Conway Ranch Mono County, California
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California Pika Consortium Mono Basin- Bodie Hills Field Trip Sunday, July 31, 2011 – Monday, August 1, 2011
California Pika Consortium Mono Basin- Bodie Hills Field Trip Sunday, July 31, 2011 – Monday, August 1, 2011 Amended with comments and observations in red font after the Field Trip: 13 August 2011 (cim) Field Trip Objectives: Provide a forum for California Pika Consortium (CPC) participants to observe and discuss topics of current interest at key and relevant field sites. In particular, to observe and contrast pika habitat abundance, quality, and connectivity in the Sierra Nevada and Bodie Hills; to visit low-elevation and high-elevation sites typical of the central-eastern Sierra Nevada; to observe and compare anthropogenic habitat (ore dumps) and native talus sites in the Bodie Hills; to discuss the relevance of these observations to climate relationships, talus thermal regimes, dispersal and connectivity (source/sink), population dynamics, and population processes in California and elsewhere in American pika’s range. Agenda Sunday, July 31 (see accompanying Road Log and Maps for specifics) 8:00 am Convene at USFS Mono Basin Scenic Area Visitor Center, consolidate vehicles (don’t forget lunch, snacks, water) 8:15 am Depart Visitor Center for Stops 1-7 Stop 1: Lundy Cyn (short walk) Stop 2: Virginia Lks Cyn Trailhead (short walk) Stop 3: Conway Highlands Overview instead we made a brief stop to “Benjamin Buttes” Stop 4: Bodie Pass – LUNCH (bring your own) Stop 5: Syndicate Mine, Bodie (short walk) Stop 6: Chemung Mine weather did not allow us to visit this site Stop 7: Serrita Mine, New York Hill, Masonic District (short walk) weather did not allow us to visit this site Note: If time gets short, we might forego one or more of the final stops ~ 7pm? Dinner (no host) at Tioga Gas Mart, Tioga Toomey’s Café, 0.25 miles west on SR 120 of junction with US 395. -
Eastern Sierra Fall Color
Quick Fall Facts When and How to Get Here WHY OUR FALL COLOR SEASON FIND OUT WHEN TO “GO NOW!” GOES ON AND ON AND ON See detailed fall color reporting at The Eastern Sierra’s varied elevations — from www.CaliforniaFallColor.com approximately 5,000 to 10,000 feet (1,512 to 3,048 m) Follow the Eastern Sierra on Facebook: — means the trees peak in color at different times. Mono County (VisitEasternSierra) Bishop Creek, Rock Creek, Virginia Lakes and Green Mammoth Lakes (VisitMammoth) Creek typically turn color first (mid-to late September), Bishop Chamber of Commerce (VisitBishop) with Mammoth Lakes, McGee Creek, Bridgeport, Conway Summit, Sonora and Monitor passes peaking next (late September), and finally June Lake Loop, Lundy Canyon, Lee Vining Canyon, Convict Lake and the West Walker River offering a grand finale from FLY INTO AUTUMN! the first to third week of October. The City of Bishop From any direction, the drive to the shows color into early November. Eastern Sierra is worth it…but the flight connecting through LAX to Mammoth Yosemite Airport is TREE SPECIES possibly more spectacular and gets you here faster: Trees that change color in the Eastern Sierra www.AlaskaAir.com include aspen, cottonwood and willow. LIKE CLOCKWORK NEED HELP PLANNING YOUR TRIP? Ever wonder how Eastern Sierra leaves know CONTACT US: to go from bright green to gold, orange and russet Bishop Chamber of Commerce & Visitor Center as soon as the calendar hits mid-September? Their 760-873-8405 www.BishopVisitor.com cue is actually from the change in air temperature 690 N. -
Exploring the Southern Sierras: Water, Snow & Ecosystem
