Geological Gems of California State Parks by California Geological Survey and California State Parks State of California Edmund G

Total Page:16

File Type:pdf, Size:1020Kb

Geological Gems of California State Parks by California Geological Survey and California State Parks State of California Edmund G CGS SPECIAL REPORT 230 Geological Gems of California State Parks By California Geological Survey and California State Parks State of California Edmund G. Brown Jr., Governor Natural Resources Agency John Laird, Secretary Department of Conservation David Bunn, Director Department of Parks and Recreation Lisa Mangat, Director California Geological Survey John G. Parrish, Ph.D., State Geologist Copyright © 2015 jointly held by California Department of Conservation, California Geological Survey, and California State Parks. All rights reserved. “The Department of Conservation makes no warranties as to the suitability of this product for any particular purpose.” This page intentionally left blank. Geological Gems of California State Parks by California Geological Survey and California State Parks 2015 SPECIAL REPORT 230 Copies of Geological Gems of California State Parks, and other related information are available at www.conservation.ca.gov/cgs. Copies are also available from the Public Information Offices of the California Geological Survey. California Geological Survey’s Public Information Office Southern California Regional Office Publications and Information Office Bay Area Regional Office 320 W. 4th Street 801 K Street Earth Science Information Center/Map Sales Suite 850 MS 14-33 Building 3, Room 3-121 Los Angeles, CA 90013 Sacramento, CA 95814-3532 Menlo Park, CA 94025 213.239.0878 916.445.5716 650.688.6327 This page intentionally left blank. ACKNOWLEDGEMENTS Authors: Don Braun, Marc Delattre, Ron Churchill, Tim Dawson, Jim Falls, Mike Fuller, Will Harris, Chris Higgins, Jeremy Lancaster, Dave Longstreth, Gerald Marshal, Paul Remeika, Steve Reynolds, Chris Wills, and Michael Wopat. Editors: Syd Brown, Mike Fuller, Bill Short, and Chris Wills. Photograph Credits: Gabrielle Adelman, Kenneth Adelman, Don Braun, Mike Fuller, Will Harris, Cheryl Hayhurst, Dennis Heiman, Janis Hernandez, Pam Irvine, Bret Koehler, Greg Kulak, Jeremy Lancaster, Jennifer Lotery, John Mistchenko, Christopher Mizeur, Steve Reynolds, Alan Schimierer, UC Berkeley, Shannon Utley, Chris Wills, and Michael Wopat. Diagram Credits: Alan O. Allwardt, California Geological Survey, Robert J. Lillie, and Gerald E. Weber. Map Credits: Dave Branum, Mike Fuller, and Jim Thompson. Reviewers: Brian Hausback, George Jefferson, Renee Pasquinelli, and Patrick Vaughan. RECOMMENDED CITATION Citations for the entire collection: Geological Gems of California State Parks, Special Report 230 – Fuller, M., Brown, S., Wills, C. and Short, W., editors, 2015, Geological Gems of California, California Geological Survey Special Report 230 under Interagency Agreement C01718011 with California State Parks. The author of each GeoGem Note appears at the conclusion of the GeoGem Note. Citations should be specific to individual notes when applicable. For example: Fuller, M., 2015, Ocotillo Wells State Vehicular Recreation Area, Geological Gems of California, GeoGem Note 54, Fuller, M., Brown, S., Wills, C. and Short, W., editors, California Geological Survey Special Report 230 under Interagency Agreement C01718011 with California State Parks. COPYRIGHT Copyright © 2015 jointly held by California Department of Conservation, California Geological Survey, and California State Parks. All rights reserved. DISCLAIMER The Department of Conservation makes no warranties as to the suitability of this product for any particular purpose. Information in document is not sufficient to serve as a substitute for the geologic and geotechnical site investigations required under Chapters 7.5 and 7.8 of Division 2 of the California Public Resources Code. COVER PHOTOS Castle Crags State Park (center top), photograph by Chris Mizeur; Schooner Gulch State Beach (lower left), photograph by Jennifer Lotery; McArthur-Burney Falls Memorial State Park (lower center), photograph by Michael Wopat; Red Rock Canyon State Park (lower right), photograph by Mike Fuller. This document has been prepared as a series of flyers that can be printed individually and distributed freely at visitor centers and other venues. GEOLOGICAL GEMS OF CALIFORNIA STATE PARKS Table of Contents GeoGems Note 1 Introduction 2 Geomorphology and Plate Tectonics 3 Coast Ranges Geomorphic Province 4 Del Norte Coast Redwoods State Park 5 Humboldt Redwoods State Park 6 Robert Louis Stevenson State Park 7 Mount Tamalpais State Park 8 Mount Diablo State Park 9 Hollister Hills State Recreation Vehicle Area 10 Northern Coastline Geomorphic Sub-Province 11 Patrick’s Point State Park 12 Sinkyone Wilderness State Park 13 MacKerricher State Park 14 Schooner Gulch State Beach 15 Jug Handle State Natural Reserve and Van Damme State Park 16 Salt Point State Park 17 Fort