May 23, 2018 Planning Commission for San Bernardino County C/O Ms
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Appendix G1:Phase I Cultural Resources Assessment
Appendix G1 Phase I Cultural Resources Assessment CONFIDENTIAL - NOT FOR PUBLIC DISTRIBUTION CADIZ VALLEY WATER CONSERVATION, RECOVERY, AND STORAGE PROJECT Phase I Cultural Resources Assessment Prepared for November 2011 Santa Margarita Water District 26111 Antonio Parkway Rancho Santa Margarita, CA Draft CONFIDENTIAL - NOT FOR PUBLIC DISTRIBUTION CADIZ VALLEY WATER CONSERVATION, RECOVERY, AND STORAGE PROJECT Phase I Cultural Resources Assessment Prepared for November 2011 Santa Margarita Water District 26111 Antonio Parkway Rancho Santa Margarita, CA Prepared By: ESA 626 Wilshire Blvd. Suite 1100 Los Angeles, CA 90017 Project site location: Cadiz, Cadiz Summit, Cadiz Lake NW, Cadiz Lake NE, Calumet Mine, Chubbuck, Milligan, East of Milligan, Danby Lake, Sablon, and Arica Mountains (CA) USGS 7.5’ Topographic Maps T1S R19E, 20E; T1N R18E, 19E; T2N R17E, 18E; 3N R16E, 17E; 4N R15E, 16E; 5N R14E, 15E Principal Investigator: Monica Strauss, M.A. Report Authors: Madeleine Bray, M.A, Candace Ehringer, M.A., Brian S. Marks, Ph.D. Keywords: San Bernardino County, Cadiz, Milligan, Archer, Freda, Chubbuck, Ward, Siam, Saltmarsh, Sablon, Fishel, Atchison Topeka and Santa Fe Railroad, Parker Cutoff, General George Patton Desert Training Center, Railroad Siding, Archaeological Survey 626 Wilshire Boulevard Suite 1100 Los Angeles, CA 90017 213.599.4300 www.esassoc.com Oakland Olympia Orlando Palm Springs Petaluma Portland Sacramento San Diego San Francisco Seattle Tampa Woodland Hills 210324 TABLE OF CONTENTS Cadiz Valley Water Conservation, Recovery, -
Aeolian Processes and Landforms
Aeolian Processes and Landforms Ms. Deithra L. Archie, New Mexico State University Abstract I will present an overview of Aeolian processes and landforms on Mars. The overview will consist of two components. Component one is an overview of Aeolian processes and landforms on Earth and Mars, where the two planetary bodies are shown in Figures 1a and 1b respectively The second part of this paper will consist of image comparisons using satellite and MOC (Mars Orbiter Camera) images. Figure 1a Figure 1b Introduction Understanding the aeolian activity on the planet Mars and other planets begins with the study and knowledge of similar processes on Earth. Therefore, I will discuss the following: wind, particle entrainment and landforms found in the aeolian environment. This discussion will lead into my later discussion of the Martian sand seas and sand dunes. See Table 1 for a glossary of the terms used throughout this paper. In aeolian processes, wind transports and deposits particles of sediment. Aeolian features form in areas where wind is the primary source of erosion. The particles deposited are of sand, silt and clay size (see Table 2). The particles are entrained in by one of four processes. Creep is when a particle rolls or slides across the surface. Lift is when a particle rises off the surface due to the Bernoulli effect, the same mechanism which causes aircraft to rise. If the airflow is turbulent, larger particles are trajected by a process known as saltation. Finally, impact transport occurs which one particle strikes another causing the second particle to move. Erosional Landforms Wind eroded landforms are rarely preserved on the surface of the Earth except in arid regions. -
Rice Valley Groundwater Basin Bulletin 118
