Illustrations

Total Page:16

File Type:pdf, Size:1020Kb

Illustrations Illustrations Plates (following page 52) 1. Parts of the St. Elias Range and Malaspina Glacier. 2. Hubbard Glacier entering Disenchantment Bay, Yakutat Bay area. 3. Mount Crillon (12,726 feet) and Brady Glacier. 4. Mount Crillon (12,726 feet) viewed across Johns Hopkins Inlet. 5. Nunatak Fiord, Yakutat Bay. 6. Part of the Chugach Range, including Mount Witherspoon (12,023 feet). 7. Perspective diagram of Upper Cook Inlet area showing setting of Anchorage. 8. Mount Sanford and the Wrangell Mountains. 9. Sourdough Peak in the southern foothills of the Wrangell Mountains. 10. Cliffs of Triassic limestone in the southeastern Wrangell Mountains. 11. Mount McKinley from the northeast. xii Illustrations 12. Part of the Alaska Range, including Mount McKinley. 13. Eocene coals and sandstones on Lignite Creek, near Healy. 14. Recessional moraines on the north side of Iliamna volcano. 15. Caldera of Katmai volcano. 16. Head of the Valley of Ten Thousand Smokes. 17. Dacite dome on the south flank of Trident volcano. 18. Shishaldin volcano, Unimak Island. 19. Placer gold mining near Fairbanks. 20. Typical upland terrain, northern Seward Peninsula. 21. Mount Doonerak from Amawk Mountain, Brooks Range. 22. Highest part of the Brooks Range. 23. Polygonal ground and thaw lakes near Skull Cliff, southwest of Barrow. Maps facing page 1. Physiographic provinces of Alaska. 4 2. Southeastern Alaska. 12 3. Gulf of Alaska area, Wrangell Mountains, Copper River plateau, Talkeetna Mountains, Cook Inlet and Susitna lowland, and Alaska Range. 20 4. Alaska Peninsula-Aleutian Islands. 68 5. Lowlands and plains of interior and western Alaska; interior high- lands of western and eastern Alaska; Seward Peninsula. 76 6. Brooks Range and Arctic Slope. 116 Figures 1. Evolution of Okmok caldera, Umnak Island. 62 2. Present areas occupied by glaciers and by permafrost, and areas formerly covered by glaciers at the time of their maximum spread during the Pleistocene period. facing page 80 3. Development of the Bering Sea Land Bridge. 134 .
Recommended publications
  • Harvard Mountaineering 3
    HARVARD MOUNTAINEERING 1931·1932 THE HARVARD MOUNTAINEERING CLUB CAMBRIDGE, MASS. ~I I ' HARVARD MOUNTAINEERING 1931-1932 THE HARVARD MOUNTAINEERING CLUB CAMBRIDGE, MASS . THE ASCENT OF MOUNT FAIRWEATHER by ALLEN CARPE We were returning from the expedition to Mount Logan in 1925. Homeward bound, our ship throbbed lazily across the Gulf of Alaska toward Cape Spencer. Between reefs of low fog we saw the frozen monolith of St. Elias, rising as it were sheer out of the water, its foothills and the plain of the Malaspina Glacier hidden behind the visible sphere of the sea. Clouds shrouded the heights of the Fairweather Range as we entered Icy Strait and touched at Port Althorp for a cargo of salmon; but I felt then the challenge of this peak which was now perhaps the outstanding un­ climbed mOUlitain in America, lower but steeper than St. Elias, and standing closer to tidewater than any other summit of comparable height in the world. Dr. William Sargent Ladd proved a kindred spirit, and in the early summer of 1926 We two, with Andrew Taylor, made an attempt on the mountain. Favored by exceptional weather, we reached a height of 9,000 feet but turned back Photo by Bradford Washburn when a great cleft intervened between the but­ tresses we had climbed and the northwest ridge Mount Fairweather from the Coast Range at 2000 feet of the peak. Our base was Lituya Bay, a beau­ (Arrows mark 5000 and 9000-foot camps) tiful harbor twenty miles below Cape Fair- s camp at the base of the south face of Mount Fair­ weather; we were able to land near the foot of the r weather, at 5,000 feet.