Exploring the Southern Sierras: Water, snow & ecosystem monitoring across the range The Sierra Nevada marks the geographic boundary between the great Central Valley of California to the west and the Basin and Range province to the east. The range comprises diverse ecosystems: traveling from west to east, you encounter rolling oak woodlands, dense montane coniferous forests, alpine meadows and peaks, and back down to Pinyon pine-Juniper forests and scrublands on the eastern face of the range. In this semi-arid climate, snowpack accumulation in the mountain range constitutes a critical resource for the larger region. Runoff from the Sierras is used by more than 10% of the population of the United States. Sierra Nevada runoff also sustains agriculture in the Central Valley of California, a multi-billion dollar industry providing a considerable portion of the country's produce. Research on hydrology, climate, and ecosystem interactions in this region has immense implications for regional livelihoods and policies. To study these topics in the Sierra Nevada, there are several long-term monitoring sites scattered across the region. This trip will give you a first-hand look at many of the sites, including the SNOTEL installation at Virginia Lakes Ridge, the GLORIA monitoring site, long- term collaborative monitoring of the Mono Basin , the Southern Sierra Critical Zone Observatory, and monitoring efforts by the National Park Service Inventory & Monitoring Program at Yosemite National Park. The trip will take approximately 3 days and include travel to elevations as high as 10,000’/3048 m (as well as an optional hike to near 11,000’/3353 m). -
East Walker River Watershed Assessment
East Walker River Watershed Assessment March 2012 Contributors and Acknowledgements Assessment and plan written by Rick Kattelmann Ph.D., retired hydrologist who specialized in watershed management and snow hydrology. He worked and contracted for a variety of agencies, public utilities, and conservation groups. Rick was the principal hydrologist for the Sierra Nevada Ecosystem Project in the mid-1990s and authored more than 150 scientific and technical papers. He served two terms on the Mono County Planning Commission and wrote watershed assessments for the other principal watersheds of Mono County. Rick holds B.S. and M.S. degrees in forestry and watershed hydrology at U.C. Berkeley and a Ph.D. in snow hydrology from U.C. Santa Barbara. Assessment and plan production managed by Eastern Sierra Land Trust: Aaron Johnson, Lands Director, Heather Freeman, Office Coordinator, Karen Ferrell-Ingram, Executive Director Assistance with cartographic design and spatial analysis: Kimberly Forkner Funders/Support: Funding for this project has been provided by the Sierra Nevada Conservancy, an agency of the State of California. The maps and cartographic products included in this report were made possible through a generous grant of the ArcGIS software by Environmental Systems Research Institute (ESRI) through the ESRI Conservation Program. Disclaimer Watershed Assessments are a snapshot in time of a location, synthesizing all the known information concerning that area. Omissions, errors, an d misunderstandings can occur. The authors request that corrections, additions, and suggestions be sent to the address below. Eastern Sierra Land Trust P.O. Box 755 Bishop, CA 93515 East Walker River Watershed Assessment Table of Contents Contributors and Acknowledgements ............................................................................................ -
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. -
2021 X9a and A16 Zone Hunt Info
CALIFORNIA DEPARTMENT OF FISH AND WILDLIFE DEER MANAGEMENT PROGRAM Wildlife Branch 1010 Riverside Parkway, West Sacramento, CA 95605 ZONE X9a and Area-Specific Archery Hunt A16 2021 General Deer Hunting Information (Includes Additional Hunts G-39 and J-12) GENERAL INFORMATION This information sheet has been prepared to assist deer hunters applying for, or planning to hunt in, Zone X-9a located in portions of Fresno, Inyo, Madera, and Mono counties. The following information should be useful to hunters for archery season (A- 16; Zone X-9a Archery Hunt), Zone X-9a general season, and any “additional hunts” within this geographic area. For more specific information or additional questions regarding this area, contact the