Death Valley Summer Visitor Guide
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Hecastocleideae (Hecastocleidoideae)
Chapter 16 Hecastocleideae (Hecastocleidoideae) Vicki A. Funk and D.J. Nicholas Hind HISTORICAL OVERVIEW AND MORPHOLOGY Carduoideae—'rest of the family' split (see Chapters 12 and 44) and this placement has 100% bootstrap support. Hecastodeis shockleyi A. Gray was described in 1882 and its Its current position is supported by its distinct morphol- unusual morphology and restricted distribution has made ogy and strong support from molecular data. Its near- it sought after for herbarium specimens. This shrub is est downstream neighbor, however, is somewhat tenu- easily identified because of its single flowered heads that ous, because the position of the branch just below it are re-aggregated on a receptacle in groups of one to five (Gochnatieae) has only 65% bootstrap support (Panero heads; each group of heads is subtended by a relatively and Funk 2008) and might collapse into a polytomy large spiny whitish or greenish bract (Fig. 16.1). Gray with Mutisieae s.str. If one does the phylogenetic analysis (1882) commented that is was "a remarkable addition without Hecastodeis, there is no change in the phylogeny to the few known North American Mutisieae, to stand of the family. near Ainsliaea DC. but altogether sui generis and of pecu- liar habit." According to Williams (1977) the generic name Hecastodeis, "... comes from the Greek roots, ekastos TAXONOMY meaning 'each' and kleio meaning 'to shut up'", referring to each flower having its own involucre. The species The genus is monotypic and has always been recognized was named after William H. Shockley one of the first as such since its original description by Gray (1882). -
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. -
Volume 66 Issue 1 Winter 2021
Preservation By David Blacker, Executive Director From the Director DVNHA One of the biggest highlights of visiting Death Valley National Park or Ash Meadows National Wildlife Refuge is seeing and maybe getting a photo of a desert bighorn sheep. You see the desert bighorn in our logo, a strong and majestic animal with iconic large curling horns, but your chance of seeing one of these incredible creatures is shrinking. Surprisingly the biggest reason is not climate change, but the spread of an invasive species that dominates and destroys their water sources and bullies them out of their historic range. In the economic downturn of the early 2000s, people stopped adopting burros and the Bureau of Land Management (BLM) pens filled up. A growing unchecked burro population began to grow and spread. I began to hear reports of sightings in Panamint Valley and the Nevada Triangle back in 2005. Now there are herds occupying Butte Valley, Skidoo, Wildrose, and southern areas of the park. Everywhere burros appear, the impact is predictable. First they seize control of the local water source, trampling or eating the native vegetation. Being very territorial, they use their size and aggressive nature to chase off any competition. Once burros move into a water source, bighorn sheep will not use it. Our partners at NPS are working diligently to reduce and remove invasive burros from the park. They have partnered with Peaceful Valley Donkey Rescue to roundup and adopt out burros from Death Valley. Burro numbers increase by 20-30% a year, so more than 750 burros need to be rounded up annually to stay ahead of reproduction. -
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. -
Death Valley Springs Geochemical Investigation Yucca Mountain Nuclear Repository, Inyo County Oversight-1998
The HYDRODYNAMICS Group studies in mass and energy transport in the earth Death Valley Springs Geochemical Investigation Yucca Mountain Nuclear Repository, Inyo County Oversight-1998 Submitted to: Inyo County Planning Department: Yucca Mountain Repository Oversight Program March, 1999 Michael J. King, R.G., C.HG. John D. Bredehoeft, Ph.D., NAE The HYDRODYNAMICS Group 16711 76th Avenue West, Edmonds, WA 98026 Phone (425) 787-6728, Fax (425) 742-8493 Page 1 The Hydrodynamics Group DEATH VALLEY SPRINGS GEOCHMICAL INVESTIGATION YUCCA MOUNTAIN NUCLEAR WASTE REPOSITORY, INYO COUNTY OVERSIGHT-1998 EXECUTIVE SUMMARY Yucca Mountain, Nevada is under study as the site of the only proposed high-level nuclear waste repository in the United States. The repository concept uses the philosophy of multiple barriers, both engineered and natural, each of which impedes the movement of radionuclides into the accessible environment. The proposed repository would be in