Of California Has Identified the Cuyama Valley
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Pamphlet to Accompany Geologic Map of the Apache Canyon 7.5
GEOLOGIC MAP AND DIGITAL DATABASE OF THE APACHE CANYON 7.5’ QUADRANGLE, VENTURA AND KERN COUNTIES, CALIFORNIA By Paul Stone1 Digital preparation by P.M. Cossette2 Pamphlet to accompany: Open-File Report 00-359 Version 1.0 2000 This report is preliminary and has not been reviewed for conformity with U. S. Geological Survey editorial standards. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U. S. Government. This database, identified as "Geologic map and digital database of the Apache Canyon 7.5’ quadrangle, Ventura and Kern Counties, California," has been approved for release and publication by the Director of the USGS. Although this database has been reviewed and is substantially complete, the USGS reserves the right to revise the data pursuant to further analysis and review. This database is released on condition that neither the USGS nor the U. S. Government may be held liable for any damages resulting from its use. U.S. Geological Survey 1 345 Middlefield Road, Menlo Park, CA 94025 2 West 904 Riverside Avenue, Spokane, WA 99201 1 CONTENTS Geologic Explanation............................................................................................................. 3 Introduction................................................................................................................................. 3 Stratigraphy................................................................................................................................ 4 Structure .................................................................................................................................... -
Habitat Connectivity Planning for Selected Focal Species in the Carrizo Plain
Habitat Connectivity Planning for Selected Focal Species in the Carrizo Plain BLM Chuck Graham Chuck Graham Agena Garnett-Ruskovich Advisory Panel Members: Paul Beier, Ph.D., Northern Arizona University Patrick Huber, Ph.D., University of California Davis Steve Kohlmann, Ph.D., Tierra Resource Management Bob Stafford, California Department of Fish and Game Brian Cypher, Ph.D., University of Stanislaus Endangered Species Recovery Program also served as an Advisory Panel Member when this project was under the California Energy Commission’s jurisdiction. Preferred Citation: Penrod, K., W. Spencer, E. Rubin, and C. Paulman. April 2010. Habitat Connectivity Planning for Selected Focal Species in the Carrizo Plain. Prepared for County of San Luis Obsipo by SC Wildlands, http://www.scwildlands.org Habitat Connectivity Planning for Selected Focal Species in the Carrizo Plain Table of Contents 1. Executive Summary 2. Introduction 2.1. Background and Project Need 3. Project Setting 3.1. The Study Area 3.1.1. Location 3.1.2. Physical Features 3.1.3. Biological Features 3.1.4. Human Features 3.2. The Proposed Energy Projects 3.2.1. Topaz Solar Farm 3.2.2. SunPower – California Valley Solar Ranch 4. The Focal Species 4.1. Pronghorn antelope 4.2. Tule elk 4.3. San Joaquin kit fox 5. Conservation Planning Approach 5.1. Modeling Baseline Conditions Of Habitat Suitability And Connectivity For Each Focal Species 5.1.1. Compilation And Refinement Of Digital Data Layers 5.1.2. Modeling Habitat Suitability 5.1.3. Modeling Landscape Permeability 5.1.4. Species-Specific Model Input Data And Conceptual Basis For Model Development 5.1.4.1. -
Geologic Map of the Northwestern Caliente Range, San Luis Obispo County, California
USGS L BRARY RESTON 1111 111 1 11 11 II I I II 1 1 111 II 11 3 1818 0001k616 3 DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geologic map of the northwestern Caliente Range, San Luis Obispo County, California by J. Alan Bartowl Open-File Report 88-691 This map is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by USGS 'Menlo Park, CA 1988 it nedelitil Sow( diSti) DISCUSSION INTRODUCTION The map area lies in the southern Coast Ranges of California, north of the Transverse Ranges and west of the southern San Joaquin Valley. This region is part of the Salinia-Tujunga composite terrane that is bounded on the northeast by the San Andreas fault (fig. 1) and on the southwest by the Nacimiento fault zone (Vedder and others, 1983). The Chimineas fault of this map is inferred to be the boundary between the Salinia and the Tujunga terranes (Ross, 1972; Vedder and others, 1983). Geologic mapping in the region of the California Coast Ranges that includes the area of this map has been largely the work of T.W. Dibblee, Jr. Compilations of geologic mapping at a scale of 1:125,000 (Dibblee, 1962, 1973a) provide the regional setting for this map, the northeast border of which lies about 6 to 7 km southwest of the San Andreas fault. Ross (1972) mapped the crystalline basement rocks in the vicinity of Barrett Creek, along the northeast side of the Chimineas fault ("Barrett Ridge" of Ross, 1972). -