Ross State Historic Park 18 Wilder Ranch State Park 19 Point Lobos State Natural Reserve 20 Montaña de Oro and Morro Bay State Parks 21 Point Sal State Beach 22 Klamath Mountains Geomorphic Province 23 Castle Crags State Park 24 Cascade Range Geomorphic Province 25 McArthur-Burney Falls Memorial State Park 26 Modoc Plateau Geomorphic Province 27 Ahjumawi Lava Springs State Park (continued on next page) GEOLOGICAL GEMS OF CALIFORNIA STATE PARKS Table of Contents GeoGems Note 28 Great Valley Geomorphic Province 29 Sutter Buttes State Park 30 Sierra Nevada Geomorphic Province 31 Malakoff Diggins State Historic Park 32 South Yuba River State Park 33 Marshall Gold Discovery State Historic Park 34 Emerald Bay State Park 35 Grover Hot Springs State Park 36 Basin and Range Geomorphic Province 37 Mono Lake Tufa State Natural Reserve 38 Red Rock Canyon State Park 39 Transverse Ranges Geomorphic Province 40 Hungry Valley State Vehicular Recreation Area 41 Gaviota State Park 42 Malibu Creek State Park 43 Mojave Desert Geomorphic Province 44 Providence Mountains State Recreation Area 45 Picacho State Recreation Area 46 Peninsular Ranges Geomorphic Province 47 Anza-Borrego Desert State Park (Earthquake, deformation) 48 Anza-Borrego Desert State Park (Erosion, alluvial fans) 49 Cuyamaca Rancho State Park 50 Southern Coastline Geomorphic Sub-Province 51 Torrey Pines State Beach and Torrey Pines State Natural Reserve 52 San Onofre State Beach 53 Colorado Desert Geomorphic Province 54 Anza-Borrego Desert State Park (Badlands, fossils) 55 Ocotillo Wells State Vehicular Recreation Area GEOLOGICAL GEMS OF CALIFORNIA STATE PARKS | GEOGEM NOTE 1 Introduction alifornia is a veritable treasure chest of nationally acclaimed natural landmarks Cand much adored scenery. This geologic legacy on display in the landscape can be observed throughout California’s State Park system. The mission of California State Parks is “to provide for the health, inspiration and education of the people of California by helping to preserve the state’s extraordinary biological This abundant biodiversity … diversity, protecting its most valued natural and everything from the alpine cultural resources, and creating opportunities for to the saline. high-quality outdoor recreation.” We selected exemplary units of the State Park system to highlight California’s geologic legacy. The selected parks are dubbed “GeoGems.” Of these, a third have been bestowed various national accolades and recognitions. This GeoGem Note 1 is the first in a series of more than 50 notes that describe individual GeoGems, the geomorphic provinces in which they exist, and the processes that created them, leading off with a general explanation of plate tectonics in relation to the geomorphic provinces. Introduction GeoGem Note 1 California’s topography is one of the most diverse in the conterminous United States, including a splendid coastline; the largest estuary on the west coast; the famously fertile Great Valley; formidable mountain ranges studded with jewel-like lakes; parched, desolate deserts; snow-capped volcanoes; and extensive plateaus of lava. Elevations are extreme, ranging from 282 feet below sea level at Badwater in Death Valley to 14,495 feet above sea level at the top of Mount Whitney; both the lowest valley and the highest peak in the conterminous United States are less than 90 miles apart. Along with complex landscape comes rich Both the lowest valley and the habitat diversity. California inherited the most highest peak in the conterminous diverse flora in the country; including majestic, ancient redwood and sequoia forests; kelp United States are less than forests teeming with life; and grasslands and 90 miles apart. wetlands that support the famous Pacific Flyway—the main lifeline for migratory birds in western North America. This abundant biodiversity results from habitat heterogeneity (diversity), everything from the alpine to the saline. California’s annual precipitation ranges from less than two inches in Death Valley in the south to over 100 inches at Honeydew in Humboldt County in the north. The abundant rainfall in the north feeds the many coastal streams that are the lifelines for the migratory Pacific salmon. Throughout an inland network of thousands of miles of streams, the life cycles of these anadromous fish both begin and end. GEOLOGICAL GEMS OF CALIFORNIA STATE PARKS Introduction GeoGem Note 1 GeoGem Parks with Special Recognition National Natural Landmarks World Heritage Site Anza-Borrego Desert State Park (1974) Redwood National and State Parks includes Del Norte Coast Redwoods State Park Emerald Bay State Park (1968) International Biosphere Reserve McArthur-Burney Falls Memorial State Park (1984) Redwood National and State Parks includes Del Norte Coast Redwoods State Park Mount Diablo State Park (1982) National Estuary Mitchell Caverns
Recommended publications
  • Lesson 3 Forces That Build the Land Main Idea
