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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. -
Bulletin of the United States Fish Commission
SALMON-TAGGING EXPERIMENTS IN ALASKA, 1924 AND 1925 1 .:I- By WILLIS H. RICH, Ph. D. Director, U. S. Biological Station, Seattle, Wash; .:I CONTENTS Page Introduction _ 109 Experiments in southeastern Alaska__hhu u __nn_h__u u u _ 116 Tagging record _ 116 Returns from experiments in Icy Strait__ n h_u u_..u u _ 119 Returns from experiments in Frederick Sound u huh _ 123 Returns from experiments in Chatham Strait; h u • _ 123 Returns from experiments in Sumner Strait, u_uuu .. u _ 128 Returns from experiments at Cape Muzon and Kaigani Point, ~ _ 135 Returns from experiments at Cape Chacon u n u h _ 137 Returns from experiments near Cape Fox and Duke Islandu _ 141 Variations in returns of tagged fish; h _u u n n h n __ h u_ 143 Conelusions _ 144 Experiments at Port Moller, 1925un__h_uu uu __ 145 INTRODUCTION The extensive salmon-tagging experiments conducted during 1922 and 1923 2 in the region of the Alaska Peninsula proved so productive of information, both of scientific interest and of practical application in the care of these fisheries, that it was considered desirable to undertake similar investigations in other districts; Accordingly, experiments were carried on in southeastern Alaska in 1924 and again in 1925. In 1925, also, at the request of one of the companies engaged in packing salmon in the Port Moller district, along the northern shore of the Alaska Penin sula, the work done there in 1922 was repeated. The results of these experiments form the basis for the following report. -
Gastineau Channel Juneau, Alaska Feasibility Report
Gastineau Channel Juneau, Alaska Feasibility Report CHANNEL DEEPENING FOR NAVIGATION ALASKA D l STR l CT CORPS OF ENGl NEEWS NOVEMBER 1977 FEASIBILITY REPORT APPENDIX A - ECONOMICS GASTINEAU CHANNEL, ALASKA PRESENT AND FUTURE ECONOMIC CONDITIONS Natural and human resources and developmental trends of the study area are presented to provide a general understanding of their relation to the problems and needs of the area and to establish a "most probable future" for the purpose of benefit and impact analysis. Of particular importance is the role waterways play in the social and economic well-being of the comunity. All waterborne traffic to and from Juneau must use Gastineau Channel. The channel southeast of Juneau is navigable by all classes of vessels, but the northern portion from Juneau-Douglas bridge to Fritz Cove is navigable only by shallow- draft vessels at selected tide levels. A shoaled reach, south of Juneau Airport, is navigable only at high tide and even then, only with current know1 edge of channel conditions. These restrictions cause the majority of traffic to take the longer route around Douglas Island, resulting in increased operating time and costs, a reduction in the navigation season due to adverse weather conditions, and the added risk of life and property because of the longer voyage through unprotected waters. TRIBUTARY AREA Gastineau Channel, a narrow strait about 16 miles long that separates Doug1 as Is1 and from the mainland of southeastern A1 aska, connects Stephens Passage on the east with Fritz Cove on the west. Although much of Southeast Alaska is a general tributary area, the Juneau-Douglas area is the principal contributor. -
Unabated Wastage of the Juneau and Stikine Icefields
The Cryosphere, 12, 1523–1530, 2018 https://doi.org/10.5194/tc-12-1523-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st century Etienne Berthier1, Christopher Larsen2, William J. Durkin3, Michael J. Willis4, and Matthew E. Pritchard3 1LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, 31400 Toulouse, France 2Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA 3Earth and Atmospheric Sciences Department, Cornell University, Ithaca, NY, USA 4Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, CO, USA Correspondence: Etienne Berthier ([email protected]) Received: 7 December 2017 – Discussion started: 5 January 2018 Revised: 4 April 2018 – Accepted: 9 April 2018 – Published: 27 April 2018 Abstract. The large Juneau and Stikine icefields (Alaska) al., 2002; Berthier et al., 2010; Larsen et al., 2007). Space- lost mass rapidly in the second part of the 20th century. Laser borne gravimetry and laser altimetry data indicate continuing altimetry, gravimetry and field measurements suggest contin- rapid mass loss in southeast Alaska between 2003 and 2009 uing mass loss in the early 21st century. However, two recent (Arendt et al., 2013). studies based on time series of Shuttle Radar Topographic For the JIF, Larsen et al. (2007) found a negative mass Mission (SRTM) and Advanced Spaceborne Thermal Emis- balance of −0.62 m w.e. a−1 for a time interval starting in sion and Reflection Radiometer (ASTER) digital elevation 1948/82/87 (depending on the map dates) and ending in models (DEMs) indicate a slowdown in mass loss after 2000. -
