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Northern Sea Route Cargo Flows and Infrastructure- Present State And
Northern Sea Route Cargo Flows and Infrastructure – Present State and Future Potential By Claes Lykke Ragner FNI Report 13/2000 FRIDTJOF NANSENS INSTITUTT THE FRIDTJOF NANSEN INSTITUTE Tittel/Title Sider/Pages Northern Sea Route Cargo Flows and Infrastructure – Present 124 State and Future Potential Publikasjonstype/Publication Type Nummer/Number FNI Report 13/2000 Forfatter(e)/Author(s) ISBN Claes Lykke Ragner 82-7613-400-9 Program/Programme ISSN 0801-2431 Prosjekt/Project Sammendrag/Abstract The report assesses the Northern Sea Route’s commercial potential and economic importance, both as a transit route between Europe and Asia, and as an export route for oil, gas and other natural resources in the Russian Arctic. First, it conducts a survey of past and present Northern Sea Route (NSR) cargo flows. Then follow discussions of the route’s commercial potential as a transit route, as well as of its economic importance and relevance for each of the Russian Arctic regions. These discussions are summarized by estimates of what types and volumes of NSR cargoes that can realistically be expected in the period 2000-2015. This is then followed by a survey of the status quo of the NSR infrastructure (above all the ice-breakers, ice-class cargo vessels and ports), with estimates of its future capacity. Based on the estimated future NSR cargo potential, future NSR infrastructure requirements are calculated and compared with the estimated capacity in order to identify the main, future infrastructure bottlenecks for NSR operations. The information presented in the report is mainly compiled from data and research results that were published through the International Northern Sea Route Programme (INSROP) 1993-99, but considerable updates have been made using recent information, statistics and analyses from various sources. -
View of Theoretical Approaches 51
University of Alberta Caribou Hunting at Ice Patches: Seasonal Mobility and Long-term Land-Use in the Southwest Yukon By Vandy E. Bowyer A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Doctor of Philosophy Department of Anthropology © Vandy E. Bowyer Spring 2011 Edmonton, Alberta Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission. In memory of Tagish ABSTRACT Recently documented ice patch sites in the southwest Yukon are ideal for evaluating precontact hunter-gatherer land-use patterns in the western subarctic. Located in the alpine of the mountainous regions of the boreal forest, ice patches are associated with well preserved hunting equipment, caribou (Rangifer tarandus) dung and an abundance of faunal remains dating to over 8000 years ago. However, current models are inadequate for explaining caribou hunting at ice patches as they tend to emphasize large-scale communal hunts associated with latitudinal movements of caribou. Much less is known about the alititudinal movment of caribou and the associated hunting forays to ice patches in the alpine. -
High-Mountain Permafrost in the Austrian Alps (Europe)
HIGH-MOUNTAIN PERMAFROST IN THE AUSTRIAN ALPS (EUROPE) Gerhard Karl Lieb Institute of Geography University of Graz Heinrichstrasse 36 A-8010 Graz e-mail: [email protected] Abstract Permafrost research in the Austrian Alps (Eastern Alps) is based on a variety of methods, including at large scales, the measurement of the temperature of springs and of the base of winter snow cover, and at small scales, mainly an inventory of some 1450 rock glaciers. Taking all the information available into consideration, the lower limit of discontinuous permafrost is situated near 2500 m in most of the Austrian Alps. These results can be used for modelling the permafrost distribution within a geographical information system. Detailed investi- gations were carried out in the Doesen Valley (Hohe Tauern range) using additional methods, including several geophysical soundings. In this way, realistic estimates of certain permafrost characteristics and the volume of a large active rock glacier (some 15x106m3) were possible. This rock glacier has been chosen as a monitoring site to observe the effects of past and future climatic