Table 1. Summary of Major Metallogenic Belts for Northeast Asia
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List of Rivers of Mongolia
Sl. No River Name Russian Name Draining Into 1 Yenisei River Russia Arctic Ocean 2 Angara River Russia, flowing out of Lake Baikal Arctic Ocean 3 Selenge River Сэлэнгэ мөрөн in Sükhbaatar, flowing into Lake Baikal Arctic Ocean 4 Chikoy River Arctic Ocean 5 Menza River Arctic Ocean 6 Katantsa River Arctic Ocean 7 Dzhida River Russia Arctic Ocean 8 Zelter River Зэлтэрийн гол, Bulgan/Selenge/Russia Arctic Ocean 9 Orkhon River Орхон гол, Arkhangai/Övörkhangai/Bulgan/Selenge Arctic Ocean 10 Tuul River Туул гол, Khentii/Töv/Bulgan/Selenge Arctic Ocean 11 Tamir River Тамир гол, Arkhangai Arctic Ocean 12 Kharaa River Хараа гол, Töv/Selenge/Darkhan-Uul Arctic Ocean 13 Eg River Эгийн гол, Khövsgöl/Bulgan Arctic Ocean 14 Üür River Үүрийн гол, Khövsgöl Arctic Ocean 15 Uilgan River Уйлган гол, Khövsgöl Arctic Ocean 16 Arigiin River Аригийн гол, Khövsgöl Arctic Ocean 17 Tarvagatai River Тарвагтай гол, Bulgan Arctic Ocean 18 Khanui River Хануй гол, Arkhangai/Bulgan Arctic Ocean 19 Ider River Идэр гол, Khövsgöl Arctic Ocean 20 Chuluut River Чулуут гол, Arkhangai/Khövsgöl Arctic Ocean 21 Suman River Суман гол, Arkhangai Arctic Ocean 22 Delgermörön Дэлгэрмөрөн, Khövsgöl Arctic Ocean 23 Beltes River Бэлтэсийн Гол, Khövsgöl Arctic Ocean 24 Bügsiin River Бүгсийн Гол, Khövsgöl Arctic Ocean 25 Lesser Yenisei Russia Arctic Ocean 26 Kyzyl-Khem Кызыл-Хем Arctic Ocean 27 Büsein River Arctic Ocean 28 Shishged River Шишгэд гол, Khövsgöl Arctic Ocean 29 Sharga River Шарга гол, Khövsgöl Arctic Ocean 30 Tengis River Тэнгис гол, Khövsgöl Arctic Ocean 31 Amur River Russia/China -
Late Quaternary Environment of Central Yakutia (NE' Siberia
Late Quaternary environment of Central Yakutia (NE’ Siberia): Signals in frozen ground and terrestrial sediments Spätquartäre Umweltentwicklung in Zentral-Jakutien (NO-Sibirien): Hinweise aus Permafrost und terrestrischen Sedimentarchiven Steffen Popp Steffen Popp Alfred-Wegener-Institut für Polar- und Meeresforschung Forschungsstelle Potsdam Telegrafenberg A43 D-14473 Potsdam Diese Arbeit ist die leicht veränderte Fassung einer Dissertation, die im März 2006 dem Fachbereich Geowissenschaften der Universität Potsdam vorgelegt wurde. 1. Introduction Contents Contents..............................................................................................................................i Abstract............................................................................................................................ iii Zusammenfassung ............................................................................................................iv List of Figures...................................................................................................................vi List of Tables.................................................................................................................. vii Acknowledgements ........................................................................................................ vii 1. Introduction ...............................................................................................................1 2. Regional Setting and Climate...................................................................................4 -
North and Central Asia FAO-Unesco Soil Tnap of the World 1 : 5 000 000 Volume VIII North and Central Asia FAO - Unesco Soil Map of the World
