Fall Color at North Lake, Bishop Creek Canyon Ancient Bristlecone Pine
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Birch Lake and Red Lake Trailheads Inyo National Forest
Birch Lake and Red Lake Trailheads Inyo National Forest To Access the Trailheads: Both of these trails are accessed via McMurry Meadows Road west of Big Pine. At the flashing yellow light in Big Pine, turn west onto Crocker Street (Glacier Lodge Road). After 2.5 miles, just after crossing Big Pine Creek, turn left onto McMurry Meadows Road and immediately turn left again. The road will soon turn to the south/southwest. McMurry Meadows Road is 2WD-accessible for the first 7.3 miles; beyond this point a high-clearance 4WD vehicle is required. A high-clearance 4WD vehicle is also required to access the Birch Lake trailhead once leaving McMurry Meadows Road. Birch Lake Trailhead: From the Glacier Lodge Road/McMurry Meadows intersection, drive 5.9 miles and turn right. Drive another 0.6 miles and turn left at a second sign for Birch Lake. Past the fence (0.1 mile further) the road is impassable even for 4WD vehicles. It is recommended that vehicles park before the final junction as it can be difficult to turn around at the gate. Please leave the roadway clear. Hike along the road for 0.5 miles past the gate until the road forks. Do not take the left fork toward the stream. Follow the road to the right into a draw until it turns into a trail. The distance from here to Birch Lake is approximately 5 miles. Trailhead elevation is 6,600 feet; Birch Lake elevation is 10,800 feet. Red Lake Trailhead: From the Glacier Lodge/McMurry Meadows intersection, drive 7.7 miles. -
Motor Vehicle Use
350000 360000 370000 380000 118°45'0"W 30E301A 118°37'30"W Continued on Casa Diablo Map 118°30'0"W 118°22'30"W T OPERATOR RESPONSIBILITIES EXPLANATION OF LEGEND ITEMS 04S15B o PINE GROVE 04S15 M Legend PICNIC AREA 3 04S15E a 0 Operating a motor vehicle on National Forest System Roads Open to Highway Legal Vehicles Only: m " LOWER E m Roads Open to Highway Legal Vehicles 5" 3 roads, National Forest System trails, and in areas on 04S15C 9 & 0 o 1 UPPER t PINE h National Forest System lands carries a greater These roads are open only to motor vehicles licensed under Roads Open to All Vehicles 04S18 " 2 9 0 GROVE 3 responsibility than operating that vehicle in a city or other State law for general operation on all public roads within the 04S18B E Trails Open to All Vehicles CAMPGROUND 0 developed setting. Not only must you know and follow all State. 3 applicable traffic laws, you need to show concern for the Trails Open to Vehicles 50" or Less in Width 04S12O 04S18A environment as well as other forest users. The misuse of Roads Open to All Vehicles: ! ! ! ! ! ! ! ! ! Trails Open to Motorcycles Only 06S08 0 6 motor vehicles can lead to the temporary or permanent S 06S08A G Rock 0 04S12P o Seasonal Designation 6 r closure of any designated road, trail, or area. As a motor These roads are open to all motor vehicles, including smaller 9" Creek g (See Seasonal Designation Table) e 04S12Q vehicle operator, you are also subject to State traffic law, off-highway vehicles that may not be licensed for highway Lake R d including State requirements for licensing, registration, and use (but not to oversize or overweight vehicles under State Highways, US, State 9" 06S06A MOSQUITO FLAT operation of the vehicle in question. -
Upper Neogene Stratigraphy and Tectonics of Death Valley — a Review
Earth-Science Reviews 73 (2005) 245–270 www.elsevier.com/locate/earscirev Upper Neogene stratigraphy and tectonics of Death Valley — a review J.R. Knott a,*, A.M. Sarna-Wojcicki b, M.N. Machette c, R.E. Klinger d aDepartment of Geological Sciences, California State University Fullerton, Fullerton, CA 92834, United States bU. S. Geological Survey, MS 975, 345 Middlefield Road, Menlo Park, CA 94025, United States cU. S. Geological Survey, MS 966, Box 25046, Denver, CO 80225-0046, United States dTechnical Service Center, U. S. Bureau of Reclamation, P. O. Box 25007, D-8530, Denver, CO 80225-0007, United States Abstract New tephrochronologic, soil-stratigraphic and radiometric-dating studies over the last 10 years have generated a robust numerical stratigraphy for Upper Neogene sedimentary deposits throughout Death Valley. Critical to this improved stratigraphy are correlated or radiometrically-dated tephra beds and tuffs that range in age from N3.58 Ma to b1.1 ka. These tephra beds and tuffs establish relations among the Upper Pliocene to Middle Pleistocene sedimentary deposits at Furnace Creek basin, Nova basin, Ubehebe–Lake Rogers basin, Copper Canyon, Artists Drive, Kit Fox Hills, and Confidence