Proposed Northern & Eastern Colorado Desert Coordinated
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San Antonio Del Desierto Mobile Home Park Expansion Project Mecca, Riverside County, California
San Antonio Del Desierto Mobile Home Park Expansion Project Mecca, Riverside County, California Biological Resources Assessment Prepared for: Terra Nova Planning and Research, Inc. 42635 Melanie Place, Ste 101 Palm Desert, CA 92211 Tel: (760) 341-4800 Contact: John D. Criste, Principal Prepared by: Wood Environment & Infrastructure, Inc. 1845 Chicago Avenue, Suite D Riverside, CA 92507 (951) 369-8060 Wood E&I Job # 322520099 Principal Investigator: Stephen J. Myers Document Author: Carla Sanchez May 2019 San Antonio Del Desierto Project Biological Resources Assessment Mecca, Riverside County, CA May 2019 TABLE OF CONTENTS PAGE 1.0 INTRODUCTION ............................................................................................................. 1 1.1 Project Description ............................................................................................... 1 1.2 Project Site Description/Existing Conditions ......................................................... 1 1.3 Regulatory Framework ......................................................................................... 3 1.3.1 Federal ................................................................................................ 3 1.3.2 State .................................................................................................... 4 1.3.3 CVAG/Coachella Valley Conservation Commission ............................. 6 2.0 METHODS ...................................................................................................................... 7 2.1 -
California Vegetation Map in Support of the DRECP
CALIFORNIA VEGETATION MAP IN SUPPORT OF THE DESERT RENEWABLE ENERGY CONSERVATION PLAN (2014-2016 ADDITIONS) John Menke, Edward Reyes, Anne Hepburn, Deborah Johnson, and Janet Reyes Aerial Information Systems, Inc. Prepared for the California Department of Fish and Wildlife Renewable Energy Program and the California Energy Commission Final Report May 2016 Prepared by: Primary Authors John Menke Edward Reyes Anne Hepburn Deborah Johnson Janet Reyes Report Graphics Ben Johnson Cover Page Photo Credits: Joshua Tree: John Fulton Blue Palo Verde: Ed Reyes Mojave Yucca: John Fulton Kingston Range, Pinyon: Arin Glass Aerial Information Systems, Inc. 112 First Street Redlands, CA 92373 (909) 793-9493 [email protected] in collaboration with California Department of Fish and Wildlife Vegetation Classification and Mapping Program 1807 13th Street, Suite 202 Sacramento, CA 95811 and California Native Plant Society 2707 K Street, Suite 1 Sacramento, CA 95816 i ACKNOWLEDGEMENTS Funding for this project was provided by: California Energy Commission US Bureau of Land Management California Wildlife Conservation Board California Department of Fish and Wildlife Personnel involved in developing the methodology and implementing this project included: Aerial Information Systems: Lisa Cotterman, Mark Fox, John Fulton, Arin Glass, Anne Hepburn, Ben Johnson, Debbie Johnson, John Menke, Lisa Morse, Mike Nelson, Ed Reyes, Janet Reyes, Patrick Yiu California Department of Fish and Wildlife: Diana Hickson, Todd Keeler‐Wolf, Anne Klein, Aicha Ougzin, Rosalie Yacoub California -
Winter Observations on the Colorado Desert
MAR., 1902. ( THE CONDOR 37 In some respects the Oregon song sparrow is a remarkable form. It is darker than the races north and south of its range, and duplicates in coloring the sooty song sparrow of the Sitkan District. The races along the coast seem thus to alternate light and dark. But whilephea is nearly identical with ru@a in color, it is conspicuously smaller, and the ranges of the two are separated by several hundred miles. The present form occupies a strip along the coast from the northern limit of the redwoods (?) or at least from Rogue River north to Yaquina. The specimens from Crescent City are probably migrants as the breeding birds seem nearer deonensis (tho not precisely typical). The area ofi intergradation between cdeonen- sis and phcza is probably small, extending perhaps from Crescent City to Chetco R. (northern limit of Sequoia sempervivens). Lack of specimens prevents the exact determination of the limits of$hcPa at the north. I am indebted to Mr. Robert Ridgway and to Dr. C. Hart Merriam forthe use of specimens and types in the collection of the National Museum and in that of the Biological Survey. Winter Observations on the Colorado Desert. IT. S. DAGGETT, PASADENA, CAL. ROM Oct. 27 to Nov. 16, 1901, I dead birds floating on its surface, was spent at the American Girl Gold the cyanide tanks, two in number, con- F Mining Co.s‘ camp, located in the taining a strong solution of cyanide of Cargo Murchacho Mts on the Colorado potassium. Birds that essayed to Desert, five and one-half miles north- quench their thirst at this fount top- east of Ogilby, Cal., and some sixteen pled over dead in an instant. -
