Supertopo for Fairview Dome's Regular Route
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Gear Brands List & Lexicon
Gear Brands List & Lexicon Mountain climbing is an equipment intensive activity. Having good equipment in the mountains increases safety and your comfort level and therefore your chance of having a successful climb. Alpine Ascents does not sell equipment nor do we receive any outside incentive to recommend a particular brand name over another. Our recommendations are based on quality, experience and performance with your best interest in mind. This lexicon represents years of in-field knowledge and experience by a multitude of guides, teachers and climbers. We have found that by being well-equipped on climbs and expeditions our climbers are able to succeed in conditions that force other teams back. No matter which trip you are considering you can trust the gear selection has been carefully thought out to every last detail. People new to the sport often find gear purchasing a daunting chore. We recommend you examine our suggested brands closely to assist in your purchasing decisions and consider renting gear whenever possible. Begin preparing for your trip as far in advance as possible so that you may find sale items. As always we highly recommend consulting our staff of experts prior to making major equipment purchases. A Word on Layering One of the most frequently asked questions regarding outdoor equipment relates to clothing, specifically (and most importantly for safety and comfort), proper layering. There are Four basic layers you will need on most of our trips, including our Mount Rainier programs. They are illustrated below: Underwear -
Climb Antarctica Required Clothing and Equipment List
CLIMB ANTARCTICA REQUIRED CLOTHING AND EQUIPMENT LIST Conditions in Antarctica change drastically throughout our season and vary depending on your location. At Union Glacier, the climate is very dry and generally sunny but wind chill can impact temperatures greatly with early November being as cold as -22°F (-30°C). Average mid-season temperatures range from -12°F to 30°F (-24°C to -1°C). To be prepared for all conditions, it is important to have a selection of items you can mix and match. The layering system described below will keep you safe and comfortable in all conditions—it is also the same system utilized by our Antarctic field staff. You do not need to wear ALL of these layers ALL of the time. Dress for the weather conditions and the activity level you expect to encounter and bring extra layers with you in your backpack in case conditions change. Base Layer Materials Polyester, Merino Wool, or Silk but NO COTTON Examples Patagonia Capilene or Smartwool Description Your first layer consists of a lightweight or midweight long- sleeved thermal top and bottom. We recommend materials that wick moisture away from your body like polyester or merino wool. If you cannot wear artificial fibers or wool, silk is an alternate option. Cotton traps moisture and can cause you to chill more rapidly. Zip T-necks are a great option as they allow ventilation. Bring undergarments, sports bras, and/or camisoles in a similar wicking material. Mid Layer Materials Polyester, Merino Wool, Stretch Fleece, Grid Fleece Examples Patagonia R1 Fleece or Rab Power Stretch Description Your second layer consists of a long-sleeved heavyweight (expedition weight) base layer top and bottom or lightweight stretch fleece top and bottom. -
2020 January Scree