following Department office(s): • Inland Deserts Region (Region 6), Bishop Field Office (760-872-1171). REGULATIONS Laws and regulations are designed to conserve wildlife and to provide for an equitable distribution of game mammals. All hunters should read and be familiar with the Current Hunting Regulations. Remember, if you are hunting on private property you must obtain, and have in your possession, written permission to hunt on private property. Hunter trespass laws are strictly enforced. NON-LEAD RESTRICTIONS As of July 1, 2019, all hunters must use nonlead ammunition when taking any wildlife in California, except when hunting with a pellet rifle for approved species. • CCR T14 250.1(d)(3) Effective July 1, 2019, it shall be unlawful to use, or possess with any firearm capable of firing, any projectile(s) not certified as nonlead when taking any wildlife for any purpose in this state. -
Conway and Mattly Ranches Conservation Easement
Conway and Mattly Ranches Conservation Easement Mono County, California EASTERN SIERRA LAND TRUST BASELINE DOCUMENTATION REPORT Eastern Sierra Land Trust P.O. Box 755 Bishop, CA 93514 NOVEMBER __, 2014 1. OWNER ACKNOWLEDGEMENT OF PROPERTY CONDITION 2. METHODOLOGY 3. BACKGROUND INFORMATION 3.1 Property Introduction 3.2 Ownership Information 3.3 Ownership History 3.4 Summary of Significance and Public Benefit 3.5 ESLT Board Resolution for Project 4. PROPERTY DESCRIPTION 4.1 Directions to the Property 4.2 Legal Information i. Legal Description ii. Current Zoning iii. Title Policy 4.3 Land Use i. Historic Land Uses ii. Surrounding Land Uses iii. Current Land Uses iv. Mono County Ordinance: Public Use of Conway Ranch 4.4 Geology, soils, and climate 4.5 Hydrology 4.6 Improvements 5. RESOURCES AND CONSERVATION VALUES 5.1 Biological Characteristics i. Habitat and Vegetation ii. Wildlife 5.2 Cultural Resources 5.3 Scenic Resources 6. CURRENT CONDITIONS 6.1 Main Conway Ranch 6.2 Mattly Ranch 6.3 Aquaculture Area 6.4 Subdivision 7. MAPS 8. PROPERTY PHOTOGRAPHS 9. REFERENCES 10. EXHIBITS ESLT/Conway and Mattly Ranches Baseline/ October 9, 2014 1 Conway and Mattly Ranches Conservation Easement Baseline Documentation Report Acknowledgement of Property Condition The undersigned accept and acknowledge that this Baseline Documentation Report is an accurate representation of the property at the time the Conservation Easement was transferred to the grantee. Grantor_____________________________ Date:_________________ Larry K. Johnston: Chairman, Board of Supervisors For MONO COUNTY Grantee_____________________________ Date:_________________ Kay Ogden: Executive Director For EASTERN SIERRA LAND TRUST ESLT/Conway and Mattly Ranches Baseline/ October 9, 2014 2 2. -
Section 2 - Mono Basin Planning Area
SECTION 2 - MONO BASIN PLANNING AREA DESCRIPTION OF THE PLANNING AREA PHYSICAL CHARACTERISTICS CLIMATIC CONDITIONS DIVERSION OF TRIBUTARY STREAMS (1941-PRESENT) Mono Basin PM-10 SIP 11 May 1995 12 Section 2 - Mono Basin Planning Area _____________________________________________________________________________ 2.1 Description of the Planning Area Mono Basin Planning Area is located in eastern California in the center of Mono County about 300 miles north of Los Angeles and 190 miles east of San Francisco (Figure 2-1). Immediately to the west is Yosemite National Park. The Planning Area has been defined by the EPA as the Mono County, California portion of hydrologic unit number 18090101 on the State of California Hydrologic Unit Map 1978. The area is approximately 35 miles long and 45 miles wide. Mono Basin is walled in by the eastern escarpment of the Sierra Nevada to the west and by Great Basin ranges to the north, south, and east. The Sierra Nevada delineate the western boundary of the area from approximately Excelsior Mountain down to San Joaquin Mountain. The southern boundary extends just beneath the Mono Craters to Cowtrack Mountain, then the eastern edge runs northeast to the Anchorite Hills near the Nevada Stateline. At the Anchorite Hills, the northern boundary heads west crossing the Alkali Valley and the Bodie Hills to Conway Summit and on to the ridge line of the Sierra Nevada. The Planning Area is rural in character with pockets of ranching activity and contains small, unincorporated communities, such as Lee Vining, Mono City, and June Lake. The permanent population of the Planning Area is approximately 2,600 people.2 Most of the land is public land under the jurisdiction of U.S. -