change. Introduction snow cover (BTS) and geophysical soundings, such as seismic, geoelectric, electromagnetic and ground pene- Although mountain permafrost in the Austrian Alps trating radar surveys have been published (survey and has caused construction problems and damage to buil- references in Lieb, 1996). The best results for mapping dings at several high-altitude locations, specific investi- the mere existence of permafrost were obtained by mea- gations of permafrost did not start until 1980. Since suring spring temperatures and BTS, both procedures then, studies of the distribution and certain characteris- being easily applicable and providing quite accurate tics of permafrost have been carried out at a number of interpretation. -
Late Wisconsin Climate Inferences from Rock Glaciers in South-Central
LateWisconsin climatic inlerences from rock glaciers in south-centraland west-central New Mexico andeast-central Arizona byJohn W. Blagbrough, P0 Box8063, Albuquerque, NewMexico 87198 Abstract Inactive rock glaciersof late Wisconsin age occur at seven sites in south-central and west-central New Mexico and in east-centralArizona. They are at the base of steep talus in the heads of canyons and ravines and have surfacefeatures indicating they are ice-cemented (permafrost) forms that moved by the flow of interstitial ice. The rock glaciersindicate zones of alpine permafrost with lower levels that rise from approximately 2,400m in the east region to 2,950 m in the west. Within the zones the mean annual temperaturewas below freezing, and the climatewas marked by much diurnal freezing and thawing resulting in the production of large volumes of talus in favorableterrain. The snow cover was thin and of short duration, which fa- vored ground freezing and cryofraction. The rock glaciers in the east region occur near the late Wisconsin 0'C air isotherm and implv that the mean annual temperature was depressedapproximately 7 to 8'C during a periglacial episodein the late Wisconsin.A dry continental climate with a seasonaldistribution of precipitation similar to that of the present probably prevailed, and timberline former timberlines. may have been depresseda minimum of 1,240m. The rise in elevation of the rock glaciersfrom east to west acrossthe region is attributed to greater snowfall in west-centralNew Mexico and east-centralArizona, which reducedthe inten- sity and depth of ground freezing near the late Wisconsin 0"C air isotherm. -
Russian Museums Visit More Than 80 Million Visitors, 1/3 of Who Are Visitors Under 18
Moscow 4 There are more than 3000 museums (and about 72 000 museum workers) in Russian Moscow region 92 Federation, not including school and company museums. Every year Russian museums visit more than 80 million visitors, 1/3 of who are visitors under 18 There are about 650 individual and institutional members in ICOM Russia. During two last St. Petersburg 117 years ICOM Russia membership was rapidly increasing more than 20% (or about 100 new members) a year Northwestern region 160 You will find the information aboutICOM Russia members in this book. All members (individual and institutional) are divided in two big groups – Museums which are institutional members of ICOM or are represented by individual members and Organizations. All the museums in this book are distributed by regional principle. Organizations are structured in profile groups Central region 192 Volga river region 224 Many thanks to all the museums who offered their help and assistance in the making of this collection South of Russia 258 Special thanks to Urals 270 Museum creation and consulting Culture heritage security in Russia with 3M(tm)Novec(tm)1230 Siberia and Far East 284 © ICOM Russia, 2012 Organizations 322 © K. Novokhatko, A. Gnedovsky, N. Kazantseva, O. Guzewska – compiling, translation, editing, 2012 [email protected] www.icom.org.ru © Leo Tolstoy museum-estate “Yasnaya Polyana”, design, 2012 Moscow MOSCOW A. N. SCRiAbiN MEMORiAl Capital of Russia. Major political, economic, cultural, scientific, religious, financial, educational, and transportation center of Russia and the continent MUSEUM Highlights: First reference to Moscow dates from 1147 when Moscow was already a pretty big town. -