Flora and Fauna Values
includes many endemic species – those species found nowhere else in the world except for within one specific region. Roughly 30 endemic animal As part of one of the top 35 global biodiversity hotspots, species and 35 endemic plant species are found in the Santa Barbara Santa Barbara County is home to a remarkable array of region.6 Many have evolved in this area of California because of geograph- species, habitats and transition zones which stem from the ic isolation, rare soil substrates, and limited mobility. Examples of endemic regions unique mix of topography and climate.1 The species in the County include the Lompoc kangaroo rat, kinsel oak, and the FLORA AND County is unique within the California Floristic Province Santa Barbara jewel flower. Many other species are endemic to our region (the biodiversity hotspot the County is in) as it has fewer of California but are found outside the County including the Mount Pinos FAUNA developed or altered natural landscapes than other parts chipmunk, black bellied slender salamander and Cristina’s timema. of the hotspot; this adds to the value for conservation within Santa Barbara County. Vegetation provides habitat and home for the many unique and common animal species in the County, and varies greatly from north to Vegetation communities and species from California’s south, east to west, and often from valley to valley. Of the 31 vegetation Central Coast and South Coast, the Sierra Nevada, and the macrogroups found in California, 19 are found within Santa Barbara San Joaquin Valley can all be found locally due to conver- County.9 Chaparral is the most common vegetation type in the County gence of four ecoregions within the County: Southern and covers much of the upland watersheds where it also serves as a California Coast, Southern California Mountains and Central Coast riverine, riparian ecosystems, and wetlands provide some of natural buffer against erosion. -
Archaeological Investigations at the Oak Flat Site (Ca-Sba-3931) Santa Barbara County, California
ARCHAEOLOGICAL INVESTIGATIONS AT THE OAK FLAT SITE (CA-SBA-3931) SANTA BARBARA COUNTY, CALIFORNIA by ESTHER LOUISE DRAUCKER A thesis submitted to the Master of Arts Graduate Program in Anthropology at California State University, Bakersfield, in partial fulfillment of the requirements for the degree of MASTER OF ARTS in ANTHROPOLOGY Bakersfield, California 2014 Copyright By Esther Louise Draucker 2014 Frontispiece: Overview of CA-SBA-3931 (Oak Flat), looking west. The base of the rock feature can be discerned in the center. i ABSTRACT The region occupied by the Chumash of south-central California were divided into sub-groups who occupied different territories and spoke separate, but related languages. The Cuyama sub-group occupied the Cuyama Valley and the surrounding hills and mountains. Branch Canyon leads roughly south from Cuyama Valley and is known to contain prehistoric archaeological sites. The site chosen for this investigation was not previously recorded, but is a large, level area where many artifacts have been found. The area is covered with little other than wildflowers and grasses, but broken groundstone is visible, and an extensive looter’s hole exists, which suggests a possible prehistoric habitation site. Local residents have recovered many artifacts here, including glass beads, indicating occupation during the historic era. The base of a large, square rock feature overlays the prehistoric site. Very little archaeological exploration has been carried out in Cuyama Valley and its surrounding environs. Few site records exist for the valley, although many sites have been recorded for the southern canyons and the potreros at the top of the Sierra Madre Range. -
October 3, 2018
Cuyama Valley Groundwater Basin Groundwater Sustainability Plan Hydrogeologic Conceptual Model Draft Prepared by: October 2018 Table of Contents Chapter 2 Basin Setting .......................................................................................................2-2 Acronyms 2-3 2.1 Hydrogeologic Conceptual Model ..........................................................................2-4 2.1.1 Useful Terminology ................................................................................................2-4 2.1.2 Regional Geologic and Structural Setting ..............................................................2-5 2.1.3 Geologic History ....................................................................................................2-5 2.1.4 Geologic Formations/Stratigraphy .........................................................................2-8 2.1.5 Faults and Structural Features ............................................................................. 