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Ramsar Sites in Order of Addition to the Ramsar List of Wetlands of International Importance
Ramsar sites in order of addition to the Ramsar List of Wetlands of International Importance RS# Country Site Name Desig’n Date 1 Australia Cobourg Peninsula 8-May-74 2 Finland Aspskär 28-May-74 3 Finland Söderskär and Långören 28-May-74 4 Finland Björkör and Lågskär 28-May-74 5 Finland Signilskär 28-May-74 6 Finland Valassaaret and Björkögrunden 28-May-74 7 Finland Krunnit 28-May-74 8 Finland Ruskis 28-May-74 9 Finland Viikki 28-May-74 10 Finland Suomujärvi - Patvinsuo 28-May-74 11 Finland Martimoaapa - Lumiaapa 28-May-74 12 Finland Koitilaiskaira 28-May-74 13 Norway Åkersvika 9-Jul-74 14 Sweden Falsterbo - Foteviken 5-Dec-74 15 Sweden Klingavälsån - Krankesjön 5-Dec-74 16 Sweden Helgeån 5-Dec-74 17 Sweden Ottenby 5-Dec-74 18 Sweden Öland, eastern coastal areas 5-Dec-74 19 Sweden Getterön 5-Dec-74 20 Sweden Store Mosse and Kävsjön 5-Dec-74 21 Sweden Gotland, east coast 5-Dec-74 22 Sweden Hornborgasjön 5-Dec-74 23 Sweden Tåkern 5-Dec-74 24 Sweden Kvismaren 5-Dec-74 25 Sweden Hjälstaviken 5-Dec-74 26 Sweden Ånnsjön 5-Dec-74 27 Sweden Gammelstadsviken 5-Dec-74 28 Sweden Persöfjärden 5-Dec-74 29 Sweden Tärnasjön 5-Dec-74 30 Sweden Tjålmejaure - Laisdalen 5-Dec-74 31 Sweden Laidaure 5-Dec-74 32 Sweden Sjaunja 5-Dec-74 33 Sweden Tavvavuoma 5-Dec-74 34 South Africa De Hoop Vlei 12-Mar-75 35 South Africa Barberspan 12-Mar-75 36 Iran, I. R. -
2007 UNEP-WCMC Global List of Transboundary Protected Areas Lysenko I., Besançon C., Savy C
2007 UNEP-WCMC Global List of Transboundary Protected Areas Lysenko I., Besançon C., Savy C. No TBPA Name Country Protected Areas Sitecode Category PA Size, km 2 TBPA Area, km 2 Ellesmere/Greenland 1 Canada Quttinirpaaq 300093 II 38148.00 Transboundary Complex Greenland Hochstetter Forland 67910 RAMSAR 1848.20 Kilen 67911 RAMSAR 512.80 North-East Greenland 2065 MAB-BR 972000.00 North-East Greenland 650 II 972000.00 1,008,470.17 2 Canada Ivvavik 100672 II 10170.00 Old Crow Flats 101594 IV 7697.47 Vuntut 100673 II 4400.00 United States Arctic 2904 IV 72843.42 Arctic 35361 Ia 32374.98 Yukon Flats 10543 IV 34925.13 146,824.27 Alaska-Yukon-British Columbia 3 Canada Atlin 4178 II 2326.95 Borderlands Atlin 65094 II 384.45 Chilkoot Trail Nhp 167269 Unset 122.65 Kluane 612 II 22015.00 Kluane Wildlife 18707 VI 6450.00 Kluane/Wrangell-St Elias/Glacier Bay/Tatshenshini-Alsek 12200 WHC 31595.00 Tatshenshini-Alsek 67406 Ib 9470.26 United States Admiralty Island 21243 Ib 3803.76 Chilkat 68395 II 24.46 Chilkat Bald Eagle 68396 II 198.38 Glacier Bay 1010 II 13045.50 Glacier Bay 22485 V 233.85 Glacier Bay 35382 Ib 10784.27 Glacier Bay-Admiralty Island Biosphere Reserve 11591 MAB-BR 15150.15 Kluane/Wrangell-St Elias/Glacier Bay/Tatshenshini-Alsek 2018 WHC 66796.48 Kootznoowoo 101220 Ib 3868.24 Malaspina Glacier 21555 III 3878.40 Mendenhall River 306286 Unset 14.57 Misty Fiords 21247 Ib 8675.10 Misty Fjords 13041 IV 4622.75 Point Bridge 68394 II 11.64 Russell Fiord 21249 Ib 1411.15 Stikine-LeConte 21252 Ib 1816.75 Tetlin 2956 IV 2833.07 Tongass 13038 VI 67404.09 Global List of Transboundary Protected Areas ©2007 UNEP-WCMC 1 of 78 No TBPA Name Country Protected Areas Sitecode Category PA Size, km 2 TBPA Area, km 2 Tracy Arm-Fords Terror 21254 Ib 2643.43 Wrangell-St Elias 1005 II 33820.14 Wrangell-St Elias 35387 Ib 36740.24 Wrangell-St. -
Geography, M.V