Cold-Climate Landform Patterns in the Sudetes. Effects of Lithology, Relief and Glacial History
ACTA UNIVERSITATIS CAROLINAE 2000 GEOGRAPHICA, XXXV, SUPPLEMENTUM, PAG. 185–210 Cold-climate landform patterns in the Sudetes. Effects of lithology, relief and glacial history ANDRZEJ TRACZYK, PIOTR MIGOŃ University of Wrocław, Department of Geography, Wrocław, Poland ABSTRACT The Sudetes have the whole range of landforms and deposits, traditionally described as periglacial. These include blockfields and blockslopes, frost-riven cliffs, tors and cryoplanation terraces, solifluction mantles, rock glaciers, talus slopes and patterned ground and loess covers. This paper examines the influence, which lithology and structure, inherited relief and time may have had on their development. It appears that different rock types support different associations of cold climate landforms. Rock glaciers, blockfields and blockstreams develop on massive, well-jointed rocks. Cryogenic terraces, rock steps, patterned ground and heterogenic solifluction mantles are typical for most metamorphic rocks. No distinctive landforms occur on rocks breaking down through microgelivation. The variety of slope form is largely inherited from pre- Pleistocene times and includes convex-concave, stepped, pediment-like, gravitational rectilinear and concave free face-talus slopes. In spite of ubiquitous solifluction and permafrost creep no uniform characteristic ‘periglacial’ slope profile has been created. Mid-Pleistocene trimline has been identified on nunataks in the formerly glaciated part of the Sudetes and in their foreland. Hence it is proposed that rock-cut periglacial relief of the Sudetes is the cumulative effect of many successive cold periods during the Pleistocene and the last glacial period alone was of relatively minor importance. By contrast, slope cover deposits are usually of the Last Glacial age. Key words: cold-climate landforms, the Sudetes 1. -
Rocky Mountain National Park Lawn Lake Flood Interpretive Area (Elevation 8,640 Ft)
1 NCSS Conference 2001 Field Tour -- Colorado Rocky Mountains Wednesday, June 27, 2001 7:00 AM Depart Ft. Collins Marriott 8:30 Arrive Rocky Mountain National Park Lawn Lake Flood Interpretive Area (elevation 8,640 ft) 8:45 "Soil Survey of Rocky Mountain National Park" - Lee Neve, Soil Survey Project Leader, Natural Resources Conservation Service 9:00 "Correlation and Classification of the Soils" - Thomas Hahn, Soil Data Quality Specialist, MLRA Office 6, Natural Resources Conservation Service 9:15-9:30 "Interpretive Story of the Lawn Lake Flood" - Rocky Mountain National Park Interpretive Staff, National Park Service 10:00 Depart 10:45 Arrive Alpine Visitors Center (elevation 11,796 ft) 11:00 "Research Needs in the National Parks" - Pete Biggam, Soil Scientist, National Park Service 11:05 "Pedology and Biogeochemistry Research in Rocky Mountain National Park" - Dr. Eugene Kelly, Colorado State University 11:25 - 11:40 "Soil Features and Geologic Processes in the Alpine Tundra"- Mike Petersen and Tim Wheeler, Soil Scientists, Natural Resources Conservation Service Box Lunch 12:30 PM Depart 1:00 Arrive Many Parks Curve Interpretive Area (elevation 9,620 ft.) View of Valleys and Glacial Moraines, Photo Opportunity 1:30 Depart 3:00 Arrive Bobcat Gulch Fire Area, Arapaho-Roosevelt National Forest 3:10 "Fire History and Burned Area Emergency Rehabilitation Efforts" - Carl Chambers, U. S. Forest Service 3:40 "Involvement and Interaction With the Private Sector"- Todd Boldt; District Conservationist, Natural Resources Conservation Service 4:10 "Current Research on the Fire" - Colorado State University 4:45 Depart 6:00 Arrive Ft. Collins Marriott 2 3 Navigator’s Narrative Tim Wheeler Between the Fall River Visitors Center and the Lawn Lake Alluvial Debris Fan: This Park, or open grassy area, is called Horseshoe Park and is the tail end of the Park’s largest valley glacier. -
Glacial Processes and Landforms
