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Geologic Map of the Long Valley Caldera, Mono-Inyo Craters
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-1933 US. GEOLOGICAL SURVEY GEOLOGIC MAP OF LONG VALLEY CALDERA, MONO-INYO CRATERS VOLCANIC CHAIN, AND VICINITY, EASTERN CALIFORNIA By Roy A. Bailey GEOLOGIC SETTING VOLCANISM Long Valley caldera and the Mono-Inyo Craters Long Valley caldera volcanic chain compose a late Tertiary to Quaternary Volcanism in the Long Valley area (Bailey and others, volcanic complex on the west edge of the Basin and 1976; Bailey, 1982b) began about 3.6 Ma with Range Province at the base of the Sierra Nevada frontal widespread eruption of trachybasaltic-trachyandesitic fault escarpment. The caldera, an east-west-elongate, lavas on a moderately well dissected upland surface oval depression 17 by 32 km, is located just northwest (Huber, 1981).Erosional remnants of these mafic lavas of the northern end of the Owens Valley rift and forms are scattered over a 4,000-km2 area extending from the a reentrant or offset in the Sierran escarpment, Adobe Hills (5-10 km notheast of the map area), commonly referred to as the "Mammoth embayment.'? around the periphery of Long Valley caldera, and The Mono-Inyo Craters volcanic chain forms a north- southwestward into the High Sierra. Although these trending zone of volcanic vents extending 45 km from lavas never formed a continuous cover over this region, the west moat of the caldera to Mono Lake. The their wide distribution suggests an extensive mantle prevolcanic basement in the area is mainly Mesozoic source for these initial mafic eruptions. Between 3.0 granitic rock of the Sierra Nevada batholith and and 2.5 Ma quartz-latite domes and flows erupted near Paleozoic metasedimentary and Mesozoic metavolcanic the north and northwest rims of the present caldera, at rocks of the Mount Morrisen, Gull Lake, and Ritter and near Bald Mountain and on San Joaquin Ridge Range roof pendants (map A). -
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. -
Short Range Transit Plan – 2009 (PDF)
Eastern Sierra Transit Authority Short Range Transit Plan Volume 1 Service and Financial Plan Final Report January 2009 Eastern Sierra Transit Authority Short Range Transit Plan Table of Contents Executive Summary ......................................................................... ES-1 Short Range Transit Plan Objectives ....................................................................... ES-1 Overview of Existing Services.................................................................................... ES-1 Transit Needs .............................................................................................................. ES-1 Transit Dependent Population ...........................................................................ES-1 Tourist and Visitor Market ................................................................................ES-2 Seamless Transit System ...................................................................................ES-3 ESTA Mission, Goals and Performance Standards................................................. ES-3 395 Corridor Services................................................................................................. ES-4 Rural Transit Services................................................................................................ ES-5 Bishop Local Services................................................................................................. ES-6 Mammoth Local Services.......................................................................................... -
Lower Owens River Draft Recreation Use Plan
LOWER OWENS RIVER RECREATION USE PLAN JANUARY 2012 DRAFT MIG, Inc. 815 SW 2ND AVE. SUITE 200 PORTLAND, OR 97204 503.297.1005 www.migcom.com TABLE OF CONTENTS Executive Summary..............................................................................i I. Introduction ................................................................................1 II. Existing Conditions ....................................................................6 III. Recreation Preferences and Goals ...........................................11 IV. Recreation Use Plan Alternatives.............................................20 V. Next Steps.................................................................................37 Appendix A: Potential Impacts for Further Study ......................... A-1 Appendix B: Community Involvement Findings ............................ B-1 LOWER OWENS RIVER RECREATION USE PLAN TABLE OF CONTENTS Executive Summary..............................................................................i I. Introduction ................................................................................1 II. Existing Conditions ....................................................................6 III. Recreation Preferences and Goals ...........................................11 IV. Recreation Use Plan Alternatives.............................................20 V. Next Steps.................................................................................37 Appendix A: Potential Impacts for Further Study ......................... A-1 Appendix -