    Lesson 3 Forces That Build the Land Main Idea Many landforms result from changes and movements in Earth’s crust. Objectives Identify types of landforms and the processes that form them. Describe what happens when an earthquake occurs. Vocabulary fault focus aftershock seismic wave epicenter seismograph magnitude vent What forces change Earth’s crust? At transform boundaries, the pieces of rock rub together in a force called shearing, like the blades of a pair of scissors, causing the rock to break. At convergent boundaries, plates collide and this force is called compression, squeezing the rock together. At divergent boundaries, plates separate causing tension, making the crust longer and thinner eventually breaking and creating a fault. Faults are usually located along the boundaries between tectonic plates. Three Kinds of Faults Shearing forms strike-slip faults. Tension forms normal faults. The rock above the fault moves down. Compression forms reverse faults. The rock above the fault moves up. Uplifted Landforms Folded mountains are mostly made up of rock layers folded by being squeezed together. Fault-block mountains are made by huge, tilted blocks of rock separated from the surrounding rock by faults. The Colorado Plateau was formed when rock layers were pushed upward. The Colorado River eventually formed the Grand Canyon. Quick Check Infer Why are faults often produced along plate boundaries? Forces act on the crust most directly at plate boundaries, because these locations are where plates are moving, relative to each other. Critical Thinking Why do some mountains form as folded mountains and others form as fault-block mountains? Compression forces form folded mountains, and tension forms fault- block mountains.
    [Show full text]
  • Part 3: Normal Faults and Extensional Tectonics
    12.113 Structural Geology Part 3: Normal faults and extensional tectonics Fall 2005 Contents 1 Reading assignment 1 2 Growth strata 1 3 Models of extensional faults 2 3.1 Listric faults . 2 3.2 Planar, rotating fault arrays . 2 3.3 Stratigraphic signature of normal faults and extension . 2 3.4 Core complexes . 6 4 Slides 7 1 Reading assignment Read Chapter 5. 2 Growth strata Although not particular to normal faults, relative uplift and subsidence on either side of a surface breaking fault leads to predictable patterns of erosion and sedi­ mentation. Sediments will fill the available space created by slip on a fault. Not only do the characteristic patterns of stratal thickening or thinning tell you about the 1 Figure 1: Model for a simple, planar fault style of faulting, but by dating the sediments, you can tell the age of the fault (since sediments were deposited during faulting) as well as the slip rates on the fault. 3 Models of extensional faults The simplest model of a normal fault is a planar fault that does not change its dip with depth. Such a fault does not accommodate much extension. (Figure 1) 3.1 Listric faults A listric fault is a fault which shallows with depth. Compared to a simple planar model, such a fault accommodates a considerably greater amount of extension for the same amount of slip. Characteristics of listric faults are that, in order to maintain geometric compatibility, beds in the hanging wall have to rotate and dip towards the fault. Commonly, listric faults involve a number of en echelon faults that sole into a low­angle master detachment.
    [Show full text]
  • Appendix A: Project Partners
    Humboldt County Coastal Trail Implementation Strategy Technical Appendix JANUARY 2011 Prepared for: State of California Coastal Conservancy Project team: Natural Resources Services Division of Redwood Community Action Agency Alta Planning + Design Planwest Partners Streamline Planning Consultants Humboldt County Coastal Trail Implementation Strategy TECHNICAL APPENDICES Thank you to the community members and agency staff who provided input during public meetings and advisory team workshops throughout the planning process. Your participation and contributions are key to this and future efforts to bring the CCT to fruition. Peter Jarausch Project Manager State of California Coastal Conservancy [email protected] This plan was made possible through Proposition 40 funding Photo credits: Kids on bicycles, N. Wynne; Trail horses, U. Driscoll; Eureka boardwalk, J. Kalt All other photos by project team Appendix A: Project Partners Primary Partners ................................................................................................................................................................... 2 Federal Agencies .............................................................................................................................................................. 2 Bureau of Land Management (BLM) ....................................................................................................................... 2 U.S. Fish and Wildlife Service (USFWS) ................................................................................................................