    [Show full text]
  • The Ascent of Mt. St. Agnes, Chugach Range, Alaska 207
    THE ASCENT OF MT. ST. AGNES, CHUGACH RANGE, ALASKA 207 THE ASCENT OF MT. ST. AGNES, CHUGACH RANGE, ALASKA BY BRADFORD WASHBURN DRING the months of May and June 1938 a small expedition was sent out by the Institute of Geographical Exploration of Harvard University to make a thorough reconnaissance of the Chugach mountains in the Alaska Coast . Range, and to attempt the ascent of Mt. St. Agnes (13,250 ft.), the highest peak in the group. The Chugaches are geologically a western prolongation of the St. Elias Range, much in the same way as the Fairweather Range is a southern offshoot of this massif. Sweeping in a jagged arc about the head of Prince William Sound, this rugged little range of mountains enjoys probably the most constantly diabolical weather on the entire North American Continent. An almost unbroken series of S.E. and S.W. storms, finding their origin in the Bering Sea area, deluges Prince William Sound with an annual rainfall of over 200 ins. This rainfall, converted into snow on the upper reaches of the Chugach Range, has resulted in one of the wildest and most rugged glacier systems in the world. On the S. or seaward side of the range, where this precipitation is heaviest, only a score of truly clear days occurs during the course of an entire year. On this side the mountains are particularly jagged on account of the heavy frost action due to the variable climate. The rock is dominantly schistose. In many cases its beds stand directly on end and, except under extraordinary conditions of drought, every platform and cranny in these great southerly cliffs is buried deep in fresh snow, or plastered with ice.
    [Show full text]
  • 1934 the MOUNTAINEERS Incorpora.Ted T�E MOUNTAINEER VOLUME TWENTY-SEVEN Number One
    THE MOUNTAINEER VOLUME TWENTY -SEVEN Nom1-0ae Deceml.er, 19.34 GOING TO GLACIER PUBLISHED BY THE MOUNTAIN�ER.S INCOaPOllATBD SEATTLI: WASHINGTON. _,. Copyright 1934 THE MOUNTAINEERS Incorpora.ted T�e MOUNTAINEER VOLUME TWENTY-SEVEN Number One December, 1934 GOING TO GLACIER 7 •Organized 1906 Incorporated 1913 EDITORIAL BOARD, 1934 Phyllis Young Katharine A. Anderson C. F. Todd Marjorie Gregg Arthur R. Winder Subscription Price, $2.00 a Year Annual (only) Seventy-five Cents Published by THE MOUNTAINEERS Incorporated Seattle, Washington Entered as second class matter, December 15, 1920, at the Postofflce at Seattle, Washington, under the Act of March 3, 1879. TABLE OF CONTENTS Greeting ........................................................................Henr y S. Han, Jr. North Face of Mount Rainier ................................................ Wolf Baiter 3 r Going to Glacier, Illustrated ............... -.................... .Har iet K. Walker 6 Members of the 1934 Summer Outing........................................................ 8 The Lake Chelan Region ............. .N. W. <J1·igg and Arthiir R. Winder 11 Map and Illustration The Climb of Foraker, Illitstrated.................................... <J. S. Houston 17 Ascent of Spire Peak ............................................... -.. .Kenneth Chapman 18 Paradise to White River Camp on Skis .......................... Otto P. Strizek 20 Glacier Recession Studies ................................................H. Strandberg 22 The Mounta,ineer Climbers................................................