Colorado River Hydrologic Region California’s Groundwater Rice Valley Groundwater Basin Bulletin 118 Rice Valley Groundwater Basin • Groundwater Basin Number: 7-4 • County: Riverside, San Bernardino • Surface Area: 189,000 acres (295 square miles) Basin Boundaries and Hydrology This groundwater basin underlies Rice Valley in northeast Riverside and southeast San Bernardino Counties. Elevation of the valley floor ranges from about 675 feet above sea level near the center of the valley to about 1,000 feet along the outer margins. The basin is bounded by nonwater- bearing rocks of the Turtle Mountains on the north, the Little Maria and Big Maria Mountains on the south, the Arica Mountains on the west, and by the West Riverside and Riverside Mountains on the east. Low-lying alluvial drainage divides form a portion of the basin boundaries on the northwest and northeast, and the Colorado River bounds a portion of the basin on the east. Maximum elevations of the surrounding mountains range to about 2,000 feet in the Arica Mountains, about 3,000 feet in the Big Maria Mountains, and 5,866 feet at Horn Peak in the Turtle Mountains (Bishop 1963; Jennings 1967; USGS 1971a, 1971b, 1983a, 1983b, 1983c). Annual average precipitation ranges from about 3 to 5 inches. Surface runoff from the mountains drains towards the center of the valley, except in the eastern part of the valley, where Big Wash drains to the Colorado River (USGS 1971a, 1971b, 1983a, 1983b, 1983c). Hydrogeologic Information Water Bearing Formations Alluvium is the water-bearing material that forms the basin and includes unconsolidated Holocene age deposits and underlying unconsolidated to semi-consolidated Pleistocene deposits (DWR 1954, 1963). -
Quaternary Geomorphic Processes and Landform Development in the Thar Desert of Rajasthan
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/302902544 Quaternary Geomorphic Processes and Landform Development in the Thar Desert of Rajasthan Chapter · January 2011 CITATIONS READS 6 4,293 1 author: Amal Kar Central Arid Zone Research Institute (CAZRI) 90 PUBLICATIONS 1,166 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Thar Desert Natural resources and their management View project Late Quaternary paleoclimate of the Thar Desert View project All content following this page was uploaded by Amal Kar on 11 May 2016. The user has requested enhancement of the downloaded file. acb publications Landforms Processes & Environment Management Kolkata, India Editor: S. Bandyopadhyay et al. [email protected] ISBN 81-87500-58-1 2011 (223-254) Quaternary Geomorphic Processes and Landform Development in the Thar Desert of Rajasthan Amal Kar1 Abstract: Evolution of landforms in the Thar Desert of Rajasthan is very much influenced by the exogenic and endogenic processes operating in the region during the Quaternary period. Studies have revealed that several fluctuations in climate between drier and wetter phases and periodic earth movements decided the type and intensity of geomorphic processes. The paper describes the broad sedimentation pattern in the desert, known facets of Quaternary climate and landform characteristics. It also discusses the influence of Quaternary climate change, neotectonism and human activities on landform evolution. Introduction The Thar, or the Great Indian Sand Desert, is situated in the arid western part of Rajasthan state in India and the adjoining sandy terrain of Pakistan. -
Genesis Solar Energy Project PA/FEIS 1 August 2010 Relationship to the Genesis Solar Energy Project Staff Assessment and DEIS
Bureau of Land Management PLAN AMENDMENT/FINAL EIS FOR THE GENESIS SOLAR ENERGY PROJECT Volume 1 of 3 August 2010 DOI Control #: FES 10-42 Publication Index #: BLM/CA/ES-2010-016+1793 NEPA Tracking # DOI-BLM-CA-060-0010-0015-EIS ,,..--...... United States Department ofthe Interior _.... _-- Bureau ofLand Management 1201 Bird Center Drive Palm Springs, CA 92262 Phone (760) 833·7100 IFax (760) 833-7199 http://www.blm.gov/calpalmsprings/ In reply refer to: CACA 048880 August 27, 20 I0 Dear Reader: Enclosed is the Proposed Resource Management Plan-Amendment/Final Environmental Impact Statement (PAIFEIS) for the California Desert Conservation Area (COCA) Plan and Genesis Solar Energy Project (GSEP). The Bureau of Land Management (BLM) prepared the PAiFEIS in consultation with cooperating agencies, taking into account public comments received during the National Environmental Policy Act (NEPA) process. The proposed decision on the plan amendment would add the GSEP site to those identified in the current COCA Plan, as amended, for solar energy production. The preferred alternative on the GSEP is to approve the dry