    [Show full text]
  • Under Western Stars by Howard Kazanjian and Chris Enss
    Under Western Stars By Howard Kazanjian and Chris Enss King of the Cowboys Roy Rogers made his starring mo- tion picture debut in Republic Studio’s engaging western mu- sical “Under Western Stars.” Released in 1938, the charm- ing, affable Rogers portrayed the most colorful Congressman Congressional candidate Roy Rogers gets tossed into a water trough by his ever to walk up the steps of the horse to the amusement of locals gathered to hear him speak at a political rally. nation’s capital. Rogers’ character, Courtesy Library of Congress Collection. a fearless, two-gun cowboy and ranger from the western town of Sageville, is elected culties with Herbert Yates, head of Republic Studios, to office to try to win legislation favorable to dust bowl paved the way for Rogers to ride into the leading role residents. in “Under Western Stars.” Yates felt he alone was responsible for creating Autry’s success in films and Rogers represents a group of ranchers whose land wanted a portion of the revenue he made from the has dried up when a water company controlling the image he helped create. Yates demanded a percent- only dam decides to keep the coveted liquid from the age of any commercial, product endorsement, mer- hard working cattlemen. Spurred on by his secretary chandising, and personal appearance Autry made. and publicity manager, Frog Millhouse, played by Autry did not believe Yates was entitled to the money Smiley Burnette, Rogers campaigns for office. The he earned outside of the movies made for Republic portly Burnette provides much of the film’s comic re- Studios.
    [Show full text]
  • International Geology Review Unroofing History of Alabama And
    This article was downloaded by: [Canadian Research Knowledge Network] On: 2 March 2010 Access details: Access Details: [subscription number 918588849] Publisher Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37- 41 Mortimer Street, London W1T 3JH, UK International Geology Review Publication details, including instructions for authors and subscription information: http://www.informaworld.com/smpp/title~content=t902953900 Unroofing history of Alabama and Poverty Hills basement blocks, Owens Valley, California, from apatite (U-Th)/He thermochronology Guleed A. H. Ali a; Peter W. Reiners a; Mihai N. Ducea a a Department of Geosciences, University of Arizona, Tucson, AZ, USA To cite this Article Ali, Guleed A. H., Reiners, Peter W. and Ducea, Mihai N.(2009) 'Unroofing history of Alabama and Poverty Hills basement blocks, Owens Valley, California, from apatite (U-Th)/He thermochronology', International Geology Review, 51: 9, 1034 — 1050 To link to this Article: DOI: 10.1080/00206810902965270 URL: http://dx.doi.org/10.1080/00206810902965270 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.informaworld.com/terms-and-conditions-of-access.pdf This article may be used for research, teaching and private study purposes. Any substantial or systematic reproduction, re-distribution, re-selling, loan or sub-licensing, systematic supply or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date. The accuracy of any instructions, formulae and drug doses should be independently verified with primary sources.
    [Show full text]
  • NPCA Comments on Proposed Silurian
    Stanford MillsLegalClinic Environmental Law Clinic Crown Quadrangle LawSchool 559 Nathan Abbott Way Stanford, CA 94305-8610 Tel 650 725-8571 Fax 650 723-4426 www.law.stanford.edu September 9, 2014 Via Electronic Mail and Federal Express James G. Kenna, State Director Bureau of Land Management California State Office 2800 Cottage Way, Suite W-1623 Sacramento, CA 95825 (916) 978-4400 [email protected] Katrina Symons Field Manager Bureau of Land Management Barstow Field Office 2601 Barstow Road Barstow, CA 92311 (760) 252-6004 [email protected] Dear State Director Kenna and Field Manager Symons: Enclosed please find comments by the National Parks Conservation Association (“NPCA”) on the solar and wind projects proposed by Iberdrola Renewables, Inc., in Silurian Valley, California. We understand that the U.S. Bureau of Land Management (“BLM”) is currently considering whether to grant the Silurian Valley Solar Project a variance under the October 2012 Record of Decision for Solar Energy Development in Six Southwestern States. We also understand that BLM is currently evaluating the Silurian Valley Wind Project under the National Environmental Policy Act. As the enclosed comments make clear, NPCA has serious concerns about the proposed projects’ compliance with applicable laws and policies, and about their potentially significant adverse effects on the Silurian Valley and surrounding region. We thank you for your consideration of these comments. NPCA looks forward to participating further in the administrative processes associated with the proposed projects. Respectfully submitted, Elizabeth Hook, Certified Law Student Community Law ❖ Criminal Defense ❖ Environmental Law ❖ Immigrants’ Rights ❖ International Human Rights and Conflict Resolution ❖ Juelsgaard Intellectual Property and Innovation ❖ Organizations and Transactions ❖ Religious Liberty ❖Supreme Court Litigation ❖ Youth and Education Law Project Mr.
