Newell, J. 2004. the Russian Far East
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FLOODS in EASTERN SIBERIA This Final Report Is Intended for Reporting on Emergency Appeals Appeal No
RUSSIAN FEDERATION: 8 January, 2002 FLOODS IN EASTERN SIBERIA This Final Report is intended for reporting on emergency appeals Appeal No. 16/01 Launched on: 28 May 2001 for 8 months for CHF 480,000 DREF Allocated: CHF 50,000 Beneficiaries: 15,000 Operations Update No. 4 (Final); Period covered: 10 November - 25 December 2001 (last Ops. Update No. 3 issued 12 November 2001) “At a glance” Appeal coverage: 85.6% Related Appeals: 01.59/2001; Russian Federation 2001 Annual Appeal Update/Summary: Timely donor support and effective coordination on the part of the Federation has enabled the intended relief activities to be implemented according to the plans set out in the appeal. The CHF 33,000 balance remaining (see attached provisional final financial report) will be used for disaster response and training activities, as well for the replenishment of contingency stocks. Operational Developments: In May, severe floods in eastern Siberia inundated 87 settlements in Yakutia and several towns in Irkutsk region and Tyva Republic causing enormous losses to people and infrastructures. According to official estimations the cost of losses in Yakutia only made USD 241 million. There, 12,000 houses were damaged, 5,000 of which were smashed by water and ice; 366 social objects and 597 industrial buildings were destroyed; 407 km of road were uprooted, 160 bridges flashed away; a lot of cultivated land and cattle were lost. Over 12,000 victims turned out without any means for existence. 50,305 citizens had been evacuated. On 25 May, the Government of Yakutia issued Resolution No. 305 establishing an interagency commission to take charge of humanitarian aid and reconstruction. -
Article of a Given In- with Postdepositional Erosion
Earth Surf. Dynam., 8, 769–787, 2020 https://doi.org/10.5194/esurf-8-769-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Timing of exotic, far-traveled boulder emplacement and paleo-outburst flooding in the central Himalayas Marius L. Huber1,a, Maarten Lupker1, Sean F. Gallen2, Marcus Christl3, and Ananta P. Gajurel4 1Geological Institute, Department of Earth Sciences, ETH Zurich, Zurich 8092, Switzerland 2Department of Geosciences, Colorado State University, Fort Collins, Colorado 80523, USA 3Laboratory of Ion Beam Physics (LIP), Department of Physics, ETH Zurich, Zurich 8093, Switzerland 4Department of Geology, Tribhuvan University, Kirtipur, Kathmandu, Nepal acurrent address: Université de Lorraine, CNRS, CRPG, 54000 Nancy, France Correspondence: Marius L. Huber ([email protected]) Received: 28 February 2020 – Discussion started: 20 March 2020 Revised: 21 July 2020 – Accepted: 11 August 2020 – Published: 22 September 2020 Abstract. Large boulders, ca. 10 m in diameter or more, commonly linger in Himalayan river channels. In many cases, their lithology is consistent with source areas located more than 10 km upstream, suggesting long trans- port distances. The mechanisms and timing of “exotic” boulder emplacement are poorly constrained, but their presence hints at processes that are relevant for landscape evolution and geohazard assessments in mountainous regions. We surveyed river reaches of the Trishuli and Sunkoshi, two trans-Himalayan rivers in central Nepal, to improve our understanding of the processes responsible for exotic boulder transport and the timing of em- placement. Boulder size and channel hydraulic geometry were used to constrain paleo-flood discharge assuming turbulent, Newtonian fluid flow conditions, and boulder exposure ages were determined using cosmogenic nu- clide exposure dating. -
Sediment Transport to the Laptev Sea-Hydrology and Geochemistry of the Lena River
Sediment transport to the Laptev Sea-hydrology and geochemistry of the Lena River V. RACHOLD, A. ALABYAN, H.-W. HUBBERTEN, V. N. KOROTAEV and A. A, ZAITSEV Rachold, V., Alabyan, A., Hubberten, H.