cooling alternative to the right-of-way grant applied for by Genesis Solar, LLC. This PAIFEIS for the GSEP has been developed in accordance with NEPA and the Federal Land Policy and Management Act of 1976. The PA is largely based on the preferred alternative in the Draft Resource Management Plan·AmendmentlDraft Environmentallmpact Statement (DRMP-AiDEIS), which was released on April 9, 2010. The PAIFEIS for the GSEP contains the proposed plan and project description, a summary of changes made between the DRMP·AlDEIS and PRMP-AiFEIS, an analysis of the impacts of the decisions, a summary ofwritten comments received during the public review period for the DRMP AlDEIS and responses to comments. -
Last Glacial Aeolian Landforms and Deposits in the Rhône Valley
Last Glacial aeolian landforms and deposits in the Rhône Valley (SE France): Spatial distribution and grain-size characterization Mathieu Bosq, Pascal Bertran, Jean-Philippe Degeai, Sebastian Kreutzer, Alain Queffelec, Olivier Moine, Eymeric Morin To cite this version: Mathieu Bosq, Pascal Bertran, Jean-Philippe Degeai, Sebastian Kreutzer, Alain Queffelec, et al.. Last Glacial aeolian landforms and deposits in the Rhône Valley (SE France): Spatial dis- tribution and grain-size characterization. Geomorphology, Elsevier, 2018, 318, pp.250 - 269. 10.1016/j.geomorph.2018.06.010. hal-01844757 HAL Id: hal-01844757 https://hal.archives-ouvertes.fr/hal-01844757 Submitted on 16 Jun 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Last Glacial aeolian landforms and deposits in the Rhône Valley (SE France): Spatial distribution and grain-size characterization Mathieu Bosqa, Pascal Bertrana,b, Jean-Philippe Degeaic, Sebastian Kreutzerd, Alain Queffeleca, Olivier Moinee, Eymeric Morinf,g a PACEA, UMR 5199 CNRS - Université Bordeaux, Bâtiment B8, allée Geoffroy -
USGS Topographic Maps of California
USGS Topographic Maps of California: 7.5' (1:24,000) Planimetric Planimetric Map Name Reference Regular Replace Ref Replace Reg County Orthophotoquad DRG Digital Stock No Paper Overlay Aberdeen 1985, 1994 1985 (3), 1994 (3) Fresno, Inyo 1994 TCA3252 Academy 1947, 1964 (pp), 1964, 1947, 1964 (3) 1964 1964 c.1, 2, 3 Fresno 1964 TCA0002 1978 Ackerson Mountain 1990, 1992 1992 (2) Mariposa, Tuolumne 1992 TCA3473 Acolita 1953, 1992, 1998 1953 (3), 1992 (2) Imperial 1992 TCA0004 Acorn Hollow 1985 Tehama 1985 TCA3327 Acton 1959, 1974 (pp), 1974 1959 (3), 1974 (2), 1994 1974 1994 c.2 Los Angeles 1994 TCA0006 (2), 1994, 1995 (2) Adelaida 1948 (pp), 1948, 1978 1948 (3), 1978 1948, 1978 1948 (pp) c.1 San Luis Obispo 1978 TCA0009 (pp), 1978 Adelanto 1956, 1968 (pp), 1968, 1956 (3), 1968 (3), 1980 1968, 1980 San Bernardino 1993 TCA0010 1980 (pp), 1980 (2), (2) 1993 Adin 1990 Lassen, Modoc 1990 TCA3474 Adin Pass 1990, 1993 1993 (2) Modoc 1993 TCA3475 Adobe Mountain 1955, 1968 (pp), 1968 1955 (3), 1968 (2), 1992 1968 Los Angeles, San 1968 TCA0012 Bernardino Aetna Springs 1958 (pp), 1958, 1981 1958 (3), 1981 (2) 1958, 1981 1981 (pp) c.1 Lake, Napa 1992 TCA0013 (pp), 1981, 1992, 1998 Agua Caliente Springs 1959 (pp), 1959, 1997 1959 (2) 1959 San Diego 1959 TCA0014 Agua Dulce 1960 (pp), 1960, 1974, 1960 (3), 1974 (3), 1994 1960 Los Angeles 1994 TCA0015 1988, 1994, 1995 (3) Aguanga 1954, 1971 (pp), 1971, 1954 (2), 1971 (3), 1982 1971 1954 c.2 Riverside, San Diego 1988 TCA0016 1982, 1988, 1997 (3), 1988 Ah Pah Ridge 1983, 1997 1983 Del Norte, Humboldt 1983 -
Doi: 10.1103/Physreve.84.031304
ChinaXiv合作期刊 J Arid Land (2019) 11(5): 701–712 https://doi.org/ 10.1007/s40333-019-0108-4 Science Press Springer-Verlag Wind regime for long-ridge yardangs in the Qaidam Basin, Northwest China GAO Xuemin1,2,3*, DONG Zhibao4, DUAN Zhenghu1, LIU Min5, CUI Xujia5, LI Jiyan5,6 1 Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; 2 University of Chinese Academy of Sciences, Beijing 100049, China; 3 School of Tourism and Public Administration, Jinzhong University, Jinzhong 030619, China; 4 School of Geography and Tourism, Shaanxi Normal University, Xi'an 710062, China; 5 School of Geography Science, Taiyuan Normal University, Jinzhong 