Exhibition Catalogue with Descriptions (Please Return After Viewing the Exhibition)
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Golden Eagle Trans-Siberian Express Via the BAM and Yakutsk
Golden Eagle Trans-Siberian Express via the BAM and Yakutsk https://www.irtsociety.com/journey/golden-eagle-trans-siberian-express-bam-line/ Overview The Highlights - Explore smaller and remote towns of Russia, rarely visited by tourists - Grand Moscow’s Red Square, the Kremlin Armoury Chamber, St. Basil's Cathedral and Cafe Pushkin - Yekaterinburg, infamous execution site of Tsar Nicholas II, his wife Alexandra, their son, daughters and servants, by the Bolsheviks in 1918 - Fantastic Sayan Mountain scenery, including the Dzheb double horse-shoe curves The Society of International Railway Travelers | irtsociety.com | (800) 478-4881 Page 1/7 - Visit one of the biggest hydro-electric dams in the world in Bratsk and one of the world’s largest open cast mines in Neryungri - Stop at the unique and mysterious 3.7-mile (6km) long Chara Sand Dunes - Learn about the history and building of the BAM line at the local museum in Tynda - Marvel at Komsomolsk's majestic and expansive urban architecture of the Soviet era, including the stupendous Pervostroitelei Avenue, lined with Soviet store fronts and signage intact - City tour of Vladivostok, including a preserved World War II submarine - All meals, fine wine with lunch and dinner, hotels, gratuities, off-train tours and arrival/departure transfers included The Tour Travel by private train through an outstanding area of untouched natural beauty of Siberia, along the Baikal-Amur Magistral (BAM) line, visiting some of the lesser known places and communities of remote Russia. The luxurious Golden Eagle will transport you from Moscow to Vladivostok along the less-traveled, northerly Trans-Siberian BAM line. -
New Taxa of Butterflies from Transbaikalia, Russia (Rhopalocera: Satyridae, Nymphalidae) 107-124 ©Ges
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Atalanta Jahr/Year: 1999 Band/Volume: 29 Autor(en)/Author(s): Churkin Sergei V. Artikel/Article: New taxa of butterflies from Transbaikalia, Russia (Rhopalocera: Satyridae, Nymphalidae) 107-124 ©Ges. zur Förderung d. Erforschung von Insektenwanderungen e.V. München, download unter www.zobodat.at Atalanta (May 1999) 29(1/4): 107-124, colour plates VIII, IX, Wurzburg, ISSN 0171-0079 New taxa of butterflies from Transbaikalia, Russia (Rhopalocera: Satyridae, Nymphalidae) by Sergei V. C h u r k in received 3.XII.1998 Summary: Erebia dabanensis chingiza subspec. nov., Erebia kefersteini arnica subspec. nov., Erebia erinnyn chara subspec. nov., Oeneis norna radnaevi subspec. nov., Boloria alaskensis bato subspec. nov., Clossiana erda puella subspec. nov. and Boloria purpurea spec. nov. are described from the Barguzin and Kodar Mountains (Transbaikalia). The status of the species Erebia erinnyn W arren , 1932 was confirmed by the characteristic of its genitalia. The status of Erebia troubridgei D ubatolov , 1992 is under discussion. Pe3K)Me: Erebia dabanensis chingiza subspec. nov., Erebia kefersteini arnica subspec. nov., Erebia erinnyn chara subspec. nov., Oeneis norna radnaevi subspec. nov., Boloria alaskensis bato subspec. nov., Clossiana erda puella subspec. nov. m Boloria purpurea spec. nov. onnca- Hbi c 5apry3HHCKoro m KoaapcKoro xpebTOB. Ha ocHOBaHMM MccneaoBaHMH rem ianm noAT- BepwaeH bmaobom CTaTyc Erebia erinnyn W arren , 1932. ObcywAaemR CTaTyc TaKCOHa Erebia troubridgei D ubatolov , 1992. Introduction In the course of his work to investigate the Rhopalocera of Transbaikalia, the author and a group of enthusiasts and professional entomologists have undertaken a number of collecting trips to the Barguzin and Kodar Mts. -
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. -
Extensive Glaciation in Transbaikalia, Siberia, at the Last Glacial Maximum