FAO-Unesco S oilmap of the 'world 1:5 000 000 Volume VII North and Central Asia FAO-Unesco Soil tnap of the world 1 : 5 000 000 Volume VIII North and Central Asia FAO - Unesco Soil map of the world Volume I Legend Volume II North America Volume III Mexico and Central America Volume IV South America Volume V Europe Volume VI Africa Volume VII South Asia Volume VIIINorth and Central Asia Volume IX Southeast Asia Volume X Australasia FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS UNITED NATIONS EDUCATIONAL, SCIENTIFIC AND CULTURAL ORGANIZATION FAO-Unesco Soilmap of the world 1: 5 000 000 Volume VIII North and Central Asia Prepared by the Food and Agriculture Organization of the United Nations Unesco-Paris 1978 The designations employed and the presentation of material in this publication do not irnply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations or of the United Nations Educa- tional, Scientific and Cultural Organization con- cerning the legal status of any country, territory, city or area or of its authorities, or concerning the delirnitation of its frontiers or boundaries. Printed by Tipolitografia F. Failli, Rome, for the Food and Agriculture Organization of the United Nations and the United Nations Educational, Scientific and Cultural Organization Published in 1978 by the United Nations Educational, Scientific and Cultural Organization Place de Fontenoy, 75700 Paris C) FAO/Unesco 1978 ISBN 92-3-101345-9 Printed in Italy PREFACE The project for a joint FAO/Unesco Soil Map of vested with the responsibility of compiling the techni- the World was undertaken following a recommenda- cal information, correlating the studies and drafting tion of the International Society of Soil Science. -
PERMAFROST DYNAMICS in 20™ and 21 St CENTURIES ALONG the EAST-SIBERIAN and ALASKAN TRANSECTS a THESIS Presented to the Faculty
Permafrost Dynamics In 20Th And 21St Centuries Along The East-Siberian And Alaskan Transects Item Type Thesis Authors Sazonova, Tatiana Sergeevna Download date 26/09/2021 06:03:10 Link to Item http://hdl.handle.net/11122/8665 PERMAFROST DYNAMICS IN 20™ AND 21 st CENTURIES ALONG THE EAST-SIBERIAN AND ALASKAN TRANSECTS A THESIS Presented to the Faculty of the University of Alaska Fairbanks in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY By Tatiana Sergeevna Sazonova Fairbanks, Alaska May 2003 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: 3092294 Copyright 2003 by Sazonova, Tatiana Sergeevna All rights reserved. ® UMI UMI Microform 3092294 Copyright 2003 by ProQuest Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. ProQuest Information and Learning Company 300 North Zeeb Road P.O. Box 1346 Ann Arbor, Ml 48106-1346 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. PERMAFROST DYNAMICS IN 20™ AND 21 st CENTURIES ALONG THE EAST-SIBERIAN AND ALASKAN TRANSECTS By Tatiana Sergeevna Sazonova RECOMMENDED: O f a ' b r n 'US % ~ OmnJ VmJmL 3 APr il m 3 *Z i . - . Advisory Copialptee Chajrg/ -A*” y" / -y , y / Z/■ .Zyk. Z K--^‘' Chair, Department oT Geology and Geophysics APPROVED: v :,) C c h o d a Dean, College of Science, Engineering and Mathematics Dean of tlje/Graduate School Date Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Abstract High latitude ecosystems where the mean annual ground surface temperature is around or below 0°C are highly sensitive to global warming. -
Loanwords in Sakha (Yakut), a Turkic Language of Siberia Brigitte Pakendorf, Innokentij Novgorodov
Loanwords in Sakha (Yakut), a Turkic language of Siberia Brigitte Pakendorf, Innokentij Novgorodov To cite this version: Brigitte Pakendorf, Innokentij Novgorodov. Loanwords in Sakha (Yakut), a Turkic language of Siberia. In Martin Haspelmath, Uri Tadmor. Loanwords in the World’s Languages: a Comparative Handbook, de Gruyter Mouton, pp.496-524, 2009. hal-02012602 HAL Id: hal-02012602 https://hal.univ-lyon2.fr/hal-02012602 Submitted on 23 Jul 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. Chapter 19 Loanwords in Sakha (Yakut), a Turkic language of Siberia* Brigitte Pakendorf and Innokentij N. Novgorodov 1. The language and its speakers Sakha (often referred to as Yakut) is a Turkic language spoken in northeastern Siberia. It is classified as a Northeastern Turkic language together with South Sibe- rian Turkic languages such as Tuvan, Altay, and Khakas. This classification, however, is based primarily on geography, rather than shared linguistic innovations (Schönig 1997: 123; Johanson 1998: 82f); thus, !"erbak (1994: 37–42) does not include Sakha amongst the South Siberian Turkic languages, but considers it a separate branch of Turkic. The closest relative of Sakha is Dolgan, spoken to the northwest of the Republic of Sakha (Yakutia). -