-W., Korotaev, V. N. & Zaitsev, A. A. 1996: Sediment transport to the Laptev Sea-hydrology and geochemistry of the Lena River. Polar Research 15(2), 183-196. This study focuses on the fluvial sediment input to the Laptev Sea and concentrates on the hydrology of the Lena basin and the geochemistry of the suspended particulate material. The paper presents data on annual water discharge, sediment transport and seasonal variations of sediment transport. The data are based on daily measurements of hydrometeorological stations and additional analyses of the SPM concentrations carried out during expeditions from 1975 to 1981. Samples of the SPM collected during an expedition in 1994 were analysed for major, trace, and rare earth elements by ICP-OES and ICP-MS. Approximately 700 h3freshwater and 27 x lo6 tons of sediment per year are supplied to the Laptev Sea by Siberian rivers, mainly by the Lena River. Due to the climatic situation of the drainage area, almost the entire material is transported between June and September. However, only a minor part of the sediments transported by the Lena River enters the Laptev Sea shelf through the main channels of the delta, while the rest is dispersed within the network of the Lena Delta. Because the Lena River drains a large basin of 2.5 x lo6 km2,the chemical composition of the SPM shows a very uniform composition. -
Terminal Evaluation of the UNEP/GEF Project
United Nations Environment Programme Terminal Evaluation of the UNEP/GEF Project “Russian Federation – Support to the National Programme of Action for the Protection of the Arctic Marine Environment” Prof. Dr. Ivan Holoubek & Oleg Sutkaitis UNEP Evaluation Office September 2012 Table of Contents Project Identification Table _________________________________________________ i Executive summary ________________________________________________________ ii 1. Evaluation background ________________________________________________ 1 A. Context _____________________________________________________________________________ 1 B. The Project __________________________________________________________________________ 2 C. Evaluation objectives, scope and methodology ____________________________________________ 4 C. 1 Objective and Scope of the Evaluation ________________________________________________ 4 C. 2 Overall Approach and Methods ______________________________________________________ 4 C. 3. Limitations and Constraints ________________________________________________________ 5 2. Project performance and impact ___________________________________________ 6 A. Attainment of objectives and planned results ___________________________________ 6 A.1 Achievement of outputs and activities __________________________________________________ 6 A.2 Relevance __________________________________________________________________________ 7 A. 3 Effectiveness _______________________________________________________________________ 9 A.4 Efficiency _________________________________________________________________________ -
The Effect of Grazing on the Temperature Regime of the Alas
land Article The Effect of Grazing on the Temperature Regime of the Alas Soils of Central Yakutia Victor Makarov * , Grigory Savvinov , Lyudmila Gavrilieva and Anna Gololobova Scientific Research Institute of Applied Ecology of the North, M.K. Ammosov North-Eastern Federal University, 43 Lenin Prospekt, 677980 Yakutsk, Russia; [email protected] (G.S.); [email protected] (L.G.); [email protected] (A.G.) * Correspondence: [email protected]; Tel.: +7-4112-33-68-51 Received: 7 September 2020; Accepted: 22 September 2020; Published: 1 October 2020 Abstract: There are numerous studies on the effect of grazing on the physical and chemical parameters of soils. However, the impact of grazing on the temperature regime of the alas soils in Central Yakutia is still poorly understood. This paper presents the results of long-term observations of the state of the soil-and-plant cover of thermokarst basins—i.e., alases—located in the Lena-Amga interfluve and actively used as pastureland. Observations of the process of the self-restoration of grass cover and changes in the temperature regime of alas soils were carried out on different variants (with isolation from grazing and without isolation). A significant increase in the average height of the grass stand and its foliage projective cover was observed with a gradual reduction in the number of species when isolated from grazing. Changes in the structure of the alas vegetation cover influence the microclimate of the soil. As a result of livestock grazing, the mean annual soil temperature rises and the amount and depth of the penetration of active temperatures increase. -
2002 Annual Report of Alrosa Table of Contents