Hills. New geologic formations have been described in the Confidence Hills and at Mormon Point. This new geochronology also establishes maximum and minimum ages for Quaternary alluvial fans and Lake Manly deposits. Facies associated with the tephra beds show that ~3.3 Ma the Furnace Creek basin was a northwest–southeast-trending lake flanked by alluvial fans. This paleolake extended from the Furnace Creek to Ubehebe. Based on the new stratigraphy, the Death Valley fault system can be divided into four main fault zones: the dextral, Quaternary-age Northern Death Valley fault zone; the dextral, pre-Quaternary Furnace Creek fault zone; the oblique–normal Black Mountains fault zone; and the dextral Southern Death Valley fault zone. -
Caliwomenbotany00hollrich.Pdf
88/51 Regional Oral History Office University of California The Bancroft Library Berkeley, California CALIFORNIA WOMEN IN BOTANY Annetta Carter UC Herbarium Botanist, Collector and Interpreter of Baja California Plants Mary DeDecker Botanist and Conservationist of the Inyo Region Elizabeth McClintock California Academy of Sciences Curator, Ornamental Plant Specialist With Interview Introductions by Lincoln Constance, Betty Gilchrist, Peter Rowlands, John Hunter Thomas Interviews Conducted by Carol Holleuffer 1985 Copyright (c) 1987 by The Regents of the University of California This manuscript is made available for research purposes. No part of the manuscript may be quoted for publication without the written permission of the Director of The Bancroft Library of the University of California at Berkeley. Requests for permission to quote for publication should be addressed to the Regional Oral History Office, 486 Library, and should include identification of the specific passages to be quoted, anticipated use of the passages, and identification of the user. It is recommended that this oral history be cited as follows: To cite the volume: California Women in Botany, an oral history conducted in 1985, Regional Oral History Office, The Bancroft Library, University of California, Berkeley, 1987. To cite individual interview: Annetta Carter, "UC Herbarium Botanist, Collector and Interpreter of Baja California Plants," an oral history conducted 1985 by Carol Holleuffer, in California Women in Botany, Regional Oral History Office, The Bancroft Library, University of California, Berkeley, 1987. Copy No. /| OAKLAND THE DAILY CALIFORNIAN TRIBUNE 1991 May 17, 1991 May 16, I ' . .-,<. TVjW'-wiKjs Annetta Carter, ^UC'Berkeleyl 'botanist dies UC botanist ' I" W-! f . -: ^.,.v X **\; -':. -
2021 Magazine
July 2021 Welcome to the July 2021 edition of BADWATER® Magazine! We are AdventureCORPS®, producers of ultra-endurance sports events and adventure travel across the globe, and the force behind the BADWATER® brand. This magazine celebrates the entire world-wide Badwater® / AdventureCORPS® series of races, all the Badwater Services, Gear, Drinks, and Clothing, and what we like to call the Badwater Family and the Badwater Way of Life. Adventure is our way of life, so – after the sad and disastrous 2020 when we were not able to host any of our life-changing events – we are pleased to be fully back in action in 2021! Well, make that almost fully: Due to pandemic travel bans still in place, international participation in our USA-based events is not where we want it and that’s really unfortunate. Badwater 135 is the de facto Olympics of Ultrarunning and the 135-Mile World Championship, so we always want as many nationalities represented as possible. (The inside front cover of this magazine celebrates all sixty-one nationalities which have been represented on the Badwater 135 start line over the years.) Our new six-day stage race across Armenia – Artsakh Ultra – will have to wait yet another year to debut in 2022, two years later than planned. But it will be incredible, the ultimate stage race with six days of world-class trail running through several millennia of incredible culture and history, and across the most dramatic and awe-inspiring landscapes. This year, we are super excited to have brought two virtual races to life, first for the 31 days of January, and then for 16 days in April. -
Syn-Eruptive, Soft-Sediment Deformation of Deposits
