A Changing Climate: Consequences S K a for Subsistence Communities ______18 L a the Frozen Past of Wrangell-St
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Post-Glacial Sea-Level Change Along the Pacific Coast of North America Dan H
University of Washington Tacoma UW Tacoma Digital Commons SIAS Faculty Publications School of Interdisciplinary Arts and Sciences 8-1-2014 Post-glacial sea-level change along the Pacific coast of North America Dan H. Shugar University of Washington Tacoma, [email protected] Ian J. Walker Olav B. Lian Jordan BR Eamer Christina Neudorf See next page for additional authors Follow this and additional works at: https://digitalcommons.tacoma.uw.edu/ias_pub Recommended Citation Shugar, Dan H.; Walker, Ian J.; Lian, Olav B.; Eamer, Jordan BR; Neudorf, Christina; McLaren, Duncan; and Fedje, Daryl, "Post-glacial sea-level change along the Pacific oc ast of North America" (2014). SIAS Faculty Publications. 339. https://digitalcommons.tacoma.uw.edu/ias_pub/339 This Article is brought to you for free and open access by the School of Interdisciplinary Arts and Sciences at UW Tacoma Digital Commons. It has been accepted for inclusion in SIAS Faculty Publications by an authorized administrator of UW Tacoma Digital Commons. Authors Dan H. Shugar, Ian J. Walker, Olav B. Lian, Jordan BR Eamer, Christina Neudorf, Duncan McLaren, and Daryl Fedje This article is available at UW Tacoma Digital Commons: https://digitalcommons.tacoma.uw.edu/ias_pub/339 1 Post-glacial sea-level change along the Pacific coast of North 2 America 3 Dan H. Shugar1,*, Ian J. Walker1, Olav B. Lian2, Jordan B.R. Eamer1, Christina 4 Neudorf2,4, Duncan McLaren3,4, Daryl Fedje3,4 5 6 1Coastal Erosion & Dune Dynamics Laboratory, Department of Geography, 7 University of Victoria, Victoria, BC, -
Denali National Park and Preserve
National Park Service U.S. Department of the Interior Natural Resource Program Center Water Resources Stewardship Report Denali National Park and Preserve Natural Resource Technical Report NPS/NRPC/WRD/NRTR—2007/051 ON THE COVER Photograph: Toklat River, Denali National Park and Preserve (Guy Adema, 2007) Water Resources Stewardship Report Denali National Park and Preserve Natural Resource Technical Report NPS/NRPC/WRD/NRTR-2007/051 Kenneth F. Karle, P.E. Hydraulic Mapping and Modeling P.O. Box 181 Denali Park, Alaska 99755 September 2007 U.S. Department of the Interior National Park Service Natural Resources Program Center Fort Collins, Colorado The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer- reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. The Natural Resources Technical Reports series is used to disseminate the peer-reviewed results of scientific studies in the physical, biological, and social sciences for both the advancement of science and the achievement of the National Park Service’s mission. The reports provide contributors with a forum for displaying comprehensive data that are often deleted from journals because of page limitations. Current examples of such reports include the results of research that addresses natural resource management issues; natural resource inventory and monitoring activities; resource assessment reports; scientific literature reviews; and peer reviewed proceedings of technical workshops, conferences, or symposia. -
Highlights for Fiscal Year 2013: Denali National Park
Highlights for FY 2013 Denali National Park and Preserve (* indicates action items for A Call to Action or the park’s strategic plan) This year was one of changes and challenges, including from the weather. The changes started at the top, with the arrival of new Superintendent Don Striker in January 2013. He drove across the country to Alaska from New River Gorge National River in West Virginia, where he had been the superintendent for five years. He also served as superintendent of Mount Rushmore National Memorial (South Dakota) and Fort Clatsop National Memorial (Oregon) and as special assistant to the Comptroller of the National Park Service. Some of the challenges that will be on his plate – implementing the Vehicle Management Plan, re-bidding the main concession contract, and continuing to work on a variety of wildlife issues with the State of Alaska. Don meets Skeeter, one of the park’s sled dogs The park and its partners celebrated a significant milestone, the centennial of the first summit of Mt. McKinley, with several activities and events. On June 7, 1913, four men stood on the top of Mt. McKinley, or Denali as it was called by the native Koyukon Athabaskans, for the first time. By achieving the summit of the highest peak in North America, Walter Harper, Harry Karstens, Hudson Stuck, and Robert Tatum made history. Karstens would continue to have an association with the mountain and the land around it by becoming the first Superintendent of the fledgling Mt. McKinley National Park in 1921. *A speaker series featuring presentations by five Alaskan mountaineers and historians on significant Denali mountaineering expeditions, premiered on June 7thwith an illustrated talk on the 1913 Ascent of Mt. -