2002 ANNUAL REPORT OF ALROSA TABLE OF CONTENTS: Members of Supervisory Council Members of the Board Members of Auditing Committee Structure of ALROSA Group President’s Statement Activities of Supervisory Council Report by the Board on the Company’s Activities in the Main Fields of Operations Mining Operations Marketing Policy. Sales of Rough Diamonds. Polished Diamond Manufacture and Sales Geological Exploration Capital Construction Supplies and Logistics Research and Development Diversification of the Company’s Activities. Subsidiaries and Affiliated Companies Personnel Management External Relations Environmental Safety Accounting and Financial Results Accounting Policy Audit Statement Consolidated Financial Statement of ALROSA Co. Ltd. Basic Performance Indicators of ALROSA Co. Ltd. Information for Shareholders Historic Highlights of ALROSA Addresses of ALROSA Offices 2 Supervisory Council Co-Chairmen of Supervisory Council: Alexey Leonidovich KUDRIN Deputy Chairman of RF Government, Minister of Finance of the Russian Federation, Chairman of ALROSA Supervisory Council Vyacheslav Anataloyevich SHTYROV President of Republic of Sakha (Yakutia), First Deputy Chairman of ALROSA Supervisory Council Andrei Dmitrievich KIRILLIN Chairman of ALROSA Supervisory Council Members of Supervisory Council: Gennady Fedorovich ALEXEYEV Minister of Property Relations of Republic of Sakha (Yakutia) Alexandr Vasilyevich ANOSHKIN Assistant of Head of RF President’s Administration Ernst Borisovich BEREZKIN Minister of Finance of Republic of Sakha (Yakutia) -
Chapter 7. Cities of the Russian North in the Context of Climate Change
? chapter seven Cities of the Russian North in the Context of Climate Change Oleg Anisimov and Vasily Kokorev Introduction In addressing Arctic urban sustainability, one has to deal with the com- plex interplay of multiple factors, such as governance and economic development, demography and migration, environmental changes and land use, changes in the ecosystems and their services, and climate change.1 While climate change can be seen as a factor that exacerbates existing vulnerabilities to other stressors, changes in temperatures, precipitation, snow accumulation, river and lake ice, and hydrological conditions also have direct implications for Northern cities. Climate change leads to a reduction in the demand for heating energy, on one hand, and heightens concerns about the fate of the infrastruc- ture built upon thawing permafrost, on the other. Changes in snowfall are particularly important and have direct implications for the urban economy, because, together with heating costs, expenses for snow removal from streets, airport runways, roofs, and ventilation spaces underneath buildings standing on pile foundations built upon perma- frost constitute the bulk of a city’s maintenance budget during the long cold period of the year. Many cities are located in river valleys and are prone to fl oods that lead to enormous economic losses, inju- ries, and in some cases human deaths. The severity of the northern climate has a direct impact on the regional migration of labor. Climate could thus potentially be viewed as an inexhaustible public resource that creates opportunities for sustainable urban development (Simp- 142 | Oleg Anisimov and Vasily Kokorev son 2009). Long-term trends show that climate as a resource is, in fact, becoming more readily available in the Russian North, notwith- standing the general perception that globally climate change is one of the greatest challenges facing humanity in the twenty-fi rst century. -
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 -
Description of Map Units Northeast Asia Geodynamics Map
DESCRIPTION OF MAP UNITS NORTHEAST ASIA GEODYNAMICS MAP OVERLAP ASSEMBLAGES (Arranged alphabetically by map symbol) ad Adycha intermountain sedimentary basin (Miocene and Pliocene) (Yakutia) Basin forms a discontinuous chain along the foot of southwestern slope of Chersky Range in the Yana and Adycha Rivers basins. Contain Miocene and Pliocene sandstone, pebble gravel conglomerate, claystone, and minor boulder gravel conglomerate that range up to 400 m thick. REFERENCES: Grinenko and others, 1998. ag Agul (Rybinsk) molasse basin (Middle Devonian to Early Carboniferous) (Eastern Sayan) Consists of Middle Devonian through Early Carboniferous aerial and lacustrine sand-silt-mudstone, conglomerate, marl, and limestone with fauna and flora. Tuff, tuffite, and tuffaceous rock occur in Early Carboniferous sedimentary rocks. Ranges up to 2,000 m thick in southwestern margin of basin. Unconformably overlaps Early Devonian rocks of South Siberian volcanic-plutonic belt and Precambrian and early Paleozoic rocks of the Siberian Platform and surrounding fold belts. REFERENCES: Yanov, 1956; Graizer, Borovskaya, 1964. ags Argun sedimentary basin (Early Paleozoic) (Northeastern China) Occurs east