Deepsprings Rangeimproveme
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Interest and the Panamint Shoshone (E.G., Voegelin 1938; Zigmond 1938; and Kelly 1934)
109 VyI. NOTES ON BOUNDARIES AND CULTURE OF THE PANAMINT SHOSHONE AND OWENS VALLEY PAIUTE * Gordon L. Grosscup Boundary of the Panamint The Panamint Shoshone, also referred to as the Panamint, Koso (Coso) and Shoshone of eastern California, lived in that portion of the Basin and Range Province which extends from the Sierra Nevadas on the west to the Amargosa Desert of eastern Nevada on the east, and from Owens Valley and Fish Lake Valley in the north to an ill- defined boundary in the south shared with Southern Paiute groups. These boundaries will be discussed below. Previous attempts to define the Panamint Shoshone boundary have been made by Kroeber (1925), Steward (1933, 1937, 1938, 1939 and 1941) and Driver (1937). Others, who have worked with some of the groups which border the Panamint Shoshone, have something to say about the common boundary between the group of their special interest and the Panamint Shoshone (e.g., Voegelin 1938; Zigmond 1938; and Kelly 1934). Kroeber (1925: 589-560) wrote: "The territory of the westernmost member of this group [the Shoshone], our Koso, who form as it were the head of a serpent that curves across the map for 1, 500 miles, is one of the largest of any Californian people. It was also perhaps the most thinly populated, and one of the least defined. If there were boundaries, they are not known. To the west the crest of the Sierra has been assumed as the limit of the Koso toward the Tubatulabal. On the north were the eastern Mono of Owens River. -
Late Cenozoic Displacement Transfer Analysis Within Deep Springs
LATE CENOZOIC DISPLACEMENT TRANSFER ANALYSIS WITHIN DEEP SPRINGS VALLEY, EASTERN CALIFORNIA WITH GRAVITY MODELING by Sarah Anne Sokol APPROVED BY SUPERVISORY COMMITTEE: ___________________________________________ John F. Ferguson, Chair ___________________________________________ John W. Geissman ___________________________________________ Carlos L. V. Aiken Copyright 2019 Sarah Anne Sokol All Rights Reserved Dedicated to Saul and Gladys Sokol, and Perry Leynor LATE CENOZOIC DISPLACEMENT TRANSFER ANALYSIS WITHIN DEEP SPRINGS VALLEY, EASTERN CALIFORNIA WITH GRAVITY MODELING by SARAH ANNE SOKOL, BS THESIS Presented to the Faculty of The University of Texas at Dallas in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE IN GEOSCIENCES THE UNIVERSITY OF TEXAS AT DALLAS May 2019 ACKNOWLEDGMENTS I would like to thank my advisors and committee members, John Ferguson, John Geissman, and Carlos Aiken, for their support in this endeavor. Their aid and expertise was integral to the completion of this research. In addition, I thank John Oldow for his assistance in the field and for laying the foundation on which this research was built. My appreciation for the support and assistance I received from other University of Texas at Dallas students cannot be understated. I thank Nicholas Mueller and August Ridde for assisting in the collection of data for this research and for their continued support following the field season. Apart from all others, I thank Lauren Landreneau whose partnership is invaluable and whose assistance and encouragement was an immeasurable source of fortitude. I thank The University of Texas at Dallas Department of Geosciences for their support and confidence in the pursuit of this research. This work was supported by Pioneer Natural Resources and The University of Texas at Dallas. -
Deep Springs College Community Newsletter Spring 2018
Deep Springs College Community Newsletter Spring 2018 “Deep Springs really helped give me an ethical framework - a loving education in what it meant to be sincere - what it meant to care about and believe in something.” - Nathan Deuel DS97 “Deep Springs is a place that values a combination of the intellectual and the practical. That’s kind of what appealed to me about journalism. On one hand it gives you an opportunity to grapple with big ideas and big problems, but it’s also very grounded in physical reality of actual daily life.” - Zach Mider DS96 President’s Letter Current Courses Deep Springs is not conventional in its methods, and any attempt to introduce conventional methods or any radical Power - Jennifer Smith change would destroy its usefulness altogether. What is power? What does it mean to possess power, and to exercise it over or against others? What are the resources and conditions that make people and groups powerful or powerless, and how do power relations condition interactions between persons? How can we study So wrote L.L. Nunn sometime after 1917, in an aspirational job description for the next head of the college he called The Man Re- the abstraction “power” as a thing in the world, in order to know its ways? This course undertakes a broad exploration of the theme of quired for Deep Springs. power, seeking to answer these and other questions about power’s nature, scope, and operation. Readings include analyses of power and related concepts from political and social theorists, and also a diverse collection of studies of power as a thing used/possessed in the world Now, over one hundred years after its founding, Deep Springs is a few days away from a major change—the admission of its first by real individuals and groups. -