Rockaway Resiliency Projects & Fema Funding
ROCKAWAY RESILIENCY PROJECTS & FEMA FUNDING PS/MS 42 Robert Vernam School December 12, 2016 TONIGHT’S MEETING . Anticipate excess Rockaway Boardwalk funds . Mayoral commitment to use funds for resiliency projects in Rockaways . Submitted Alternate Projects need to be approved by FEMA prior to the completion of Rockaway boardwalk (Anticipated completion date is Memorial Day 2017) TONIGHT . Present potential projects . Get your feedback! 2 ROCKAWAYS RECOVERY & RESILIENCY INVESTMENTS 3 PROPOSED USACE ROCKAWAY REFORMULATION 4 FEMA SECTION 428 PILOT PROGRAM . The FEMA 428 program allows for anticipated savings from a FEMA 428 project to be applied to Alternate Projects . NYS and FEMA determines eligibility of projects and approves use of underrun funding FEMA ELIGIBILITY ELIGIBLE NOT ELIGIBLE . Raised Shoreline Work . Landscaping projects: . Parks and Recreational . New Trees Facilities . Plantings . Buildings . Lawns . Elevation of Structures . Buyouts . Engineered Natural . Studies Structures 5 PROJECT CONSIDERATIONS Projects build off existing studies: . HPD Resilient Edgemere Initiative . Rockaway Parks Conceptual Plan Project Considerations: Resiliency . Protect neighborhoods from tidal flooding . Environmental restoration . Improve access/activate waterfront Recovery . Restore/replace facilities directly lost during Hurricane Sandy Community . Provide recreational or community CONSIDERATIONS amenities/priorities Does not meet Public Feedback Partially meets Fully meets 6 PROJECT SOURCE Rockaway Parks Conceptual Plan Resilient Edgemere Plan NYC Parks Projects presented geographically east to west 7 PROJECT #1 BAYSWATER PARK Renovate community park $50M - $60M Projects presented geographically east to west 8 PROJECT #1 BAYSWATER PARK Existing Bayswater Park Resiliency Recovery Community 9 PROJECT #1 BAYSWATER PARK Resiliency Features: . Raised Berm with Trail . Permeable Pavement . Stormwater Retention . Shoreline Bank Stabilization . Wetland and Coastal Forest Restoration Resiliency Recovery Community 10 PROJECT #1 BAYSWATER PARK Community Features: . -
Alaska Park Science Anchorage, Alaska
National Park Service U.S. Department of Interior Alaska Regional Office Alaska Park Science Anchorage, Alaska PROCEEDINGS OF THE CentrCentralal AlaskAlaskaa PParkark SciencSciencee SymposiumSymposium SeptemberSeptember 12-14,12-14, 2006 2006 Denali Park, Alaska Volume 6, Issue 2 Parks featured in this Table of Contents issue of Alaska Park Science Keynote Address Alaska Parks in a Warming Climate: Conserving a Changing Future __________________________ 6 S K A Yukon-Charley Rivers Synthesis L A National Preserve Crossing Boundaries in Changing Environment: Norton Sound A A Synthesis __________________________________________12 Monitoring a Changing Climate Denali National Park and Preserve Long-term Air Quality Monitoring Wrangell-St. Elias in Denali National Park and Preserve __________________18 National Park and Preserve Monitoring Seasonal and Long-term Climate Changes and Extremes in the Central Alaska Network__________ 22 Physical Environment and Sciences Glacier Monitoring in Denali National Park and Preserve ________________________________________26 Applications of the Soil-Ecological Survey of Denali National Park and Preserve__________________31 Bristol Bay Gulf of Alaska Using Radiocarbon to Detect Change in Ecosystem Carbon Cycling in Response to Permafrost Thawing____34 A Baseline Study of Permafrost in the Toklat Basin, Denali National Park and Preserve ____________________37 Dinosauria and Fossil Aves Footprints from the Lower Cantwell Formation (latest Cretaceous), Denali National Park and Preserve ____________________41 -
Glaciomarine Deltas of Maine and Their Relation to Late Pleistocene-Holocene Crustal Movements
