California Essential Habitat Connectivity Plan
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Subsequent Initial Study of Environmental Impact
Cayucos Sanitary District 200 Ash Avenue Cayucos CA 93430 www.cayucossd.org • 805-773-4658 Cayucos Sustainable Water Project (CSWP) Subsequent Mitigated Negative Declaration for the Estero Marine Terminal Ocean Outfall Project Component Subsequent Initial Study of Environmental Impact I. ENVIRONMENTAL DETERMINATION FORM 1. Project Title: Cayucos Sustainable Water Project Ocean Outfall 2. Lead Agency Name and Address: Cayucos Sanitary District 200 Ash Avenue / PO Box 333 Cayucos CA 93430 3. Contact Person and Phone Number: David Foote, c/o firma, (805) 781-9800 4. Project Location: Chevron Estero Marine Terminal 4000 Highway 1, Morro Bay, California 93442 5. Project Sponsor's Name and Address: Cayucos Sanitary District 200 Ash Avenue / PO Box 333 Cayucos CA 93430 6. General Plan Designation: The proposed pipeline tie-in site is designated Agriculture. The effluent pipeline conveyances are within public right-of-way (State Route 1) and Waters of the U.S. and State. 7. Zoning: Agriculture (County) and Open Area I/PD (City of Morro Bay west of State Route 1 and the mean high tide line) Cayucos Sustainable Water Project Ocean Outfall Initial Environmental Study Final January 2019 1 Cayucos Sanitary District 200 Ash Avenue Cayucos CA 93430 www.cayucossd.org • 805-773-4658 Cayucos Sustainable Water Project (CSWP) Subsequent Mitigated Negative Declaration for the Estero Marine Terminal Ocean Outfall Project Component 8. Project Description & Regulatory and Environmental setting LOCATION AND BACKGROUND The Project consists of the reuse of an existing ocean conveyance pipe for treated effluent disposal from the proposed and permitted Cayucos Sustainable Water Project’s (CSWP) Water Resource Recovery Facility (WRRF) by the Cayucos Sanitary District (CSD). -
Biological Report
Biological Report 3093 Beachcomber Drive APN: 065-120-001 Morro Bay, CA Owner: Paul LaPlante Permit #29586 Prepared by V. L. Holland, Ph.D. Plant and Restoration Ecology 1697 El Cerrito Ct. San Luis Obispo, CA 93401 Prepared for: John K Construction, Inc. 110 Day Street Nipomo, CA 93444 [email protected] and Paul LaPlante 1935 Beachcomber Drive Morro Bay, CA 93442 March 5, 2013 BIOLOGICAL SURVEY OF 3093 BEACHCOMBER DRIVE, MORRO BAY, CA 2 TABLE OF CONTENTS EXECUTIVE SUMMARY ..................................................................................... 3 INTRODUCTION AND PURPOSE ...................................................................... 4 LOCATION AND PHYSICAL FEATURES ........................................................ 10 FLORISTIC, VEGETATION, AND WILDLIFE INVENTORY ............................. 11 METHODS ......................................................................................................... 11 RESULTS: FLORA AND VEGETATION ON SITE .......................................... 12 FLORA .............................................................................................................. 12 VEGETATION ..................................................................................................... 13 1. ANTHROPOGENIC (RUDERAL) COMMUNITIES ................................................... 13 2. COASTAL DUNE SCRUB ................................................................................. 15 SPECIAL STATUS PLANT SPECIES .............................................................. -
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. -
California State Parks
1 · 2 · 3 · 4 · 5 · 6 · 7 · 8 · 9 · 10 · 11 · 12 · 13 · 14 · 15 · 16 · 17 · 18 · 19 · 20 · 21 Pelican SB Designated Wildlife/Nature Viewing Designated Wildlife/Nature Viewing Visit Historical/Cultural Sites Visit Historical/Cultural Sites Smith River Off Highway Vehicle Use Off Highway Vehicle Use Equestrian Camp Site(s) Non-Motorized Boating Equestrian Camp Site(s) Non-Motorized Boating ( Tolowa Dunes SP C Educational Programs Educational Programs Wind Surfing/Surfing Wind Surfing/Surfing lo RV Sites w/Hookups RV Sites w/Hookups Gasquet 199 s Marina/Boat Ramp Motorized Boating Marina/Boat Ramp Motorized Boating A 101 ed Horseback Riding Horseback Riding Lake Earl RV Dump Station Mountain Biking RV Dump Station Mountain Biking r i S v e n m i t h R i Rustic Cabins Rustic Cabins w Visitor Center Food Service Visitor Center Food Service Camp Site(s) Snow Sports Camp Site(s) Geocaching Snow Sports Crescent City i Picnic Area Camp Store Geocaching Picnic Area Camp Store Jedediah Smith Redwoods n Restrooms RV Access Swimming Restrooms RV Access Swimming t Hilt S r e Seiad ShowersMuseum ShowersMuseum e r California Lodging