RUSSIAN GEOGRAPHICAL SOCIETY FACULTY OF GEOGRAPHY, M.V. LOMONOSOV MOSCOW STATE UNIVERSITY INSTITUTE OF GEOGRAPHY, RUSSIAN ACADEMY OF SCIENCES No. 01 [v. 04] 2011 GEOGRAPHY ENVIRONMENT SUSTAINABILITY ggi111.inddi111.indd 1 003.08.20113.08.2011 114:38:054:38:05 EDITORIAL BOARD EDITORS-IN-CHIEF: Kasimov Nikolay S. Kotlyakov Vladimir M. Vandermotten Christian M.V. Lomonosov Moscow State Russian Academy of Sciences Université Libre de Bruxelles 01|2011 University, Faculty of Geography Institute of Geography Belgique Russia Russia 2 GES Tikunov Vladimir S. (Secretary-General) Kroonenberg Salomon, M.V. Lomonosov Moscow State University, Delft University of Technology Faculty of Geography, Russia. Department of Applied Earth Sciences, Babaev Agadzhan G. The Netherlands Turkmenistan Academy of Sciences, O’Loughlin John Institute of deserts, Turkmenistan University of Colorado at Boulder, Baklanov Petr Ya. Institute of Behavioral Sciences, USA Russian Academy of Sciences, Malkhazova Svetlana M. Pacific Institute of Geography, Russia M.V. Lomonosov Moscow State University, Baume Otfried, Faculty of Geography, Russia Ludwig Maximilians Universitat Munchen, Mamedov Ramiz Institut fur Geographie, Germany Baku State University, Chalkley Brian Faculty of Geography, Azerbaijan University of Plymouth, UK Mironenko Nikolay S. Dmitriev Vasily V. M.V. Lomonosov Moscow State University, Sankt-Petersburg State University, Faculty of Faculty of Geography, Russia. Geography and Geoecology, Russia Palacio-Prieto Jose Dobrolubov Sergey A. National Autonomous University of Mexico, M.V. Lomonosov Moscow State University, Institute of Geography, Mexico Faculty of Geography, Russia Palagiano Cosimo, D’yakonov Kirill N. Universita degli Studi di Roma “La Sapienza”, M.V. Lomonosov Moscow State University, Instituto di Geografia, Italy Faculty of Geography, Russia Richling Andrzej Gritsay Olga V. -
Icing Mound on Sadlerochit River, Alaska
Short Papers and Notes ICING MOUND ON SADLERO- Sadlerochithas emerged from the CHIT RIVER, ALASKA* mountains, has arelatively low gra- dient and flows in a broad, braided bed Icing mounds- small to large domes, characterized by manyanastomosing mounds,and ridges resulting from an shallowchannels separated by bare, upwardarching of soiland ice asso- gravelly and bouldery bars (Fig. 2). AS ciated with fields of aufeis - have been is characteristic of all riversof the Arc- described in detailfor Siberia1. Icing tic Slope, the change from a single deep mounds have also been mentioned brief- channel to a braided pattern of many ly inconnection with aufeisfields in shallow channels allows the formation Alaskaby Leffigwell (ref. 2, p. 158) of an aufeis field every year near the and Taber (ref. 3, p. 1528; ref. 4, p. 249), mountain front. During the fall the but there is little descriptive literature shallow channels freeze early and the on this phenomenon in theNorth Amer- obstruction of the resulting ice causes ican Arctic. One such icing mound was the river to overflow its bars;this over- examined briefly by the author on June flow then freezes and by repeated freez- 25,1959 during the course of a trip down ing,overflow and freezingsuccessive the SadlerochitRiver in northeastern layers of ice are built up toform an Alaska (Fig. 1). aufeis field. Another factor contributing Fig. 1. Locationmap, Arctic Slope, Alaska. The SadlerochitRiver rises in the to the formation of large aufeis fields is Franklin Mountains of the eastern a source of water that persists for some Brooks Range and flows northwardin a time after freezingbegins. -
“Mongolia's Network of Managed Resource
