NOTES on the GEOGRAPHY and GEOLOGY of LITUYA BAY by J. B
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1922 Elizabeth T
co.rYRIG HT, 192' The Moootainetro !scot1oror,d The MOUNTAINEER VOLUME FIFTEEN Number One D EC E M BER 15, 1 9 2 2 ffiount Adams, ffiount St. Helens and the (!oat Rocks I ncoq)Ora,tecl 1913 Organized 190!i EDITORlAL ST AitF 1922 Elizabeth T. Kirk,vood, Eclttor Margaret W. Hazard, Associate Editor· Fairman B. L�e, Publication Manager Arthur L. Loveless Effie L. Chapman Subsc1·iption Price. $2.00 per year. Annual ·(onl�') Se,·ent�·-Five Cents. Published by The Mountaineers lncorJ,orated Seattle, Washington Enlerecl as second-class matter December 15, 19t0. at the Post Office . at . eattle, "\Yash., under the .-\0t of March 3. 1879. .... I MOUNT ADAMS lllobcl Furrs AND REFLEC'rION POOL .. <§rtttings from Aristibes (. Jhoutribes Author of "ll3ith the <6obs on lltount ®l!!mµus" �. • � J� �·,,. ., .. e,..:,L....._d.L.. F_,,,.... cL.. ��-_, _..__ f.. pt",- 1-� r�._ '-';a_ ..ll.-�· t'� 1- tt.. �ti.. ..._.._....L- -.L.--e-- a';. ��c..L. 41- �. C4v(, � � �·,,-- �JL.,�f w/U. J/,--«---fi:( -A- -tr·�� �, : 'JJ! -, Y .,..._, e� .,...,____,� � � t-..__., ,..._ -u..,·,- .,..,_, ;-:.. � --r J /-e,-i L,J i-.,( '"'; 1..........,.- e..r- ,';z__ /-t.-.--,r� ;.,-.,.....__ � � ..-...,.,-<. ,.,.f--· :tL. ��- ''F.....- ,',L � .,.__ � 'f- f-� --"- ��7 � �. � �;')'... f ><- -a.c__ c/ � r v-f'.fl,'7'71.. I /!,,-e..-,K-// ,l...,"4/YL... t:l,._ c.J.� J..,_-...A 'f ',y-r/� �- lL.. ��•-/IC,/ ,V l j I '/ ;· , CONTENTS i Page Greetings .......................................................................tlristicles }!}, Phoiitricles ........ r The Mount Adams, Mount St. Helens, and the Goat Rocks Outing .......................................... B1/.ith Page Bennett 9 1 Selected References from Preceding Mount Adams and Mount St. -
1961 Climbers Outing in the Icefield Range of the St
the Mountaineer 1962 Entered as second-class matter, April 8, 1922, at Post Office in Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and December by THE MOUNTAINEERS, P. 0. Box 122, Seattle 11, Wash. Clubroom is at 523 Pike Street in Seattle. Subscription price is $3.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of Northwest America; To make expeditions into these regions in fulfillment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor Zif e. EDITORIAL STAFF Nancy Miller, Editor, Marjorie Wilson, Betty Manning, Winifred Coleman The Mountaineers OFFICERS AND TRUSTEES Robert N. Latz, President Peggy Lawton, Secretary Arthur Bratsberg, Vice-President Edward H. Murray, Treasurer A. L. Crittenden Frank Fickeisen Peggy Lawton John Klos William Marzolf Nancy Miller Morris Moen Roy A. Snider Ira Spring Leon Uziel E. A. Robinson (Ex-Officio) James Geniesse (Everett) J. D. Cockrell (Tacoma) James Pennington (Jr. Representative) OFFICERS AND TRUSTEES : TACOMA BRANCH Nels Bjarke, Chairman Wilma Shannon, Treasurer Harry Connor, Vice Chairman Miles Johnson John Freeman (Ex-Officio) (Jr. Representative) Jack Gallagher James Henriot Edith Goodman George Munday Helen Sohlberg, Secretary OFFICERS: EVERETT BRANCH Jim Geniesse, Chairman Dorothy Philipp, Secretary Ralph Mackey, Treasurer COPYRIGHT 1962 BY THE MOUNTAINEERS The Mountaineer Climbing Code· A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
Changes in Snow, Ice and Permafrost Across Canada
CHAPTER 5 Changes in Snow, Ice, and Permafrost Across Canada CANADA’S CHANGING CLIMATE REPORT CANADA’S CHANGING CLIMATE REPORT 195 Authors Chris Derksen, Environment and Climate Change Canada David Burgess, Natural Resources Canada Claude Duguay, University of Waterloo Stephen Howell, Environment and Climate Change Canada Lawrence Mudryk, Environment and Climate Change Canada Sharon Smith, Natural Resources Canada Chad Thackeray, University of California at Los Angeles Megan Kirchmeier-Young, Environment and Climate Change Canada Acknowledgements Recommended citation: Derksen, C., Burgess, D., Duguay, C., Howell, S., Mudryk, L., Smith, S., Thackeray, C. and