    [Show full text]
  • 2012Bibarxiuizardfllibres Per
    BIBLIOTECA ARXIU IZARD-LLONCH FORRELLAD DE LLEIDA 1 de 82. 21/05/2012 GRAL. X TITOL. Arxiu IZARD FORRELLAD. "Biblioteca" t/v Vol. AUTOR EDITORIAL Lloc Any Pags Fots Graf Maps Idioma Lleida 1949(I-IX), 1950(I-XII), 1951(I-XII) i 1952(I-XII+esp) t 1949 a 1952 CIUDAD LLEIDA 1949 castellà RomBeat rev Les pintures murals de Mur a la col.lecció Plandiura W 28 oct 1919, ed. tarda, pàg 6 La Veu de Catalunya Barcelona 1919 CATALÀ lleida rev AU VIGNEMALE. Les grottes du comte Russell dans les Pyrénées t A. de L. ILLUSTRATION, L' Paris 1898 2 10 FRENCH RomBeat La Batalla del Adopcionismo. t ABADAL i VINYALS/MILLÀS R Acad Buenas Letras de Barcelona 1949 190 0 castellà Osca DE NUESTRA FABLA t ABALOS, J. URRIZA, Lib y Enc de R. LLEIDA 64 0 castellà Lleida ELS PIRINEUS I LA FOTOGRAFIA t ABEL,Ton i JMª Sala Alb Novaidea Barcelona 2004 60 104 CATALÀ Lleida NOTES PER A LA HISTÒRIA DE PUIGCERCÓS t 7 Abella/Armengol/Català/PR GARSINEU EDICIONS TREMP 1992 93 40 div CATALÀ Lleida EL PALLARS REVISITAT. .... J.Morelló..... t 5 Abella/Cuenca/Ros/Tugues GARSINEU EDICIONS TREMP 2002 36 83 CATALÀ Lleida CATÀLEG de Bitllets dels Ajuntaments Catalans, 1936-38 t ABELLÓ/VIÑAS Auto Edició Reus/Barna 1981 102 0 molts CATALÀ Lleida EL INDICE DE PRIVILEGIOS DEL VALLE DE ARAN t ABIZANDA, Manel Institut Estudis Ilerdencs Balaguer 1944 85 3 castellà Arreu JANNU t ABREGO, Mari ARAMBURU IRUNEA 1982 132 +++ + castellà Arreu EN LA CIMA K-2 / CHOGOLISA t ABREGO/ARIZ KAIKU IRUNEA 1987 117 +++ castellà Osca Tras las Huellas de Lucien Briet.
    [Show full text]
  • A, Index Map of the St. Elias Mountains of Alaska and Canada Showing the Glacierized Areas (Index Map Modi- Fied from Field, 1975A)
    Figure 100.—A, Index map of the St. Elias Mountains of Alaska and Canada showing the glacierized areas (index map modi- fied from Field, 1975a). B, Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the St. Elias Mountains in summer 1995. National Oceanic and Atmospheric Administration image from Mike Fleming, USGS, EROS Data Center, Alaska Science Center, Anchorage, Alaska. K122 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD St. Elias Mountains Introduction Much of the St. Elias Mountains, a 750×180-km mountain system, strad- dles the Alaskan-Canadian border, paralleling the coastline of the northern Gulf of Alaska; about two-thirds of the mountain system is located within Alaska (figs. 1, 100). In both Alaska and Canada, this complex system of mountain ranges along their common border is sometimes referred to as the Icefield Ranges. In Canada, the Icefield Ranges extend from the Province of British Columbia into the Yukon Territory. The Alaskan St. Elias Mountains extend northwest from Lynn Canal, Chilkat Inlet, and Chilkat River on the east; to Cross Sound and Icy Strait on the southeast; to the divide between Waxell Ridge and Barkley Ridge and the western end of the Robinson Moun- tains on the southwest; to Juniper Island, the central Bagley Icefield, the eastern wall of the valley of Tana Glacier, and Tana River on the west; and to Chitistone River and White River on the north and northwest. The boundar- ies presented here are different from Orth’s (1967) description. Several of Orth’s descriptions of the limits of adjacent features and the descriptions of the St.