Solid Earth, 6, 553–572, 2015 www.solid-earth.net/6/553/2015/ doi:10.5194/se-6-553-2015 © Author(s) 2015. CC Attribution 3.0 License. Syn-eruptive, soft-sediment deformation of deposits from dilute pyroclastic density current: triggers from granular shear, dynamic pore pressure, ballistic impacts and shock waves G. A. Douillet1, B. Taisne2, È. Tsang-Hin-Sun3, S. K. Müller4, U. Kueppers1, and D. B. Dingwell1 1Earth and Environmental Sciences, Ludwig-Maximilians-Universität, Munich, Germany 2Earth Observatory of Singapore, Nanyang Technological University, Singapore 3Université of Brest and CNRS, Laboratoire Domaines Océaniques, Plouzaré, France 4Meteorological Institute, Ludwig-Maximilians-Universität, Munich, Germany Correspondence to: G. A. Douillet ([email protected]) Received: 17 November 2014 – Published in Solid Earth Discuss.: 16 December 2014 Revised: 16 April 2015 – Accepted: 20 April 2015 – Published: 21 May 2015 Abstract. Soft-sediment deformation structures can provide to be the signature of shear instabilities occurring at the valuable information about the conditions of parent flows, boundary of two granular media. They may represent the sediment state and the surrounding environment. Here, the frozen record of granular, pseudo Kelvin–Helmholtz examples of soft-sediment deformation in deposits of dilute instabilities. Their recognition can be a diagnostic for pyroclastic density currents are documented and possible flows with a granular basal boundary layer. Vertical syn-eruptive triggers suggested. Outcrops from six different inter-penetration and those folds-and-faults features related volcanoes have been compiled in order to provide a to slumps are driven by their excess weight and occur | downloaded: 11.10.2021 broad perspective on the variety of structures: Soufrière after deposition but penecontemporaneous to the eruption. -
Death Valley National Park
COMPLIMENTARY $3.95 2019/2020 YOUR COMPLETE GUIDE TO THE PARKS DEATH VALLEY NATIONAL PARK ACTIVITIES • SIGHTSEEING • DINING • LODGING TRAILS • HISTORY • MAPS • MORE OFFICIAL PARTNERS T:5.375” S:4.75” PLAN YOUR VISIT WELCOME S:7.375” In T:8.375” 1994, Death Valley National SO TASTY EVERYONE WILL WANT A BITE. Monument was expanded by 1.3 million FUN FACTS acres and redesignated a national park by the California Desert Protection Act. Established: Death Valley became a The largest national park below Alaska, national monument in 1933 and is famed this designation helped focus protection for being the hottest, lowest and driest on one the most iconic landscapes in the location in the country. The parched world. In 2018 nearly 1.7 million people landscape rises into snow-capped mountains and is home to the Timbisha visited the park, a new visitation record. Shoshone people. Death Valley is renowned for its colorful Land Area: The park’s 3.4 million acres and complex geology. Its extremes of stretch across two states, California and elevation support a great diversity of life Nevada. and provide a natural geologic museum. Highest Elevation: The top of This region is the ancestral homeland Telescope Peak is 11,049 feet high. The of the Timbisha Shoshone Tribe. The lowest is -282 feet at Badwater Basin. Timbisha established a life in concert Plants and Animals: Death Valley with nature. is home to 51 mammal species, 307 Ninety-three percent of the park is bird species, 36 reptile species, two designated wilderness, providing unique amphibian species and five fish species. -
Open-File/Color For
Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4). -
Boyhood Days in the Owens Valley 1890-1908
Boyhood Days in the Owens Valley 1890-1908 Beyond the High Sierra and near the Nevada line lies Inyo County, California—big, wild, beautiful, and lonely. In its center stretches the Owens River Valley, surrounded by the granite walls of the Sierra Nevada to the west and the White Mountains to the east. Here the remote town of Bishop hugs the slopes of towering Mount Tom, 13,652 feet high, and here I was born on January 6, 1890. When I went to college, I discovered that most Californians did not know where Bishop was, and I had to draw them a map. My birthplace should have been Candelaria, Nevada, for that was where my parents were living in 1890. My father was an engineer in the Northern Belle silver mine. I was often asked, "Then how come you were born in Bishop?" and I replied, "Because my mother was there." The truth was that after losing a child at birth the year before, she felt Candelaria's medical care was not to be trusted. The decline in the price of silver, the subsequent depression, and the playing out of the mines in Candelaria forced the Albright family to move to Bishop permanently. We had a good life in Bishop. I loved it, was inspired by its aura, and always drew strength and serenity from it. I have no recollection of ever having any bad times. There weren't many special things to do, but what- ever we did, it was on horseback or afoot. Long hours were spent in school. -
Edible Seeds and Grains of California Tribes
