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Breeding Birds of Four Isolated Mountains in Southern California
WESTERN BIRDS Volume 24, Number 4, 1993 BREEDING BIRDS OF FOUR ISOLATED MOUNTAINS IN SOUTHERN CALIFORNIA JOAN EASTON LENTZ, 433 PimientoLn., Santa Barbara,California 93108 The breedingavifaunas of FigueroaMountain and Big PineMountain in SantaBarbara County and Pine Mountain and Mount Pinos in Venturaand Kern countiesare of great ornithologicalinterest. These four mountains supportislands of coniferousforest separated by otherhabitats at lower elevations. Little information on the birds of the first three has been publishedpreviously. From 1981 to 1993, I, withthe helpof a numberof observers,censused the summer residentbirds of these four mountains,paying particular attentionto the speciesrestricted to highelevations. By comparingthese avifaunaswith each other, as well as with those of the San Gabriel,San Bernardino,and San Jacinto mountains, and the southernSierra Nevada, I hopeto addto currentknowledge of thestatus and distribution of montane birds in southern California. VEGETATIO51AND GEOGRAPHY The patternof vegetationin the surveyareas is typicalof thatfound on manysouthern California mountains. Generally, the south- and west-facing slopesof the mountainsare coveredwith chaparralor pinyon-juniper woodlandalmost to the summits.On the north-facingslopes, however, coolertemperatures and more mesic conditions support coniferous forest, which often reaches far down the mountainsides. Because the climate is arid, few creeksor streamsflow at high elevations,and most water is availablein the form of seepsor smallsprings. BothFigueroa (4528 feet, 1380 m) andBig Pine (6828 feet,2081 m) mountainsare locatedin the San RafaelRange, the southernmostof the CoastRanges (Figure 1, Norrisand Webb 1990). The San RafaelMoun- tainsare borderedby the SierraMadre, a low chaparral-coveredrange, to the northand the CuyamaValley to the northeast.The SisquocRiver drains west from the San Rafael Mountains and Sierra Madre to the Santa Maria River.To the southlies the foothillgrassland of the SantaYnez Valley. -
4.2 Agriculture and Forest Resources
4.2 Agriculture and Forest Resources 4.2 AGRICULTURE AND FOREST RESOURCES This section evaluates the potential impacts to agriculture and forest resources associated with implementation of the 2050 RTP/SCS. The information presented was compiled from multiple sources, including the County of San Diego, the State of California Department of Conservation (DOC), the United States Department of Agriculture (USDA), CAL FIRE, and local jurisdictions. 4.2.1 EXISTING CONDITIONS Agriculture Overview of Agriculture in the Region Agriculture is not only an important contributor to the economy of the San Diego region; it also is a primary land use in the unincorporated area of the region. San Diego County contains 6,687 farms and agriculture ranked fifth as a component of the region’s economic resources (County of San Diego 2010). San Diego County is the 16th largest agricultural economy among all counties in the nation. The region’s unique topography creates a wide variety of microclimates resulting in nearly 30 different types of vegetation communities. This diversity allows San Diego farmers to grow over 200 different agricultural commodities, such as strawberries along the coast, apples in the mountain areas, and palm trees in the desert (County of San Diego 2010). The region ranks first in both California and the nation in production value of nursery plants, floriculture, and avocados. Statewide, San Diego County is in the top five counties for producing cucumbers, mushrooms, tomatoes, boysenberries and strawberries, grapefruit, Valencia oranges, tangelos and tangerines, honey, and eggs. San Diego County has the largest community of organic growers in the state and nation, with 374 farms growing more than 175 crops (County of San Diego 2009). -
Springs of California
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIBECTOB WATER- SUPPLY PAPER 338 SPRINGS OF CALIFORNIA BY GEKALD A. WARING WASHINGTON GOVERNMENT PRINTING OFFICE 1915 CONTENTS. Page. lntroduction by W. C. Mendenhall ... .. ................................... 5 Physical features of California ...... ....... .. .. ... .. ....... .............. 7 Natural divisions ................... ... .. ........................... 7 Coast Ranges ..................................... ....•.......... _._._ 7 11 ~~:~~::!:: :~~e:_-_-_·.-.·.·: ~::::::::::::::::::::::::::::::::::: ::::: ::: 12 Sierra Nevada .................... .................................... 12 Southeastern desert ......................... ............. .. ..... ... 13 Faults ..... ....... ... ................ ·.. : ..... ................ ..... 14 Natural waters ................................ _.......................... 15 Use of terms "mineral water" and ''pure water" ............... : .·...... 15 ,,uneral analysis of water ................................ .. ... ........ 15 Source and amount of substances in water ................. ............. 17 Degree of concentration of natural waters ........................ ..· .... 21 Properties of mineral waters . ................... ...... _. _.. .. _... _....• 22 Temperature of natural waters ... : ....................... _.. _..... .... : . 24 Classification of mineral waters ............ .......... .. .. _. .. _......... _ 25 Therapeutic value of waters .................................... ... ... 26 Analyses -