GOVERNMENT OF MINISTRY OF MONGOLIA ENVIRONMENT AND TOURISM “MONGOLIA’S NETWORK OF MANAGED RESOURCE PROTECTED AREAS” МОN/13/303 PROJECT THE PROJECT GOAL: The goal is to ensure integrity of Mongolia’s diverse ecosystems to secure viability of nation’s globally significant biodiversity. IMPLEMENTING PARTNERS: • Ministry of the Environment and Tourism THE PROJECT OBJECTIVE: • United Nations Development Program The project objective is to catalyze strategic expansion of Mongolia’s FUNDING: protected areas system through estab- • Global Environmental Facility – 1,309,091 $ lishment of a network of community • UN Development Program – 200,000 $ conservation areas covering • Ministry of the Environment and Tourism -500,000 $ (in-kind) under-represented terrestrial ecosystems. PROGRAMME PERIOD: TOTAL BUDGET: 2013-2018 1,509,091 $ PROJECT IMPLEMENTATION SITES: 1. “Gulzat” LPA (Uvs aimag, Bukhmurun soums) 203,316 ha 2. “Khavtgar” LPA (Batshireet soum of Khentii aimag) 104,900 ha 3. “Tumenkhan-shalz” LPA (Tsgaaan ovoo, Bayan-uul soums of Dornod aimag, and Norovlin soum of Khentii aimag) 374,499 ha Expanded area under local protection by 600 thousand ha: ACHIEVEMENTS AND OUTPUTS: Expanded area under local protection by about 600.0 thousand hectare and created ecological corridor areas Created under local protection, the ecological corridors/ connectivity support wildlife movement between the state and local pro- 1 tected areas in west and east regions. These are а. 433,9 thousand ha б. 278.9 thousand ha Total of 433,9 thousand ha area, a migration and calv- Argali sheep migration and distribution area of ing land of gazelle located between Tosonkhulstai NR 284.4 thousand ha, that connects Tsagaan shuvuut and Onon Balj NP in Bayan-uul, Tsagaan ovoo and Nor- and Turgen mountain SPAs in Sagil and Buhmurun ovlin soums of Dornod and Khenti aimags; soums of Uvs aimag. -
Mesoproterozoic Frost Action at the Base of the Svinsaga Formation 291
NORWEGIAN JOURNAL OF GEOLOGY Mesoproterozoic frost action at the base of the Svinsaga Formation 291 Mesoproterozoic frost action at the base of the Svinsaga Formation, central Telemark, South Norway Juha Köykkä & Kauko Laajoki Köykkä, J. & Laajoki, K. 2009: Mesoproterozoic frost action ath the base of the Svinsaga Formation, central telemark, South Norway. Norwegain Journal of Geology, vol 89, pp 291-303. Trondheim 2009, ISSN 029-196X. The Mesoproterozoic Svinsaga Formation (SF) in central Telemark, South Norway, was unconformably deposited after ca. 1.347 Ga on the quartz arenite of the upper member of the Brattefjell Formation (UB), which is part of the Vindeggen Group. The unconformity is marked by a fracture zone a few meters thick developed in the UB quartz arenite. The lower part of the fracture zone, which contains sparse and closed fractures, and microfractures, grades upwards into a system of wider and mostly random oriented fractures and fracture patterns. The fractures are filled with mudstone. The fracture zone is overlain by several meters of in situ SF breccia, in which the fragments consist solely of the UB quartz arenite. The in situ breccia gradually grades into a basal breccia and clast- or matrix-supported conglomerates. The SF conglomerate beds contain solitary quartz arenite fragments and blocks up to 9.0 m3 that were derived from the UB. The fractures, fracture patterns, and microfractures in the UB quartz arenite and shattered quartz arenite fragments in the in situ SF breccia are ascribed to in situ fracturing, brecciation, and the accumulation of slightly moved blocks in a cold climate. -
Historical and Recent Aufeis, the Indigirka River Basin (Russia)
1 Historical and recent aufeis, the Indigirka river basin 2 (Russia) 3 *Olga Makarieva1,2,, Andrey Shikhov3, Nataliia Nesterova2,4, Andrey Ostashov2 4 1Melnikov Permafrost Institute of RAS, Yakutsk 5 2St. Petersburg State University, St. Petersburg 6 3Perm State University, Perm 7 4State Hydrological institute, St. Petersburg 8 RUSSIA 9 *[email protected] 10 Abstract: A detailed spatial geodatabase of aufeis (or naleds in Russian) within the 11 Indigirka River watershed (305 000 km2), Russia, was compiled from historical Russian 12 publications (year 1958), topographic maps (years 1970–1980’s), and