    [Show full text]
  • Cover and Final Landform Design for the B-Zone Waste Rock Pile at Rabbit Lake Mine
    Cover and final landform design for the B-zone waste rock pile at Rabbit Lake Mine Brian Ayres1, Pat Landine2, Les Adrian2, Dave Christensen1, Mike O’Kane1 1O’Kane Consultants Inc., Saskatoon, Saskatchewan, Canada 2Cameco Corporation, Saskatoon, Saskatchewan, Canada Abstract. A detailed study was undertaken to evaluate various cover system and final landform designs for the B-zone waste rock pile at Rabbit Lake Mine in Can- ada. Several tasks were completed including physical and hydraulic characteriza- tion of the waste and potential cover materials and numerical modelling to exam- ine erosion and slope stability. Soil-atmosphere numeric simulations were conducted to predict net infiltration and oxygen ingress rates through several cover system alternatives. A seepage numerical modelling programme was com- pleted to predict current and future seepage rates from the base of the pile for al- ternate cover system designs. Several final landform alternatives were developed for the pile along with a preliminary design for a surface water management sys- tem. The potential impact of various physical, chemical, and biological processes on the sustainable performance of the final landform was also considered. This paper provides an overview of the investigations completed towards the develop- ment of a cover system and final landform design for the B-zone waste rock pile. Introduction Rabbit Lake Mine, owned and operated by Cameco Corporation, began operation in 1975, and is the longest operating uranium production facility in Saskatchewan, Canada. The operation is located 700 km north of Saskatoon (Fig. 1). Historic and current operations at this site include four open pits, one underground mine, sev- eral mine waste storage facilities, and a mill.
    [Show full text]
  • King Range National Conservation Area Case Study
    University of Colorado Law School Colorado Law Scholarly Commons Getches-Wilkinson Center for Natural Books, Reports, and Studies Resources, Energy, and the Environment 2004 King Range National Conservation Area Case Study Ann Morgan Doug Cannon University of Colorado Boulder. Natural Resources Law Center Follow this and additional works at: https://scholar.law.colorado.edu/books_reports_studies Part of the Natural Resources and Conservation Commons, Natural Resources Law Commons, and the Natural Resources Management and Policy Commons Citation Information Ann Morgan & Doug Cannon, King Range National Conservation Area Case Study (Natural Res. Law Ctr., Univ. of Colo. Sch. of Law 2004). Ann Morgan & Doug Cannon, KING RANGE NATIONAL CONSERVATION AREA CASE STUDY (Natural Res. Law Ctr., Univ. of Colo. Sch. of Law 2004). Reproduced with permission of the Getches-Wilkinson Center for Natural Resources, Energy, and the Environment (formerly the Natural Resources Law Center) at the University of Colorado Law School. KING RANGE NATIONAL CONSERVATION AREA CASE STUDY Ann Morgan and Doug Cannon Natural Resources Law Center January 9, 2004 Table of Contents BACKGROUND................................................................................................................................. 1 PUBLIC LAW 91-476....................................................................................................................... 2 LEGISLATIVE HISTORY .................................................................................................................