Area Adventure Hat Creek Ranger District Lassen National Forest
Area Adventure Hat Creek Ranger District Lassen National Forest Welcome The following list of recreation activities are avail- able in the Hat Creek Recreation Area. For more detailed information please stop by the Old Station Visitor Information Center, open April - December, or our District Office located in Fall River Mills. Give Hat Creek Rim Overlook - Nearly 1 million years us a call year-around Mon.- Fri. at (530) 336-5521. ago, active faulting gradually dropped a block of Enjoy your visit to this very interesting country. the Earth’s crust (now Hat Creek Valley) 1,000 feet below the top of the Hat Creek Rim, leaving behind Subway Cave - See an underground cave formed this large fault scarp. This fault system is still “alive by flowing lava. Located just off Highway 89, 1/4 and cracking”. mile north of Old Station junction with Highway 44. The lava tube tour is self guided and the walk is A heritage of the Hat Creek area’s past, it offers mag- 1/3 mile long. Bring a lantern or strong flashlight nificent views of Hat Creek Valley, Lassen Peak, as the cave is not lighted. Sturdy Shoes and a light Burney Mountain, and, further away, Mt. Shasta. jacket are advisable. Subway Cave is closed during the winter months. Fault Hat Creek Rim Fault Scarp Vertical movement Hat Creek V Cross Section of a Lava Tube along this fault system alley dropped this block of earth into its present position Spattercone Trail - Walk a nature trail where volca- nic spattercones and other interesting geologic fea- tures may be seen. -
Geologic Gems of California's State Parks
STATE OF CALIFORNIA – EDMUND G. BROWN JR., GOVERNOR NATURAL RESOURCES AGENCY – JOHN LAIRD, SECRETARY CALIFORNIA GEOLOGICAL SURVEY DEPARTMENT OF PARKS AND RECREATION – LISA MANGAT, DIRECTOR JOHN D. PARRISH, Ph.D., STATE GEOLOGIST DEPARTMENT OF CONSERVATION – DAVID BUNN, DIRECTOR PLATE 1 The rugged cliffs of Del Norte Coast Redwoods State Park are composed of some of California’s Bio-regions the most tortured, twisted, and mobile rocks of the North American continent. The California’s Geomorphic Provinces rocks are mostly buried beneath soils and covered by vigorous redwood forests, which thrive in a climate famous for summer fog and powerful winter storms. The rocks only reveal themselves in steep stream banks, along road and trail cut banks, along the precipitous coastal cliffs and offshore in the form of towering rock monuments or sea stacks. (Photograph by CalTrans staff.) Few of California’s State parks display impressive monoliths adorned like a Patrick’s Point State Park displays a snapshot of geologic processes that have castle with towering spires and few permit rock climbing. Castle Crags State shaped the face of western North America, and that continue today. The rocks Park is an exception. The scenic beauty is best enjoyed from a distant exposed in the seacliffs and offshore represent dynamic interplay between the vantage point where one can see the range of surrounding landforms. The The Klamath Mountains consist of several rugged ranges and deep canyons. Klamath/North Coast Bioregion San Joaquin Valley Colorado Desert subducting oceanic tectonic plate (Gorda Plate) and the continental North American monolith and its surroundings are a microcosm of the Klamath Mountains The mountains reach elevations of 6,000 to 8,000 feet. -
Nativeandintroducedearthworms
United States Department of Native and Introduced Earthwormsfrom Agriculture Forest Service Selected Chaparral, Woodland, and Pacific Southwest Research Station Riparian Zones in Southern California General Technical Report PSW-GTR-142 Hulton B. Wood Samuel W. James Wood, Hulton B.; James, Samuel W. 1993. Native and introduced earthworms from selected chaparral, woodland, and riparian zones in southern California. Gen. Tech. Rep. PSW-GTR142. Albany, CA: Pacific Southwest Research Station, Forest Service, U.S. Department of Agriculture; 20 p. Relatively little is known about the earthworm fauna of southern California. Some 20 different species of earthworms were collected and identified in a survey of various southern California wildland habitats. The ecology and biology of earthworms are outlined, and the results of the survey are documented. Introduced species belonging to the Lumbricidae family were encountered most often; however, native species, primarily of genera Argilophilus and Diplocardia, are