August 5, 2019 Jan Cutts District Ranger
California Program Office 980 Ninth Street, Suite 1730 | Sacramento, California 95814 | tel 916.313.5800 www.defenders.org August 5, 2019 Jan Cutts District Ranger Bridgeport Ranger District HC 62 Box 1000 Bridgeport, CA, 93517 Via email to: [email protected]; comments-intermtn-humboldt-toiyabe- [email protected] Re: Scoping comments on Bridgeport Southwest Rangeland Project Dear Ms. Cutts; Thank you for the opportunity to submit scoping comments on the Bridgeport Southwest Rangeland Project. Scoping comments included in this letter are submitted by Defenders of Wildlife (Defenders) on behalf of its 1.8 million members and supporters in the U.S., including 279,000 in California. Defenders is a national non-profit environmental dedicated to protecting all wild animals and plants in their natural communities. To this end, Defenders uses science, public education and participation, media, legislative advocacy, litigation, and proactive on-the-ground solutions in order to impede the accelerating rate of extinction of species, associated loss of biological diversity, and habitat alteration and destruction. Project background The Humboldt-Toiyabe National Forest, Bridgeport Ranger District is preparing an environmental assessment (EA) for proposed cattle grazing on the existing Cameron Canyon, Dunderberg, Summers Meadow, and Tamarack grazing allotments in Mono County, California, which comprise 19,360 acres of federal land. The allotments include a portion of the Hoover Wilderness where livestock grazing is allowed since it was an existing use prior to enactment of the Wilderness Act and its designation in 1964. National Headquarters | 1130 17th Street, N.W. | Washington, D.C. 20036-4604 | tel 202.682.9400 | fax 202.682.1331 | www.defenders.org The project area includes designated critical habitat for the Sierra Nevada Bighorn Sheep (SNBS), which was listed as endangered under the Endangered Species Act (ESA) in 1999. -
Historical Society Quarterly, 40:1 (Spring 1997), 28, 33, Fig
HistoricalNevada Society Quarterly John B. Reid Hillary Velázquez Juliet S. Pierson Editor-in-Chief & Frank Ozaki Manuscript Editor Production & Design Joyce M. Cox Proofreader Volume 56 Spring/Summer 2013 Numbers 1-2 Contents 3 Editor’s Note 7 Geologic Sources of Obsidian Artifacts from Spirit Cave, Nevada RICHARD E. HUGHES 14 Salmon’s Presence in Nevada’s Past ALISSA PRAGGASTIS AND JACK E. WILLIAMS 33 Mabel Wright and the Prayer that Saved Cui-ui Pah (Pyramid Lake) MICHAEL HITTMAN Front Cover: Katie Frazier, a Pauite, prepares cui-ui fish at Pyramid Lake, ca. 1930. Photographer unknown. (Nevada Historical Society) 76 Wovoka and the 1890 Ghost Dance Religion Q & A with Gunard Solberg MICHAEL HITTMAN 93 Cumulative Index – Volume 55 3 Editor’s Note My beautiful Lake— Used to be full, Just plumb full! Long time ago Lots of fishes… Mabel Wright’s protest prayer-song begins with these words. Sung in May 1964 on the south beach of Pyramid Lake, and accompanied only by a drum, Wright’s song called upon the traditional Paiute power of the spoken word to evoke the lake’s past and to protest threats to its survival. She chose a perfect location. From there, she could view the shoreline and hills where Wizards Beach Man lived more than 9,000 years ago and where fishing tools—a hook, a line made from sagebrush, and a sinker—were found and dated to 9,600 years ago. She could see the place where Sarah Winnemucca—Nevada’s greatest advocate for Native American rights—was born and lived her early years. -