030619, China; 6 Key Laboratory of Education Ministry on Environment and Resources in Tibetan Plateau, Qinghai Normal University, Xining 810008, China Abstract: Yardangs are typical aeolian erosion landforms, which are attracting more and more attention of geomorphologists and geologists for their various morphology and enigmatic formation mechanisms. In order to clarify the aeolian environments that influence the development of long-ridge yardangs in the northwestern Qaidam Basin of China, the present research investigated the winds by installing wind observation tower in the field. We found that the sand-driving winds mainly blow from the north-northwest, northwest and north, and occur the most frequent in summer, because the high temperature increases atmospheric instability and leads to downward momentum transfer and active local convection during these months. The annual drift potential and the ratio of resultant drift potential indicate that the study area pertains to a high-energy wind environment and a narrow unimodal wind regime. -
Transverse Aeolian Ridges on Mars: First Results from Hirise Images
Geomorphology 121 (2010) 22–29 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Transverse Aeolian Ridges on Mars: First results from HiRISE images James R. Zimbelman ⁎ Center for Earth and Planetary Studies, MRC 315, National Air and Space Museum, Smithsonian Institution, Washington, D.C. 20013-7012, United States article info abstract Article history: Three images obtained by the High Resolution Imaging Science Experiment (HiRISE) were analyzed for the Received 11 July 2008 information they could provide regarding Transverse Aeolian Ridges (TARs) on Mars. TARs from five locations Received in revised form 23 February 2009 in a HiRISE image of the floor of Ius Chasma show remarkably symmetric (cross-sectional) profiles, with Accepted 26 May 2009 average slopes for the entire feature of ~15°; these results apply to TARs that span an order of magnitude in Available online 2 June 2009 wavelength and a factor of 6 in height. A HiRISE image of Gamboa impact crater in the northern lowlands shows low albedo sand patches b2 m high that are covered with sand ripples, surrounded by larger TAR-like Keywords: fi Sand ripples that are very similar in pro le to surveyed granule ripples on Earth. TARs in a HiRISE image from Terra Dune Sirenum, in the cratered southern highlands, are comparable in height to those in Ius Chasma, but many have Ripple tapered extensions that are more consistent with them being erosional remnants rather than the result of Granule ripple extension of the TAR by deposition from the tapered end. The new observations generally support a reversing Topography transverse dune origin for TARs with heights ≥1 m, and a granule ripple origin for TAR-like ripples with Transverse dune heights ≤0.5 m. -
Mesozoic Tectonics of the Maria Fold and Thrust Belt and Mccoy Basin : an Examination of Polyphase Deformation and Synorogenic Response Anthony C
University of New Mexico UNM Digital Repository Earth and Planetary Sciences ETDs Electronic Theses and Dissertations 8-27-2009 Mesozoic tectonics of the Maria fold and thrust belt and McCoy basin : an examination of polyphase deformation and synorogenic response Anthony C. Salem Follow this and additional works at: https://digitalrepository.unm.edu/eps_etds Recommended Citation Salem, Anthony C.. "Mesozoic tectonics of the Maria fold and thrust belt and McCoy basin : an examination of polyphase deformation and synorogenic response." (2009). https://digitalrepository.unm.edu/eps_etds/75 This Dissertation is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Earth and Planetary Sciences ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. MESOZOIC TECTONICS OF THE MARIA FOLD AND THRUST BELT AND MCCOY BASIN, SOUTHEASTERN CALIFORNIA: AN EXAMINATION OF POLYPHASE DEFORMATION AND SYNOROGENIC RESPONSE BY ANTHONY CHRISTOPHER SALEM B.S., Arizona State University, 1999 M.S.., Geological Sciences, Arizona State University, 2005 DISSERTATION Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy Earth & Planetary Sciences The University of New Mexico Albuquerque, New Mexico August, 2009 ©2009, Anthony C. Salem iii DEDICATION For Audrey, my best friend, chief advisor, drill sergeant, sounding board, editor extraordinaire, GIS wizard, partner in crime and great love. Without her love and support, life and this work would have been a lonely endeavor. iv ACKNOWLEDGMENTS All the work that goes into conducting research and writing a dissertation may be indeed done by one person, but is actually the result of the efforts and support of many people who should be acknowledged. -