the SCREE Mountaineering Club of Alaska January 2020 Volume 63, Number 1 Contents Mount Anno Domini Peak 2330 and Far Out Peak Devils Paw North Taku Tower Randoism via Rosie’s Roost "The greatest danger for Berlin Wall most of us is not that our aim is too high and we Katmai and the Valley of Ten Thousand Smokes miss it, but that it is too Peak of the Month: Old Snowy low and we reach it." – Michelangelo JANUARY MEETING: Wednesday, January 8, at 6:30 p.m. Luc Mehl will give the presentation. The Mountaineering Club of Alaska www.mtnclubak.org "To maintain, promote, and perpetuate the association of persons who are interested in promoting, sponsoring, im- proving, stimulating, and contributing to the exercise of skill and safety in the Art and Science of Mountaineering." This issue brought to you by: Editor—Steve Gruhn assisted by Dawn Munroe Hut Needs and Notes Cover Photo If you are headed to one of the MCA huts, please consult the Hut Gabe Hayden high on Devils Paw. Inventory and Needs on the website (http://www.mtnclubak.org/ Photo by Brette Harrington index.cfm/Huts/Hut-Inventory-and-Needs) or Greg Bragiel, MCA Huts Committee Chairman, at either [email protected] or (907) 350-5146 to see what needs to be taken to the huts or repaired. All JANUARY MEETING huts have tools and materials so that anyone can make basic re- Wednesday, January 8, at 6:30 p.m. at the BP Energy Center at pairs. Hutmeisters are needed for each hut: If you have a favorite 1014 Energy Court in Anchorage. -
VF Corporation on January 1, 2017 Current CEO Eric Wiseman to Remain Executive Chairman
UNITED STATES SECURITIES AND EXCHANGE COMMISSION Washington, D.C. 20549 FORM 8-K CURRENT REPORT Pursuant to Section 13 or 15(d) of the Securities Exchange Act of 1934 Date of Report (Date of earliest event reported): October 3, 2016 V. F. Corporation (Exact Name of Registrant as Specified in Charter) Pennsylvania 001-05256 23-1180120 (State or other jurisdiction (Commission (IRS Employer of incorporation) File Number) Identification No.) 105 Corporate Center Boulevard Greensboro, North Carolina 27408 (Address of principal executive offices) (zip code) (336) 424-6000 (Registrant’s telephone number, including area code) Check the appropriate box below if the Form 8-K filing is intended to simultaneously satisfy the filing obligation of the registrant under any of the following provisions: Written communications pursuant to Rule 425 under the Securities Act (17 CFR 230.425) Soliciting material pursuant to Rule 14a-12 under the Exchange Act (17 CFR 240.14a-12) Pre-commencement communications pursuant to Rule 14d-2(b) under the Exchange Act (17 CFR 240.14d-2(b)) Pre-commencement communications pursuant to Rule 13e-4(c) under the Exchange Act (17 CFR 240.13e-4(c)) Item 5.02. Departure of Directors or Certain Officers; Election of Directors; Appointment of Certain Officers; Compensatory Arrangements of Certain Officers. On October 3, 2016, the Board of Directors of V.F. Corporation (“VF”), in furtherance of its management succession plan, elected Steven E. Rendle as Chief Executive Officer, effective January 1, 2017. Mr. Rendle, 57, has been President and Chief Operating Officer, and a member of the VF Board of Directors (the “Board”), since June 2015. -
Ley, So the Still Deeper Cañon of Lower Two Miles,That Is, Beyond Rather Than
THE CANON OF YOSEMITE 87 As Merced Cañon forms the southeast branch of Yosemite Val- ley, so the still deeper cañon of Tenaya Creek isits northeastern arm.Here the glacial story is less plain, and on first sight, from the heights on either side, it might be overlooked.For above the cañon's lower two miles,that is, beyond the foot of Mt. Watkins,it crowds to a narrow box-cañon between that great cliff and the steep incline of Clouds Rest.This might seem to be a V-shaped, stream-cut gorge, rather than to have the broader bottom commonly left by a glacier. But alittle exploration discovers glacial footprints in the terminal moraines and the lakes and filled lake-beds,withfineconnecting waterfalls, that mark aglacier's descent from the Cathedral Peak Range, south of the Tuolumne. We Overhung at Summit of the Half Dont,-. nrart have hardly entered the cañon, in- a tulle above the Valley floor nn.l Tena-u deed, before we are reminded of (allan.El Caption Is seen in the tllatanee. El Capitan moraine and the enclosed Yosemite Lake. A similar boulder ridge, thrown across the cañon here, is traversed by the road as it carries visitors on their early morning trips to see the sunrise reflections in Mirror Lake.This lakelet evidently occupies the lowermost of the glacial steps.It is a mere reminder of its former size, the delta of Tenaya Creek having stolen a mile from its upper end.Farther up the cañon, below and above Mt. Watkins, stream sediment has already turned similar lakes into meadows. -