Alaska's Capital City, Juneau Is Nestled in a Spectacular Wilderness
JUNEAU PRIVATE SHORE EXCURSIONS Alaska’s Capital City, Juneau is nestled in a spectacular wilderness of mountains rising from the sea. An extraordinary population of whales and other marine mammals frolic and feed in the sea nearby, and offshore wilderness islands are everywhere, complete with their resident wildlife. High above it all is the Juneau Icefield a sea of ice covering nearly 3500 square miles! Almost anywhere you look you can catch a glimpse of one of the dozens of massive glaciers that pour from the icefield into the valleys below. It is truly the perfect base for an adventure in the Alaska wilderness! GUIDED BROWN BEAR VIEWING AT PACK CREEK 6 HOURS ALPINE ZIPLINE ADVENTURE 3.75 HOURS The Pack Creek Brown Bear Sanctuary is located 30 air miles outside of Juneau on On this unique Zipline Tour set in the mountains of a sub-alpine rainforest, you will Admiralty Island. Accessed by floatplane, the native Tlingit people call this impressive experience seven ziplines and cross a 150-foot suspension bridge that hovers above island “Kootznoowoo,” meaning “Fortress of the Bear.” Indeed, Admiralty Island is home the headwaters of a salmon spawning stream. Your Certified Green Zipline Tour will to the highest concentration of brown bears in the world; more than all the lower 48 see you fly through the trees as your guides lead you through a series of themed states combined. On this excursion, you’ll enjoy the Pack Creek Brown Bear Sanctuary tree houses, the highest of which is 90 feet above the ground. Once the Zipline Tour under the expertise of your private guide. -
Executive Council of the Central Council
CENTRAL COUNCIL Tlingit and Haida Indian Tribes of Alaska Edward K. Thomas Building 9097 Glacier Highway • Juneau, Alaska 99801 CENTRAL COUNCIL OF TLINGIT & HAIDA INDIAN TRIBES OF ALASKA Eighty-Fifth Annual Tribal Assembly October 1, 2020 Juneau, Alaska Resolution TA 20-25 Title: Declaration of a Climate Emergency and Commitment to Climate Mobilization By: Seattle Tlingit & Haida Community Council WHEREAS, the Central Council of Tlingit & Haida Indian Tribes of Alaska (Tlingit & Haida) is a federally recognized tribe with more than 32,000 citizens; and WHEREAS, the Tlingit and Haida people have existed since time immemorial as the guardians of their lands and waters; and WHEREAS, in 2019 the Taku Glacier, the last remaining glacier to retreat on the planet, began to recede and shrink since measurements first began in 1946; and WHEREAS, the current rate of ocean acidification is faster than any time on record; ten times faster than the last major acidification event 55 million years ago; and WHEREAS, unprecedented extreme local weather events such as sustained ocean warming and regional droughts have afflicted our lands and waters in recent years; and WHEREAS, the Tongass National Forest, the world’s fourth largest forest, has significant global carbon sink and is currently being studied by the United States Department of Agriculture (USDA) Forest Service for alternatives that would open it up for additional logging, threatening our local ability to combat climate change; and WHEREAS, in 2019 Tlingit & Haida recognized the threat of climate -
Wildlife & Wilderness 2022