widely, distributed. Several of the natives collected are believed to be new species. Habitats for both the native and introduced species ranged from riparian zones to relatively dry chaparral sites. Preference of earthworms for certain types of plant communities began to emerge even in this somewhat limited survey: oak and grass being the most preferred, and conifers the least. Geographical separation of the two principal native genera occurs at about 34°N. Further research is needed relative to earthworm ecology, impacts on soils, ecosystem dynamics, and fire. An appendix includes all collection records by location, and vegetation and soil type. Retrieval terms: earthworms, Mediterranean ecosystems, southern California, new species, Lumbricidae, Megascolecidae, Acanthodrilinae, Ocnerodrilinae, Sparganophilidae, soil, habitat, chaparral, grassland, woodland, riparian, aquatic The Authors: Hulton B. -
V. R. Todd and R. E. Learned and Thomas J. Peters and Ronald T
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP MF-1547-A ^UNITED STATES GEOLOGICAL SURVEY MINERAL RESOURCE POTENTIAL OF THE SILL HILL, HADSER, AND CALIENTE ROADLESS AREAS, SAN DIEGO COUNTY, CALIFORNIA SUMMARY REPORT By V. R. Todd and R. E. Learned U.S. Geological Survey and Thomas J. Peters and Ronald T. Mayerle U.S. Bureau of Mines STUDIES RELATED TO WILDERNESS Under the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and the Joint Conference Report on Senate Bill 4, 88th Congress, the U.S. Geological Survey and the U.S. Bureau of Mines have been conducting mineral surveys of wilderness and primitive areas. Areas officially designated as "wilderness," "wild," or "canoe" when the act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied. The act provided that areas under consideration for wilderness designation should be studied for suitability for incorporation into the Wilderness System. The mineral surveys constitute one aspect of the suitability studies. The act directs that the results of such surveys are to be made available to the public and be submitted to the President and the Congress. This report discusses the results of min eral surveys of the Sill Hill (5-304), Hauser (5-021), and Caliente (5-017) Roadless Areas, Cleveland National Forest, San Diego dpunty, California. SUMMARY The Sill Hill, Hauser, and Caliente Roadless Areas comprise approximately 20,000 acres in the Cleveland National Forest, San Diego County, Calif, (fig. 1). Geological and geochemical investigations have been conducted by the U.S. -
Palms to Pines Scenic Byway Corridor Management Plan
Palms to Pines Scenic Byway Corridor Management Plan PALMS TO PINES STATE SCENIC HIGHWAY CALIFORNIA STATE ROUTES 243 AND 74 June 2012 This document was produced by USDA Forest Service Recreation Solutions Enterprise Team with support from the Federal Highway Administration and in partnership with the USDA Forest Service Pacific Southwest Region, the Bureau of Land Management, the California Department of Transportation, California State University, Chico Research Foundation and many local partners. The USDA, the BLM, FHWA and State of California are equal opportunity providers and employers. In accordance with Federal law, U.S. Department of Agriculture policy and U.S. Department of Interior policy, this institution is prohibited from discriminating on the basis of race, color, national origin, sex, age or disability. (Not all prohibited bases apply to all programs.) To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326-W, Whitten Building, 1400 Independence Avenue, SW, Washington, DC 20250-9410 or call (202) 720- 5964 (voice and TDD). Table of Contents Chapter 1 – The Palms to Pines Scenic Byway .........................................................................1 Introduction ................................................................................................................................. 1 Benefits of National Scenic Byway Designation .......................................................................... 2 Corridor Management Planning ................................................................................................. -
Distribution, Status, and Origin of Water Pipits Breeding in California ’