Castleton Tower, Kor-Ingalls Route Mixture of Anticipation and Anxiety
v 1.0 Desert Towers Select Dougald MacDonald and Chris McNamara Desert Towers Select SUPERTOPOS Version 1.0 May 2002 If you received a bootleg copy of this eGuide, Published by please visit the SuperTopo web site and buy the SuperTopo latest version for yourself: 2 Bradford Way www.supertopo.com/climbingareas/towers.html Mill Valley, CA 94941 We are a tiny company that barely scrapes by www.supertopo.com and your honesty means we can continue creating SuperTopos for you and your friends. Copyright 2002 by SuperTopo LLC No part of this file or guide may be duplicated in any form, or by any electronic, mechanical or other means, without the permission in writing from the publisher. Topos and text by Dougald MacDonald, Chris McNamara, and Austin Archer. History by Chris McNamara, Huntley Ingalls, and Ed Webster. Managing Editor: Sarah Felchlin. Designers: Sarah Felchlin, David Safanda, and Chris McNamara. Acknowledgements The idea for Desert Towers Select was conceived when Mick Ryan showed Chris McNamara some nearly published desert topos he had worked on with Dougald MacDonald. Mick and Dougald kindly let SuperTopo use their work as the starting point and backbone of the current guide. From there, Chris McNamara and Sarah Felchlin climbed additional routes, researched first ascent histories and ate at all the restaurants that Corey Rich and Men’s Journal would pay for. Austin Archer offered the topos and text for Ancient Art and Owl Rock, Laurie Goodgame gave great restaurant beta, and Brian Jonas from Pagan Mountaineering pitched in additional traveler info. When you pass through Moab, visit his excellent climbing shop, Pagan Mountaineering, for gear, friendly service, and route recommendations. -
Approach to Bluff Knoll North Face for Hell Fire Gully / Devil's Nose
Bluff Knoll - Approach to North Face North Face North West Bay Hell Fire Gully Devil’s Nose (Direct) Middle Line Sophocles Pillar connection to tourist track Prickle Traverse 4 3 2 1 Approach to Bluff Knoll North Face for Hell Fire Gully / Devil’s Nose (by Ross Weiter) GPS Coordinates: ❶ S34.37380°, E118.24984° Turn-off from tourist track ❷ S34.37473°, E118.25135° Top of rock step ❸ S34.37488°, E118.25206° Below rock buttress ❹ S34.37441°, E118.25575° Start of Hell Fire Gully / Devil’s Nose Follow tourist track across for 20 minutes until it crosses a deep gully, and then heads uphill for 300 metres. Turn left at ❶ and follow overgrown dirt track along crest of ridge. Climb 4m rocky step to its top ❷. There is no track after this point, until the cliff face is gained. Go diagonally up and left to the bottom of a large rocky buttress on left side of the ridge ❸. Traverse left along the base of the buttress; then go across top of gully, staying below the tree line. Traverse along the bottom of the cliff (intermittent track) to gain the top of North Ridge. The North Face will now come into view. Continue for 300 metres, to a 5m wide by 40m high pillar leaning against the face. Hell Fire Gully / Devil’s Nose start on its left (east) side ❹. Total approach time from car park is 1 – 1½ hours, depending on your speed. There is some light bush bashing at times, so trousers are recommended. Take light approach shoes as you will be carrying them up the cliff. -
10 Climbing Areas in Crisis Page 8