California Lodging SP v ) l Klamath Iron Fishing Fishing F i i Horse Beach Hiking Beach Hiking o a Valley Gate r R r River k T Happy Creek Res. Copco Del Norte Coast Redwoods SP h r t i t e s Lake State Parks State Parks · S m Camp v e 96 i r Hornbrook R C h c Meiss Dorris PARKS FACILITIES ACTIVITIES PARKS FACILITIES ACTIVITIES t i Scott Bar f OREGON i Requa a Lake Tulelake c Admiral William Standley SRA, G2 • • (707) 247-3318 Indian Grinding Rock SHP, K7 • • • • • • • • • • • (209) 296-7488 Klamath m a P Lower CALIFORNIA Redwood K l a Yreka 5 Tule Ahjumawi Lava Springs SP, D7 • • • • • • • • • (530) 335-2777 Jack London SHP, J2 • • • • • • • • • • • • (707) 938-5216 l K Sc Macdoel Klamath a o tt Montague Lake A I m R National iv Lake Albany SMR, K3 • • • • • • (888) 327-2757 Jedediah Smith Redwoods SP, A2 • • • • • • • • • • • • • • • • • • (707) 458-3018 e S Mount a r Park h I4 E2 t 3 Newell Anderson Marsh SHP, • • • • • • (707) 994-0688 John B. -
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. -
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. -
Wilderness Study Areas
I ___- .-ll..l .“..l..““l.--..- I. _.^.___” _^.__.._._ - ._____.-.-.. ------ FEDERAL LAND M.ANAGEMENT Status and Uses of Wilderness Study Areas I 150156 RESTRICTED--Not to be released outside the General Accounting Wice unless specifically approved by the Office of Congressional Relations. ssBO4’8 RELEASED ---- ---. - (;Ao/li:( ‘I:I)-!L~-l~~lL - United States General Accounting OfTice GAO Washington, D.C. 20548 Resources, Community, and Economic Development Division B-262989 September 23,1993 The Honorable Bruce F. Vento Chairman, Subcommittee on National Parks, Forests, and Public Lands Committee on Natural Resources House of Representatives Dear Mr. Chairman: Concerned about alleged degradation of areas being considered for possible inclusion in the National Wilderness Preservation System (wilderness study areas), you requested that we provide you with information on the types and effects of activities in these study areas. As agreed with your office, we gathered information on areas managed by two agencies: the Department of the Interior’s Bureau of Land Management (BLN) and the Department of Agriculture’s Forest Service. Specifically, this report provides information on (1) legislative guidance and the agency policies governing wilderness study area management, (2) the various activities and uses occurring in the agencies’ study areas, (3) the ways these activities and uses affect the areas, and (4) agency actions to monitor and restrict these uses and to repair damage resulting from them. Appendixes I and II provide data on the number, acreage, and locations of wilderness study areas managed by BLM and the Forest Service, as well as data on the types of uses occurring in the areas. -
Beolobical Survey
UNITED STATES DEPARTMENT OF THE INTERIOR BEOLOBICAL SURVEY Generalized geologic map of the Big Maria Mountains region, northeastern Riverside County, southeastern California by Warren Hamilton* Open-File Report 84-407 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature 1984 *Denver, Colorado MAP EXPLANATION SURFICIAL MATERIALS Quaternary Qa Alluvium, mostly silt and sand, of modern Hoiocene Colorado River floodplain. Pleistocene Qe Eolian sand. Tertiary Of Fanglomerate and alluvium, mostly of local PIi ocene origin and of diverse Quaternary ages. Includes algal travertine and brackish-water strata of Bouse Formation of Pliocene age along east and south sides of Big Maria and Riverside Mountains, Fanglomerate may locally be as old as Pliocene. MIOCENE INTRUSIVE ROCKS Tertiary In Riverside Mountains, dikes of 1 e u c o r h y o 1 i t e Miocene intruded along detachment fault. In northern Big Maria Mountains, plugs and dikes of hornbl ende-bi at i te and bioti te-hornbl ende rhyodacite and quartz latite. These predate steep normal faults, and may include rocks both older and younger than low-angle detachment faults. Two hornblende K-Ar determinations by' Donna L. Martin yield calculated ages of 10. 1 ±4.5 and' 21.7 + 2 m.y ROCKS ABOVE DETACHMENT FAULTS ROCKS DEPOSITED SYNCHRONOUSLY WITH EXTENSIONAL FAULTING L o w e r Tob Slide breccias, partly monolithologic, and Mi ocene Jos extremely coarse fanglomerate. or upper Tos Fluvial and lacustrine strata, mostly red. 01i gocene Tob T o v Calc-alkalic volcanic rocks: quartz latitic ignimbrite, and altered dacitic and andesitic flow rocks. -
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). -
Sentinel 10-27