Glacial Processes and Landforms I. INTRODUCTION A. Definitions 1. Glacier- a thick mass of flowing/moving ice a. glaciers originate on land from the compaction and recrystallization of snow, thus are generated in areas favored by a climate in which seasonal snow accumulation is greater than seasonal melting (1) polar regions (2) high altitude/mountainous regions 2. Snowfield- a region that displays a net annual accumulation of snow a. snowline- imaginary line defining the limits of snow accumulation in a snowfield. (1) above which continuous, positive snow cover 3. Water balance- in general the hydrologic cycle involves water evaporated from sea, carried to land, precipitation, water carried back to sea via rivers and underground a. water becomes locked up or frozen in glaciers, thus temporarily removed from the hydrologic cycle (1) thus in times of great accumulation of glacial ice, sea level would tend to be lower than in times of no glacial ice. II. FORMATION OF GLACIAL ICE A. Process: Formation of glacial ice: snow crystallizes from atmospheric moisture, accumulates on surface of earth. As snow is accumulated, snow crystals become compacted > in density, with air forced out of pack. 1. Snow accumulates seasonally: delicate frozen crystal structure a. Low density: ~0.1 gm/cu. cm b. Transformation: snow compaction, pressure solution of flakes, percolation of meltwater c. Freezing and recrystallization > density 2. Firn- compacted snow with D = 0.5D water a. With further compaction, D >, firn ---------ice. b. Crystal fabrics oriented and aligned under weight of compaction 3. Ice: compacted firn with density approaching 1 gm/cu. cm a. -
a Pleistocene Ice Sheet in the .' Northern Boulder Mountains
, A Pleistocene Ice Sheet in the .' Northern Boulder Mountains .< Jefferson, Powell, and Lewis and Clark Counties, Montana By EDWARD T. RUPPEL CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY BULLETIN 1141-G A descriptive report of the glacial geology in the northern part of the Boulder Mountains, Montana UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Abstract- _______-_-______-__-_--____--___________--____-_-_-______ G-1 Introduction. _ _____________________________________________________ 1 Summary of bedrock geology.___-___-____.____._-___._.__--__--_.___ 4 Surficial geology.._________________________________________________ 5 Northern Boulder Mountains ice sheet- ___-____-___.----_-_--_-__ 5 Glacial erosion.___________________________________________ 7 Glacial deposits.-______--_^______-________________________ 9 Age and regional relations of glaciation.___:______.____________ 11 Postglacial erosion.---___-_--________-___---___-_-------__---__ 13 Creep-and-solifluction deposits and stone-banked terrace deposits. 14 Frost-wedged rock waste and boulders of disintegration........ 15 Landslides._______________________________________________ 19 Bog and swamp deposits. _______________________________"___ 20 Age of mass-wasting deposits--....----...--___---__---_--_. 20 References cited..____________________________ _____________________ 21 ILLUSTRATIONS [Plates in pocket] PLATE 1. Ice coverage and flow, Basin quadrangle, Jefferson, Lewis and Clark, and Powell Counties, Mont. 2. Interpretations of Pleistocene and Recent history, Montana and adjacent areas. FIGURE 1. Inferred limits of northern Boulder Mountains ice sheet, G-2 2. Typical rounded topography along Continental Divide in northern part of Boulder Mountains---.-,-.------ ------- 3 3. -
Quaternary Deposits and Landscape Evolution of the Central Blue Ridge of Virginia
Geomorphology 56 (2003) 139–154 www.elsevier.com/locate/geomorph Quaternary deposits and landscape evolution of the central Blue Ridge of Virginia L. Scott Eatona,*, Benjamin A. Morganb, R. Craig Kochelc, Alan D. Howardd a Department of Geology and Environmental Science, James Madison University, Harrisonburg, VA 22807, USA b U.S. Geological Survey, Reston, VA 20192, USA c Department of Geology, Bucknell University, Lewisburg, PA 17837, USA d Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA Received 30 August 2002; received in revised form 15 December 2002; accepted 15 January 2003 Abstract A catastrophic storm that struck the central Virginia Blue Ridge Mountains in June 1995 delivered over 775 mm (30.5 in) of rain in 16 h. The deluge triggered more than 1000 slope failures; and stream channels and debris fans were deeply incised, exposing the stratigraphy of earlier mass movement and fluvial deposits. The synthesis of data obtained from