Mono and Southeastern Great Basin
3 •. .,• .{ • ,l<. • --• - • • •• 4:"."".. • 116 •,. California’s Botanical Landscapes - 3 chapter five Mono and Southeastern Great Basin The eastern fringe of California slices The crest of the Sierra Nevada defines Above: The crest of the Sierra off a thin strand at the edge of a vast the western hydrologic edge of the Great Nevada defines the western edge of interior biome, the Great Basin. Often Basin, within which waters drain into the Great Basin in central eastern California. The Mono Basin, characterized as an immense and homo interior basins. The entirety of the Sierra with its crown jewel Mono Lake, geneous sagebrush (Artemisia sp.) sea, Nevada was built by similar geologic exemplifies the character of the this region in fact encompasses great forces that created the Great Basin. The California part of this province, topographic, geologic, climatic, and vege narrative for vegetation in this chapter with expansive cold-adapted tative diversity, haunting in expansiveness starts with the lower montane (~2,500 m sagebrush steppe intermixed with hardy forbs and grasses. of landscape, surprising in richness of at the latitude of Mono Lake) and basin Robert Wick hidden canyons and wetlands. Long lines bottom environments of the eastern Opposite: A winter evening of basin and range draw the eye outward Sierra Nevada, and goes on to embrace along Hot Creek, with rubber to where land meets sky; wave after wave the entire elevation gradients from basin rabbitbrush and sagebrush of mountain ranges pounding the sage to summits of the mountain ranges east spread over rolling hills of the surf. If only a slice, California is fortunate ward to the California-Nevada state Long Valley Caldera. -
Floods, Droughts, and Lawsuits: a Brief History of California Water Policy
1Floods, Droughts, and Lawsuits: A Brief History of California Water Policy MPI/GETTY IMAGES The history of California in the twentieth century is the story of a state inventing itself with water. William L. Kahrl, Water and Power, 1982 California’s water system might have been invented by a Soviet bureaucrat on an LSD trip. Peter Passell, “Economic Scene: Greening California,” New York Times, 1991 California has always faced water management challenges and always will. The state’s arid and semiarid climate, its ambitious and evolving economy, and its continually growing population have combined to make shortages and conflicting demands the norm. Over the past two centuries, California has tried to adapt to these challenges through major changes in water manage- ment. Institutions, laws, and technologies are now radically different from those brought by early settlers coming to California from more humid parts of the United States. These adaptations, and the political, economic, technologic, and social changes that spurred them on, have both alleviated and exacerbated the current conflicts in water management. This chapter summarizes the forces and events that shaped water man- agement in California, leading to today’s complex array of policies, laws, and infrastructure. These legacies form the foundation of California’s contemporary water system and will both guide and constrain the state’s future water choices.1 1. Much of the description in this chapter is derived from Norris Hundley Jr.’s outstanding book, The Great Thirst: Californians and Water: A History (Hundley 2001), Robert Kelley’s seminal history of floods in the Central Valley, Battling the Inland Sea (Kelley 1989), and Donald Pisani’s influential study of the rise of irrigated agriculture in California, From the Family Farm to Agribusiness: The Irrigation Crusade in California (Pisani 1984). -
Lone Pine / Mt. Whitney 23-24 Snowboarders
Inyo National Forest >>> >>> >>> >>> >>> >>> >>> >>> Visitor Guide 2011-2012 >>> >>> >>> >>> >>> >>> >>> >>> >>> >>> $1.00 Suggested Donation FRED RICHTER Inspiring Destinations © Inyo National Forest Facts xtending 165 miles along the White Mountain and Owens River Mam moth Mountain Ski California/Nevada border Headwaters wildernesses. Devils Area becomes a sum mer “Inyo” is a Paiute Ebetween Los Angeles and Postpile Na tion al Mon u ment, mecca for mountain bike Reno, the Inyo National Forest, ad min is tered by the National Park en thu si asts as they ride Indian word meaning established May 25, 1907, in cludes Ser vice, is also located within the the chal leng ing Ka mi ka ze 1,900,543 acres of pris tine lakes, Inyo Na tion al For est in the Reds Trail from the top of the “Dwelling Place of fragile mead ows, wind ing streams, Mead ow area west of Mam moth 11,053foot high rugged Sierra Ne va da peaks and Lakes. In addition, the Inyo is home Mam moth Moun tain or the Great Spirit.” arid Great Basin moun tains. El e va to the tallest peak in the low er 48 one of the many other trails tions range from 3,900 to 14,497 states, Mt. Whitney (14,497 feet) that transect the front feet, pro vid ing diverse habitats and is adjacent to the lowest point coun try of the forest. that sup port vegetation patterns in North America at Badwater in Thirtysix trailheads provideJ ranging from semiarid deserts to Death Val ley Na tion al Park (282 ac cess to over 1,200 miles of trail high al pine fellfields. -