the unsaturated zone in Tertiary tuffaceous rocks. The principal transporting mechanism for radionuclides is moving ground water. Underlying the repository is an extensive Lower Carbonate Aquifer known to be highly permeable. Inyo County, as an affected unit of local government under the Nuclear Waste Policy Act, as amended, is concerned with the connections between the Lower Carbonate Aquifer underlying Yucca Mountain and the carbonate sources of waters in Inyo County, especially the Death Valley region. This report is a summary of the investigations conducted by Inyo County’s consultants, the Hydrodynamics Group, during calendar year 1998. This report presents the results of The Hydrodynamics Group’s 1998 collection of water samples from 23 springs and 2 creeks in Death Valley. -
Death Valley
DEATH VALLEY UNITED STATES DEPARTMENT OF THE INTERIOR NATIONAL PARK SERVICE UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE ARNO B. CAMMERER, Director DEATH VALLEY NATIONAL MONUMENT CALIFORNIA OPEN ALL YEAR UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1934 CONTENTS PAGE HISTORICAL INTEREST i COLORFUL SCENERY 4 GEOLOGICAL STORY 8 FOSSILS INDICATE MARINE LIFE 8 How THE VALLEY WAS FORMED 8 ANIMAL AND PLANT LIFE 14 DEATH VALLEY SCOTTY'S CASTLE 16 ACCOMMODATIONS 18 PUBLIC CAMP GROUNDS 20 How TO REACH DEATH VALLEY 20 RULES AND REGULATIONS 27 DEATH VALLEY NATIONAL MONUMENT EATH VALLEY, celebrated in history for its tragic episode in the D California gold-rush drama of '49 and famed throughout the scien tific world as a region of weird natural wonders, became a national monument on February 11, 1933, by Presidential proclamation. The 2,500 square miles included in the monument embrace Death Val ley itself and parts of the rough-hewn mountains that rise abruptly on all sides to guard its colorful desolation. The Amargosa River provides the only natural entrance. To the west towers the Panamint Range and to the east the Amargosas, with the Last Chance Range pinching the north and the Avawatz Mountains blocking the south. Death Valley National Monument lies in the southeastern corner of Inyo County and borders the California-Nevada boundary line. It forms the northern point of the great Mojave Desert region. Approximately 400 square miles of the floor of the valley lie below sea level, and Bad Water, 276 feet below mean tide, is the lowest point in the United States. -
Death Valley Lower Carbonate Aquifer Monitoring Program- Wells Down Gradient of the Proposed Yucca Mountian Nuclear Waste Repository
iU4 MOL.20080509.0010 DEATH VALLEY LOWER CARBONATE AQUIFER MONITORING PROGRAM- WELLS DOWN GRADIENT OF THE PROPOSED YUCCA MOUNTIAN NUCLEAR WASTE REPOSITORY U.S. DEPARTMENT OF ENERGY COOPERATIVE AGREEMENT DE-FC28-06RW12368 YEAR ONE PROJECT REPORT PREPARED BY INYO COUNTY YUCCA MOUNTAIN REPOSITORY ASSESSMENT OFFICE Inyo County completed Year One of U.S. Department of Energy Cooperative Agreement No. DE-FC28-06RW12368. This report presents the results of research conducted within this cooperative agreement in the context of Inyo County's Yucca Mountain oversight program goals and objectives. The Hydrodynamics Group, LLC prepared this report for Inyo County Yucca Mountain repository Assessment Office. The overall goal of Inyo County's Yucca Mountain research program is the evaluation of far-field issues related to potential transport, by ground water, of radionuclide into Inyo County, including Death Valley, and the evaluation of a connection between the Lower Carbonate Aquifer (LCA) and the biosphere. Data collected within the cooperative agreement is included in interpretive illustrations and discussions of the results of our analysis. The central element's of this Cooperative Agreement program was the drilling of exploratory wells, analysis of geochemical data, geophysical surveys, and geological mapping of the Southern Funeral Mountain Range. The culmination of this research was two numerical ground water models of the Southern Funeral Mountain Range and Yucca Mountain region demonstrating the potential of a hydraulic connection between the LCA and the major springs in the Furnace Creek area of Death Valley. 1.0 Introduction The focus of the investigations by the Hydrodynamics Group for Inyo County is to assemble the best possible data on the Paleozoic Carbonate Aquifer, and then to use that data to assess the likelihood of contaminant transport from the planned Yucca Mountain high-level nuclear waste repository to the biosphere in Inyo County. -
NV EAS Plan Attachment 2-Operational Areas