    [Show full text]
  • Timing and Potential Causes of 19Th-Century Glacier Advances in Coastal Alaska Based on Tree-Ring Dating and Historical Accounts
    ORIGINAL RESEARCH published: 03 May 2019 doi: 10.3389/feart.2019.00082 Timing and Potential Causes of 19th-Century Glacier Advances in Coastal Alaska Based on Tree-Ring Dating and Historical Accounts Benjamin V. Gaglioti1,2*, Daniel H. Mann2, Gregory C. Wiles3, Benjamin M. Jones4, Josh Charlton3, Nicholas Wiesenberg3 and Laia Andreu-Hayles1 1 Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, United States, 2 Department of Geosciences, University of Alaska Fairbanks, Fairbanks, AK, United States, 3 Department of Earth Sciences, The College of Wooster, Wooster, OH, United States, 4 Water and Environmental Research Center, University of Alaska Fairbanks, Fairbanks, AK, United States The Little Ice Age (LIA), ca. CE 1250–1850, was a cold period of global extent, with the nature and timing of reduced temperatures varying by region. The Gulf of Alaska (GOA) is a key location to study the climatic drivers of glacier fluctuations during the LIA because dendrochronological techniques can provide precise ages of ice advances and retreats. Edited by: Lesleigh Anderson, Here, we use dendrochronology to date the most recent advance of La Perouse Glacier United States Geological Survey, in the Fairweather Range of Southeast Alaska. After maintaining a relatively contracted United States state since at least CE 1200, La Perouse advanced to its maximum LIA position between Reviewed by: CE 1850 and 1895. Like many other glaciers bordering the GOA, the La Perouse Glacier Johannes Koch, Brandon University, Canada reached this maximum position relatively late in the LIA compared with glaciers in other Olga Nikolaevna Solomina, regions. This is curious because reconstructions of paleoclimate in the GOA region Institute of Geography (RAS), Russia indicate the 19th century was not the coldest period of the LIA.
    [Show full text]
  • Shining Mountains, Nameless Valleys: Alaska and the Yukon Terris Moore and Kenneth Andrasko
    ALASKA AND THE YUKON contemplate Bonington and his party edging their way up the S face of Annapurna. In general, mountain literature is rich and varied within the bounds of a subject that tends to be esoteric. It is not easy to transpose great actions into good, let alone great literature-the repetitive nature of the Expedition Book demonstrates this very well and it may well be a declining genre for this reason. Looking to the future a more subtle and complex approach may be necessary to to give a fresh impetus to mountain literature which so far has not thrown up a Master of towering and universal appeal. Perhaps a future generation will provide us with a mountaineer who can combine the technical, literary and scientific skills to write as none before him. But that is something we must leave to time-'Time, which is the author of authors'. Shining mountains, nameless valleys: Alaska and the Yukon Terris Moore and Kenneth Andrasko The world's first scientific expedition, sent out by Peter the Great-having already proved by coasting around the E tip of Siberia that Asia must be separated from unseen America-is now, July, 1741, in the midst of its second sea voyage of exploration. In lower latitudes this time, the increasing log of sea miles from distant Petropavlovsk 6 weeks behind them, stirs Com­ mander Vitus Bering and his 2 ship captains, Sven Waxell of the 'St. Peter' and Alexei Chirikov of the 'St Paul', to keen eagerness for a landfall of the completely unexplored N American coast, somewhere ahead.
    [Show full text]
  • Geologic Resources Inventory Scoping Summary Glacier Bay
    Geologic Resources Inventory Scoping Summary Glacier Bay National Park and Preserve, Alaska Geologic Resources Division Prepared by Katie KellerLynn National Park Service November 30, 2009 US Department of the Interior The Geologic Resources Inventory (GRI) Program provides each of 270 identified natural area National Park System units with a geologic scoping meeting, a digital geologic map, and a geologic resources inventory report. Geologic scoping meetings generate an evaluation of the adequacy of existing geologic maps for resource management, provide an opportunity for discussion of park- specific geologic management issues and, if possible, include a site visit with local experts. The purpose of these meetings is to identify geologic mapping coverage and needs, distinctive geologic processes and features, resource management issues, and potential monitoring and research needs. Outcomes of this scoping process are a scoping summary (this report), a digital geologic map, and a geologic resources evaluation report. The National Park Service held a GRI scoping meeting for Glacier Bay National Park and Preserve on June 18, 2009, at park headquarters near Bartlett Cove. Participants at the meeting included NPS staff from the park, Geologic Resources Division, and Alaska Regional Office; private consultants; and cooperators from the U.S. Geological Survey, Student Conservation Association (SCA), and Colorado State University (see table 5). Superintendent Cherry Payne welcomed the group and enthusiastically expressed her interest in seeing the results of the inventory. During the meeting, Tim Connors (Geologic Resources Division) facilitated the group’s assessment of map coverage and needs, and Bruce Heise (Geologic Resources Division) led the discussion of geologic processes and features.