    [Show full text]
  • Why Did the Southern Gulf of California Rupture So Rapidly?—Oblique Divergence Across Hot, Weak Lithosphere Along a Tectonically Active Margin
    Why did the Southern Gulf of California rupture so rapidly?—Oblique divergence across hot, weak lithosphere along a tectonically active margin breakup, is mainly dependent on the thermal structure, crust- Paul J. Umhoefer, Geology Program, School of Earth Sciences & Environmental Sustainability, Northern Arizona University, al thickness, and crustal strength of the lithosphere when Flagstaff, Arizona 86011, USA; [email protected] rifting begins (e.g., Buck, 2007), as well as forces at the base of the lithosphere and far-field plate interactions (Ziegler and Cloetingh, 2004). ABSTRACT Continental rupture at its two extremes creates either large Rifts in the interior of continents that evolve to form large ocean basins or small and narrow marginal seas depending oceans typically last for 30 to 80 m.y. and longer before com- largely on the tectonic setting of the rift. Rupture of a conti- plete rupture of the continent and onset of sea-floor spreading. nent that creates large oceans most commonly initiates as A distinct style of rifts form along the active tectonic margins of rifts in old, cold continental lithosphere or within former continents, and these rifts more commonly form marginal seas large collisional belts in the interior of large continents, part and terranes or continental blocks or slivers that are ruptured of the process known as the Wilson Cycle (Wilson, 1966). away from their home continent. The Gulf of California and the Rupture to create narrow marginal seas commonly occurs in Baja California microplate make up one of the best examples active continental margins and results in the formation of of the latter setting and processes.
    [Show full text]
  • Unstable Slopes in the Franciscan Complex Terrane: Lessons Learned from Urban Quarry Slopes in the San Francisco Bay Area
    UNSTABLE SLOPES IN THE FRANCISCAN COMPLEX TERRANE: LESSONS LEARNED FROM URBAN QUARRY SLOPES IN THE SAN FRANCISCO BAY AREA Ted M. Sayre1 & John M. Wallace2 1Cotton, Shires & Associates, Inc., Consulting Engineers and Geologists, 330 Village Lane, Los Gatos, CA 95030 ([email protected]) 1Cotton, Shires & Associates, Inc., Consulting Engineers and Geologists, 330 Village Lane, Los Gatos, CA 95030 ([email protected]) Abstract: As the need for urban living space intensifies, an increasing number of former rock quarry sites have become prime real estate for residential living areas. This change in land use can result in inappropriate and potentially catastrophic consequences when residential structures are placed in close proximity to unstable quarry slopes that were not adequately investigated prior to development. Examples of this have occurred on the San Francisco peninsula where recent slope failures along several quarry faces serve as a testament to the variability of the Franciscan Complex terrane and the unique set of failure mechanisms associated with a given Franciscan rock type, underscoring the importance of a thorough geologic assessment prior to development. In two presented case studies, residential developments were adversely impacted by recent rock slope failures. Incomplete characterization of site geologic conditions and inadequate identification of critical slope failure mechanisms led to unsatisfactory setbacks and/or ineffective mitigation designs. The Knockash Hill development in San Francisco is underlain by thinly-bedded “ribbon” chert of the Franciscan Complex that was previously mined for roadway aggregate. The steep quarried slope, located immediately above new residential units, presented an excellent geologic exposure of bedded chert that displayed adversely oriented discontinuities and weak shale interbeds.
    [Show full text]
  • 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.
    [Show full text]
  • The History of Valentine Camp by Mary Farrell
    History of Valentine Camp Mary M. Farrell Trans-Sierran Archaeological Research P.O. Box 840 Lone Pine, CA 93545 November 7, 2015 Prepared for Valentine Eastern Sierra Reserve University of California, Santa Barbara, Natural Reserve System Sierra Nevada Aquatic Research Laboratory 1016 Mt. Morrison Road Mammoth Lakes, CA 93546 Abstract Located in Mammoth Lakes, California, Valentine Camp and the nearby Sierra Nevada Aquatic Research Laboratory form the Valentine Eastern Sierra Reserve, a field research station in the University of California's Natural Reserve System. The University’s tenure at Valentine Camp began over 40 years ago, but the area’s history goes back thousands of years. Before the arrival of Euroamericans in the nineteenth century, the region was home to Paiutes and other Native American tribes. Land just east of Valentine Camp was surveyed under contract with the United States government in 1856, and mineral deposits in the mountains just west of Valentine Camp brought hundreds of miners to the vicinity in the last decades of the nineteenth century. Even as mining in the region waned, grazing increased. The land that became Valentine Camp was patented in 1897 by Thomas Williams, a rancher and capitalist who lived in Owens Valley. It was Williams’s son, also Thomas, who sold the 160 acres to Valentine Camp’s founders. Those founders were very wealthy, very influential men in southern California who could have, and did, vacation wherever they wanted. Anyone familiar with the natural beauty of Mammoth Lakes would not be surprised that they chose to spend time at Valentine Camp. Valentine Camp was donated to the University of California Natural Land and Water Reserve System (now the Natural Reserve System) in 1972 to ensure the land’s continued protection.
    [Show full text]