detailed pollen studies and 39 radiometrically dated surficial deposits in the Rapidan basin gives new insights into Quaternary climatic change and landscape evolution of the central Blue Ridge Mountains. The oldest depositional landforms in the study area are fluvial terraces. Their deposits have weathering characteristics similar to both early Pleistocene and late Tertiary terrace surfaces located near the Fall Zone of Virginia. Terraces of similar ages are also present in nearby basins and suggest regional incision of streams in the area since early Pleistocene–late Tertiary time. The oldest debris-flow deposits in the study area are much older than Wisconsinan glaciation as indicated by 2.5YR colors, thick argillic horizons, and fully disintegrated granitic cobbles. -
Mineral Element Stocks in the Yedoma Domain: a First Assessment in Ice-Rich Permafrost Regions” by Arthur Monhonval Et Al
Interactive comment on “Mineral element stocks in the Yedoma domain: a first assessment in ice-rich permafrost regions” by Arthur Monhonval et al. Anonymous Referee #2 Received and published: 4 January 2021 RC= Reviewer comment ; AR= Authors response RC: I appreciate the efforts from the authors. I understand the authors created a valuable dataset for the mineral elements in the yedoma regions, and they also tried to calculated the storage of these elements. I have some comments for the authors to improve the quality of the manuscripts. We thank the reviewer for the valuable comments and suggestions to improve the manuscript. We have revised the manuscript accordingly. Please find the details in the responses to the following comments. RC1: When the authors introduce the stocks or storage, it is necessary to clarify the depth or thickness of yedoma. At least, the authors should explain the characteristics of yedoma. This is important because the potential readers will be confused about the depth and height in the dataset. AR : We agree that the choice of the thickness used to upscale to the whole Yedoma domain was not clear in the manuscript. Here, mineral element stocks are compared with C stocks using identical Yedoma domain deposits parameters (including thicknesses) like in Strauss et al., 2013 for deep permafrost carbon pool of the Yedoma region, i.e., a mean thickness of 19.6 meters deep in Yedoma deposits and 5.5 meters deep in Alas deposits. We have revised the manuscript to include that information (L 282):” Thickness used for mineral element stock estimations in Yedoma domain deposits are based on mean profile depths of the sampled Yedoma (n=19) and Alas (n=10) deposits (Table 3; Strauss et al., 2013). -
The Periglaciation of Great Britain Colin K
Cambridge University Press 978-0-521-31016-1 - The Periglaciation of Great Britain Colin K. Ballantyne and Charles Harris Index More information Index Abbot's Salford, Worcestershire, 53 aufeis, see also icings, 70 bimodal flows, see ground-ice slumps Aberayron, Dyfed, Wales, 104 Australia, 179, 261 Binbrook, Lincolnshire, 157 Aberystwyth, Dyfed, Wales, 128, 206, 207 Austrian Alps, 225 Bingham flow, 231 Acheulian hand axes, see hand axes avalanche activity, 219-22; 226-30, 236, 244, Birling Gap, Sussex, 102, 108 Achnasheen, NW Scotland, 233 295, 297 Black Mountain, Dyfed, 231, 234 active layer, see also seasonal thawing, 5, 27, avalanche boulder tongues, 220, 226, 295 Black Rock, Brighton, Sussex, 125, 126 35,41,42,114-18, 140,175 avalanche cones, 220, 226 Black Top Creek, EUesmere Island, Canada, 144 detachment slides, 115, 118, 276 avalanche impact pits, 226 Black Tors, Dartmoor, 178 glides, 118 avalanche landforms, 7, 8 blockfields, 8, 164-9, 171, 173-6, 180, 183, processes, 85-102 avalanche tongues, 227, 228 185,187,188,193,194 thickness, 107-9,281-2 avalanche-modified talus, 226-30 allochthonous, 173 Adwick-Le-Street, Yorkshire, 45, 53 Avon, 132, 134, 138, 139 autochthonous, 174, 182 aeolian, processes, see also wind action, 141, Avon Valley, 138 blockslopes, 173-6, 187, 190 155-60,161,255-67,296 Axe Valley, Devon, 103, 147 blockstreams, 173 aeolian sediments, see also loess and Bodmin Moor, Cornwall, 124, 168 coversands, 55, 96, 146-7, 150, 168, Badwell Ash, Essex, 101 Bohemian Highlands, 181 169, 257-60 Baffin Island, 103, 143,219