    [Show full text]
  • American Alpine Journal, the World’S Outstanding Mountaineering Publication
    In Memoriam Edited by KENNETH A. BROWN wirh HEIDI POMFRET H. ADAMS CARTER 1914-1995 T he sudden death of Adams Carter on April 1 brought a sense of loss and sadness to the mountaineering world. Ad, as he was known, was inter- nationally renowned as the Editor of The American Alpine Journal, the world’s outstanding mountaineering publication. His encyclopedic knowl- edge of mountains and mountaineering was extraordinary. He probably knew or communicated with more climbers than anyone on any continent, sometimes writing as many as 40 letters a day to get accurate information for the journals he edited annually for 35 years. Their high quality may never again be equaled. Ad was an avid skier, a member of the American ski team in the 193Os, who skied almost to the day he died. His mountain climbing began early. He went up Mount Washington in New Hampshire at age five, and 10 years later climbed the Matterhorn and began making ascents and new routes with guides near Kandersteg in the Swiss Alps. In the autumn of 1932 he entered Harvard College, and the following June went to Alaska to challenge 12,700-foot Mount Crillon in the Fairweather Range. Three men on this expedition were to be his close friends for over 60 years: Bob Bates, Charlie Houston and Brad Washburn. Though the summit of Mount Crillon was not quite reached in 1933, Carter and Washburn achieved it the next summer. These climbs led to Ad’s becoming a member of the National Geographic Society’s Yukon Expedition, led by Washburn, in the winter of 1935.
    [Show full text]
  • Chogori (K2) As Seen from Godwin-Austen Glacier, Karakoram Dr
    Top of the World Books Catalogue 45: February 2012 Chogori (K2) as seen from Godwin-Austen Glacier, Karakoram Dr. Jules Jacot-Guillarmod (1902) [K2]. Chogori (K2) as seen from Godwin-Austen Glacier, Karakoram - Dr. Jules Jacot-Guillarmod (1902). Limited (150 numbered copies) Edition, Image size 16” x 16”, Paper size 20” x 20”, printed on Hahnemühle Photo Rag® Matt FineArt, 308 gsm, 100% cotton paper; new. #25930, $195.- This classic view of Chogori (K2), the second highest mountain in the world at 8,611m, is the first known photograph ever made of the “mountaineer’s mountain”. It was taken by Dr. Jules Jacot-Guillarmod using a “Verascope Richard” camera, during the Eckenstein-Crowley expedition of 1902. This was the first serious attempt to climb K2 and reached a height of approximately 6,525m. Jacot-Guillarmod served as the expedition doctor and published his account of the expedition - “Six Mois dans l’Himalaya, le Karakorum et l’Hindu-Kush” (1904). This particular image has not been previously published in any account of the expedition and was selected for the cover of Alpinist 37. We are pleased to offer, from the Bob A. Schelfhout Aubertijn Collection, magnificent, never-before-published prints (both Limited and Regular Editions) of this historic first photograph of K2. —. another copy. Regular Edition, Image size 10” x 10”, Paper size 12” x 12”, printed on Fujicolor Crystal Archive Matte paper; new. #25929, $95.- Top of the World Books 182 Orchard Commons Rd Hinesburg VT 05461-8999 USA 1 Email: [email protected] www.topworldbooks.com Phone: 802-482-7287 Fax: 802-482-5050 Mountaineering (1996, 2006), Cho Oyu (1997, 2007), Aconcagua (1997), Everest (1999, 2000, 2001, 2008, 2009, 2010), Ama Dablam (2000), Gasherbrum I & II (2001), th [K2].