Aliso, 34(2), Online Supplement ISSN 0065-6275 (Print), ISSN 2327-2929 (Online)
Aliso, 34(2), Online Supplement ISSN 0065-6275 (print), ISSN 2327-2929 (online) Online Supplement for “Tomus Nominum Eriastri: The Nomenclature and Taxonomy of Eriastrum (Polemoniaceae: Loeselieae)”, Sarah J. De Groot (2016) Aliso: A Journal of Systematic and Evolutionary Botany 34 (2): 25–152. EXSICCATAE Representative specimens studied. Not all associate collectors are listed. Eriastrum abramsii JEPS116786. Along Vineyard Canyon Road just over 14 miles north U.S.A. CALIFORNIA: Lake County: Kelseyville, 15 May 1924, J.W. of Monterey-San Luis Obispo county line, 31 May 2008, S.J. De Groot Blankinship s.n., CAS165485. Mt. Konocti [near Kelseyville], 4 Jun 5879, RSA (Pop 260). San Benito County: West of Coalinga, dry 1929, J.W. Blankinship s.n., POM279114. Ridge between Burns hillside, 13 Jun 1910, I.J. Condit s.n., UC455635. Coalinga Road near Valley and Borax Lake, 12 May 1945, H.L. Mason 12585, DS342729. mile post 9.82 from its junction with Highway 25 and east of 2.5 miles south of Kelseyville, 28 Jun 1945, H.L. Mason 12606, Bitterwater, 15 Jun 2004, D. Gowen 117, JEPS105711, JEPS105712. DS342491. 2.5 miles south of Kelseyville on road to Lower Lake, 28 Coalinga Road east of Highway 25 and Bitterwater, near milepost Jun 1945, M.S. Baker 11081, CAS326268. S-facing slope ca. 1 mile 9.82, 1 Jun 2006, D. Gowen 597, JEPS116802. Along Coalinga Road WSW of Glenbrook, upper High Valley Cr. drainage, SE/4 of SW/4 at mile marker 9.82 from Highway 25, 1 Jun 2008, S.J. De Groot S32 T12N R8W, 1 Jun 1983, R.D. -
Exploring the Interaction Between Rivers and Sand Dunes – Implications for Fluvial-Aeolian Geomorphology
THE UNIVERSITY OF HULL Exploring the interaction between rivers and sand dunes – implications for fluvial-aeolian geomorphology being a Thesis submitted for the Degree of Doctor of Philosophy in the University of Hull by Baoli Liu MSc from Xiamen University, China September, 2014 For my mum Chunrong (杨春荣) and young brother Zehua (刘泽华) And in memory of my father Kefu (刘克富) Abstract The interaction between fluvial and aeolian processes can significantly influence landforms. When rivers and sand dunes meet, the interaction of sediment transport between the two systems can lead to change in either one or both systems. However, these two systems are usually studied independently which leaves many questions unresolved in terms of how they interact. This study investigated interactions between fluvial and aeolian processes, focusing on the triggers that switch the dominance between one process and the other, and the consequent changes in geomorphology that may occur. Firstly, a global inventory of fluvial-aeolian interactions at 230 globally distributed locations was collected using satellite imagery. At each site, the following attributes were measured: net sand transport direction, fluvial-aeolian meeting angle, dune type and river channel pattern. From these data, six different types of interaction were classified that reflect a shift in dominance between the fluvial and aeolian systems. Results from this classification confirm that only certain types of interaction were significant: the meeting angle and dune type, the meeting angle and interaction type and finally the channel pattern and interaction type. These results show the importance of fluvial – aeolian interactions, but also reveal the difficulties of understanding dynamic geomorphic systems from images taken at a single moment in time.