ILDLIFE ILDERNESS WALASKAOutstanding & ImagesW of Wild 2022Alaska time 9winner NATIONAL CALENDAR TM AWARDS An Alaska Photographers’An Alaska Calendar Photographers’ Calendar Eagle River Valley Sunrise photo by Brent Reynolds Celebrating Alaska's Wild Beauty r ILDLIFE ILDERNESS ALASKA W & W 2022 Sunday Monday Tuesday Wednesday Thursday Friday Saturday The Eagle River flows through the Eagle River NEW YEAR’S DAY ECEMBER EBRUARY D 2021 F Valley, which is part of the 295,240-acre Chugach State Park created in 1970. It is the third-largest 1 2 3 4 1 2 3 4 5 state park in the entire United States. The 30 31 1 6 7 8 9 10 11 12 scenic river includes the north and south fork, 5 6 7 8 9 10 11 surrounded by the Chugach Mountains that 12 13 14 15 16 17 18 13 14 15 16 17 18 19 arc across the state's south-central region. • 19 20 21 22 23 24 25 20 21 22 23 24 25 26 The Eagle River Nature Center, a not-for 26 27 28 29 30 31 27 28 -profit organization, provides natural history City and Borough of Juneau, 1970 information for those curious to explore the Governor Tony Knowles, 1943- park's beauty and learn about the wildlife Fairbanks-North Star, Kenai Peninsula, and that inhabits the area. Matanuska-Susitna Boroughs, 1964 New moon 2 ● 3 4 5 6 7 8 Alessandro Malaspina, navigator, Sitka fire destroyed St. Michael’s 1754-1809 Cathedral, 1966 President Eisenhower signed Alaska Federal government sold Alaska Railroad Barry Lopez, author, 1945-2020 Robert Marshall, forester, 1901-1939 statehood proclamation, 1959 to state, 1985 Mt. -
Alaska's Glaciers Are a Spectacular Force of Nature
Glacier GRANDEUR Alaska’s glaciers are a spectacular force of nature By Eric Lucas patrick j. endres / alaskaphotographics.com Imagine a sheet of water the size of a small city. It’s made of long, winding ribbons, and broken tabs, of ice. Its cool-hue colors range from aluminum to cerulean. Immense forces cause it to flow down a narrow valley and fold over a small ridge just outside Juneau, Alaska, and finally crumble into a slushy lake. That’s the Mendenhall Glacier—one of the most visited glaciers in the United States— and I’m standing atop its lower end under an intense spring sun with freshets of water gushing past my feet. A glacier such as the Mendenhall is, in one sense, a geologic object—a monominer- alic rock, to cite a term sometimes used by glacier scientists. It’s also a 13-mile-long river of ice that’s actually moving downhill at a distinct rate, twisting and bending around stone mountains, gathering rock debris as it scrapes past. A glacier is com- posed of water, a malleable substance whose various phases—gas, liquid, solid— frans lanting / frans lanting stock are intrinsic to the shape of Earth’s land- the Barnard glacier (above), in Wrangell–st. elias national park, is striped with the debris scape. Since all forms of water can move, it accumulates as it flows down the mountain, merging with other, smaller glaciers. standing on a glacier with water running kayakers (previous spread) paddle the ice-laden waters of Barry arm in prince William sound, near the Barry, cascade and coxe glaciers. -
North America Summary, 1968
240 CLIMBS A~D REGIONAL ?\OTES North America Summary, 1968. Climbing activity in both Alaska and Canada subsided mar kedly from the peak in 1967 when both regions were celebrating their centen nials. The lessened activity seems also to have spread to other sections too for new routes and first ascents were considerably fewer. In Alaska probably the outstanding climb from the standpoint of difficulty was the fourth ascent of Mount Foraker, where a four-man party (Warren Bleser, Alex Birtulis, Hans Baer, Peter Williams) opened a new route up the central rib of the South face. Late in June this party flew in from Talkeetna to the Lacuna glacier. By 11 July they had established their Base Camp at the foot of the South face and started up the rib. This involved 10,000 ft of ice and rotten rock at an angle of 65°. In the next two weeks three camps were estab lished, the highest at 13,000 ft. Here, it was decided to make an all-out push for the summit. On 24 July two of the climbers started ahead to prepare a route. In twenty-eight hours of steady going they finally reached a suitable spot for a bivouac. The other two men who started long after them reached the same place in ten hours of steady going utilising the steps, fixed ropes and pitons left by the first party. After a night in the bivouac, the two groups then contin ued together and reached the summit, 17,300 ft, on 25 July. They were forced to bivouac another night on the return before reaching their high camp. -
150 Years of Change