Quaternary Science Reviews 132 (2016) 161e174 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Extensive glaciation in Transbaikalia, Siberia, at the Last Glacial Maximum * Martin Margold a, , John D. Jansen a, 1, Artem L. Gurinov b, Alexandru T. Codilean c, David Fink d, Frank Preusser a, 2, Natalya V. Reznichenko e, Charles Mifsud d a Department of Physical Geography, Stockholm University, SE-106 91, Stockholm, Sweden b Department of Geomorphology & Palaeogeography, Lomonosov Moscow State University, Leninskie gory, GSP-1, Moscow, 119991, Russian Federation c School of Earth & Environmental Sciences, University of Wollongong, Northfields Avenue, Wollongong, NSW, 2522, Australia d Institute for Environmental Research, Australian Nuclear Science & Technology Organisation, Locked Bag 2001, Kirrawee DC, NSW, 2232, Australia e Department of Geography, Durham University, Lower Mountjoy, South Road, Durham, DH1 3LE, UK article info abstract Article history: Successively smaller glacial extents have been proposed for continental Eurasia during the stadials of the Received 27 March 2015 last glacial period leading up to the Last Glacial Maximum (LGM). At the same time the large moun- Received in revised form tainous region east of Lake Baikal, Transbaikalia, has remained unexplored in terms of glacial chronology 23 November 2015 despite clear geomorphological evidence of substantial past glaciations. We have applied cosmogenic Accepted 26 November 2015 10Be exposure dating and optically stimulated luminescence to establish the first quantitative glacial Available online 14 December 2015 chronology for this region. Based on eighteen exposure ages from five moraine complexes, we propose that large mountain ice fields existed in the Kodar and Udokan mountains during Oxygen Isotope Stage 2, Keywords: fi > Glaciation commensurate with the global LGM. -
Geodetic Mass Balance of Azarova Glacier, Kodar Mountains, Eastern Siberia, and Its Links to Observed and Projected Climatic Change
Annals of Glaciology 52(58) 2011 129 Geodetic mass balance of Azarova glacier, Kodar mountains, eastern Siberia, and its links to observed and projected climatic change M. SHAHGEDANOVA,1 V. POPOVNIN,2 A. ALEYNIKOV,2 C.R. STOKES3 1Department of Geography and Walker Institute for Climate System Research, University of Reading, Whiteknights, PO Box 227, Reading RG6 6AB, UK E-mail: [email protected] 2Department of Cryolithology and Glaciology, Faculty of Geography, Moscow State University, Leninskiye Gory, 119992 Moscow, Russia 3Department of Geography, Durham University, South Road, Durham DH1 3LE, UK ABSTRACT. The Kodar mountains in eastern Siberia accommodate 30 small, cold-based glaciers with a combined surface area previously estimated at 19 km2. Very little is known about these glaciers, which were first surveyed in the late 1950s. In this paper, we use terrestrial photogrammetry to calculate changes in the surface area, elevation, volume and geodetic mass balance of Azarova glacier between 1979 and 2007 and relate these to meteorological data from nearby Chara weather station (1938–2007). The glacier surface area declined by 20 Æ 6.9% and the surface lowered by an average of 20 Æ 1.8 m (mean thinning 0.71 m a–1), resulting in a strongly negative cumulative and average mass balance of –18 Æ 1.6 m w.e. and –640 Æ 60 mm w.e. a–1, respectively. The July–August air temperature increased at a rate of 0.0368Ca–1 between 1979 and 2007, and the 1980–2007 period was on average 18C warmer than 1938–79. In comparison to the 1961–90 period, regional climate projections for the A2 and B2 CO2 emission scenarios developed using the PRECIS regional climate model indicate that summer temperatures will increase by 2.6–4.78C and 4.9–6.28C, respectively, during the 2071–2100 period. -
Metallogeny of Northern, Central and Eastern Asia