Landsat images (year 13 2013-2017). Identification of aufeis by late-spring Landsat images was performed with a semi- 14 automated approach according to Normalized Difference Snow Index (NDSI) and additional 15 data. After this, a cross-reference index was set for each aufeis, to link and compare historical 16 and satellite-based aufeis data sets. 17 The aufeis coverage varies from 0.26 to 1.15% in different sub-basins within the 18 Indigirka River watershed. The digitized historical archive (Cadastre, 1958) contains the 19 coordinates and characteristics of 896 aufeis with total area of 2064 km2. The Landsat-based 20 dataset included 1213 aufeis with a total area of 1287 km2. Accordingly, the satellite-derived 21 total aufeis area is 1.6 times less than the Cadastre (1958) dataset. However, more than 600 22 aufeis identified from Landsat images are missing in the Cadastre (1958) archive. It is 23 therefore possible that the conditions for aufeis formation may have changed from the mid- 24 20th century to the present. -
Sess Report 2018
SESS REPORT 2018 The State of Environmental Science in Svalbard – an annual report Xxx 1 SESS report 2018 The State of Environmental Science in Svalbard – an annual report ISSN 2535-6321 ISBN 978-82-691528-0-7 Publisher: Svalbard Integrated Arctic Earth Observing System (SIOS) Editors: Elizabeth Orr, Georg Hansen, Hanna Lappalainen, Christiane Hübner, Heikki Lihavainen Editor popular science summaries: Janet Holmén Layout: Melkeveien designkontor, Oslo Citation: Orr et al (eds) 2019: SESS report 2018, Longyearbyen, Svalbard Integrated Arctic Earth Observing System The report is published as electronic document, available from SIOS web site www.sios-svalbard.org/SESSreport Contents Foreword .................................................................................................................................................4 Authors from following institutions contributed to this report ...................................................6 Summaries for stakeholders ................................................................................................................8 Permafrost thermal snapshot and active-layer thickness in Svalbard 2016–2017 .................................................................................................................... 26 Microbial activity monitoring by the Integrated Arctic Earth Observing System (MamSIOS) .................................................................................. 48 Snow research in Svalbard: current status and knowledge gaps ............................................ -
RCN #33 21/8/03 13:57 Page 1
RCN #33 21/8/03 13:57 Page 1 No. 33 Summer 2003 Special issue: The Transformation of Protected Areas in Russia A Ten-Year Review PROMOTING BIODIVERSITY CONSERVATION IN RUSSIA AND THROUGHOUT NORTHERN EURASIA RCN #33 21/8/03 13:57 Page 2 CONTENTS CONTENTS Voice from the Wild (Letter from the Editors)......................................1 Ten Years of Teaching and Learning in Bolshaya Kokshaga Zapovednik ...............................................................24 BY WAY OF AN INTRODUCTION The Formation of Regional Associations A Brief History of Modern Russian Nature Reserves..........................2 of Protected Areas........................................................................................................27 A Glossary of Russian Protected Areas...........................................................3 The Growth of Regional Nature Protection: A Case Study from the Orlovskaya Oblast ..............................................29 THE PAST TEN YEARS: Making Friends beyond Boundaries.............................................................30 TRENDS AND CASE STUDIES A Spotlight on Kerzhensky Zapovednik...................................................32 Geographic Development ........................................................................................5 Ecotourism in Protected Areas: Problems and Possibilities......34 Legal Developments in Nature Protection.................................................7 A LOOK TO THE FUTURE Financing Zapovedniks ...........................................................................................10 -