The Hydrology and Mineralogy of Deep Springs Lake Inyo County, California
The Hydrology and Mineralogy of Deep Springs Lake Inyo County, California GEOLOGICAL SURVEY PROFESSIONAL PAPER 502-A The Hydrology and Mineralogy of Deep Springs Lake Inyo County, California By BLAIR F. JONES CLOSED-BASIN INVESTIGATIONS GEOLOGICAL SURVEY PROFESSIONAL PAPER 502-A A study of the relation between hydrologic factors and .saline mineralogy for a small playa in the western Great Basin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract _______ ---_-----·-____ --_-- __ ------_-_-- ___ _ A1 Hydrochemistry-Continued Sampling _____________________________________ _ Introduction--------------~------------------------ 2 A25 Acknowledgments ___ .. _________________________ _ 2 pH and alkalinitY------------------------------- 26 Geography __________ .. _________________________ _ 3 Major-element analysis ____ ---------------------- 27 Sulfide _______________________________________ _ Bedrock geology of the Deep Springs Valley ______ _ 6 27 Quaternary geology_--·----- ____________________ _ Presentation and interpretation of data ___________ _ 27 8 Inflow ________________________________________ _ Hydrology ______________ .. _________________________ _ 9 32 Lake area _____________________________________ _ Precipitation ________ .. _________________________ _ 9 40 Evaporation _______ --·---- -
California Desert Protection Act of 1993 CIS-NO
93 CIS S 31137 TITLE: California Desert Protection Act of 1993 CIS-NO: 93-S311-37 SOURCE: Committee on Energy and Natural Resources. Senate DOC-TYPE: Hearing DOC-NO: S. Hrg. 103-186 DATE: Apr. 27, 28, 1993 LENGTH: iii+266 p. CONG-SESS: 103-1 ITEM-NO: 1040-A; 1040-B SUDOC: Y4.EN2:S.HRG.103-186 MC-ENTRY-NO: 94-3600 INCLUDED IN LEGISLATIVE HISTORY OF: P.L. 103-433 SUMMARY: Hearings before the Subcom on Public Lands, National Parks, and Forests to consider S. 21 (text, p. 4-92), the California Desert Protection Act of 1993, to: a. Expand or designate 79 wilderness areas, one wilderness study area in the California Desert Conservation Area, and one natural reserve. b. Expand and redesignate the Death Valley National Monument as the Death Valley National Park and the Joshua Tree National Monument as the Joshua Tree National Park. c. Establish the Mojave National Park and the Desert Lily Sanctuary. d. Direct the Department of Interior to enter into negotiations with the Catellus Development Corp., a publicly owned real estate development corporation, for an agreement or agreements to exchange public lands or interests for Catellus lands or interests which are located within the boundaries of designated wilderness areas or park units. e. Withdraw from application of public land laws and reserve for Department of Navy use certain Federal lands in the California desert. f. Permit military aircraft training and testing overflights of the wilderness areas and national parks established in the legislation. Title VIII is cited as the California Military Lands Withdrawal and Overflights Act of 1991. -
Cross Cordillera Field Trip Guide
GS Field Trip: End of Summer 2016 GS191/291 (Miller, no Klemperer (went to Tibet), Lund Snee, Gottlieb) Listed as Fall Quarter class under Miller Crossing the Cordillera: From the Colorado Plateau to the Sierra Nevada Field trip (1 credit), advanced ugrad to grad level, but all welcome Dates: September 15 to Sept. 21 (T.A. Eric Gottlieb) There is unprecedented controversy about the paleo-topographic evolution of the western United States. How thick and how high was the crust following Mesozoic crustal shortening? Did the region between the Sierra Nevada and the Colorado Plateau form a high plateau, the Nevadaplano, underlain by 60 km thick crust? When did this thick crust collapse to its present crustal thickness of only 30 km? Did extension happen as a result of, during and shortly after crustal thickening? Or did extension take place only in the Miocene, during formation of Basin and Range topography? How much stretching is represented by Basin and Range faulting? Can it account for thinning of crust by 30 km? This field trip will provide you with an exceptional opportunity to view a complete cross-section of the geology of the southern part of the North American Cordillera, from the undeformed Colorado Plateau on the east to Mount Whitney and the Mesozoic Sierra Nevada arc on the west. With these big questions in mind, our stops will focus on Mesozoic shortening, when the Cordillera is believed to have looked like the Andes, and on younger extensional structures (including a variety faults in Death Valley), with a critical view and discussion of age, geometry and offset along normal faults. -
Visiting the Park During COVID-19 Hottest, Driest, Lowest