Snowcreek Ski Area Deer Study 1994 Spring and Fall Migration Study
SNOWCREEKSKI AREA DEERSTUDY 1994SPRING AND FALL MIGRATION STUDY heparedfor: DempseyConstruction C orporation P.O.Box 657 MammothLakes, CA 93546 6191934-6,861 hepared by: TimothyTaylor & Associates P.O.Box l9l JuneLake, CA93529 619t648-7227 I\,larch1995 Tableof Contents Page Chapterl. Introductionand Methods.... .............l-l INTRODUCTTON..... ...........l-l PERMITAREA...... 1.2 METHODS....,.......... ............r-2 RadioTelemetry Studies...... ........L-2 RadioTracking ofDeer...... ..................l-2 HoldineArea Studies.............. .....14 D-eerCounts Surveys... ........14 tlabitatUse Studies................ ..............l-6 MigrationCorridor Counts...... .....1-7 InfraredSensor Equipment ...................l-7 HabitatMapping... .....l-7 WeatherData.......... ....1-7 ORGANIZATIONOF THISREPORT.. ..................l-8 Chapter2. SpringMigration Surveys..... .............2-l STAGE 1: MIGRATION BETWEEN THE WINTER RA}.IGE IN ROUNDVALLEY A}ID TI{E SFIERWINHOLDING AREA....... ........... 2.1 Locationsof DeerMovements................ ......2-l STAGE2: TIIE SHERWINHOLDING AREA....... .................2-3 Timing andIntensity of DeerUse in the SherwinHolding Area.......2-3 Radio-CollaredDeer.. ........2-3 DeerCount Surveys..... .......2-5 Estimatesof DeerAbundance in theSherwin Holding Area.............2-10 Patternsof DeerHabitat Use in theSherwin Holding Area.......... ....2-14 DeerCount Surveys..... .......2-14 Radio-CollaredDeer.. .........2-19 Patternsof DeerDistribution in the SherwinHolding Area.......... ....2-19 STAGE 3: DEER MIGRATION -
Manzanar National Historic Site Geologic Resource Evaluation
MANZANAR NATIONAL HISTORIC SITE GEOLOGIC RESOURCES MANAGEMENT ISSUES SCOPING SUMMARY Sid Covington Geologic Resources Division October 26, 2004 Executive Summary Geologic Resource Evaluation scoping meetings for three parks in the Mojave Network were held April 28 - May 1, 2003, in St George, UT, Barstow, CA, and Twentynine Palms, CA, respectively. Unfortu- nately, due to time and travel constraints, scoping was not done at Manzanar National Historic Site (MANZ). The following report identifies the major geologic issues and describes the geology of MANZ and the surrounding the area. The major geologic issues affecting the park are: 1. Flooding and erosion due to runoff from the Sierra Nevada mountains to the west. 2. Recurring seismic activity 3. The potential for volcanic activity from Long Valley Caldera 4. Proposed gravel pit upslope from MANZ Introduction The National Park Service held Geologic Resource Evaluation scoping meetings for three parks in the Mojave Network: Parashant National Monument, Mojave National Preserve, and Joshua Tree National Park. These meeting were held April 28 - May 1, 2003, in St George, UT, Barstow, CA and Twentynine Palms, CA respectively. The purpose of these meeting was to discuss the status of geologic mapping, the associated bibliography, and the geologic issues in the respective park units. The products to be derived from the scoping meeting are: (1) Digitized geologic maps covering the park units; (2) An updated and verified bibliography; (3) Scoping summary (this report); and (4) A Geologic Resources Evaluation Report which brings together all of these products. Although there was no onsite scoping for MANZ, these products will be produced for the historic site. -
Long Valley Caldera Lake and Reincision of Owens River Gorge
Long Valley Caldera Lake and Reincision of Owens River Gorge Scientific Investigations Report 2016–5120 U.S. Department of the Interior U.S. Geological Survey COVER View southwestward across Long Valley Caldera and Sierra Nevada. Caldera depression, as wide as 30 km, formed during eruption of Bishop Tuff at 767 ka. Sierra consists of Mesozoic plutonic rocks, Mesozoic metavolcanic rocks, and Paleozoic marine metasedimentary strata. Patchy white exposures in caldera are lacustrine siltstones of middle Pleistocene age that are the top of a 700-m-thick accumulation of intracaldera lake sediment. Sedimentation in the deep closed depression took 600,000 years to raise lake level to its threshold for overflow around 150 ka. Outlet arm of Lake Crowley reservoir leads into Owens River Gorge, which extends 30 km southeast across a welded