1867-2017 150 years of change Áak'w Aaní at time of the Alaska Purchase March, 2017 Richard Carstensen Discovery Southeast funding from Friends of the Juneau- Douglas City Museum Place names Contents Preface: Late in 2016, returning to Juneau from nearly a year out of town with convention family affairs, I was offered a fascinating assignment. Looking ahead to the Seward's Day .................................................... 2 In all my writing since publi- Place names convention ................................. 2 sesquicentennial year of the 1867 Alaska Purchase, Jane Lindsey of Juneau- cation of Haa L’éelk’w Hás Historical context ............................................... 4 Douglas City Museum, and her friend Michael Blackwell imagined a before- Aani Saax’ú: Our grand- Methods ........................................................... 11 &-after 'banner' with an oblique view of Juneau from the air today. Alongside parents’ names on the land Three scenes..................................................... 15 (Thornton & Martin, eds. 1) Dzantik'i Héeni ........................................... 15 would be a retrospective, showing what the same view looked like at the time of purchase, 150 years ago. 2012), I’ve used Tlingit place 2) Áak'w Táak .................................................. 23 names whenever available, 3) Aanchgaltsóow .......................................... 31 In part, Jane and Mike's idea came from a split-image view of downtown followed by their translation Appendices ....................................................... 39 Juneau that I created 8 years ago, showing a 2002 aerial oblique on the right, in italic, and IWGN (impor- Appendix 1 CBJ Natural History Project ..... 39 and on the left, my best guess as to what Dzantik'i Héeni delta looked like in tant white guy name) in Appendix 2 LiDAR ......................................... 40 1879. I, in turn, had borrowed that idea from the Mannahatta project (Sander- parentheses. -
About Juneau
Echo Cove Pt. Bridget State Pa rk Bridget Cove GLE EA CIER Yankee LA Cove G BENJAMI ISLAND N SENTINEL ISLAND CIER Eagle HERBERT GLA Beach 1 E. Gruening State Historical Park Eagle All About Juneau Harbor Windfall (Amalga) Lake Peterson Creek Jensen-Olson Arboretum Shrine of Saint Saginaw Channel Therese IER SHEL Peterson CREEK ROAD AC Lake MONT West Glacier MENDENHALLGL Nugget Montana Cr Creek Spaulding Trail TER ISLAND ANA 2015 Tee GL Mendenhall Harbor AC Lake Nugget Creek eek 5 RO SPUR IER HIGHW A Tr GLA uke Nu ail East Glacier Tr 4 CIER Loop Tr ai AD ail l Tr ail ALL NH D Lena Cove DE OA EN R M OP AY Ferry 3 LO E IV Terminal R AD D E ID River S endenhall R i E OOP RO IV MENDENHALLL 2 Auke M R Bay D on Creek R Y ACIER HW Lem VE GL ANKA STREET O C Salmon Creek ITZ ITZ Twin Lakes FR AIRPORT i Gastineau Channel Mt. Juneau ail H Tr Tr Salmon DOWNTOWNail Gold Creek NORTH DOUGLAS HIGHW Creek EGAN DR. JUNEAU Perseverance CreekFish Trail Tr Mt. Rober Outer Ditcheadwell ts Trail Point Tr ail AY Stephens Passage DOUGLAS THANE RO Sheep Creek Trail DOUGLAS ISLAND Sheep Creek Eaglecrest 6 Ski Area AD Treadwell Mine Trail JUNEA 800 Glacier Avenue, Ste. 201 Juneau, AK 99801 U CONVENTION & (907) 586-2201 • 888-581-2201 email: [email protected] www.traveljuneau.com VISITORS BUREA U ALL about JUNEau A VERY BRIEF HISTORY OF JUNEAU The Gastineau Channel region was a traditional fishing ground for local Tlingit Indians in the late 1800’s when prospectors were searching for gold deposits in southeast Alaska. -
This PDF File Is Subject to the Following Conditions and Restrictions: Copyright © 2009, the Geological Society of America
Geological Society of America 3300 Penrose Place P.O. Box 9140 Boulder, CO 80301 (303) 357-1000 • fax 303-357-1073 www.geosociety.org This PDF file is subject to the following conditions and restrictions: Copyright © 2009, The Geological Society of America, Inc. (GSA). All rights reserved. Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in other subsequent works and to make unlimited copies for noncommercial use in classrooms to further education and science. For any other use, contact Copyright Permissions, GSA, P.O. Box 9140, Boulder, CO 80301-9140, USA, fax 303-357-1073, [email protected]. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. This file may not be posted on the Internet. The Geological Society of America Special Paper 461 2009 Field glaciology and earth systems science: The Juneau Icefi eld Research Program (JIRP), 1946–2008 Cathy Connor Department of Natural Sciences, University Alaska Southeast, Juneau, Alaska 99801, USA ABSTRACT For over 50 yr, the Juneau Icefi eld Research Program (JIRP) has provided under- graduate students with an 8 wk summer earth systems and glaciology fi eld camp. This fi eld experience engages students in the geosciences by placing them directly into the physically challenging glacierized alpine landscape of southeastern Alaska.