VERTICAL TIMES The National Publication of Access Fund Winter 18/Volume 113 www.accessfund.org 10 Climbing Areas in Crisis page 8 CLIMB LIKE A LOCAL: COCHISE STRONGHOLD 5 WILLIAMSON ROCK ON PATH TO REOPENING 7 Protect America’s Climbing INNOVATING FOR SUSTAINABLE BOLT REPLACEMENT 12 AF Perspective It takes two flints to make a fire. But alongside the excitement and positivity was a common thread of concern: Our world-class climbing areas are “ – LOUISA MAY ALCOTT suffering from world-class impacts and problems. It’s ” becoming harder and harder to mitigate impacts from the ere’s a fun experiment: Throw a group of dedicated, growing number of climbers. While this has been a long- passionate climbers in a room and ask them, “How term battle, the problem is more acute than ever. So few of Hare we going to save our climbing areas?” our climbing areas are built or managed for the number of climbers using them today. I heard the same phrase again No, this isn’t Access Fund’s origin story (although it’s pretty and again: “Our climbing areas are being loved to death.” close). But it’s the premise behind Access Fund’s summits, trainings, and conferences, which we’ve been hosting for Our charge now is to love these areas back to life. And that more than 25 years. starts with getting real about the impacts, acknowledging the need for recreation infrastructure to protect these I went to my first Access Fund summit in 2009. It was in places, and bringing a whole heck of a lot more resources to Dr. -
Sierra Nevada Mountain Yellow-Legged Frog
BEFORE THE SECRETARY OF INTERIOR CENTER FOR BIOLOGICAL ) PETITION TO LIST THE SIERRA DIVERSITY AND PACIFIC RIVERS ) NEVADA MOUNTAIN YELLOW- COUNCIL ) LEGGED FROG (RANA MUSCOSA) AS ) AN ENDANGERED SPECIES UNDER ) THE ENDANGERED SPECIES ACT Petitioners ) ________________________________ ) February 8, 2000 EXECUTIVE SUMMARY The Center for Biological Diversity and Pacific Rivers Council formally request that the United States Fish and Wildlife Service (“USFWS”) list the Sierra Nevada population of the mountain yellow-legged frog (Rana muscosa) as endangered under the federal Endangered Species Act (“ESA”), 16 U.S.C. § 1531 - 1544. These organizations also request that mountain yellow- legged frog critical habitat be designated concurrent with its listing. The petitioners are conservation organizations with an interest in protecting the mountain yellow-legged frog and all of earth’s remaining biodiversity. The mountain yellow-legged frog in the Sierra Nevada is geographically, morphologically and genetically distinct from mountain yellow legged frogs in southern California. It is undisputedly a “species” under the ESA’s listing criteria and warrants recognition as such. The mountain yellow-legged frog was historically the most abundant frog in the Sierra Nevada. It was ubiquitously distributed in high elevation water bodies from southern Plumas County to southern Tulare County. It has since declined precipitously. Recent surveys have found that the species has disappeared from between 70 and 90 percent of its historic localities. What populations remain are widely scattered and consist of few breeding adults. Declines were first noticed in the 1950's, escalated in the 1970's and 1980's, and continue today. What was recently thought to be one of the largest remaining populations, containing over 2000 adult frogs in 1996, completely crashed in the past three years; only 2 frogs were found in the same area in 1999. -
Yosemite National Park National Park Service
National Park Service U.S. Department of the Interior Yosemite National Park Tuolumne Wild and Scenic River Comprehensive Management Plan Draft Environmental Impact Statement Tuolumne River Values and Baseline Conditions After five years of study and stakeholder involvement, the Tuolumne Wild and Scenic River Comprehensive Management Plan and Draft Environmental Impact Statement (Tuolumne River Plan/DEIS) will be released in summer of 2011. In advance of the plan’s release, the NPS is providing the Tuolumne River Values and Baseline Conditions chapter as a preview into one of the plan’s most foundational elements. Sharing the baseline information in advance of the plan will give members of the public an understanding of river conditions today and specific issues that will be explored in the Tuolumne River Plan. Public comments on all elements of the Tuolumne River Plan, including the baseline conditions chapter, will be accepted