Pamphlet SIM 3411: Geologic Map of the Castle Rock 7.5' Quadrangle
Geologic Map of the Castle Rock 7.5’ Quadrangle, Arizona and California By P. Kyle House, Barbara E. John, Daniel V. Malmon, Debra Block, L. Sue Beard, Tracey J. Felger, Ryan S. Crow, Jonathan E. Schwing, and Colleen E. Cassidy Pamphlet to accompany Scientific Investigations Map 3411 Kayaker's view of Castle Rock (unit Tac) looking north-northeast from Castle Rock Bay, Arizona. The northern Mohave Mountains are visible in left background, and sediments of the Chemehuevi Formation (unit Qch) are seen along right edge of photo. Photograph taken August 27, 2014, by Kyle House, USGS. 2018 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2018 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit https://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit https://store.usgs.gov. To order USGS information products, visit https://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: House, P.K., John, B.E., Malmon, D.V., Block, Debra, Beard, L.S., Felger, T.J., Crow, R.S., Schwing, J.E., and Cassidy, C.E., 2018, Geologic map of the Castle Rock 7.5’ quadrangle: U.S. -
Chemehuevi Valley Special Recreation Management Area (SRMA)
Chemehuevi Valley Special Recreation Management Area (SRMA) The Chemehuevi Valley Viewshed with the Turtle Mountains National Natural Landmark is directly west of the communities of Havasu Landing, California and Lake Havasu City, Arizona. The Turtle Mountains Natural Landmark is an excellent illustration of volcanic phenomena with superimposed sculpturing of mountain landforms. In combination, the eastern and western sections present some of the finest geological formations in the Mohave Desert. The site is of scenic value and interest; it also contains excellent examples of Mohave Desert flora and fauna. From October to April each year hundreds of travelers “snowbirds” from the northeastern United States, Canada and Europe journey to the area to enjoy the mild winter climate seeking new experiences, enjoying vast landscape which have not existed in European Nations for hundreds of years. Visitors participate in backcountry touring adventure and the discovery of new hiking trails, rock hounding sites and camping opportunities. The Chemehuevi Reservation Havasu Landing Resort depends on the naturalness of the Chemehuevi Valley to support the recreation pursuits of their visitors. The Needles Field Office has developed a system of designated trails entitled the Mojave Adventure Routes in regards to the 2002 Northern and Eastern Colorado Desert Coordinated Management Plan item 3.8.7. These routes are an outstanding network of 4x4 vehicle backcountry touring routes for motorized recreation. These routes were developed for the purpose of traveling to areas not often seen by many people. This network is a shared-use trail system providing recreation opportunities for all persons, including those who use street-legal and non-street legal (Green Sticker) vehicles, hikers, bicyclists, and equestrians. -
VGP) Version 2/5/2009
Vessel General Permit (VGP) Version 2/5/2009 United States Environmental Protection Agency (EPA) National Pollutant Discharge Elimination System (NPDES) VESSEL GENERAL PERMIT FOR DISCHARGES INCIDENTAL TO THE NORMAL OPERATION OF VESSELS (VGP) AUTHORIZATION TO DISCHARGE UNDER THE NATIONAL POLLUTANT DISCHARGE ELIMINATION SYSTEM In compliance with the provisions of the Clean Water Act (CWA), as amended (33 U.S.C. 1251 et seq.), any owner or operator of a vessel being operated in a capacity as a means of transportation who: • Is eligible for permit coverage under Part 1.2; • If required by Part 1.5.1, submits a complete and accurate Notice of Intent (NOI) is authorized to discharge in accordance with the requirements of this permit. General effluent limits for all eligible vessels are given in Part 2. Further vessel class or type specific requirements are given in Part 5 for select vessels and apply in addition to any general effluent limits in Part 2. Specific requirements that apply in individual States and Indian Country Lands are found in Part 6. Definitions of permit-specific terms used in this permit are provided in Appendix A. This permit becomes effective on December 19, 2008 for all jurisdictions except Alaska and Hawaii. This permit and the authorization to discharge expire at midnight, December 19, 2013 i Vessel General Permit (VGP) Version 2/5/2009 Signed and issued this 18th day of December, 2008 William K. Honker, Acting Director Robert W. Varney, Water Quality Protection Division, EPA Region Regional Administrator, EPA Region 1 6 Signed and issued this 18th day of December, 2008 Signed and issued this 18th day of December, Barbara A. -