Kirchmeier-Young, M. (2019): Changes in snow, ice, and permafrost across Canada; Chapter 5 in Can- ada’s Changing Climate Report, (ed.) E. Bush and D.S. Lemmen; Govern- ment of Canada, Ottawa, Ontario, p.194–260. CANADA’S CHANGING CLIMATE REPORT 196 Chapter Table Of Contents DEFINITIONS CHAPTER KEY MESSAGES (BY SECTION) SUMMARY 5.1: Introduction 5.2: Snow cover 5.2.1: Observed changes in snow cover 5.2.2: Projected changes in snow cover 5.3: Sea ice 5.3.1: Observed changes in sea ice Box 5.1: The influence of human-induced climate change on extreme low Arctic sea ice extent in 2012 5.3.2: Projected changes in sea ice FAQ 5.1: Where will the last sea ice area be in the Arctic? 5.4: Glaciers and ice caps 5.4.1: Observed changes in glaciers and ice caps 5.4.2: Projected changes in glaciers and ice caps 5.5: Lake and river ice 5.5.1: Observed changes in lake and river ice 5.5.2: Projected changes in lake and river ice 5.6: Permafrost 5.6.1: Observed changes in permafrost 5.6.2: Projected changes in permafrost 5.7: Discussion This chapter presents evidence that snow, ice, and permafrost are changing across Canada because of increasing temperatures and changes in precipitation. -
Ice Thickness Measurements on the Harding Icefield, Kenai Peninsula, Alaska
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Ice Thickness Measurements on the Harding Icefield, Kenai Peninsula, Alaska Natural Resource Data Series NPS/KEFJ/NRDS—2014/655 ON THIS PAGE The radar team is descending the Exit Glacier after a successful day of surveying Photograph by: M. Truffer ON THE COVER Ground-based radar survey of the upper Exit Glacier Photograph by: M. Truffer Ice Thickness Measurements on the Harding Icefield, Kenai Peninsula, Alaska Natural Resource Data Series NPS/KEFJ/NRDS—2014/655 Martin Truffer University of Alaska Fairbanks Geophysical Institute 903 Koyukuk Dr Fairbanks, AK 99775 April 2014 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are 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 Data Series is intended for the timely release of basic data sets and data summaries. Care has been taken to assure accuracy of raw data values, but a thorough analysis and interpretation of the data has not been completed. Consequently, the initial analyses of data in this report are provisional and subject to change. 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. -
Tsuinfo Alert, June 2008
Contents Volume 10, Number 3 June 2008 ______________________________________________________________________________________________________________________________ Special features Departments Giant wave in Lituya Bay (50th anniversary) 1 Hazard mitigation news 15 Changing roles & responsibilities of the local emergency manager 4 Websites 17 Shadowed by the glare of 1906 are faceless future dangers 12 Publications 18 Warnings on the horizon—Air patrol pilots 13 Conferences/seminars/symposium 19 Airborne tsunami alert triggers wave of text messaging 14 Classes 19 Insights into the problems of communicating tsunami warnings 14 Media 19 Un-natural disasters 20 State Emergency Management offices 21 Rural students build model tsunami shelters 26 Material added to NTHMP Library 21 Detecting tsunami genesis 11 IAQ 28 Video reservations 27 ____________________________________________________________________________________________________ 50th ANNIVERSARY OF LITUYA BAY TSUNAMI, July 9, 1958 The Alaska Earthquake of July 10, 1958*: Giant wave in Lituya Bay By Don J. Miller Bulletin of the Seismological Society of America, v. 50, no. 2, excerpts p.257-259. Map: U.S. Geological Survey Professional Paper 354-C Continued on page 3 TsuInfo Alert is prepared by the Washington State Department of Natural Resources on behalf of the National Tsunami Hazard Mitigation Program, a State/Federal Partnership funded through the National Oceanic and Atmospheric Administration (NOAA). It is assembled by Lee Walkling, Librarian, and is published bi-monthly by -
