A Right to Remoteness? a Missing Bridge and Articulations of Indigeneity Along an East Siberian Railroad
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
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. -
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. -
The Giant Sukhoi Log Gold Deposit. Siberia
RussiaaGeology ' Geoloeila - ond Geophtsics i Geofrzita Vol. 47, No. 3, pp. 3 15-341, 2N6 UDC553.,U1(571.53) THE GIANT SUKHOI LOG GOLD DEPOSIT.SIBERIA B.L. Woodl and NP. Popov* StarTechnology SystemsN.L, Moscow, Russi4 PO Box 6325 , Univenity of NSfi Sy&rey, NSW 1466, Australio + Lenzolato Open foint Stock Compoty, Bodaibo, Russia The Sukhoi Log gold deposit is cenhally located in the L,€nagoldfield region, approximately 850 lcn IrlE fmm the city of Irkutsk, aad is hoshd in Upper Proterozoic marine sandstone, carbonaceous slate and phyuita, metemorphos€d to low greensddst faci€s in an ouflying part of the major Akitkan Foldbelt. Ihe disseminated pyritic tabular orebody has no outcrop, is defined solely by assay grades and is located in the axial zone of a large, near-isoclinal, reclining anticline" Highest ore grades occur in pyritic black shale b€ds, especially where they cross the axial zone and include two elongate high€r grade ('1-9 ppn gold) cylindrical zones, term€d ore pillars, along the gently plunging anticlinal crest The anticline is exposed E-W over a length of 3 km and plunges at approximately 10' degrees NW. The uial plane and orebody dip 15" N, and the tatter is open to depth beyond 4fi) m. Three phases of syn- and post-metamorphic rnesoscopicfolding develop€d eharacteristic structures. The first two (Fr and F2) are congruent with the anticline and localized quarE-pyrite-gold veinlet mineralization in Fr axial plane deavages(St), in narro% spaced axial zonesof small non-penehative folds (Fz), in irregular ilisseminated zonesin shale,and in small inegular clusters (stringers) of q[arb-csrbonatc veins. -
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. -
Exhibition Catalogue with Descriptions (Please Return After Viewing the Exhibition)
Exhibition Catalogue with Descriptions (Please return after viewing the exhibition) Picturing the Baikal-Amur Mainline (BAM): Infrastructure, Resources, and Mobility in Siberia 2 1) The BAM Story 3 2) Introducing the Feldpraktikum 4 3) Riding the BAM 5 4) The BAM as a Lifeline 6 5) Cities and Towns along the BAM 7 6) Getting Resources to the BAM 8 7) Resource Extraction along the BAM 9 8) Individual Traffic 10 9) Performing Diversity 11 10) About Methods 12 11) Reflections on/from the Field 13 Authors and Contact Information 14 1 Picturing the Baikal-Amur Mainline (BAM): Infrastructure, Resources, and Mobility in Siberia Siberia holds a special place in the popular imagination – romantic images of undisturbed boreal forests and of simple life styles alter with dark notions of exile and slave labor, for some a place “between heaven and hell”. The industrial development of Siberia, which had been in full swing at least since the days of Stalin, typically is not prominently associated with Siberia. Our exhibition intends to fill this gap by focusing on aspects of the built environment that resulted from the construction of the Baikal-Amur Mainline (BAM). This large-scale transportation infrastructure was built in the 1970s and 1980s to extract and transport resources out of the northern parts of East Siberia and the Russian Far North. The territory traversed by the BAM is bigger than most countries in Central Europe and the distances between settlements are enormous. While the railroad line might be the defining infrastructure object of the region, it is by far not the only one. -
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. -
VI. Republic of Sakha (Yakutia) Overview of the Region Josh
Saving Russia's Far Eastern Taiga : Deforestation, Protected Areas, and Forests 'Hotspots' VI. Republic of Sakha (Yakutia) Overview of the Region Josh Newell Location The Republic of Yakutia (Sakha), situated in northeastern Siberia, stretches to the Henrietta Islands (77 N) in the far north and is washed by the Arctic Ocean (Laptev and Eastern Siberian Seas). These waters, the coldest and iciest of all seas in the northern hemisphere, are covered by ice for 9 to 10 months of the year. The Stanovoy Ridge (55 D. 30 D. N) borders Yakutia in the south, the upper reaches of the Olenyok River form the western border, and Chukotka forms the eastern border (165 E). Size Almost one-fifth of the territory of the Russian Federation (3,103,200 sq. km.) and greater than the combined areas of France, Austria, Germany, Italy, Sweden, England, Greece, and Finland. Climate Winter is prolonged and severe, with average January temperatures about -40C. Summer is short but warm; the average in July is 13C and temperatures have reached 39C in Yakutsk. In the northeast, the town of Verekhoyansk reaches -70C (-83F) and is considered the coldest inhabited place on Earth. There is little precipitation - from 150-200 mm. in Central Yakutia to 500-700 mm. in the mountains of eastern and southern Yakutia. Geography and Ecology Forty percent of Yakutia lies within the Arctic Circle and all of it is covered by eternally frozen ground- permafrost - which greatly influences the region's ecology and limits forests to the southern region. Yakutia can be divided into three great vegetation belts. -
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. -
Sensory Perception of Rock Art in East Siberia and the Far East Soviet Archeological “Discoveries” and Indigenous Evenkis
Sensory Perception of Rock Art in East Siberia and the Far East Soviet Archeological “Discoveries” and Indigenous Evenkis DONATAS BRANDIŠAUSKAS Abstract: This article shows how the sensory perception of rock art guided both archeologists’ interpretations as well as indigenous worldviews in Eastern Siberia and the Russian Far East. The research is based on the author’s ethnographic fieldwork research among in- digenous communities of the Olekma, Chara, Aldan, and Amur, and Vitim river basins in the Sakha Republic, the Amur and Zabaikalskii regions, and the Republic of Buriatiia. The article discusses Evenki herders’ and hunters’ interactions with the rock art sites and demon- strates how these sites have served as a source of ritual and cosmo- logical inspiration. Rock art research has also been inseparable from intuitive and embodied experiences for researchers in the field who interact with rock art. Keywords: archaeology, East Siberia, Far East, history of the Siberian rock art research, indigenous Evenkis, perception of rock art, rituals Everyone who had ever had a chance to be in places outlined in the monograph knows, what kind of strength, dedication and desire to overcome one’s limitations a person needs just to see these monu- ments [rock art] since the location of them often are kept in secret in order to avoid evil shamanic spirits. —A. P. Okladnikov and A. I. Mazin (1976) he region that embraces the Lena, Olekma, Aldan, and Amur rivers basins has the densest concentration of rock art paintings Tin Eastern Siberia and the Russian Far East. Starting in the eighteenth century, every famous expedition led by imperial explorers with eth- nographic, archaeological, geographical, and historical interests of this remote and unexplored region also paid attention to rock art as objects Sibirica Vol.