METALLOGENY OF NORTHERN, CENTRAL AND EASTERN ASIA Explanatory Note to the Metallogenic map of Northern–Central–Eastern Asia and Adjacent Areas at scale 1:2,500,000 VSEGEI Printing House St. Petersburg • 2017 Abstract Explanatory Notes for the “1:2.5 M Metallogenic Map of Northern, Central, and Eastern Asia” show results of long-term joint research of national geological institutions of Russia, China, Kazakhstan, Mongolia, and the Republic of Korea. The latest published geological materials and results of discussions for Uzbekistan, Kyrgyzstan, Tajikistan, Turkmenistan, and North Korea were used as well. Described metallogenic objects: 7,081 mineral deposits, 1,200 ore knots, 650 ore regions and ore zones, 231 metallogenic areas and metallogenic zones, 88 metallogenic provinces. The total area of the map is 30 M km2. Tab. 10, fig. 15, list of ref. 94 items. Editors-in-Chief: O.V. Petrov, A.F. Morozov, E.A. Kiselev, S.P. Shokalsky (Russia), Dong Shuwen (China), O. Chuluun, O. Tomurtogoo (Mongolia), B.S. Uzhkenov, M.A. Sayduakasov (Kazakhstan), Hwang Jae Ha, Kim Bok Chul (Korea) Authors G.A. Shatkov, O.V. Petrov, E.M. Pinsky, N.S. Solovyev, V.P. Feoktistov, V.V. Shatov, L.D. Rucheykova, V.A. Gushchina, A.N. Gureev (Russia); Chen Tingyu, Geng Shufang, Dong Shuwen, Chen Binwei, Huang Dianhao, Song Tianrui, Sheng Jifu, Zhu Guanxiang, Sun Guiying, Yan Keming, Min Longrui, Jin Ruogu, Liu Ping, Fan Benxian, Ju Yuanjing, Wang Zhenyang, Han Kunying, Wang Liya (China); Dezhidmaa G., Tomurtogoo O. (Mongolia); Bok Chul Kim, Hwang Jae Ha (Republic of Korea); B.S. Uzhkenov, A.L. -
Eastern Siberia.', Global and Planetary Change., 101
Durham Research Online Deposited in DRO: 16 May 2013 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Stokes, C.R. and Shahgedanova, M. and Evans, I.S. and Popovnin, V.V. (2013) 'Accelerated loss of alpine glaciers in the Kodar Mountains, south-eastern Siberia.', Global and planetary change., 101 . pp. 82-96. Further information on publisher's website: http://dx.doi.org/10.1016/j.gloplacha.2012.12.010 Publisher's copyright statement: NOTICE: this is the author's version of a work that was accepted for publication in Global and planetary change. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reected in this document. Changes may have been made to this work since it was submitted for publication. A denitive version was subsequently published in Global and planetary change, 101, 2013, 10.1016/j.gloplacha.2012.12.010 Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. -
Arctic Explorer a Quest to See the Northern Lights Norway
golden eagle luxury trains VOYAGES OF A LIFETIME BY PRIVATE TRAINTM ARCTIC EXPLORER A QUEST TO SEE THE NORTHERN LIGHTS NORWAY SWEDEN GERMANY Kirkenes (Norway) Nikel Murmansk FINLAND POLAND ESTONIAST. PETERSBURG LATVIA LITHUANIA Petrozavodsk GOLDEN EAGLE BELARUS ROUTE MAP ROMANIA MOSCOW UKRAINE Vladimir & Suzdal COLOUR KEY Kazan TRANS-SIBERIAN EXPRESS Moscow - Vladivostok Vladivostok - Moscow Yekaterinburg TRANS-MONGOLIAN EXPRESS Moscow - Ulaan Baatar Ulaan Baatar - Moscow GEORGIA Gori, Uplistsikhe & Mtskheta WINTER WONDERLAND Tbilisi TURKEY Lake Sevan Moscow - Ulaan Baatar - Vladivostok Vladivostok - Moscow YEREVAN Baku KAZAKHSTAN ARCTIC EXPLORER Turkmenbashi Moscow - St Petersburg Baikonur St Petersburg - Moscow CASPIAN UZBEKISTAN SEA CASPIAN ODYSSEY Khiva Yerevan - Almaty Darvaza Ashgabat ALMATY SILK ROAD IRAN Bukhara Merv Bishkek Beijing - Moscow Samarkand Tashkent Almaty - Moscow TURKMENISTAN Shahrisabz Kokand Andizhan Lake Issyk-Kul Margiland KYRGYZSTAN Osh REPUBLICS OF THE SILK ROAD Dushanbe Moscow - Almaty AFGHANISTAN Kirkenes (Norway) Kamchatka Peninsula RUSSIA Yekaterinburg Novaya Chara Tynda Novy Urgal Novosibirsk Khabarovsk Nerchinsk Abakan Lake Baikal Irkutsk Ulan Ude ULAAN BAATAR ALMATY CHINA VLADIVOSTOK MONGOLIA Lake Issyk-Kul KYRGYZSTAN Turpan BEIJING JAPAN Dunhuang Xian CONTENTS Foreword by Tim Littler, President & Founder Rail Cruising By Private Train What’s