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. -
Hydrologic and Mass-Movement Hazards Near Mccarthy Wrangell-St
Hydrologic and Mass-Movement Hazards near McCarthy Wrangell-St. Elias National Park and Preserve, Alaska By Stanley H. Jones and Roy L Glass U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 93-4078 Prepared in cooperation with the NATIONAL PARK SERVICE Anchorage, Alaska 1993 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY ROBERT M. HIRSCH, Acting Director For additional information write to: Copies of this report may be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Earth Science Information Center 4230 University Drive, Suite 201 Open-File Reports Section Anchorage, Alaska 99508-4664 Box 25286, MS 517 Denver Federal Center Denver, Colorado 80225 CONTENTS Abstract ................................................................ 1 Introduction.............................................................. 1 Purpose and scope..................................................... 2 Acknowledgments..................................................... 2 Hydrology and climate...................................................... 3 Geology and geologic hazards................................................ 5 Bedrock............................................................. 5 Unconsolidated materials ............................................... 7 Alluvial and glacial deposits......................................... 7 Moraines........................................................ 7 Landslides....................................................... 7 Talus.......................................................... -
The Dynamics and Mass Budget of Aretic Glaciers
DA NM ARKS OG GRØN L ANDS GEO L OG I SKE UNDERSØGELSE RAP P ORT 2013/3 The Dynamics and Mass Budget of Aretic Glaciers Abstracts, IASC Network of Aretic Glaciology, 9 - 12 January 2012, Zieleniec (Poland) A. P. Ahlstrøm, C. Tijm-Reijmer & M. Sharp (eds) • GEOLOGICAL SURVEY OF D EN MARK AND GREENLAND DANISH MINISTAV OF CLIMATE, ENEAGY AND BUILDING ~ G E U S DANMARKS OG GRØNLANDS GEOLOGISKE UNDERSØGELSE RAPPORT 201 3 / 3 The Dynamics and Mass Budget of Arctic Glaciers Abstracts, IASC Network of Arctic Glaciology, 9 - 12 January 2012, Zieleniec (Poland) A. P. Ahlstrøm, C. Tijm-Reijmer & M. Sharp (eds) GEOLOGICAL SURVEY OF DENMARK AND GREENLAND DANISH MINISTRY OF CLIMATE, ENERGY AND BUILDING Indhold Preface 5 Programme 6 List of participants 11 Minutes from a special session on tidewater glaciers research in the Arctic 14 Abstracts 17 Seasonal and multi-year fluctuations of tidewater glaciers cliffson Southern Spitsbergen 18 Recent changes in elevation across the Devon Ice Cap, Canada 19 Estimation of iceberg to the Hansbukta (Southern Spitsbergen) based on time-lapse photos 20 Seasonal and interannual velocity variations of two outlet glaciers of Austfonna, Svalbard, inferred by continuous GPS measurements 21 Discharge from the Werenskiold Glacier catchment based upon measurements and surface ablation in summer 2011 22 The mass balance of Austfonna Ice Cap, 2004-2010 23 Overview on radon measurements in glacier meltwater 24 Permafrost distribution in coastal zone in Hornsund (Southern Spitsbergen) 25 Glacial environment of De Long Archipelago