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, -
U.S. Geological Survey and A. M. Leszcykowski and J. D. Causey U.S
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP MF-1603-A UNITED STATES GEOLOGICAL SURVEY MINERAL RESOURCE POTENTIAL OF THE COXCOMB MOUNTAINS WILDERNESS STUDY AREA (CDCA-328), SAN BERNARDINO AND RIVERSIDE COUNTIES, CALIFORNIA SUMMARY REPORT By J. P. Calzia, J. E. Kilburn, R. W. Simpson, Jr., and C. M. Alien U.S. Geological Survey and A. M. Leszcykowski and J. D. Causey U.S. Bureau of Mines STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S. Bureau of Mines to conduct mineral surveys on certain areas to determine their mineral resource potential. Results must be made available to the public and be submitted to the President and the Congress. This report presents the results of a mineral survey of the Coxcomb Mountains Wilderness Study Area (CDCA-328), California Desert Conservation Area, Riverside and San Bernardino Counties, California. SUMMARY Geologic, geochemical, geophysical, and mineral surveys within the Coxcomb Mountains Wilderness Study Area in south eastern California define several areas with low to moderate potential for base and precious metals. Inferred subeconomic re sources of gold at the Moser mine (area Ha) are estimated at 150,000 tons averaging 1.7 ppm Au. The remainder of the study area has low potential for other mineral and energy resources including radioactive minerals and geothermal resources. Oil, gas, and coal resources are not present within the wilderness study area. INTRODUCTION Hope (1966), Greene (1968), and Calzia (1982) indicate that the wilderness study area is underlain by metaigneous and The Coxcomb Mountains Wilderness Study Area metasedimentary rocks of Jurassic and (or) older age intruded (CDCA-328) is located in the Mojave Desert of southeastern by granitic rocks of Late Jurassic to Late Cretaceous age. -
Green Access and Equity for Orange County
HEALTHY PARKS, SCHOOLS AND COMMUNITIES: Green Access and Equity for Riverside County ABOUT THIS REPORT This policy report is a summary for Riverside County of The City Project’s 2011 report, Healthy Parks, Schools, and Communities: Mapping Green Access and Equity for Southern California, which maps and analyzes green access and equity in nine counties in Southern California—Los Angeles, Orange, Ventura, San Bernardino, Riverside, San Diego, Kern, Santa Barbara and Imperial—using narrative and legal analyses, geographic information system (GIS) mapping tools, and demographic and economic data. Unlike other studies, which plot either green space or population, the maps in this report plot green space in relation to population and other metrics that indicate accessibility, such as distance to the park. This report also provides multidisciplinary analyses of the vital benefits of parks and other green space to people and the environment. It describes the consequences of disparities in green access and the benefits that could be reaped in “park poor” and “income poor” communities if resources were fairly allocated. It concludes with recommendations for equitable investments in green space in Riverside County and throughout California and the nation. The goal of this work is to combine research and analyses with effective outreach to provide concerned citizens, community groups, elected and other government officials, planners, funders and other stakeholders with the best available information upon which to prioritize actions and decisions that positively impact green access and quality of life for all. Together we can help children be active, eat well, stay healthy and do their best in school and life. -
BLM Worksheets
10 18 " 13 4 47 ! ! ! 47 " " 11 Piute Valley and Sacramento Mountains 54 " ! ! 87 12 ! 81 " 4 55 61 22 " ! " Pinto Lucerne Valley and Eastern Slopes ! 63 33 " 56 " " " 36 25 Colorado Desert " 20 ! " " 59 37 ! 2 ! 19 " ! 16 19 ! 56 21 " ! ! 15 27 ! 38 Arizona Lake Cahuilla 72 Lake Cahuilla 48 57 " ! ! 57 ! " 34 35 84 ! " 42 76 ! 26 41 ! " 0 5 10 14 58I Miles 28 " " 43 ! ! ! ! 