Included In The Tour Price Golden Eagle – Train Information Dining On Board Bar Lounge Car On Board Accommodation Tour Itineraries Arctic Explorer - A Quest to see the Northern Lights Important Information About Our Tours Tour Previews 2021-2022 Booking Conditions WELCOME TO CONTENTS GOLDEN EAGLE LUXURY TRAINS Since launching the company as GW Travel in to take, the level of tipping required, or having that 1989, we have developed a whole range of fully extra glass of wine with your meal complemented by escorted rail cruises across Europe, Asia, Africa your very own private en-suite cabin. -
Retreat Pattern and Dynamics of Glaciers and Ice Sheets: Reconstructions Based on Meltwater Features
Retreat pattern and dynamics of glaciers and ice sheets: reconstructions based on meltwater features Martin Margold Department of Physical Geography and Quaternary Geology Stockholm University © 2012 Martin Margold ISSN: 1653-7211 ISBN: 978-91-7447-429-9 Paper I © 2012 Taylor & Francis Paper II © 2011 Journal of Maps Paper III © 2011 Journal of Maps Paper IV © 2011 Elsevier Printed by Universitetsservice US-AB, Stockholm, Sweden Doctoral dissertation 2012 Department of Physical Geography and Quaternary Geology Stockholm University ABSTRACT Glaciers and ice sheets covered extensive areas in the Northern Hemisphere during the last glacial period. Subsequently to the Last Glacial Maximum (LGM), they retreated rapidly and, except for Greenland and some other ice caps and glaciers, they vanished after the last glacial termination. This thesis examines the dynamics of deglacial environments by analysing the glacial geomorphological record with focus on the landforms created by glacial meltwater. The aims are (i) to evaluate the data available for mapping glacial meltwater features at the regional scale, and (ii) to demonstrate the potential of such features for regional ice retreat reconstructions in high- relief landscapes. Meltwater landforms such as ice-marginal meltwater channels, eskers, deltas and fossil glacial lake shorelines are used to infer former ice surface slope directions and successive positions of retreating ice margins. Evaluated high-resolution satellite imagery and digital elevation models reveal their potential to replace aerial photographs as the primary data for regional mapping surveys including the glacial meltwater system. Following a methods study, reconstructions of the deglacial dynamics are carried out for the area of central Transbaikalia, Siberia, Russia, and for the Cordilleran Ice Sheet (CIS) in central British Columbia, Canada, using regional geomorphological mapping surveys. -
Waterbirds of Lake Baikal, Eastern Siberia, Russia
FORKTAIL 25 (2009): 13–70 Waterbirds of Lake Baikal, eastern Siberia, Russia JIŘÍ MLÍKOVSKÝ Lake Baikal lies in eastern Siberia, Russia. Due to its huge size, its waterbird fauna is still insufficiently known in spite of a long history of relevant research and the efforts of local and visiting ornithologists and birdwatchers. Overall, 137 waterbird species have been recorded at Lake Baikal since 1800, with records of five further species considered not acceptable, and one species recorded only prior to 1800. Only 50 species currently breed at Lake Baikal, while another 11 species bred there in the past or were recorded as occasional breeders. Only three species of conservation importance (all Near Threatened) currently breed or regularly migrate at Lake Baikal: Asian Dowitcher Limnodromus semipalmatus, Black-tailed Godwit Limosa limosa and Eurasian Curlew Numenius arquata. INTRODUCTION In the course of past centuries water levels in LB fluctuated considerably (Galaziy 1967, 1972), but the Lake Baikal (hereafter ‘LB’) is the largest lake in Siberia effects on the local avifauna have not been documented. and one of the largest in the world. Avifaunal lists of the Since the 1950s, the water level in LB has been regulated broader LB area have been published by Gagina (1958c, by the Irkutsk Dam. The resulting seasonal fluctuations 1960b,c, 1961, 1962b, 1965, 1968, 1988), Dorzhiyev of water levels significantly influence the distribution and (1990), Bold et al. (1991), Dorzhiyev and Yelayev (1999) breeding success of waterbirds (Skryabin 1965, 1967a, and Popov (2004b), but the waterbird fauna has not 1995b, Skryabin and Tolchin 1975, Lipin et al. -