Nevada Emergency Alert System Plan Attachment 2. Nevada EAS Operational Areas ATTACHMENT 2 NEVADA EAS OPERATIONAL AREAS The Nevada EAS Operational Area is divided into three sections. Western Nevada/Eastern California . Southern Nevada/Inyo County, California . Eastern Nevada Jurisdictions within the Nevada EAS Operational Areas Western Nevada/Eastern Eastern Nevada Southern Nevada/Inyo County, California California Carson City Elko County Clark County Churchill County Eureka County Esmeralda County Douglas County Humboldt County Lincoln County Lyon County Lander County Nye County (southern) Mineral County White Pine County Inyo County (CA) Nye County (northern) San Bernardino County (CA) Pershing County Mohave County (AZ) Washoe County Storey County Alpine County (CA)* El Dorado County (CA)* Lassen County (CA) Modoc County (CA)* Mono County (CA) Placer County (CA)* Nevada EAS Operational Areas Plumas County (CA)* . Sierra County (CA)* 2 *Areas east of the Sierra Nevada crest. Italicized text refers to non-Nevada jurisdictions. Southern Inyo County, California covers the area from the village of Independence in the north to the south county line and includes the communities of Shoshone, Death Valley National Park and headquarters, Furnace Creek, Cartagom, Barlett, Stovepipe Wells, Panamint Springs, Keeler, Olancha, Little Lake, Lone Pine, and Lake Owens. The area north of Independence is in Attachment the Western Nevada/Eastern California Operational Area. No broadcast stations in the Northern Inyo County area are able to receive signals from Las Vegas or Reno broadcast stations. Local EAS activations can be made through the use of CAP EAS by originating officials or by going through the California Governor's Office of Emergency Services. -
Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs: Finding Aid
http://oac.cdlib.org/findaid/ark:/13030/tf2p30028s No online items Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs: Finding Aid Finding aid prepared by Jennifer Watts. The Huntington Library, Art Collections, and Botanical Gardens Photo Archives 1151 Oxford Road San Marino, California 91108 Phone: (626) 405-2191 Email: [email protected] URL: http://www.huntington.org © August 1999 The Huntington Library. All rights reserved. Historical Society of Southern photCL 400 volume 2 & volume 3 1 California Collection -- Charles Puck Collection of Negatives a... Overview of the Collection Title: Historical Society of Southern California Collection -- Charles Puck Collection of Negatives and Photographs Dates (inclusive): 1864-1963 Bulk dates: 1920s-1950s Collection Number: photCL 400 volume 2 & volume 3 Creator: Puck, Charles, 1882-1968 Extent: 11,400 photographs in 42 boxes (30.29 linear feet) Repository: The Huntington Library, Art Collections, and Botanical Gardens. Photo Archives 1151 Oxford Road San Marino, California 91108 Phone: (626) 405-2191 Email: [email protected] URL: http://www.huntington.org Abstract: The Puck Collection consists of more than 11,000 photographs and negatives both taken and collected by Los Angeles resident and local history enthusiast Charles Puck (1882-1968), which he donated to the Historical Society of Southern California over more than twenty years in the mid-20th century. The photographs date from 1864 to 1963 (bulk 1920s-1950s) and depict buildings, monuments, civic happenings, modes of transportation, flora and fauna, and anything else that captured his particular interests. Puck compiled several scrapbooks on topics such as adobes and buildings of Los Angeles, illustrating them with his photographs and annotating them with historical anecdotes and personal recollections. -
5 Day Itinerary
by a grant from Travel Nevada. Travel from grant a by possible made brochure This JUST 98 MILES NORTH OF LAS VEGAS ON HIGHWAY 95. HIGHWAY ON VEGAS LAS OF NORTH MILES 98 JUST www.beattynevada.org Ph: 1.866.736.3716 Ph: Studio 401 Arts & Salon & Arts 401 Studio Mama’s Sweet Ice Sweet Mama’s Smash Hit Subs Hit Smash VFW Chow VFW Smokin’ J’s BBQ J’s Smokin’ shoot out or two performed by our local cowboys. cowboys. local our by performed two or out shoot Gema’s Café Gema’s historical area you might catch a glimpse of a a of glimpse a catch might you area historical Death Valley Coffee Time Coffee Valley Death of our local eateries. If you are in the downtown downtown the in are you If eateries. local our of Roadhouse 95 Roadhouse After your day trips into the Valley, relax at one one at relax Valley, the into trips day your After Sourdough Saloon & Eatery & Saloon Sourdough lunch at Beatty’s Cottonwood Park. Park. Cottonwood Beatty’s at lunch Hot Stuff Pizza Stuff Hot