Mono County Community Development Department P.O
Mono County Community Development Department P.O. Box 347 Planning Division P.O. Box 8 Mammoth Lakes, CA 93546 Bridgeport, CA 93517 (760) 924-1800, fax 924-1801 (760) 932-5420, fax 932-5431 [email protected] www.monocounty.ca.gov March 2007 MONO BASIN WATERSHED ASSESSMENT 1. Introduction Watershed approach California watershed programs and Mono County’s involvement What is a watershed assessment? Publicly perceived problems and issues Water quantity Water quality Aquatic habitat Recreation Wildfire Invasive species List of assorted issues Publicly perceived key resources Driving questions Watershed boundaries 2. Descriptive geography Climate Precipitation Snowpack Air temperature Wind Evaporation Climate change impacts Topography Geology and soils Upland vegetation Special-status plants Wildfire history and risk 3. Riparian areas and wetlands Rush Creek Parker Creek Walker Creek Bohler Creek Horse Creek Lee Vining Creek Post Office Creek Mill Creek Planning / Building / Code Compliance / Environmental / Collaborative Planning Team (CPT) Local Agency Formation Commission (LAFCO) / Local Transportation Commission (LTC) / Regional Planning Advisory Committees (RPACs Wilson Creek DeChambeau Creek 4. Fish and wildlife Fish Invasive species Wildlife 5. Human history and land use Land use Agriculture Timber harvesting Mining Gravel extraction Roads Hydroelectric development Residential development Recreation Land ownership and interagency cooperation 6. Descriptive hydrology Runoff generation processes Water balance Streamflow averages and extremes Floods and droughts Lakes Groundwater Diversions and storage Water rights, use and management Domestic water systems Lee Vining Public Utility District Lundy Mutual Water Company June Lake Public Utility District Conway Ranch Wastewater treatment and disposal 7. Descriptive geomorphology Stream channels Surface erosion Hillslope processes Sediment transport Human influences Restoration 8. -
Drainage Reversals in Mono Basin During the Late Pliocene and Pleistocene
Drainage reversals in Mono Basin during the late Pliocene and Pleistocene Marith C. Reheis* U.S. Geological Survey, M.S. 980, Federal Center, Denver, Colorado 80225, USA Scott Stine Department of Geography and Environmental Studies, California State University, 25800 Carlos Bee Boulevard, Hayward, California 94542, USA Andrei M. Sarna-Wojcicki U.S. Geological Survey, M.S. 975, 345 Middle®eld Road, Menlo Park, California 94025, USA ABSTRACT Basin between the hydrologically distinct vive out of water for even short periods) can Lahontan and Owens±Death Valley sys- expand their range across otherwise insur- Mono Basin, on the eastern ¯ank of the tems, as long postulated by biologists, and mountable drainage divides. Biologists, point- central Sierra Nevada, is the highest of the also con®rms a probable link during the ing to several such species that today occur in large hydrographically closed basins in the Pleistocene for species adapted to travel up- the hydrologically distinct Lahontan and Basin and Range province. We use geo- stream in fast-¯owing water. Owens±Death Valley systems (e.g., Hubbs morphic features, shoreline deposits, and and Miller, 1948; Minckley et al., 1986; basalt-®lled paleochannels to reconstruct Keywords: biogeography, drainage chang- Hershler and Sada, 2002), have long specu- an early to middle Pleistocene record of es, ®sh, Great Basin, Mono Basin. lated that Mono Basin may have linked these shorelines and changing spillways of Lake two systems at some time in the past (e.g., Russell in Mono Basin. During this period INTRODUCTION Hubbs and Miller, 1948; Taylor, 1985). This of time, Lake Russell repeatedly attained study con®rms that linkage and places the altitudes between 2205 and 2280 mÐlevels The Mono Basin abuts the eastern ¯ank of transfer from north to south at sometime after far above the present surface of Mono Lake the central Sierra Nevada (Fig.