Maine Geological Survey Neotcctonics of Maine 1989 Glaciomarine Deltas of Maine and Their Relation to Late Pleistocene-Holocene Crustal Movements Woodrow B. Thompson Maine Geological Survey Augusta, Maine 04333 Kristine J . Crossen Geology Department University ofAlaska Anchorage, Alaska 99507 Harold W. Borns, Jr. Institute for Quaternary Studies University of Maine Orono, Maine 04469 Bjorn G. Andersen University of Oslo Oslo, Norway ABSTRACT The deglaciation of southern Maine in late Wisconsinan time was accompanied by marine submergence of the isostatically-depressed coastal lowland. Glacial meltwater streams deposited over 100 Gilbert-type deltas into the sea during the transgressive phase of submergence, between about 14,000 and 13,000 yr B.P. These deltas were deposited either in contact with the ice margin or very close to it. They are classified into four categories based on depositional environment: ice-contact deltas (39% ), esker-fed ice-contact deltas (30% ), leeside deltas (26% ), and distal outwash deltas (5% ). Most of the deltas for which subsurface data are available accumulated in water less than 80 m deep, and the ice-contact deltas are believed to have formed along a grounded tidewater-glacier margin. Bedrock strike ridges and other hills slowed the retreat of the ice margin, causing brief stillstands during which deltas were deposited adjacent to these topographic highs. The sequence of glaciomarine deltas in Maine probably formed when the transgressing sea had reached its maximum depth and relative sea level was beginning to fall in response to isostatic crustal uplift. The elevations of the contacts between the topset and foreset beds of 65 deltas in Maine and New Brunswick were measured in order to locate the positions of sea level to which the deltas were graded. -
Raised Shoreline Phenomena and Postglacial Emergence in South
Document généré le 26 sept. 2021 07:54 Géographie physique et Quaternaire Raised Shoreline Phenomena and Postglacial Emergence in South-Central Newfoundland Les lignes de rivage soulevées et l'émersion postglaciaire au centre-sud de Terre-Neuve Вoзвышeнный peльeф пoбepeжья и пocлeлeдникoвый пpиpocт cуши нa южном подерeжьe цeнтpaльнoгo Hьюфaундлeндa C. M. Tucker, D. A. Leckie et S. B. McCann Volume 36, numéro 1-2, 1982 Résumé de l'article Dans la région de Burin-Hermitage, au sud de Terre-Neuve, on retrouve deux URI : https://id.erudit.org/iderudit/032475ar types de lignes de rivage marines soulevées: des plates-formes marines DOI : https://doi.org/10.7202/032475ar entaillées dans la roche en place ainsi que des terrasses et des plages développées dans des matériaux meubles. La plupart des plates-formes datent Aller au sommaire du numéro d'avant le Wisconsinien inférieur. Une ligne de rivage rocheuse horizontale située à 4,5 ± 1,5 m, qu'on retrouve à travers la région, fut probablement formée au cours du dernier interglaciaire. Des deltas soulevés et des épandages Éditeur(s) fluvioglaciaires côtiers, associés à des plans d'eau marins qui marquent la limite marine du Wisconsinien inférieur dans la partie nord de la zone d'étude, Les Presses de l'Université de Montréal sont mis en relation avec des terrasses et des plages soulevées existant plus au sud dans la péninsule de Burin. L'altitude de ces formes sert à établir le mode ISSN régional d'émersion post-glaciaire. Il s'est produit une emersion de plus de 30 m dans le nord-ouest, alors que l'extrême-sud de la région est en phase de 0705-7199 (imprimé) submersion. -
Deglacial Patterns and Ice-Sheet Dynamics in the Fjords of Southern Nordland, Norway
NORWEGIAN JOURNAL OF GEOLOGY Vol 98 Nr. 4 https://dx.doi.org/10.17850/njg98-4-07 Deglacial patterns and ice-sheet dynamics in the fjords of southern Nordland, Norway Fredrik Høgaas1, Lars Olsen1, Lina Gislefoss1, Oddvar Longva1, Anders Romundset1 & Harald Sveian1 1Geological Survey of Norway, P.O. Box 6315 Torgarden, NO–7491 Trondheim, Norway. E-mail corresponding author (Fredrik Høgaas): [email protected] This paper presents results from glacial geomorphology mapping in and adjacent to Velfjorden and Ursfjorden in the southern Nordland region of Norway. Submarine and terrestrial landforms were studied and mapped using high-resolution multibeam bathymetric and airborne LiDAR data, in addition to reconnaissance in the field. The work unites ice-marginal deposits related to the established Tautra and Tjøtta glacial events which took place during the Younger Dryas (YD) chronozone. In Ursfjorden, an outlet glacier deposited a c. 100 m-high terminal moraine, whereas moraine ridges and a large sedimentary wedge were deposited in the inner part of Velfjorden. Highly elongated subglacial bedforms located inside the ice-marginal landforms reveal that the fjords were occupied by fast-flowing ice streams during YD. Eighteen new radiocarbon dates from the region, along with twelve recalibrated dates from previous studies, provide time-constraints for ice-sheet configuration and dynamics during deglaciation. Radiocarbon dates suggest that the outer coastal islands became ice-free prior to 14 cal ka BP. Glacially overridden shell-rich units dated to the Allerød Interstadial indicate that the YD ice sheet readvanced at least 5 km before depositing the terminal moraine in Ursfjorden. The ages of shells found near the distinct, regionally correlative, YD raised shoreline indicate that the glacial readvance culminated around early to mid-YD. -