Store or enjoy walking your dog or having a picnic picnic a having or dog your walking enjoy or Store Mel’s Diner Mel’s Town, the Famous Death Valley Nut and Candy Candy and Nut Valley Death Famous the Town, Happy Burro Chili & Beer & Chili Burro Happy open daily from 10 am to 3 pm, Rhyolite Ghost Ghost Rhyolite pm, 3 to am 10 from daily open The Death Valley Nut & Candy Store Candy & Nut Valley Death The can find in our little town, the Beatty Museum, Museum, Beatty the town, little our in find can LOCAL SHOPS & EATERIES & SHOPS LOCAL Day area, be sure to visit the unique businesses that you you that businesses unique the visit to sure be area, BEATTY Between trips to explore the Death Valley Valley Death the explore to trips Between your plan for each day, and set up a check in time. -
California State University, Northridge
CALIFORNIA STATE UNIVERSITY, NORTHRIDGE THE CHANGING FACE OF TOURISM IN DEATH VALLEY A thesis submitted in partial fulfillment of the requirements For the degree of Master of Arts in Geography By Tina White December 2013 The thesis of Tina White is approved: ____________________________________ _____________________ Ronald Davidson, Ph.D. Date ____________________________________ _____________________ Edward Jackiewicz, Ph.D. Date ____________________________________ _____________________ Julie E. Laity, Ph.D., Chair Date California State University, Northridge ii ACKNOWLEDGEMENTS I acknowledge, and most heartily thank, the CSUN faculty members who have continuously supported and encouraged me through the (too) many years I have spent working towards this degree. First and foremost, I am grateful for and to my thesis advisor, Professor Julie Laity, who has taught me about physical geography and academic success in the classroom, in the field, and during our talks in her office. And, of course, there is she from whom I have learned so much geomorphology and with whom I have had so much fun in the field: Professor Amalie Orme. To my thesis committee members Ron Davidson and Ed Jackiewicz, thank you so much for your time and assistance; I appreciate your expertise and input. Further, I have been fortunate to have taken classes with and/or had the opportunity to learn informally from the entire CSUN Geography Department faculty teaching from 1997 through the present at one time or another, as well as from some great folks in the CSUN Geology Department. I have learned something from each and every one of you, and will be eternally grateful. I also want to thank multiple employees at Death Valley National Park, in particular Terry Baldino and Alex Cabana and their numerous staff members, who took the time to speak with me about this topic; their input was invaluable and their insights intriguing. -
Geology of the Panamint Butte Quadrangle, Inyo County, California
Geology of the Panamint Butte Quadrangle, Inyo County, California By WAYNE E; HALL GEOLOGICAL SURVEY BULLETIN 1299 Prepared in cooperation with the California Department of Conservation, Division of Mines and Geology KhCEIVED JUL161971 u.8.1 teuisfiUt, it UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 75-610447 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract_________________________________-_.-______-__--_-_--_--- 1 Introduction. ___________-______--_____--_----.--___--__-__--------- 2 Climate.and vegetation._________.__....__.._____-___________-__ 3 Water supply-________________________________________________ 3 Previous work__________________________.___._____._1________ 4 Acknowledgments- _______________._______..____-__-_---------_- 4 General geology.__________________________-__..____--_----_-_--__-- 5 Precambrian(?) rocks._____________.__________.._----___-___-_-_-__- 7 Paleozoic rocks._____.__.___--________-___-____-_-----_---_--.-.-_- 8 Cambrian System_____________________________________________ 8 Carrara Formation.__________________..-_____--____---__-_- 8 Bonanza King Formation___._.______..__._._.....____.____ 10 Nopah Formation._____...____-_-_.....____________-_-_-__- 11 Ordovician System___________________________________________ 13 Pogonip Group_____-__-______-____-_-..----------_--._-_-_- 13 Eureka Quartzite.______________-_____..___-_-_---_-----_--_ 16 Ely Springs Dolomite__---__-______________________________ 18 Silurian and Devonian Systems___________..__-_-__----_-__-___- 21 Hidden Valley Dolomite......._____________________________ 21 Devonian System_____________________________________________ 22 Lost Burro Formation.....__________________________________ 22 Mississippian System.___._____..____._.._..__.___..._._._..__.