2021 X9a and A16 Zone Hunt Info
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Late Holocene Forest Dynamics, Volcanism, and Climate Change at Whitewing Mountain and San Joaquin Ridge, Mono County, Sierra Nevada, CA, USA ⁎ Constance I
Quaternary Research 66 (2006) 273–287 www.elsevier.com/locate/yqres Late Holocene forest dynamics, volcanism, and climate change at Whitewing Mountain and San Joaquin Ridge, Mono County, Sierra Nevada, CA, USA ⁎ Constance I. Millar a, , John C. King b, Robert D. Westfall a, Harry A. Alden c, Diane L. Delany a a USDA Forest Service, Sierra Nevada Research Center, Pacific Southwest Research Station, Berkeley, CA 94701, USA b Lone Pine Research, Bozeman, MT 59715, USA c Smithsonian Institution, Center for Materials Research and Education, Suitland, MD 20746, USA Received 17 June 2005 Available online 16 June 2006 Abstract Deadwood tree stems scattered above treeline on tephra-covered slopes of Whitewing Mtn (3051 m) and San Joaquin Ridge (3122 m) show evidence of being killed in an eruption from adjacent Glass Creek Vent, Inyo Craters. Using tree-ring methods, we dated deadwood to AD 815– 1350 and infer from death dates that the eruption occurred in late summer AD 1350. Based on wood anatomy, we identified deadwood species as Pinus albicaulis, P. monticola, P. lambertiana, P. contorta, P. jeffreyi, and Tsuga mertensiana. Only P. albicaulis grows at these elevations currently; P. lambertiana is not locally native. Using contemporary distributions of the species, we modeled paleoclimate during the time of sympatry to be significantly warmer (+3.2°C annual minimum temperature) and slightly drier (−24 mm annual precipitation) than present, resembling values projected for California in the next 70–100 yr. © 2006 University of Washington. All rights reserved. Keywords: Paleoecology; Medieval climate; Late Holocene; Climate change; Long Valley volcanism; Inyo Craters; Forest history; Paleoclimatic modeling; Tree-ring dating Introduction bance remain poorly understood. -
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. -
YOSEMITE NATIONAL PARK O C Y Lu H M Tioga Pass Entrance 9945Ft C Glen Aulin K T Ne Ee 3031M E R Hetc C Gaylor Lakes R H H Tioga Road Closed
123456789 il 395 ra T Dorothy Lake t s A Bond C re A Pass S KE LA c i f i c IN a TW P Tower Peak Barney STANISLAUS NATIONAL FOREST Mary Lake Lake Buckeye Pass Twin Lakes 9572ft EMIGRANT WILDERNESS 2917m k H e O e O r N V C O E Y R TOIYABE NATIONAL FOREST N Peeler B A Lake Crown B C Lake Haystack k Peak e e S Tilden r AW W Schofield C TO Rock Island OTH IL Peak Lake RI Pass DG D Styx E ER s Matterhorn Pass l l Peak N a Slide E Otter F a Mountain S Lake ri e S h Burro c D n Pass Many Island Richardson Peak a L Lake 9877ft R (summer only) IE 3010m F LE Whorl Wilma Lake k B Mountain e B e r U N Virginia Pass C T O Virginia S Y N Peak O N Y A Summit s N e k C k Lake k c A e a C i C e L C r N r Kibbie d YO N C n N CA Lake e ACK AI RRICK K J M KE ia in g IN ir A r V T e l N k l U e e pi N O r C S O M Y Lundy Lake L Piute Mountain N L te I 10541ft iu A T P L C I 3213m T Smedberg k (summer only) Lake e k re e C re Benson Benson C ek re Lake Lake Pass C Vernon Creek Mount k r e o Gibson e abe Upper an r Volunteer McC le Laurel C McCabe E Peak rn Lake u Lake N t M e cCa R R be D R A Lak D NO k Rodgers O I es e PLEASANT EA H N EL e Lake I r l Frog VALLEY R i E k G K C E LA e R a e T I r r Table Lake V North Peak T T C N Pettit Peak A INYO NATIONAL FOREST O 10788ft s Y 3288m M t ll N Fa s Roosevelt ia A e Mount Conness TILT r r Lake Saddlebag ILL VALLEY e C 12590ft (summer only) h C Lake ill c 3837m Lake Eleanor ilt n Wapama Falls T a (summer only) N S R I Virginia c A R i T Lake f N E i MIGUEL U G c HETCHY Rancheria Falls O N Highway 120 D a MEADOW -
Matthew Greene Were Starting to Understand the Grave the Following Day