MOUNT Mckinley I Adolph Murie
I (Ie De/;,;;I; D·· 3g>' I \N ITHE :.Tnf,';AGt:: I GRIZZLIES OF !MOUNT McKINLEY I Adolph Murie I I I I I •I I I II I ,I I' I' Ii I I I •I I I Ii I I I I r THE GRIZZLIES OF I MOUNT McKINLEY I I I I I •I I PlEASE RETURN TO: TECHNICAL INfORMATION CENTER I f1r,}lVER SiRV~r.r Gs:t.!TER ON ;j1,l1uNAl PM~ :../,,;ICE I -------- --- For sale h~' the Super!u!p!u]eut of Documents, U.S. Goyernment Printing Office I Washing-ton. D.C. 20402 I I '1I I I I I I I I .1I Adolph Murie on Muldrow Glacier, 1939. I I I I , II I I' I I I THE GRIZZLIES I OF r MOUNT McKINLEY I ,I Adolph Murie I ,I I. I Scientific Monograph Series No. 14 'It I I I U.S. Department of the Interior National Park Service Washington, D.C. I 1981 I I I As the Nation's principal conservation agency, the Department of the,I Interior has responsibility for most ofour nationally owned public lands and natural resources. This includes fostering the wisest use ofour land and water resources, protecting our fish and wildlife, preserving the environmental and cultural values of our national parks and historical places, and providing for the enjoyment of life through outdoor recre- I ation. The Department assesses our energy and mineral resources and works to assure that their development is in the best interests of all our people. The Department also has a major responsibility for American Indian reservation communities and for people who live in Island Ter- I ritories under U.S. -
The Mount Eielson District Alaska
Please do not destroy or throw away this publication. If you have no further use for it, write to the Geological Survey at Washington and ask for a frank to return it UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 849 D THE MOUNT EIELSON DISTRICT ALASKA BY JOHN C. REED Investigations in Alaska Railroad belt, 1931 ( Pages 231-287) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1933 For sale by the Superintendent of Documents, Washington, D.C. - Pricf 25 cents CONTENTS Page Foreword, by Philip S. Smith.______________________________________ v Abstract.._._-_.-_____.___-______---_--_---_-_______._-________ 231 Introduction__________________________-__-_-_-_____._____________.: 231 . Arrangement with the Alaska Railroad._--_--_-_--...:_-_._.--__ 231 Nature of field work..__________________________________... 232 Acknowledgments..._._.-__-_.-_-_----------_-.------.--.__-_. 232 Summary of previous work..___._-_.__-_-_...__._....._._____._ 232 Geography.............._._._._._.-._--_-_---.-.---....__...._._. 233 Location and extent.___-___,__-_---___-__--_-________-________ 233 Routes of approach....__.-_..-_-.---__.__---.--....____._..-_- 234 Topography.................---.-..-.-----------------.------ 234 Relief _________________________________________________ 234 Drainage.-.._.._.___._.__.-._._--.-.-__._-._.__.._._... 238 Climate.---.__________________...................__ 240 Vegetation--.._-____-_____.____._-___._--.._-_-..________.__. 244 Wild animals.__________.__.--.__-._.----._a-.--_.-------_.____ 244 Population._-.____-_.___----_-----__-___.--_--__-_.-_--.___. -
Pumice in the North Atlantic
Ocean-transported pumice in the North Atlantic Anthony Newton PhD University of Edinburgh 1999 Declaration I, Anthony Newton hereby declare that the work contained herein is my own and has not previously been presented for examination. Any contributions by others is acknowledged in the text. September 1999 ii For Keith Newton 1930-1984 iii “Some days we would pass through pumice lying in ridges, each piece uniformly the size and appearance of a bath sponge, then again we should pass through perfect fields of small yellow pumice spread evenly over the surface just for all the world like a green field of grass covered all over with buttercups, and the undulation of the swell of the trade wind produced an indescribably pretty appearance.” (Reeves, 1884). iv Abstract The overall aims of this study are to identify the sources of the widespread Holocene pumice deposits found along the coasts of the North Atlantic region and establish the ages of the source eruptions. In order to tackle this, it is necessary to determine whether it is possible to “fingerprint” the pumice of individual eruptions and link ocean-transported material with the established tephrochronological framework based on the stratigraphy of airfall deposits. Over 1500 electron probe microanalyses and over 200 Secondary Ion Mass Spectrometry analyses have been undertaken on pumice and tephra samples. These are the first high quality grain specific analyses carried out on ocean-transported pumice in the North Atlantic. Current knowledge of the extent of pumice distribution in the North Atlantic region is assessed for both shoreline (natural) and archaeological contexts.