National Plant Data Team August 2012 Edible Seeds and Grains of California Tribes and the Klamath Tribe of Oregon in the Phoebe Apperson Hearst Museum of Anthropology Collections, University of California, Berkeley August 2012 Cover photos: Left: Maidu woman harvesting tarweed seeds. Courtesy, The Field Museum, CSA1835 Right: Thick patch of elegant madia (Madia elegans) in a blue oak woodland in the Sierra foothills The U.S. Department of Agriculture (USDA) prohibits discrimination in all its pro- grams and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sex- ual orientation, genetic information, political beliefs, reprisal, or because all or a part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, SW., Washington, DC 20250–9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. Acknowledgments This report was authored by M. Kat Anderson, ethnoecologist, U.S. Department of Agriculture, Natural Resources Conservation Service (NRCS) and Jim Effenberger, Don Joley, and Deborah J. Lionakis Meyer, senior seed bota- nists, California Department of Food and Agriculture Plant Pest Diagnostics Center. Special thanks to the Phoebe Apperson Hearst Museum staff, especially Joan Knudsen, Natasha Johnson, Ira Jacknis, and Thusa Chu for approving the project, helping to locate catalogue cards, and lending us seed samples from their collections. -
Ice Rafts Not Sails: Floating the Rocks at Racetrack Playa ͒ Ralph D
Ice rafts not sails: Floating the rocks at Racetrack Playa ͒ Ralph D. Lorenza Applied Physics Laboratory, Johns Hopkins University, Laurel, Maryland 20723 ͒ Brian K. Jacksonb NASA Goddard Spaceflight Center, Greenbelt, Maryland 20771 ͒ Jason W. Barnesc Department of Physics, University of Idaho, Moscow, Idaho 83844 ͒ Joe Spitaled Space Science Institute, Boulder, Colorado 80301 ͒ John M. Kellere Department of Physics, California Polytechnic State University, San Luis Obispo, California 93407 ͑Received 15 February 2010; accepted 27 August 2010͒ We suggest that the existence of many of the rock-carved trails at Racetrack Playa in Death Valley National Park is predominantly due to the effect of arbitrarily weak winds on rocks that are floated off the soft bed by small rafts of ice, as also occurs in arctic tidal beaches to form boulder barricades. These ice cakes need not have a particularly large surface area if the ice is adequately thick—the ice cakes allow the rocks to move by buoyantly reducing the reaction and friction forces at the bed, not by increasing the wind drag. The parameter space of ice thickness and extent versus rock size for flotation is calculated and found to be reasonable. We demonstrate the effect with a simple experiment. © 2011 American Association of Physics Teachers. ͓DOI: 10.1119/1.3490645͔ I. INTRODUCTION literature. All the discussions involve a sheet of ice acting as a means of increasing the area on which wind can act ͑for Among the many geological attractions1 in Death Valley example, Ref. 4 refers to ice sheets 20 mϫ20 m and National Park in California is Racetrack Playa. -
MOUNT Mckinley NATIONAL PARK ALASKA
UNITED STATES DEPARTMENT OF THE INTERIOR HUBERT WORK. SECRETARY NATIONAL PARK SERVICE STEPHEN T. MATHER, DIRECTOR RULES AND REGULATIONS MOUNT McKINLEY NATIONAL PARK ALASKA Courtesy Alaska Railroad MOUNT McKINLEY AND REFLECTION SEASON FROM JUNE 1 TO SEPTEMBER 15 U.S. GOVERNMENT PRINTING OFFICE : 1927 Courtesy Bragaw'8 Studio, Anchorage, Alaska CARIBOU IN MOUNT McKINLEY NATIONAL PARK Courtesy Brogaw's Studio, Anchorage, Alaska AN ALASKAN DOG TEAM CONTENTS Pane General description 1 Glaciers . 2 Plant life 2 The mammals and birds of Mount McKinley National Park ", Fishing 1) Climate 9 Administration 12 Park season 12 How to reach the park 12 Roads and trails 13 Accommodations 14 Rules and regulations It! Government publications: General IS Other national parks 18 Authorized rates for public utilities 1!) ILLUSTRATIONS COVER Mount McKinley and reflection Front, Caribou.in Mount McKinley National Park Inside front An Alaskan dog team Inside front A male surf bird on his nest Inside back Mountain sheep at Double Mountain Inside hack Mount McKinley Outside back Lake on divide at Sanctuary River Outside back TEXT Map of Alaska showing national park and monuments 10,11 Map of Mount McKinley National Park 15 52087°—27 1 j THE NATIONAL PARKS AT A GLANCE [Number, 10; total area, 11,801 square miles] Area in National parks in Location square Distinctive characteristics order of creation miles Hot Sprints Middle Arkansas . 1M •10 hot springs possessing curative properties— 1832 Many hotels and hoarding houses—19 bath houses under Government supervision. Yellowstone Northwestern Wyo 3, 348 More geysers than in all rest of world together- 1872 ming.