8!9 Existing " Proposed DRECPSubareas 66 62 Colorado Desert Desert Renewable Energy Conservation Plan (DRECP) ACECs within the Colorado Desert Subarea # Proposed ACECs 12 Cadiz Valley Chuckwalla Central 19 (covered in Chuckwalla, see below)) Chuckwalla Extension 20 (covered in Chuckwalla, see below) Chuckwalla Mountains Central 21 (covered in Corn Springs, see below) 22 Chuckwalla to Chemehuevi Tortoise Linkage Joshua Tree to Palen Corridor 33 (covered in Chuckwalla to Chemehuevi Tortoise Linkage) 36 McCoy Valley 37 McCoy Wash 38 Mule McCoy 44 Palen Ford Playa Dunes 48 Picacho Turtle Mountains Corridor 55 (covered in Chuckwalla to Chemehuevi Tortoise Linkage) 56 Upper McCoy # Existing ACECs (within DRECP boundary) 2 Alligator Rock 15 Chuckwalla 16 Chuckwalla Valley Dune Thicket 19 Corn Springs 25 Desert Lily Preserve 56 Mule Mountains 59 Palen Dry Lake 61 Patton's Iron Mountain Divisional Camp 81 Turtle Mountains Cadiz Valley Description/Location: North of Hwy 62, south of Hwy 40 between the Sheep Hole mountains to the west and the Chemehuevi ACEC to the east. Nationally Significant Values: Ecological: The Cadiz Valley contains an enormous variation of Mojave vegetation, from Ajo Lilies to Mojave Yucca. Bighorn, deer and mountain lion easily migrate between basin and range mountains of the Sheephole, Calumet Mountains, Iron Mountains, Kilbeck Hills and Old Woman Mountains with little or no human infrastructure limits. -
Chemehuevi Valley Groundwater Basin Bulletin 118
Hydrologic Region Colorado River California’s Groundwater Chemehuevi Valley Groundwater Basin Bulletin 118 Chemehuevi Valley Groundwater Basin • Groundwater Basin Number: 7-43 • County: San Bernardino • Surface Area: 273,000 acres (427 square miles) Basin Boundaries and Hydrology This basin underlies Chemehuevi Valley in eastern San Bernardino County. The basin is bounded by Havasu Lake on the east and by nonwater-bearing rocks of the Sacramento Mountains on the north, of the Chemehuevi Mountains on the northeast, of the Whipple Mountains on the southeast, of the Turtle Mountains on the west and south (Bishop 1963). The valley is drained by Chemehuevi Wash to Havasu Lake. Annual average precipitation ranges from about 4 to 6 inches. Hydrogeologic Information Water Bearing Formations Groundwater in the basin is found in alluvium and the Bouse Formation. Alluvium. Holocene age younger alluvium, which is found in washes and the floodplain of the Colorado River, is composed of sand, silt and gravel (Metzger and Loeltz 1973). Older alluvium consists of unconsolidated, fine- to coarse-grained sand, pebbles, and boulders with variable amounts of silt and clay. Bouse Formation. The Pliocene age Bouse Formation is composed of a basal limestone bed overlain by interbedded clay, silt, and sand. Thickness of the formation reaches 254 feet (Metzger and Loeltz 1973). The formation is underlain by locally derived fanglomerate and overlain by alluviums of the Colorado River and its tributaries. Restrictive Structures An unnamed fault crosses a portion of the southern side of the basin (Bishop 1963), but it is not known whether or not this fault impedes groundwater flow in the basin. -
Understanding the Source of Water for Selected Springs Within Mojave Trails National Monument, California
ENVIRONMENTAL FORENSICS, 2018 VOL. 19, NO. 2, 99–111 https://doi.org/10.1080/15275922.2018.1448909 Understanding the source of water for selected springs within Mojave Trails National Monument, California Andy Zdon, PG, CHg, CEGa, M. Lee Davisson, PGb and Adam H. Love, Ph.D.c aTechnical Director – Water Resources, PARTNER ENGINEERING AND SCIENCE, INC., Santa Ana, CA, Sacramento, CA; bML Davisson & Associates, Inc., Livermore, CA; cVice President/Principal Scientist, Roux Associates, Inc., Oakland, CA ABSTRACT KEYWORDS While water sources that sustain many of the springs in the Mojave Desert have been poorly Water resources; clipper understood, the desert ecosystem can be highly dependent on such resources. This evaluation mountains; bonanza spring; updates the water resource forensics of Bonanza Spring, the largest spring in the southeastern groundwater; forensics; Mojave Desert. The source of spring flow at Bonanza Spring was evaluated through an integration isotopes of published geologic maps, measured groundwater levels, water quality chemistry, and isotope data compiled from both published sources and new samples collected for water chemistry and isotopic composition. The results indicate that Bonanza Spring has a regional water source, in hydraulic communication with basin fill aquifer systems. Neighboring Lower Bonanza Spring appears to primarily be a downstream manifestation of surfacing water originally discharged from the Bonanza Spring source. Whereas other springs in the area, Hummingbird, Chuckwalla, and Teresa Springs, each appear to be locally sourced as “perched” springs. These conclusions have important implications for managing activities that have the potential to impact the desert ecosystem. Introduction above Bonanza Spring. Identification of future impacts General information and data regarding springs in the from water resource utilization becomes problematic if Mojave Desert are sparse, and many of these springs are initial baseline conditions are unknown or poorly under- not well understood.