2-17 2.1.6 Basin Boundaries ................................................................................................ 2-26 2.1.7 Principal Aquifers and Aquitards .......................................................................... 2-26 2.1.8 Natural Water Quality Characterization ................................................................ 2-32 2.1.9 Topography, Surface Water and Recharge .......................................................... 2-36 2.1.10 Hydrogeologic Conceptual Model Data Gaps ..................................................... -
DRAFT GROUNDWATER SUSTAINABILITY PLAN SECTION July 2018
DRAFT GROUNDWATER SUSTAINABILITY PLAN SECTION July 2018 CUYAMA VALLEY GROUNDWATER BASIN GROUNDWATER SUSTAINABILITY PLAN DESCRIPTION OF PLAN AREA - DRAFT 2175 North California Blvd., Suite 315 Walnut Creek, CA 94596 925-647-4100 woodardcurran.com COMMITMENT & INTEGRITY DRIVE RESULTS TABLE OF CONTENTS SECTION PAGE 1. PLAN AREA ...................................................................................................................... 1 1.1 Introduction .......................................................................................................... 1 1.2 Plan Area Definition ............................................................................................. 1 1.3 Plan Area Setting ................................................................................................. 1 1.4 Existing Surface Water Monitoring Programs ..................................................... 24 1.5 Existing Groundwater Monitoring Programs ....................................................... 26 1.5.1 Groundwater Elevation Monitoring ............................................................ 26 1.5.2 Groundwater Quality Monitoring ................................................................ 27 1.5.3 Subsidence Monitoring .............................................................................. 28 1.6 Existing Water Management Programs .............................................................. 29 1.6.1 Santa Barbara County Integrated Regional Water Management Plan 2013 ................................................................................................................. -
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. -
The San Joaquin Desert of California: Ecologically Misunderstood and Overlooked
Natural Areas Journal . to advance the preservation of natural diversity A publication of the Natural Areas Association - www.naturalarea.org © Natural Areas Association The San Joaquin Desert of California: Ecologically Misunderstood and Overlooked David J. Germano1,6 1Department of Biology California State University Bakersfield, California, 93311-1022 Galen B. Rathbun2 Lawrence R. Saslaw3 Brian L. Cypher4 Ellen A. Cypher4 Larry M. Vredenburgh5 2Department of Ornithology and Mammalogy California Academy of Sciences Golden Gate Park, San Francisco c/o P.O. Box 202 Cambria, California 93428 3U.S. Bureau of Land Management Bakersfield, California 93308 4Endangered Species Recovery Program California State University-Stanislaus P.O. Box 9622 Bakersfield, CA 93389 5U. S. Bureau of Land Management Bakersfield, California 93308 6 Corresponding author: [email protected]; 661-654-2471 Natural Areas Journal 31:138–147 R E S E A R C H A R T I C L E ABSTRACT: The vegetation community of the San Joaquin Valley of California has been formally classified as a perennial grassland based largely on assumptions of past climax state. However, histori- cal records suggest that the region might be more accurately classified as a desert. The distinction is important in determining the appropriate management strategies for this ecosystem, particularly for the • many rare and endemic taxa that reside there. Abiotic and biotic factors–including low precipitation, arid soils, and desert-adapted plants and vertebrate–are consistent with conditions typical of desert ar- eas. We examined the distributions of these factors to define the extent of the San Joaquin Desert. We conclude that the San Joaquin Desert historically encompassed 28,493 km2 including the western and The San Joaquin southern two thirds of the San Joaquin Valley, and the Carrizo Plain and Cuyama Valley to the south- west. -
Cuyama Valley Groundwater Basin (3-13) Boundary Modification Request