    [Show full text]
  • A Cultural and Environmental History of Mountaineering in Alaska Allison M
    Claremont Colleges Scholarship @ Claremont CMC Senior Theses CMC Student Scholarship 2014 Summiting in the Last Wilderness: A Cultural and Environmental History of Mountaineering in Alaska Allison M. Barnwell Claremont McKenna College Recommended Citation Barnwell, Allison M., "Summiting in the Last Wilderness: A Cultural and Environmental History of Mountaineering in Alaska" (2014). CMC Senior Theses. Paper 858. http://scholarship.claremont.edu/cmc_theses/858 This Open Access Senior Thesis is brought to you by Scholarship@Claremont. It has been accepted for inclusion in this collection by an authorized administrator. For more information, please contact [email protected]. CLAREMONT MCKENNA COLLEGE Summiting in the Last Wilderness: A Cultural and Environmental History of Mountaineering in Alaska SUBMITTED TO Professor Tamara Venit-Shelton AND DEAN NICHOLAS WARNER BY Allison Barnwell for SENIOR THESIS Fall, Spring 2014 April 28, 2014 1 TABLE OF CONTENTS INTRODUCTION ……………………………. 2 ENVIRONMENT AND CLIMBERS ……………………………. 13 COLONIZING CLIMBERS ……………………………. 39 WOMEN CLIMBERS ……………………………. 61 CONCLUSION: A BETTER WAY TO CLIMB ……………………………. 83 BIBLIOGRAPHY ……………………………. 89 2 Introduction Climbers, backpackers, and skiers are an elite corps, you might say, in preserving the values of the environment. Who better knows that we need the wilderness to bring people closer to their original nature, that we need a place to be alone, where nature can bring us its good tidings. But we outdoor people know full well that we also need, for survival, the raw materials found in nature. Our backpacks of aluminum, our pitons of steel. We need synthetic fabrics and insulation- the products of petroleum. Even as we stand alone on some outcrop of rock looking at a landscape few may have ever seen, we know we are very much a part of the world of men and women, of industry and energy, of expanding demands on the fragile environment of the plant… There must be a balance.
    [Show full text]
  • The United States Geological Survey in Alaska: Accomplishments During 1975 the United States Geological Survey in Alaska: Accomplishments During 1975
    GEOLOGICAL SURVEY CIRCULAR 733 The United States Geological Survey in Alaska: Accomplishments During 1975 The United States Geological Survey in Alaska: Accomplishments During 1975 Edward H. Cobb, Editor GEOLOGICAL SURVEY CIRCULAR 733 7976 United States Department of the Interior THOMAS S. KLEPPE, Secretary Geological Survey V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Cobb, Edward H. The United States Geological Survey in Alaska. (Geological Survey Circular 733) Supt.ofDocs.no.: 119.4/2:733 1. United States Geological Survey 2. Geological research-Alaska. 3. Geology-Alaska- Bibliography. I. Cobb, Edward Huntington, 1916- II. United States Geological Survey HI. Series: United States Geological Survey Circular 733. QE75.C5no. 733[QE74] 557.3'08s[557.98] 76-608093 Free on application to Branch of Distribution, U.S. Geological Survey, 1200 South Eads Street, Arlington, VA 22202 CONTENTS Page Page Abstract _________________ _ 1 Summary of important results, 1975 Continued Summary of important results, 1975 _ 1 Northern Alaska __________________________ 16 Introduction ____________ _ 1 Seabed morphology adjacent to an "island" of Statewide __________. _ 1 grounded ice in the Arctic Ocean northwest of Computer files of Alaskan data, by M. Elizabeth Point Barrow, by L. J. Toimil and Arthur Yount _________________________ 1 Grantz _______________________ 16 Mineral resources of Alaska, by Edward H. Possible solid gas hydrate and natural gas de­ Cobb ___________________________ 2 posits beneath the continental slope of the New gravity map of Alaska, by David F. Beaufort Sea, by Arthur Grantz, GaryrBoucher, Bames ______________________ 2 and Olive Therese Whitney _____________ 17 Exploration geochemistry in Alaska, by G.
    [Show full text]