of the Argun River in a discontinuously exposed, northeast-trending belt and consists of Cambrian and Ordovician marine, terrigenous detrital, and carbonate rocks. Cambrian units are composed of of feldspar- quartz sandstone, siltstone, shale and limestone and contain abundant Afaciacyathus sp., Bensocyathus sp., Robustocyathus yavorskii, Archaeocyathus yavorskii(Vologalin), Ethomophyllum hinganense Gu,o and other fossils. Ordovicain units consist of feldspar-quartz sandstone, siltstone, fine-grained sandstone and phylitic siltstone, and interlayered metamorphosed muddy siltstone and fine-grained sandstone with brachiopods, corals, and trilobites. Total thickness ranges up to 4,370 m. Basin unconformably overlies the Argunsky metamorphic terrane. -
Personnel - Conflict of Interest: Clements, William” of the Philip Buchen Files at the Gerald R
The original documents are located in Box 37, folder “Personnel - Conflict of Interest: Clements, William” of the Philip Buchen Files at the Gerald R. Ford Presidential Library. Copyright Notice The copyright law of the United States (Title 17, United States Code) governs the making of photocopies or other reproductions of copyrighted material. Gerald R. Ford donated to the United States of America his copyrights in all of his unpublished writings in National Archives collections. Works prepared by U.S. Government employees as part of their official duties are in the public domain. The copyrights to materials written by other individuals or organizations are presumed to remain with them. If you think any of the information displayed in the PDF is subject to a valid copyright claim, please contact the Gerald R. Ford Presidential Library. Digitized from Box 37 of the Philip Buchen Files at the Gerald R. Ford Presidential Library MEMORANDUM NATIONAL SECURITY COUNCIL ADMINISTRATIVELY June 10, 1975 CONFIDENTIAL MEMORANDUM FOR GENERAL SCOWCROFT FROM: Mr. Clift ~......-- SUBJECT: Status of NSSM 214: "Implications of US Participation in Siberian Development" Attached is a copy of the interagency response to NSSM 214. All agencies except Defense have concurred with the principal conclusions of the response, though several have suggested minor revisions. With regard to Defense, we understand that someone at a high level (we think Deputy Secretary Clements) objected to the conclusions of the study and thereby caused the delay in the Defense response. Subsequently his objections have been overcome and the response is now on its way back through Defense channels for official concurrence. -
Late Precambrian Mafic Dyke Swarms of the Aldan Shield and Their Importance in Ore-Magmatic Processes
МИНИСТЕРСТВО НАУКИ И ВЫСШЕГО ОБРАЗОВАНИЯ РОССИЙСКОЙ ФЕДЕРАЦИИ НАЦИОНАЛЬНЫЙ ИССЛЕДОВАТЕЛЬСКИЙ ТОМСКИЙ ГОСУДАРСТВЕННЫЙ УНИВЕРСИТЕТ LARGE IGNEOUS PROVINCES THROUGH EARTH HISTORY: MANTLE PLUMES, SUPERCONTINENTS, CLIMATE CHANGE, METALLOGENY AND OIL-GAS, PLANETARY ANALOGUES (LIP – 2019) Abstract volume of the 7 International Conference Tomsk, Russia, 28 August – 8 September 2019 КРУПНЫЕ ИЗВЕРЖЕННЫЕ ПРОВИНЦИИ В ИСТОРИИ ЗЕМЛИ: МАНТИЙНЫЕ ПЛЮМЫ, СУПЕРКОНТИНЕНТЫ, КЛИМАТИЧЕСКИЕ ИЗМЕНЕНИЯ, МЕТАЛЛОГЕНИЯ, ФОРМИРОВАНИЕ НЕФТИ И ГАЗА, ПЛАНЕТЫ ЗЕМНОЙ ГРУППЫ (КИП – 2019) Тезисы VII Международной конференции Томск, Россия 28 августа – 8 сентября 2019 LATE PRECAMBRIAN MAFIC DYKE SWARMS OF THE ALDAN SHIELD AND THEIR IMPORTANCE IN ORE-MAGMATIC PROCESSES Okrugin A. V.1, Ernst R. E.2,3, Beryozkin V. I.1, Popov N. V.4 1 Diamond and Precious Metal Geology Institute (DPMGI), SB RAS, Yakutsk, Russia 2Carleton University, Ottawa, Canada 3 Tomsk State University, Tomsk, Russia 4Trofimuk Institute of Petroleum Geology and Geophysics, SB RAS, Novosibirsk, Russia Keywords: Dyke swarm, basite, mafic magmatism, mantle plume, Aldan Shield Introduction (Fig.1). The dykes dip steeply (70-90o) showing clear intrusive contacts with the enclosing rocks. Their traceable length varies Integrated petrological-geochemical, geochronologi- from a few to 15 km and the thickness – from several to 200- cal, and ore-mineralogical studies of mafic magmatism are 300 m. The dykes form 200-500 km long and 20-60 km wide of prime importance in reconstructing the formation history swarms crosscutting different terranes. The ENE dyke swarms and metallogeny of ancient platforms (Gladkochub et al., occur mainly in the western part of the Aldan shield where the 2012; Guryanov et al., 2013; Okrugin et al., 2018; Ernst et al., Nirekta (NR), Olondo (OL), Udokan-Tommot (UT), and Kalar- 2016). -
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).