Winter Death Valley National Park Visitor Guide ANDERLAY Sunset from Dantes View .VT Welcome to Your Death Valley Adventure Visiting the Park Hottest, Driest, Lowest Death Valley National Park is the In the cooler winter months, endless During COVID-19 hottest place on Earth, with a recorded exploration and a diversity of temperature of 134 °F (57°C) on experiences await you. Hiking, visiting Death Valley takes the health of its visitors, staff, July 10, 1913. It is also the driest historic sites, traveling backcountry and partners seriously. We encourage you to follow U.S. national park, and Badwater roads, and seeing the night skies CDC guidance to reduce the spread of COVID-19. Basin (-282 feet) features the lowest are only a few of the opportunities elevation in North America! available! You Should: What to Expect These conditions come together to With over 3 million acres of federally make Death Valley a land of extremes, designated Wilderness, so many where the powerful heat is a force adventures await! Walk among majestic Maintain a 6-foot During this pandemic, park of nature, and the air further dries sand dunes, navigate twisted slot distance from others managers will be assessing local everything it contacts. canyons, climb rocky peaks, or stroll who aren't in your conditions & guidance from local, along salt flats during your Death group. state, and national health officials, This summer, Death Valley reached Valley adventure. and will respond to changing 128°F, which was the hottest recorded Cover your mouth when conditions. temperature anywhere on Earth since Inside this trip-planning guide learn you cough or sneeze. -
Alumni Newsletter #95 Fall 2018
ALUMNI NEWSLETTER #95 FALL 2018 While Deep Springs is in one way isolated geographically, the idea was that you were going to be wed to the campus, ranch, farm, garden, garage or shop and to the intel- lectual rigor. Thinking and doing were meant to be complementary. Surgery is a craft and isn’t that different from fixing a tractor or working as a cowboy. I’m working with my hands in a very real way. I have to know intellectually what the right thing to do is, but, at the end of the day, I have to use my hands to deliver that craft in an exacting way. - Brendan Visser DS90 Table of Contents President’s Letter ................................................................................................................................................................... 3 Director of Development’s Letter ....................................................................................................................................... 5 SB President’s Letter ............................................................................................................................................................. 6 Farm, Ranch, and Garden Report ...................................................................................................................................... 7 Fall Courses ............................................................................................................................................................................ 8 Babies ..................................................................................................................................................................................... -
California Desert Protection Act of 1994
California Desert Protection Act of 1994 IN THE HOUSE OF REPRESENTATIVES, U. S., The California Desert Protection Act July 27, 1994 of 1994 designated 44,000 acres of Resolved, That the bill from the Senate (S. 21) entitled new wilderness in the “Nevada "An Act to designate certain lands in the California Triangle” of Death Valley National Desert as wilderness, to establish Death Valley, Joshua Park. Tree, and Mojave National Parks, and for other purposes," do pass with the following AMENDMENTS: Strike out all after the enacting clause, and insert: That this Act may be cited as the "California Desert Protection Act of 1994." FINDINGS AND POLICY SEC. 2. (a) The Congress finds and declares that-- •(1) the federally owned desert lands of Southern California constitute a public wildland resource of extraordinary and inestimable value for this and future generations; •(2) these desert wildlands display unique scenic, historical, archeological, environmental, ecological, wildlife, cultural, scientific, educational, and recreational values used and enjoyed by millions of Americans for hiking and camping, scientific study and scenic appreciation; •(3) the public land resources of the California desert now face and are increasingly threatened by adverse pressures which would impair, dilute, and destroy their public and natural values; •(4) the California desert, embracing wilderness lands, units of the National Park System, other Federal lands, State parks and other State lands, and private lands, constitutes a cohesive unit posing unique and difficult resource protection and management challenges; •(5) through designation of national monuments by Presidential proclamation, through enactment of general public land statutes (including section 601 of the Federal Land Policy and Management Act of 1976, 90 Stat. -
Following the Rivers: Historical Reconstruction of California Voles Microtus Californicus (Rodentia: Cricetidae) in the Deserts of Eastern California
