantially natural landscapes without constructed and maintained roads. Some improvements and past activities are acceptable within roadless areas. Inventoried roadless areas are identified in a set of maps contained in the Forest Service Roadless Area Conservation Final Environmental Impact Statement (FEIS), Volume 2, November 2000. These areas may contain important environmental values that warrant protection and are, as a general rule, managed to preserve their roadless characteristics. In the past, roadless areas were evaluated as potential additions to the National Wilderness Preservation System. Roadless areas have maintained their ecological and social values, and are important both locally and nationally. Recognition of the values of roadless areas is increasing as our population continues to grow and demand for outdoor recreation and other uses of the Forests rises. These unroaded and undeveloped areas provide the Forests with opportunities for potential wilderness, as well as non-motorized recreation, commodities and amenities. The original Forest Plans evaluated Roadless Area Review and Evaluation (RARE II) data from the mid- 1980s and recommended wilderness designation for some areas. Most areas were left in a roadless, non- motorized use status. This revision of Forest Plans analyzes a new and more complete land inventory of inventoried roadless areas as well as other areas identified by the public during scoping.