VANISHED An account of the mysterious disappearance of a climber in the Sierra Nevada BY MONICA PRELLE ILLUSTRATIONS BY BRETT AFFRUNTI CLIMBING.COM — 61 VANISHED Three months earlier in July, the 39-year-old high school feasted on their arms. They went hiking together often, N THE SMALL SKI TOWN of Mammoth Lakes in math teacher dropped his car off at a Mammoth auto shop even in the really cold winters common to the Northeast. California’s Eastern Sierra, the first snowfall of the for repairs. He was visiting the area for a summer climb- “The ice didn’t slow him down one bit,” Minto said. “I strug- ing vacation when the car blew a head gasket. The friends gled to keep up.” Greene loved to run, competing on the track year is usually a beautiful and joyous celebration. Greene was traveling with headed home as scheduled, and team in high school and running the Boston Marathon a few Greene planned to drive to Colorado to join other friends times as an adult. As the student speaker for his high school But for the family and friends of a missing for more climbing as soon as his car was ready. graduation, Greene urged his classmates to take chances. IPennsylvania man, the falling flakes in early October “I may have to spend the rest of my life here in Mam- “The time has come to fulfill our current goals and to set moth,” he texted to a friend as he got more and more frus- new ones to be conquered later,” he said in his speech. -
Native Sustainment: the North Fork Mono Tribe's
Native Sustainment The North Fork Mono Tribe's Stories, History, and Teaching of Its Land and Water Tenure in 1918 and 2009 Jared Dahl Aldern Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy from Prescott College in Education with a Concentration in Sustainability Education May 2010 Steven J. Crum, Ph.D. George Lipsitz, Ph.D. Committee Member Committee Member Margaret Field, Ph.D. Theresa Gregor, Ph.D. External Expert Reader External Expert Reader Pramod Parajuli, Ph.D. Committee Chair Native Sustainment ii Copyright © 2010 by Jared Dahl Aldern. All rights reserved. No part of this dissertation may be used, reproduced, stored, recorded, or transmitted in any form or manner whatsoever without written permission from the copyright holder or his agent(s), except in the case of brief quotations embodied in the papers of students, and in the case of brief quotations embodied in critical articles and reviews. Requests for such permission should be addressed to: Jared Dahl Aldern 2658 East Alluvial Avenue, #103 Clovis, CA 93611 Native Sustainment iii Acknowledgments Gratitude to: The North Fork Mono Tribe, its Chairman, Ron Goode, and members Melvin Carmen (R.I.P.), Lois Conner, Stan Dandy, Richard Lavelle, Ruby Pomona, and Grace Tex for their support, kindnesses, and teachings. My doctoral committee: Steven J. Crum, Margaret Field, Theresa Gregor, George Lipsitz, and Pramod Parajuli for listening, for reading, and for their mentorship. Jagannath Adhikari, Kat Anderson, Steve Archer, Donna Begay, Lisa -
Phil Collh CHAPTER IV
Phil Collh CHAPTER IV. Management Direction Introduction This chapter documents how the Inyo National Forest vnll be managed during this planning pericd. It provides dj"x'on to Forest land managers and explains to the public the rem why specific areas are managed for specific reasons and how that will be accanplxshed. The chapter is divided into five sections: 1. Forest Goals lists the resources of the Forest with their respective manag-t goals. 2. Forest Objectives lists outputs for each resource that will result fran inplementing the Plan. 3. Forest-wide Standards and Guidelines are the bases for all management activities on the Forest. Each resource has a set of standards and guides to that the resource is protected, maintained or developd in an emimmentally sound and ewnanically cost-effective way. These standards and guides apply to all areas of the Forest. 4. w"t PresQliptiOns prescribe how areas on the Forest will be managed with a specific resource -is. For example, any Wildemess on the Forest no matter where it is located will be managed under Prescription #1 - Designated Wildemess. Each prescription describes the ObJeCtive of manag€inent and the area's resource -is. 5. Manag5wn t Area D-im delineates boundaries of the twenty management areas on the Forest. Each of these has a different mix of prescriptions, but all are managed under the Forest-wide Standards and Guidelines. National Forests are managed under a variety of federal laws rqirg fmthe U.S. Minirq Laws of 1872 to the National Forest Managmt Act of 1976. Forest Semice iVamals and Handbooks and the Pacific southwest Regimal Guide provide additional policy diredion. -