Yakutia) “…The Republic of Sakha (Yakutia) Is the Largest Region in the Russian Federation and One of the Richest in Natural Resources
Investor's Guide to the Republic of Sakha (Yakutia) “…The Republic of Sakha (Yakutia) is the largest region in the Russian Federation and one of the richest in natural resources. Needless to say, the stable and dynamic development of Yakutia is of key importance to both the Far Eastern Federal District and all of Russia…” President of the Russian Federation Vladimir Putin “One of the fundamental priorities of the Government of the Republic of Sakha (Yakutia) is to develop comfortable conditions for business and investment activities to ensure dynamic economic growth” Head of the Republic of Sakha (Yakutia) Egor Borisov 2 Contents Welcome from Egor Borisov, Head of the Republic of Sakha (Yakutia) 5 Overview of the Republic of Sakha (Yakutia) 6 Interesting facts about the Republic of Sakha (Yakutia) 7 Strategic priorities of the Republic of Sakha (Yakutia) investment policy 8 Seven reasons to start a business in the Republic of Sakha (Yakutia) 10 1. Rich reserves of natural resources 10 2. Significant business development potential for the extraction and processing of mineral and fossil resources 12 3. Unique geographical location 15 4. Stable credit rating 16 5. Convenient conditions for investment activity 18 6. Developed infrastructure for the support of small and medium-sized enterprises 19 7. High level of social and economic development 20 Investment infrastructure 22 Interaction with large businesses 24 Interaction with small and medium-sized enterprises 25 Other organisations and institutions 26 Practical information on doing business in the Republic of Sakha (Yakutia) 27 Public-Private Partnership 29 Information for small and medium-sized enterprises 31 Appendix 1. -
Siberia, the Wandering Northern Terrane, and Its Changing Geography Through the Palaeozoic ⁎ L
Earth-Science Reviews 82 (2007) 29–74 www.elsevier.com/locate/earscirev Siberia, the wandering northern terrane, and its changing geography through the Palaeozoic ⁎ L. Robin M. Cocks a, , Trond H. Torsvik b,c,d a Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK b Center for Geodynamics, Geological Survey of Norway, Leiv Eirikssons vei 39, Trondheim, N-7401, Norway c Institute for Petroleum Technology and Applied Geophysics, Norwegian University of Science and Technology, N-7491 NTNU, Norway d School of Geosciences, Private Bag 3, University of the Witwatersrand, WITS, 2050, South Africa Received 27 March 2006; accepted 5 February 2007 Available online 15 February 2007 Abstract The old terrane of Siberia occupied a very substantial area in the centre of today's political Siberia and also adjacent areas of Mongolia, eastern Kazakhstan, and northwestern China. Siberia's location within the Early Neoproterozoic Rodinia Superterrane is contentious (since few if any reliable palaeomagnetic data exist between about 1.0 Ga and 540 Ma), but Siberia probably became independent during the breakup of Rodinia soon after 800 Ma and continued to be so until very near the end of the Palaeozoic, when it became an integral part of the Pangea Supercontinent. The boundaries of the cratonic core of the Siberian Terrane (including the Patom area) are briefly described, together with summaries of some of the geologically complex surrounding areas, and it is concluded that all of the Palaeozoic underlying the West Siberian -
Post-Earthquake Reconstruction Continues to Blaze Trail Into