Advances in the Study of Mega-Tsunamis in the Geological Record Raphael Paris, Kazuhisa Goto, James Goff, Hideaki Yanagisawa
Advances in the study of mega-tsunamis in the geological record Raphael Paris, Kazuhisa Goto, James Goff, Hideaki Yanagisawa To cite this version: Raphael Paris, Kazuhisa Goto, James Goff, Hideaki Yanagisawa. Advances in the study of mega-tsunamis in the geological record. Earth-Science Reviews, Elsevier, 2020, 210, pp.103381. 10.1016/j.earscirev.2020.103381. hal-02964184 HAL Id: hal-02964184 https://hal.uca.fr/hal-02964184 Submitted on 12 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Advances in the study of mega-tsunamis in the geological record 2 3 Raphaël Paris1, Kazuhisa Goto2, James Goff3, Hideaki Yanagisawa4 4 1 Université Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et Volcans, F-63000 Clermont- 5 Ferrand, France. 6 2 Department of Earth and Planetary Science, The University of Tokyo, Hongo 7-3-1, Tokyo, Japan. 7 3 PANGEA Research Centre, UNSW Sydney, Sydney, NSW 2052, Australia. 8 4 Department of Regional Management, Tohoku Gakuin University, Tenjinsawa 2‑ 1‑ 1, Sendai, Japan. 9 10 Abstract 11 Extreme geophysical events such as asteroid impacts and giant landslides can generate mega- 12 tsunamis with wave heights considerably higher than those observed for other forms of 13 tsunamis. -
Kachemak Bay Research Reserve: a Unit of the National Estuarine Research Reserve System
Kachemak Bay Ecological Characterization A Site Profile of the Kachemak Bay Research Reserve: A Unit of the National Estuarine Research Reserve System Compiled by Carmen Field and Coowe Walker Kachemak Bay Research Reserve Homer, Alaska Published by the Kachemak Bay Research Reserve Homer, Alaska 2003 Kachemak Bay Research Reserve Site Profile Contents Section Page Number About this document………………………………………………………………………………………………………… .4 Acknowledgements…………………………………………………………………………………………………………… 4 Introduction to the Reserve ……………………………………………………………………………………………..5 Physical Environment Climate…………………………………………………………………………………………………… 7 Ocean and Coasts…………………………………………………………………………………..11 Geomorphology and Soils……………………………………………………………………...17 Hydrology and Water Quality………………………………………………………………. 23 Marine Environment Introduction to Marine Environment……………………………………………………. 27 Intertidal Overview………………………………………………………………………………. 30 Tidal Salt Marshes………………………………………………………………………………….32 Mudflats and Beaches………………………………………………………………………… ….37 Sand, Gravel and Cobble Beaches………………………………………………………. .40 Rocky Intertidal……………………………………………………………………………………. 43 Eelgrass Beds………………………………………………………………………………………… 46 Subtidal Overview………………………………………………………………………………… 49 Midwater Communities…………………………………………………………………………. 51 Shell debris communities…………………………………………………………………….. 53 Subtidal soft bottom communities………………………………………………………. 54 Kelp Forests…………………………………………………….…………………………………….59 Terrestrial Environment…………………………………………………………………………………………………. 61 Human Dimension Overview………………………………………………………………………………………………. -
Glaciers of the Canadian Rockies
Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter -
Alaska Tsunami Hazard Maps and Modeling Slides
Seismically Glacial Near-field active plate fjords tsunami hazard boundary 1964 Great Alaska Earthquake 2015, Taan Fjord 92% of fatalities 193 m runup were due to 4th largest tsunamis 76% of them 1958, Lituya Bay were due to 524 m runup local landslide WORLD RECORD tsunamis 1946 1936, Lituya Bay Earthquake 149 m runup Tsunami killed 5th largest 159 in Hilo, HI Barry Arm slide and 5 in Unimak Island, AK when??? History of the product line: 1998 - 2021 High-resolution maps and reports 2018 Update 1998 Regional maps 2014 Maritime 2016 Pedestrian Subsidence Brochures 2020 FY 2019-2020 project areas A l a s k a Bering Sea Seward Bristol Bay Kodiak Is. Gulf of Alaska Regional tsunami hazard assessment: Bristol Bay Bristol Bay Tectonic and landslide tsunami sources Maximum tsunami energy Tectonic tsunamis Landslide tsunamis Tsunami hazard is higher