when it is released for review this summer. What follows is a description of the unique values that make the Tuolumne stand apart from all other rivers in the nation. This chapter also provides a snapshot in time, documenting overall conditions and implications for future management. In particular the baseline chapter examines, • What are the outstandingly remarkable values that make the Tuolumne River worthy of special protection under the Wild and Scenic Rivers Act (WSRA)? • What do we know about the condition of these values (in addition to water quality and free-flow), both at time of designation in 1984 and -
Lichens and Lichenicolous Fungi of Yosemite National Park, California
North American Fungi Volume 8, Number 11, Pages 1-47 Published September 9, 2013 Lichens and Lichenicolous Fungi of Yosemite National Park, California M. Hutten1, U. Arup2, O. Breuss3, T. L. Esslinger4, A. M. Fryday5, K. Knudsen6, J. C. Lendemer7, C. Printzen8, H. T. Root9, M. Schultz10, J. Sheard11, T. Tønsberg12, and B. McCune9 1Lassen Volcanic National Park, P.O. Box 100, Mineral, CA 96063 USA. 2Botanical Museum, Lund University, Box 117, 221 00 Lund, Sweden 3Naturhistorisches Museum Wien, Botanische Abteilung, Burgring 7, A-1010 Wien, Austria 4Dept. of Biological Sciences #2715, P.O. Box 6050, North Dakota State University, Fargo ND 58108, U.S.A. 5Dept. of Plant Biology, Michigan State University, East Lansing, MI 48824, U.S.A. 6Dept. of Botany & Plant Sciences, University of California, Riverside, CA 92521, U.S.A. 7New York Botanical Garden, Bronx, NY 10458-5126, U.S.A. 8Abt. Botanik & Molek. Evol., Forschungsinstitut Senckenberg, Senckenberganlage 25, D-60325 Frankfurt am Main, Germany 9Dept. Botany and Plant Pathology, Oregon State University, Corvallis OR 97331, U.S.A. 10Biocenter Klein Flottbek, University of Hamburg, Ohnhorststr. 18, D-22609 Hamburg, Germany 11Dept. of Biology, University of Saskatchewan, 112 Science Place, Saskatoon, SK S7N 5E2, Canada 12Museum of Natural History, University of Bergen, Allégaten 41, N-5007 Bergen, Norway Hutten, M., U. Arup, O. Breuss, T. L. Esslinger, A. M. Fryday, K. Knudsen, J. C. Lendemer, C. Printzen, H. T. Root, M. Schultz, J. Sheard, T. Tønsberg, and B. McCune. 2013. Lichens and Lichenicolous Fungi of Yosemite National Park, California. North American Fungi 8(11): 1-47. -
Factors Contributing to the Formation of Sheeting Joints
FACTORS CONTRIBUTING TO THE FORMATION OF SHEETING JOINTS: A STUDY OF SHEETING JOINTS ON A DOME IN YOSEMITE NATIONAL PARK A THESIS SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI„I AT MĀNOA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTERS OF SCIENCE IN GEOLOGY AND GEOPHYSICS AUGUST 2010 By Kelly J. Mitchell Thesis Committee: Steve Martel, Chairperson Fred Duennebier Paul Wessel Keywords: sheeting joints, exfoliation joints, topographic stresses, curvature, mechanics, spectral filtering, Yosemite Acknowledgements I would like to extend my sincerest gratitude to those who helped make this thesis possible. Thanks to the National Science Foundation for funding this research. Thank you to my graduate advisor, Dr. Steve Martel, for your advice and support through the past few years. This has been a long and difficult project but you have been patient and supportive through it all. Special thanks to my committee, Dr. Fred Duennebier and Dr. Paul Wessel for their advice and contributions; without your help I do not think this project would have been possible. I appreciate the time all of you have spent discussing the project with me. Thank you to Chris Hurren, Shay Chapman, and Carolyn Parcheta for your hard work and moral support in the field; you kept a great attitude during the field season. Special thanks to the National Park Service staff in Yosemite, particularly Dr. Greg Stock and Brian Huggett for their assistance. I wish to thank NCALM, Ole Kaven, Nicholas VanDerElst, and Emily Brodsky for LIDAR data collection. Thank you to Carolina Anchietta Fermin, Lisa Swinnard, and Darwina Griffin for their moral support.