Biological Journal of the Linnean Society, 2016, 119, 80–98. With 6 figures. Following the rivers: historical reconstruction of California voles Microtus californicus (Rodentia: Cricetidae) in the deserts of eastern California CHRIS J. CONROY1*, JAMES L. PATTON1, MARISA C. W. LIM2, MARK A. PHUONG3, BRETT PARMENTER4 and SEBASTIAN HOHNA€ 5 1Museum of Vertebrate Zoology, University of California, 3101 Valley Life Sciences Building, Berkeley, CA, 94720, USA 2Department of Ecology & Evolution, Stony Brook University, 650 Life Sciences Building, Stony Brook, NY, 11794-5245, USA 3Department of Ecology & Evolutionary Biology, University of California, 612 Charles E. Young Dr., South Los Angeles, CA, 90095, USA 4Department of Biology, Warren Wilson College, P.O. Box 9000, Asheville, NC, 28815, USA 5Department of Integrative Biology, University of California, 1005 Valley Life Sciences Building #3140, Berkeley, CA, 94720, USA Received 20 November 2015; revised 1 February 2016; accepted for publication 2 February 2016 The California vole, Microtus californicus, restricted to habitat patches where water is available nearly year- round, is a remnant of the mesic history of the southern Great Basin and Mojave deserts of eastern California. The history of voles in this region is a model for species-edge population dynamics through periods of climatic change. We sampled voles from the eastern deserts of California and examined variation in the mitochondrial cytb gene, three nuclear intron regions, and across 12 nuclear microsatellite markers. Samples are allocated to two mitochondrial clades: one associated with southern California and the other with central and northern California. The limited mtDNA structure largely recovers the geographical distribution, replicated by both nuclear introns and microsatellites. -
Death Valley Backcountry & Wilderness Access
Death Valley National Park Death Valley Backcountry & Wilderness Access National Park Service Death Valley is the largest national park outside of Alaska, with a great mix of both Wilderness recreation and backcountry driving opportunities. The park is over 93% federally protected Wilderness and has more than 1,000 miles of paved and dirt roads. This map provides information to help you access the backcountry safely while protecting this spectacular resource. Backcountry Safety Dispersed (Backcountry) Camping Hazards Camping is allowed one mile away from any developed area, paved road, • Most areas of the backcountry do not have cell phone service. or “day use only” area. Specific areas closed to camping include: • Mine shafts, tunnels, and buildings are extremely hazardous to enter. • On the valley floor, from Ashford Mill in the south to the north end of the shifting sands of the • Watch for rattlesnakes, especially near old structures and vegetated areas near water. Mesquite Flat Sand Dunes • Hantavirus, a potentially fatal disease, is spread through feces, urine, and saliva of rodents. Avoid disturbing or camping in confined areas where there are signs of rodent activity. Backcountry cabins may be unsafe to enter. • On the Eureka and Mesquite Flat Sand Dunes • Watch for Illegal marijuana grows near remote natural springs. If discovered, get out immediately and report location to a ranger. • Within one mile of Greenwater Canyon • Darwin Falls Trail Weather • ”Day Use Only” dirt roads: Titus Canyon Rd, Mosaic Canyon Rd, Natural Bridge Rd, Mustard Canyon, • Heat and very low humidity create extreme dehydration and heat stroke potential during summer. We do not suggest lower elevation hiking between May and October. -
The California Desert Conservation Area
United States Department of the Interior BUREAU OF LAND MANAGEMENT SEPTEMBER 19 8 BLM LIBRARY 88065097 Final Environmental Impact Statement and Proposed Plan Sbc APPENDIX •Volume C APPENDIX IV: AREAS OF CRITICAL ENVIRONMENTAL \\ CONCERN APPENDIX V: RECREATION ^ m APPENDIX VI: MOTORIZED VEHICLE ACCESS r-j *^ CALIFORNIA DESERT CONSERVATION AREA »>«S3A, Bunding 00 PES APPENDIX IV AREAS OF CRITICAL ENVIRONMENTAL CONCERN APPENDIX V RECREATION APPENDIX VI MOTORIZED VEHICLE ACCESS BUREAU OF LAND MANAGEMENT LIBRARY, D • 245A BLDG. 50, DENVER FEDERAL CENTEt DENVER, CO 80225 • Table of Contents VOLUME C Book Title Page IV Areas of Critical Environmental Concern 1 V Recreation 79 VI Motorized Vehicle Access 335 APPENDIX IV AREAS OF CRITICAL ENVIRONMENTAL CONCERN . Table of Contents APPENDIX IV AREAS OF CRITICAL ENVIRONMENTAL CONCERN Part Title Page la Special Interim Management Prescriptions for Proposed ACECs 1 1. White Mountain City 1 2. Deep Springs Valley Black Toad Habitat 1 3. Eureka Valley Dunes 2 4. Saline Valley 3 5. Cerro Gordo 3 6. Darwin Falls/Canyon 4 7. Rose Spring Area 5 8. Surprise Canyon 6 9. Greenwater Canyon 7 10. Fossil Falls 8 1 1 Sand Canyon 8 12. Great Falls Basin Area 9 13. Amargosa River/Grimshaw Lake 10 14. Kingston Range 11 15. Mesquite Lake 12 16. Trona Pinnacles 13 17. Denning Spring 13 18. Salt Creek (Dumont) 14 19. Clark Mountain 15 20. Jawbone-Butterbread Area 16 21. Last Chance Canyon 17 22. Desert Tortoise Research Natural Area 17 23. Christmas Canyon 18 24. Bedrock Spring 19 25. Steam Well 19 26. Squaw Spring 20 27. Goldstone 20 28.