Devils Postpile National Monument Geologic Resources Inventory Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Devils Postpile National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/160 THIS PAGE: The dramatic columns of Devils Postpile are between 12 and 18 m (40 and 60 ft) tall and up to 1.1 m (3.5 ft) in diameter. Seismic and weathering processes fracture the columns along joints. Broken columns litter the slopes beneath Devils Postpile. ON THE COVER: Top view of the 100,000 year-old columns of Devils Postpile. The columns are world-renowned and many form the ideal hexagonal shape. The striations and scratches are evidence that glaciers advanced over the columns, scouring their surface. National Park Service photographs. Devils Postpile National Monument Geologic Resources Inventory Report Natural Resource Report NPS/NRPC/GRD/NRR—2009/160 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 February 2010 U.S. Department of the Interior National Park Service Natural Resource Program Center Denver, Colorado The National Park Service, Natural Resource Program Center publishes a range of reports that address natural resource topics of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate high-priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. All manuscripts in the series receive the appropriate level of peer review to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and designed and published in a professional manner. -
ARTICLE in PRESS + Model
ARTICLE IN PRESS + model YQRES-02727; No. of pages: 15; 4C: Quaternary Research xx (2006) xxx–xxx 1 www.elsevier.com/locate/yqres 2 Late holocene forest dynamics, volcanism, and climate change at whitewing 3 mountain and San Joaquin Ridge, Mono County, Sierra Nevada, CA, USA ⁎ 4 Constance I. Millar a, , John C. King b, Robert D. Westfall a, Harry A. Alden c, Diane L. Delany a 5 a USDA Forest Service, Sierra Nevada Research Center, Pacific Southwest Research Station, Berkeley, CAOF 94701, USA 6 b Lone Pine Research, Bozeman, MT 59715, USA 7 c Smithsonian Institution, Center for Materials Research and Education, Suitland, MD 20746, USA 8 Received 17 June 2005 9 Abstract 10 Deadwood tree stems scattered above treeline on tephra-covered slopes of Whitewing Mtn (3051 m) and San Joaquin Ridge (3122 m) show 11 evidence of being killed in an eruption from adjacent Glass Creek Vent, Inyo Craters. Using tree-ring methods, we dated deadwood to AD 815– 12 1350, and infer from death dates that the eruption occurred in late summer AD 1350. Based on wood anatomy, we identified deadwood species as 13 Pinus albicaulis, P. monticola, P. lambertiana, P. contorta, P. jeffreyi, and Tsuga mertensiana. Only P. albicaulis grows at these elevations 14 currently; P. lambertiana is not locally native. Using contemporary distributionsED of the species, PRO we modeled paleoclimate during the time of 15 sympatry to be significantly warmer (+3.2°C annual minimum temperature) and slightly drier (−24 mm annual precipitation) than present, 16 resembling values projected for California in the next 70–100 yr. -
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 ............................................................................................ -
CAMP: SUMMER Trail Survey On-Site Computer Stations Photo 1
CAMP Online Trails Surveys In cooperation with the Town of Mammoth Lakes, Alta Planning + Design, and Trail Solutions, MLTPA provided feedback on both the Summer and Winter Online Trail Survey questions and format, which were developed by the TOML and the consultant teams with assistance from the survey hosting company, Leisure Trends. MLTPA also conducted the majority of public outreach for these surveys, the methods of which are discussed below. The Summer Online Trail Survey ran from October 27, 2007, to March 14, 2008, and was completed by 330 people. The Winter Online Trail Survey ran from December 18, 2007, to March 14, 2008, and was completed by 316 people. (An unknown number of participants in both cases started taking the surveys, but did not finish; as a result, their input is not reflected in these totals.) Results and copies of the survey contents are available in Appendix E, “CAMP: Summer Survey Data (TOML),” and Appendix F, “CAMP: Winter Survey Data (TOML).” • Business cards Beginning with CAMP: WINTER outreach efforts, MLTPA designed, produced, and distributed business cards driving people to the MLTPA website to take both the Summer and Winter surveys. Cards were handed out by individuals and also were provided to a number of local businesses with display-ready cardholders to minimize point-of-sale clutter. • E-mail campaigns As part of their regular e-mail blasts for both events, MLTPA invited recipients to participate in both the Summer and Winter trail surveys, providing direct links to the survey URLs. Please see the “E-mail campaigns” chapters of the “CAMP: SUMMER” and “CAMP: WINTER” reports for further detail.