Plume Moths of Siberia and the Russian Far East P. Y
©Ges. zur Förderung d. Erforschung von Insektenwanderungen e.V. München, download unter www.zobodat.at Atalanta (May 1996) 27 (1/2): 345-409, Wurzburg, ISSN 0171-0079 Plume moths of Siberia and the Russian Far East (Lepidoptera, Pterophoridae) by P. Ya . U s t ju z h a n in received 4.XI.1994 Sum m ary: The study of rich material of Pterophoridae from Siberia and the Russian Far East revealed 96 species to inhabit these regions. 24 of them are reported for the first time from Asian Russia and 11 species and 2 genera (S ibiretta gen. nov. and Septuaginta gen. nov.) are described as new. Furthermore the genus Snellenia gen. nov. is described and isolated from the genus Stenoptilia, and previously unknown females are described for three species. Pe3K>Me: kteyHeHMe öoraToro MaTepnana no Pterophoridae Cn 6npn m fla/ibHero B octoio POCCMM BblflBM/10, MTO Ha 3T0M TeppMTOpHM BCTpeMaiOTCfl 96 BMflOB, 24 H3 KOTOpbIX npMBOflflTCfl Ann AskiaTCKOM P occmm BnepBbie. 11 bmaob h 2 poaa (S ibiretta m Septuaginta) onncbiBaioTCH Kax HOBbie, KpoMe Toro, M3 pofla Stenoptilia BbiaeneH poa Snellenia, a Ann Tpex bmaob onM- CblBaKDTCfl paHee HeM3BeCTHbie C3MKM. This paper summarises an extensive study of rich material of Pterophoridae from Siberia and the Russian Far East, which is referenced below in detail. As a result of this study 96 species were recorded in Asian Russia, 24 of which for the first time, and numerous novel data on species distribution were obtained. Eleven new species and two new genera were estab lished and a new genus S nellenia was isolated from the genus Stenoptilia Hubner . -
Field Course on the Chara River Country: Russia Institution
Field course on the Chara river Country: Russia Institution: Tyumen State Oil and Gas University, Department of Earth Cryology; Institute of Earth Cryosphere of Russian Academy of Science (Siberian Department of Russian Academy of Science) Category: Room course combined with field course Level: PhD, master’s, bachelor’s Course title: Studying the interaction between the permafrost and glaciers Period: 06 July-07August Languages: English, Russian Course instructor: Vladimir S. Sheinkman, associate professor Contact person: Vladimir S. Sheinkman, associate professor E-mail: [email protected] Coordinator: scientific secretary Elena V. Ustinova, tel.: +7 3452 688 785 Short description: Annually, Department of Earth Cryology of Tyumen State Oil and Gas University jointly with Institute of Earth Cryosphere of Russian Academy of Science (Siberian Department of Russian Academy of Science) organizes field course on the Chara river (Zabaykalsky krai) for students. This site is unique thanks to the unique permafrost objects situated next to the Novaya Chara railroad station (three days to go by train from Moscow and two days from Tyumen) among the taiga at the foot of the Kodar ridge (Fig. 1). Fig. 1.The Chara river valley and the Kodar ridge In the cliffs of the river, there are outcrops of ice wedges. (Fig. 2). They are always perfectly seen thanks to the constant river undermining. Fig. 2.Ice wedges in the cliff if the right Chara river bank Besides, right beyond the outcrops, there are moraine fields of ancient glaciers and associated permafrost phenomena. It is possible to reach the headwater of the Sredny Sukan river at the foot of the Pik BAM mountain (3072 m), where the largest glaciers of the South part of Eastern Siberia are situated.