than expected Nelson Lagoon Platinum High-resolution modeling: Kodiak villages • Regional tsunami hazard assessment was completed in 2018 • In FY2019-2020 project period, we performed high- resolution modeling and mapping for 7 Kodiak communities. From regional assessment to high-resolution maps Regional tsunami hazard High-resolution tsunami assessment inundation map Visiting Kodiak communities New tsunami shelter in Chiniak New tsunami shelter in Ouzinkie Updating tsunami hazard map of Seward 1964 inundation • The previous report was published before Old report the 2011 Tohoku tsunami. New sources • We made a new set of potential tsunami sources that include large amount of slip in the shallow part of the megathrust, similar to that in the Tohoku earthquake. • We also consider splay faults that have been mapped offshore Kenai Peninsula. -
Chapter 7 Glaciers
CHAPTER 7 GLACIERS 1. INTRODUCTION 1.1 Before the era of universal air travel, which commenced less than half a century ago, few of the world’s population had seen a glacier. I suspect that majority of class members in this course have seen a glacier—if not close up, then out of a jetliner window. In the Canadian Rockies, you can drive to within almost a stone’s throw of the terminus of the Athabasca Glacier, a classic active valley glacier. In many other parts of the world, valley glaciers are accessible to even casual day hikers. The great ice sheets of the world, in Antarctica and Greenland, remain much less accessible. 1.2 In the broad context of geologic history, the Earth is in an “icehouse” time, with recurrent major ice-sheet advances across the Northern Hemisphere continents. (There have been several other such icehouse periods in Earth history, separated by long intervals of ice-free times, called “greenhouse” periods, with no evidence of glaciation.) The Earth has only recently emerged from the latest episode of continental glaciation. Does it surprise you to learn that a mere twenty thousand years ago the Boston area was beneath a mile of glacier ice moving slowly southward toward its terminus south of what is now the south coast of New England? 1.3 The Earth is in many senses a glacial planet: • 10% of the Earth is covered with glacier ice (about 15 million square kilometers). • About 40% of the Northern Hemisphere in winter is covered with solid water at any given time (land and sea). -
Tsunami Hazard to North and West Vancouver, British Columbia
NSEMO tsunami report Tsunami Hazard to North and West Vancouver, British Columbia Prepared by: Dr. John J. Clague PGeo Dr. John Orwin Centre for Natural Hazard Research Simon Fraser University Presented to: North Shore Emergency Planning Office Date: December 5, 2005 i NSEMO tsunami report Table of Contents List of tables ……………………………………………………………………….. iii List of figures ……………………………………………………………………… iii Summary ………………………………………………………………………….. iv 1 Scope of report …………………………………………………………………. 1 2 Anatomy of a tsunami ………………………………………………………… 1 3 Past tsunamis in British Columbia …………………………………………. 2 3.1 1964 Alaska tsunami ………………………………………………………. 2 3.2 1700 Cascadia tsunami ……………………………………………………. 3 4 Potential sources of tsunamis that might affect the North Shore ……. 3 4.1 Subduction zone earthquakes ……………………………………………. 3 4.1.1 Earthquakes at the Cascadia subduction zone ………………………….. 4 4.1.2 Earthquakes at other Pacific subduction zones ………………………….. 5 4.2 Shallow local earthquakes ………………………………………………… 5 4.3 Landslides at the front of the Fraser delta ………………………………. 5 4.4 Landslides in Howe Sound or Indian Arm ……………………………….. 6 5 Documenting past tsunamis from the geologic record …………………. 6 5.1 2005 field work ………………………………………………………………. 7 6 Tsunami inundation risk maps ……………………………………………….. 7 6.1 North Vancouver …………………………………………………………….. 7 6.2 West Vancouver ……………………………………………………………… 8 7 North Shore tsunami risk ……………………………………………………… 8 8 Preparedness, mitigation, and response strategies ……………………… 9 8.1 Preparedness ………………………………………………………………… 9 8.2 Mitigation