lakyara vol.190 Special Edition Post-earthquake reconstruction continues to blaze trail into uncharted territory - Interview with Shinya Endo, General Manager, Miyagi Prefecture Civil Engineering Department - 18.March 2014 Special Edition Post-earthquake reconstruction continues to blaze trail into uncharted territory vol.190 Executive Summary Miyagi Prefecture was particularly hard-hit by the catastrophic Great East Japan Earthquake of March 2011. It is now implementing a ten-year reconstruction plan in three phases. The first phase (three years) is restoration to the pre-earthquake status quo. In the second phase (four years), the Prefecture plans to revitalize (upgrade) its infrastructure to where it would have been if the earthquake had never occurred. In the third phase (three years), the Prefecture aims to better fortify itself against future natural disasters. With no model to follow for any of the three phases, Miyagi Prefecture is grappling with difficult challenges on a daily basis. NRI's Fumihiko Kamio spoke to Shinya Endo, head of Miyagi Prefecture's reconstruction program, about the challenges that lie ahead in 2014, the first year of the ten-year plan's revitalization phase. Shinya Endo General Manager, Miyagi Prefecture Civil Engineering Department Hired by Miyagi Prefecture in 1979. Has worked at prefecture's Ishinomaki Civil Engineering Office, Urban Planning Section, Sendai-Higashi Civil Engineering, Kessennuma Civil Engineering, Road Construction Section, Civil Engineering General Affairs Section, Tokyo Office, and Planning Department's Policy Section. Promoted to Deputy General Manager of Civil Engineering Department in April 2011 after managing Urban Planning Section and Roads Section. Assumed current post in April 2013. -
Subject of the Russian Federation)
How to use the Atlas The Atlas has two map sections The Main Section shows the location of Russia’s intact forest landscapes. The Thematic Section shows their tree species composition in two different ways. The legend is placed at the beginning of each set of maps. If you are looking for an area near a town or village Go to the Index on page 153 and find the alphabetical list of settlements by English name. The Cyrillic name is also given along with the map page number and coordinates (latitude and longitude) where it can be found. Capitals of regions and districts (raiony) are listed along with many other settlements, but only in the vicinity of intact forest landscapes. The reader should not expect to see a city like Moscow listed. Villages that are insufficiently known or very small are not listed and appear on the map only as nameless dots. If you are looking for an administrative region Go to the Index on page 185 and find the list of administrative regions. The numbers refer to the map on the inside back cover. Having found the region on this map, the reader will know which index map to use to search further. If you are looking for the big picture Go to the overview map on page 35. This map shows all of Russia’s Intact Forest Landscapes, along with the borders and Roman numerals of the five index maps. If you are looking for a certain part of Russia Find the appropriate index map. These show the borders of the detailed maps for different parts of the country. -
Baikal Project 2012-2014 Results and Events Booklet.Pdf
Photo by Elena Chumak GEF: “The GEF unites 182 countries in partnership with international institutions, non-governmental organizations (NGOs), and the private sector to address global environmental issues while supporting national sustainable development initiatives. Today the GEF is the largest public funder of projects to improve the global environment. An independently operating financial organization, the GEF provides grants for projects related to biodiversity, climate change, international waters, land degradation, the ozone layer, and persistent organic pollutants. Since 1991, GEF has achieved a strong track record with developing countries and countries with economies in transition, providing $9.2 billion in grants and leveraging $40 billion in co-financing for over 2,700 projects in over 168 countries. www.thegef.org” UNDP: “UNDP partners with people at all