The San Bernardino County News of Note from Around the Largest County in the Lower 48 States Friday, OctoberSentinel 27, 2017 A Fortunado Publication in conjunction with Countywide News Service 10808 Foothill Blvd. Suite 160-446 Rancho Cucamonga, CA 91730 (951) 567-1936 Wonder Valley Chromium & Arsenic H2O Levels 1,000 Times Over Limit Industry’s Tres By Mark Gutglueck Indications are, how- miles northeast of the Amboy Road and State nent living structures Hermanos Sun The San Bernardino ever, that there is no east entrance to Joshua Route 62 run through built by homesteaders County Fire Depart- county agency mandated Tree National Park. The Wonder Valley and ex- under the Small Tract Power Plan ment’s reflexive move to with responsibility to town lies south of the ist as the community’s Act, also known as the Begets Greater protect its firefighters in safeguard residents and Sheep Hole Mountains primary paved roads, “Baby Homestead Act,” reaction to the discovery their drinking water sup- and Bullion Mountains with the vast major- between 1938 and the Uncertainty of well water contamina- ply in the face of the risk and north of the Pinto ity of the community’s mid-1960s, once dot- tion in Wonder Valley that has been identified. Mountains at an eleva- streets existing as dirt ted the landscape in the is raising the specter of Wonder Valley is an tion range of 1,200 feet roads or ones that have 150-square-mile area, a wider contamination unincorporated com- to 1,800 feet near the been oiled and impacted. -
Appendix D Building Descriptions and Climate Zones
Appendix D Building Descriptions and Climate Zones APPENDIX D: Building Descriptions The purpose of the Building Descriptions is to assist the user in selecting an appropriate type of building when using the Air Conditioning estimating tools. The selected building type should be the one that most closely matches the actual project. These summaries provide the user with the inputs for the typical buildings. Minor variations from these inputs will occur based on differences in building vintage and climate zone. The Building Descriptions are referenced from the 2004-2005 Database for Energy Efficiency Resources (DEER) Update Study. It should be noted that the user is required to provide certain inputs for the user’s specific building (e.g. actual conditioned area, city, operating hours, economy cycle, new AC system and new AC system efficiency). The remaining inputs are approximations of the building and are deemed acceptable to the user. If none of the typical building models are determined to be a fair approximation then the user has the option to use the Custom Building approach. The Custom Building option instructs the user how to initiate the Engage Software. The Engage Software is a stand-alone, DOE2 based modeling program. July 16, 2013 D-1 Version 5.0 Prototype Source Activity Area Type Area % Area Simulation Model Notes 1. Assembly DEER Auditorium 33,235 97.8 Thermal Zoning: One zone per activity area. Office 765 2.2 Total 34,000 Model Configuration: Matches 1994 DEER prototype HVAC Systems: The prototype uses Rooftop DX systems, which are changed to Rooftop HP systems for the heat pump efficiency measures. -
Desert Bighorn Sheep Report
California Department of Fish and Wildlife Region 6 Desert Bighorn Sheep Status Report November 2013 to October 2016 A summary of desert bighorn sheep population monitoring and management by the California Department of Fish and Wildlife Authors: Paige Prentice, Ashley Evans, Danielle Glass, Richard Ianniello, and Tom Stephenson Inland Deserts Region California Department of Fish and Wildlife Desert Bighorn Status Report 2013-2016 California Department of Fish and Wildlife Inland Deserts Region 787 N. Main Street Ste. 220 Bishop, CA 93514 www.wildlife.ca.gov This document was finalized on September 6, 2018 Page 2 of 40 California Department of Fish and Wildlife Desert Bighorn Status Report 2013-2016 Table of Contents Executive Summary …………………………………………………………………………………………………………………………………4 I. Monitoring ............................................................................................................................................ 6 A. Data Collection Methods .................................................................................................................. 7 1. Capture Methods .......................................................................................................................... 7 2. Survey Methods ............................................................................................................................ 8 B. Results and Discussion .................................................................................................................... 10 1. Capture Data ..............................................................................................................................