CUYAMA VALLEY GROUNDWATER BASIN (3-13) BOUNDARY MODIFICATION REQUEST TECHNICAL MEMORANDUM April 3, 2018 Prepared for GRAPEVINE CAPITAL MANAGEMENT April 3, 2018 CLEATH-HARRIS GEOLOGISTS 71 Zaca Lane, Suite 140 San Luis Obispo, California 93401 (805) 543-1413 TABLE OF CONTENTS SECTION PAGE INTRODUCTION………………………………………………………………………………….1 DESCRIPTION OF PROPOSED BOUNDARY MODIFICATION (§ 344.6)…………….……...3 Overview of Request for Boundary Modification (§ 344.6(a))……………………………..……...3 Category of Proposed Boundary Modification (§ 344.6(a)(1))…………………………………….3 Identification of all Affected Basins or Subbasins (§ 344.6(a)(2))………………………………….3 Proposed name for each new subbasin (§ 344.6 (a)(3)…….…………….…………………………4 GENERAL INFORMATION (§344.10)…………………………………………………………...5 Description of lateral basin boundaries and definable bottom (§ 344.10(a))……………………….5 Graphical Map of lateral basin boundaries (§344.10 (b)).………………………………………….5 HYDROGEOLOGIC CONCEPTUAL MODEL (§ 344.12)……………………………………….6 Principal Aquifers and Regional Aquitard (§ 344.12(1))…………………………………………..6 Lateral Boundaries (§ 344.12(2))……………………………………………………………….......8 Geologic Features Impacting Groundwater Flow (§ 344.12(2)(A,B,C))…………………………...9 Key Surface Water Bodies and Significant Recharge Sources (§ 344.12(2)(D))…………………12 Recharge and Discharge Areas (§ 344.12(3)) …………………………………………………….12 Definable Bottom of the Basin (§ 344.12(4))……………………………………………………..13 TECHNICAL INFORMATION FOR SCIENTIFIC MODIFICATION (§ 344.14)……………...14 Qualified Map (§ 344.14(a)(1))…………………………………………………………………...14 Technical -
Vegetation Descriptions CENTRAL COAST and MONTANE ECOLOGICAL PROVINCE
Vegetation Descriptions CENTRAL COAST AND MONTANE ECOLOGICAL PROVINCE CALVEG ZONE 6 March 19, 2009 Note: Central California Coast Section (261A) is referred to as the “Coast” Section and Central California Coast Ranges Section (M262A) is referred to as the “Ranges” Section CONIFER FOREST / WOODLAND AB SANTA LUCIA FIR ALLIANCE Santa Lucia Fir (Abies bracteata) is found only in the Santa Lucia Range (Los Padres NF) as a narrow endemic species, usually within 15 miles (24 km) of the coast (Coast Section). This Fir is the dominant conifer in this Alliance but it also occurs as scattered inviduals or clumps of trees within Mixed Conifer – Pine sites. It is most common near the crest of the mountains and towards the north, where it often associates with Coast Live Oak (Quercus agrifolia) and low-elevation shrubs in droughty summit sites, on rocky slopes or in protected ravines. Slopes are usually steep and less fire-prone than other mixed hardwood areas of the forest; elevation ranges are in the order 2000 – 4600 ft (610 - 1402 m). DF PACIFIC DOUGLAS-FIR ALLIANCE Pacific Douglas-fir (Pseudotsuga menziesii) is generally limited to northern, central, and eastern California but occurs in scattered stands south to the Santa Ynez Mountains (Los Padres NF) close to the coast (within the South Coast and Montane Ecological zone). Within this zone, the Alliance has been mapped in four subsections of the Coast Section below about 3300 ft (1010 m). Conifer associates in this area are Redwood (Sequoia sempervirens) and Ponderosa Pine (Pinus ponderosa) with Coast Live Oak (Quercus agrifolia) and Tanoak (Lithocarpus densiflorus) the main hardwood associates. -
Carrizo Plain National Monument Map and Guide
Welcome to Beetle Carrizo Plain National Monument Things to Do Nature & Science Carrizo Plain At less than 100 air miles from Los Angeles, Carrizo Plain Carrizo Plain National Monument is a great place to Hiking Equestrian Use The Carrizo Plain is a dramatic landscape in a largely April North American Plate. During the last 11 million National Monument National Monument is a remnant of a natural habitat enjoy nature and witness human history. People visit undeveloped state. Its designation as a National April temperatures are usually more consistent and are years, the San Andreas Fault has moved the Hiking in Carrizo is generally self-guided and takes place Equestrian use is permitted on the Carrizo Plain. Trailer where antelope and elk grazed and wildflowers swept the Monument to view wildlife, to see the spectacular Monument was intended to conserve the Carrizo often in the 70s or higher, making it often times the Pacific Plate some 183 miles (295 km). The on roads, trails, and cross-country. There are only a few parking is available, but limited to already impacted areas the spring landscape. Within the Plain are vast open wildflower displays in the spring, to walk along the San Plain's many significant wild and natural values. Here, “peak” for wildflowers. All of the flowers seen in March Carrizo Plain is world-famous for spectacular developed trails within the Monument. These include the such as campgrounds and parking areas. Equestrians grasslands, white alkali flats of the ancient Soda Lake, Andreas Fault at Wallace Creek, to visit the pictographs vast open plains are backed by stark mountain ridges, will usually continue to bloom through April.