The Condor89:788-797 0 The CooperOrnithological Society 1987 DISTRIBUTION, STATUS, AND ORIGIN OF WATER PIPITS BREEDING IN CALIFORNIA ’ JON H. MILLER 1034 ShattuckAvenue, Berkeley, CA 94707 MICHAEL T. GREEN Department of Biology, Universityof North Carolina, Chapel Hill, NC 27514 Abstract. We investigatedthe racial identity, distribution, and abundanceof WaterPipits (Anthusspinoletta) breeding in the mountainsof California.This commonnesting species of alpinetundra was not knownto breedin Californiauntil the 1970s;a reviewof historical evidencesuggests recent colonization. Mensural and plumagecomparisons show California populationsto be A. s. alticola, the breedingrace of the Rocky Mountains. This is of biogeographicalinterest, because the abundantwintering and migratorypipit of California is A. s. pacificus,while alticola normally occurshundreds of miles to the east.Water Pipits currentlynest in mesicalpine vegetation throughout much of the southernand centralSierra Nevada.Breeding densities are highestand mostuniform in the southernmostpart of this range.The only known breedingpopulation in California outsideof the Sierra Nevada occurson San Gorgonio Mountain in southernCalifornia. We hypothesizethat the previous absenceor rarity of breeding Water Pipits in the Sierra Nevada may be attributable to the most recentpaleoclimatic xerothermic period, the Hypsithermal(ca. 5,000 to 2,900 years BP), whichimuoverished many alnine biotasof arctic-oldcordilleran affinitv. Climate and habitat differencesmay prevenipa$cus from breedingin California, and geographicbarriers may have hindered colonization by alticola. The occurrenceand timing of the present colonizationmay be fortuitous.Alternatively, it is possiblethat prior colonizationof Great Basinranges by alticola facilitatedeventual dispersal to the SierraNevada. Key words: Water Pipit; Anthus spinoletta;Sierra Nevada;historical status; colonization; biogeography;alpine. INTRODUCTION and Montana (Verbeek 1970; Miller and Green, The Water Pipit (Anthus spinoletta) is a principal pers. -
Deer Book Part 7 6/29/00 10:09 AM Page 1
Deer Book part 7 6/29/00 10:09 AM Page 1 81 The old adage “you can’t judge a book by its cover” holds true for the value of desert habitats to mule deer. While deer densities are low in the Southern Desert bioregion, some of the largest bucks in the state are taken each year in these arid environments. Photo by Mark Hoshovsky H. Southern Desert 1. Deer Habitats and Ecology The Mojave and Sonoran deserts of California support some of our driest and hottest habitats in the state. It comes as no surprise, then, that these areas support some of our lowest deer densities. The deer that inhabit our southern deserts are also the least understood ecologically in California. These animals, while not migratory like those in the Sierra Nevada, do move long distances in response to changes in the availability of water and forage. Summer rains in the desert cause the germination of annual grasses and forbs, and deer will move to take advantage of this forage. Desert washes and the vegetation in them are especially important for providing cover and food, and free-standing water in the summer seems to be essential for maintaining burro mule deer. Deer Book part 7 6/29/00 10:09 AM Page 2 82 A SPORTSMAN’S GUIDE TO IMPROVING DEER HABITAT IN CALIFORNIA 2. Limiting or Important Habitat Factors The availability of free-standing water in the summer in areas with other- wise appropriate vegetation is thought to be the most important habitat fac- tor for mule deer in most of our southern deserts. -
Individual Perspectives of the California Landscape
INDIVIDUAL PERSPECTIVES OF THE CALIFORNIA LANDSCAPE A Thesis Presented to the Faculty of California State Polytechnic University, Pomona In Partial Fulfillment Of the Requirements for the Degree Master of Landscape Architecture By Cristina M. Plemel 2020 SIGNATURE PAGE PROJECT: INDIVIDUAL PERSPECTIVES OF THE CALIFORNIA LANDSCAPE AUTHOR: Cristina M. Plemel DATE SUBMITTED: Spring 2020 Department of Landscape Architecture Andrew Wilcox Project Committee Chair Professor and Department Chair Philip Pregill Project Committee Member Professor of Landscape Architecture Jared Pierce Project Committee Member Forest Landscape Architect Tahoe National Forest ii ABSTRACT This study took research participants on scenic hikes throughout California to understand landscape preferences utilizing participant photography. There were 8 hikes total and 16 participants. The hikes took place at the following locations: Abbott’s Lagoon in Point Reyes National Seashore, Vivian Creek Trail in the San Gorgonio Wilderness, Strawberry Peak and Mount Baden-Powell in the Angeles National Forest, Mosaic Canyon in Death Valley National Park, Abalone Cove Shoreline Park in Palos Verdes, the South Coast Botanic Garden in Palos Verdes, Loch Lomond in Santa Cruz County, and Mount San Jacinto State Park. Participants were given a disposable camera on each hike and asked to photograph the landscape. After the hikes, film was developed, and participants were emailed digital copies of their photographs and asked to explain why each photo was taken. The literature review has two sections. Part one has a focus on plant communities found in California, while part 2 has a focus on landscape preferences, perception, and scenic beauty of landscape. iii TABLE OF CONTENTS SIGNATURE PAGE .............................................................................................................. ii ABSTRACT ........................................................................................................................ -
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.