levels of society to help build nations that can withstand crisis, and drive and sustain the kind of growth that improves the quality of life for everyone. On the ground in 177 countries and territories, we offer global perspective and local insight to help empower lives and build resilient nations. www.undp.org” UNOPS: is an operational arm of the United Nations, helping a range of partners implement $1 billion worth of aid and development projects every year. UNOPS mission is to expand the capacity of the UN system and its partners to implement peacebuilding, humanitarian and development operations that matter for people in need. Photo by Elena Chumak Contents Project Achievements -
Cambrian Plutonism in Northeast Japan and Its Significance for The
Journal of Asian Earth Sciences 108 (2015) 136–149 Contents lists available at ScienceDirect Journal of Asian Earth Sciences journal homepage: www.elsevier.com/locate/jseaes Cambrian plutonism in Northeast Japan and its significance for the earliest arc-trench system of proto-Japan: New U–Pb zircon ages of the oldest granitoids in the Kitakami and Ou Mountains ⇑ Y. Isozaki a, , M. Ehiro b, H. Nakahata a, K. Aoki a,1, S. Sakata c, T. Hirata c a Department of Earth Science & Astronomy, The University of Tokyo, Komaba, Meguro, Tokyo 153-8902, Japan b The Tohoku University Museum, Sendai 980-8578, Japan c Department of Geology & Mineralogy, Kyoto University, Sakyo, Kyoto 606-8502, Japan article info abstract Article history: In order to clarify the early history of Japan, particularly during the Early Paleozoic, pre-Devonian gran- Received 31 October 2014 itoids in the South Kitakami Belt (SKB), NE Japan were dated by U–Pb zircon age by laser-ablation induc- Received in revised form 16 April 2015 tively coupled plasma-mass spectrometry (LA-ICP-MS). Two samples of diorite/tonalite from the Accepted 23 April 2015 Nagasaka area (Shoboji Diorite) and two of mylonitic tonalite from the Isawa area (Isawagawa Available online 30 April 2015 Tonalite) yielded late Cambrian ages (500–490 Ma) for the primary magmatism. These ages newly iden- tify a ca. 500 Ma (late Cambrian) arc plutonism in central NE Japan, which has not been recognized pre- Keywords: viously and has the following geological significance. The Cambrian granitoids are the oldest felsic Zircon U–Pb age plutonic rocks in NE Japan, which are independent of the previously known ca. -
Flowchart2016bluewhite42
Air Traffic Flow Chart 2016 More Info: http://gis.icao.int Sierra Leone !e Qaanaaq Longyearbyen !e !e Grise Fiord !e Pituffik !e Svay Rieng Barrow Resolute !e !e e Pevek !e Atqasuk ! !e Point Lay e !e ! Chokurdakh Wainwright Nuiqsut Sachs Harbour Kullorsuaq Tiksi e Point!e Hope !e !e !e !e ! e !e Barter Island Nuussuaq Dikson Sashylakh Chersky ! !e Arctic Bay !e !e !e !e Keperveyem Kivalina !e Prudhoe Bay/Deadhorse !e Khatanga Ust-Kuyga !e !e e Noatak!e Ulukhaktok e Pond Inlet Innarsuit e !e !e Deputatsky ! Anaktuvuk Pass Tuktoyaktuk !e ! !e! !e Kiana !e eUpernavik !e e Arctic Village !e Kangersuatsiaq!e! Ksar Es Souk Wales !e Selawik!e ! !e Kobuk !e Paulatuk !e Aappilattoq !e Anadyr e Deering !eAmbler !e!e Bettlese Aklavik Inuvik !e Upernavik Kujalleq Heliport!e !e Teller!e !e Noorvike e ! Old Crow !e e e!e ! Hughese ! e ! Nuugaatsiaq Batagay ! Huslia ! Coldfoot !e ! Fort Mcpherson !e Samchok Nome Buckland!e !e!e Beavere Chalkyitsik e Cambridge Bay Taloyoak Clyde River !e !e !e Gambell e e Elime e !e e ! !e ! !e e e Uummannaq Qaarsut!e Olenek Indianapolis !e e ! !e !e ! Tanana ! ! ! ! !e !ee Mehamn Norilsk !e !e ! Savoonga e e!e Ruby !e Central Circle Colville Lake Kugluktuk Coppermine Igloolik !e Neerlerit Inaat !e !e e e ! eKoyuk! !e !e !e Minto e !e e !e Gjoa Haven !e Saqqaq! Ittoqqortoormiit!e Hasvike ! e Amderma ! Golovine ! !e !e ! Fort Good Hope! !e Pelly Bay Hall Beach Niaqornat!ee e e ! ! e !e Zhigansk e ! Kaltag Galena e ! ! ! Alta Berlevag Vadso! !e Emmonak Kotlik! !e ! !e Qeqertaq Heliport e !e !e e!e !e eFAI Eagle e e !