Bishop Tuff outflow sheet. Overflow and draining of the caldera lake reincised a 200-m-deep precaldera gorge (in Mesozoic granodiorite) that had been diverted by 3.3-Ma basalt and later blanketed by the Bishop Tuff. Round Valley Fault is 2-km-high east- facing scarp at left. At lower center of image, precaldera Glass Mountain rhyolite edifice was truncated by caldera collapse and draped by complexly incised apron of Bishop Tuff. Photo is a NaturalVue satellite image mosaic, which has been extracted from a global dataset of natural-color Landsat-7 multispectral images compiled by MDA Information Systems, Inc. Cover image produced and processed by Joel E. Robinson. Imagery copyright 2010, MDA Information Systems, USGS, NASA. Long Valley Caldera Lake and Reincision of Owens River Gorge By Wes Hildreth and Judy Fierstein Scientific Investigations Report 2016–5120 U.S. -
Schedule of Proposed Action (SOPA) 07/01/2017 to 09/30/2017 Inyo National Forest This Report Contains the Best Available Information at the Time of Publication
Schedule of Proposed Action (SOPA) 07/01/2017 to 09/30/2017 Inyo National Forest This report contains the best available information at the time of publication. Questions may be directed to the Project Contact. Expected Project Name Project Purpose Planning Status Decision Implementation Project Contact Projects Occurring in more than one Region (excluding Nationwide) Sierra Nevada Forest Plan - Land management planning On Hold N/A N/A Donald Yasuda Amendment (SNFPA) 916-640-1168 EIS [email protected] Description: Prepare a narrowly focused analysis to comply with two orders issued by the Eastern District Court of California on November 4, 2009. Correct the 2004 SNFPA Final SEIS to address range of alternatives and analytical consistency issues. Web Link: http://www.fs.fed.us/r5/snfpa/2010seis Location: UNIT - Eldorado National Forest All Units, Lassen National Forest All Units, Modoc National Forest All Units, Sequoia National Forest All Units, Tahoe National Forest All Units, Lake Tahoe Basin Mgt Unit, Carson Ranger District, Bridgeport Ranger District, Plumas National Forest All Units, Sierra National Forest All Units, Stanislaus National Forest All Units, Inyo National Forest All Units. STATE - California, Nevada. COUNTY - Alpine, Amador, Butte, Calaveras, El Dorado, Fresno, Inyo, Kern, Lassen, Madera, Mariposa, Modoc, Mono, Nevada, Placer, Plumas, Shasta, Sierra, Siskiyou, Tulare, Tuolumne, Yuba, Douglas, Esmeralda, Mineral. LEGAL - Along the Sierra Nevada Range, from the Oregon/California border south to Lake Isabella as well as lands in western Nevada. Sierra Nevada National Forests. R5 - Pacific Southwest Region, Occurring in more than one Forest (excluding Regionwide) Inyo, Sequoia and Sierra - Land management planning In Progress: Expected:11/2017 12/2017 Nevia Brown National Forests Land DEIS NOA in Federal Register 7075629121 Management Plans Revision 05/27/2016 [email protected] EIS Est. -
Collaborative Management and Research in the Great Basin — Examining the Issues and Developing a Framework for Action
Collaborative Management and Research in the Great Basin — Examining the Issues and Developing a Framework for Action United States Departmentof Agriculture / Forest Service Rocky Mountain Research Station General Technical Report RMRS-GTR-204 February 2008 Chambers, Jeanne C.; Devoe, Nora; Evenden, Angela, eds. 2008. Collaborative management and research in the Great Basin — examining the issues and developing a framework for action. Gen. Tech. Rep. RMRS-GTR-204. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 66 p. Abstract The Great Basin is one of the most imperiled regions in the United States. Sustaining its ecosystems, resources, and human populations requires strong collaborative partnerships among the region’s research and management organizations. This GTR is the product of a workshop on “Collaborative Watershed Research and Management in the Great Basin” held in Reno, Nevada, November 28 through 30, 2006. It provides an overview and individual issues papers describing critical research and management issues facing the Great Basin. It also includes summaries of workshop sessions on (1) developing collaborative management and research programs and (2) devising mechanisms for organization and communication. Co-sponsors of the workshop included the University of Nevada, Reno, Desert Research Institute; Great Basin Cooperative Ecosystems Studies Unit; Utah State University; Agricultural Research Service; Bureau of Land Management; State of Nevada, Department of Wildlife and Game; USDA Forest Service, Region 4; USDA Forest Service, Rocky Mountain Research Station; and U. S. Geological Survey. Keywords: Great Basin, environmental issues, collaboration, communication, research and management You may order additional copies of this publication by sending your mailing information in label form through one of the following media.