The Future of Siberia Author(S): Harald Swayne Source: the Geographical Journal, Vol
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
THE GOLDEN MOUNTAINS of ALTAI a Treasure of Biodiversity and Culture Publisher: Altai Alliance
THE GOLDEN MOUNTAINS OF ALTAI A Treasure of Biodiversity and Culture Publisher: Altai Alliance Produced by: Pacific Environment Written by: Jennifer Castner and Pacific Environment Senior Editor and Production Manager: Meerim Kylychbekova Contributors: Chagat Almashev, Matt Foley, Gleb Raygorodetsky, Don Weeden Editors: David Gordon, Leah Zimmerman, Michael Martin Contact: [email protected] Copyright 2009 Cover Photos: Carol Hiltner, World Wildlife Fund, Ashley Tindall (top), Flickrcc/Ilya Schurov (middle), Meerim Kylychbekova (bottom). Design: Design Action Collective THE GOLDEN MOUNTAINS OF ALTAI A Treasure of Biodiversity and Culture 1 THE GOLDEN MOUNTAINS OF ALTAI Introduction Nestled in the Golden Mountains of Altai in south - health, water quality, critical habitat, and the local ern Siberia, the Republic of Altai is a unique blend tourism-based economy. of ancient cultures, stunning landscapes, and extraordinarily high biodiversity. The republic bor - In this paper, we explore why the Altai is a high- ders Mongolia, China, and Kazakhstan, covering priority conservation area, what threats the region 93,000 square kilometers—an area roughly the size faces today, and where the most significant conser - of the state of Indiana. Sacred sites dot the repub - vation opportunities are located. The paper discusses lic’s varied terrain. Its lands include temperate and specific recommendations to engage in and advance boreal forests, dramatic alpine landscapes, rich agri - these conservation opportunities. It focuses on: cultural lands, the wild and scenic Katun River, and • Strengthening cultural and environmental the remote and fragile Ukok Plateau. activism; The republic’s relative isolation and lack of devel - • Promoting alternative energy and green-building opment mean that its landscape and habitats remain technologies; largely intact. -
Part II Middle Katun River Valley BRIEF INTRODUCTION
Russian Altai in the Late Pleistocene and the Holocene CONTENT Introduction 5 Key questions related to the geomorphology of this excursion 9 Princess of Ukok 12 Part I. Upper Biya River valley and the Teletskoye Lake 16 NE Altai Regional settings and Quaternary history: General overview 16 Stop B1. Former glacial-dammed lake in the Yogach valley 23 Stop B2. Former alluvial-dammed lake in the Turachak valley 27 Stop B3. Teletskoye Lake and lacustrine terrace at Yaylyu 31 Geomorphic history of the Teletskoye Lake – Biya valley system: synthesis 35 Part II. Middle Katun River valley 39 Brief introduction 39 Stop K1. Catafluvial deposits of the high (Inya) terrace in the vicinity of the Bolshoi Yaloman River 41 Stop K2. Boulder field at km 702 51 Stop K3. High terraces of the Katun and Injushka Rivers at the Inya village 57 Stop K4. Composition and geochronology of the low (Saldzhar) terrace at the Chuya River confluence 68 Part III. Middle Chuya River valley, Kuray and Chuya Basins 73 Stop C1. Early Holocene seismic fall and dammed lake formation at the Sukhoi brook 73 Stop C2. Late Pleistocene glacial damming of Chuya at Kuektanar tributary valley 77 Stop C3. Lower Chagan-Uzun river: the Late Pleistocene maximal glacial advance 84 Stop C4. Beltir village: consequences of the year 2003 seismic hazard 87 Stop C5. Earthquake triggered giant landslides in the Taldura valley 92 Stop C6. Kuray dunes 99 3 Russian Altai in the Late Pleistocene and the Holocene Stop C7. Kuray strandlines 102 Stop C8. Early Holocene lake in the western part of the Kuray Basin: the Baratal section 108 Stop C9. -
A Runic Inscription at Kalbak-Tash II, Central Altai, with Reference to the Location of the Az Tribe*
THE METAL AGES AND MEDIEVAL PERIOD DOI: 10.17746/1563-0110.2016.44.4.092-101 G.V. Kubarev Novosibirsk State University, Pirogova 2, Novosibirsk, 630090, Russia E-mail: [email protected] A Runic Inscription at Kalbak-Tash II, Central Altai, with Reference to the Location of the Az Tribe* The article introduces and interprets a new runic inscription found at the Kalbak-Tash II petroglyphic site in Centra l Altai. Whereas the adjacent petroglyphic site, Kalbak-Tash I, is the largest collection of Old Turkic runic texts in the Altai Republic and in Russia at large, Kalbak-Tash II has so far yielded only one such inscription, consisting of seven characters. Professor Marcel Erdal has suggested its transliteration, translation, and commentary. The proposed translation reads, “The Horse tribe. Hunters of the Az (tribe), open (the way)!” The inscription, evidently dating to the 8th century, marks boundaries of tribal grazing areas or those of small social units, in this case, the Az tribe. This article considers references to the Az tribe in runic texts from Mongolia and Tuva; various viewpoints regarding their location, affi nities with neighboring tribes, origin, and later history are discussed. This n ew inscription confi rms the common idea that the so-called mountain (or mountain-taiga) Az lived not only in Western Tuva, but also in Eastern and Southern Altai; whereas the steppe Az lived alongside the Qïrqïz in the Khakass- Minusinsk Basin. The culture possibly associated with the Az is the Kudyrge culture in Altai. The Kalbak-Tash II inscription, short though it is, is a signifi cant addition to the well-known Orkhon runic texts addressing the history of the Turkic Khaganates. -
Geological and Geomorphological Background of Cataclysmic Debris Flooding in the Altai Mountain Rivers
GEOGRAPHY AND TOURISM, Vol. 4, No. 2 (2016), 75-81, Semi-Annual Journal eISSN 2449-9706, ISSN 2353-4524, DOI: 10.5281/zenodo.223926 © Copyright by Kazimierz Wielki University Press, 2016. All Rights Reserved. http://geography.and.tourism.ukw.edu.pl Gennady Y. Baryshnikov Altai State University, Barnaul, Russia, email: [email protected] Geological and geomorphological background of cataclysmic debris flooding in the Altai mountain rivers Abstract: Article discusses effects of catastrophic floods on the rivers in the Altai Mountains. The whole complex of flood- plain terraces of the main rivers – the Biya and Katun was formed by insertion of these rivers in the loose deposits, that was formed as the one-act occurrence associated with glacial-dammed lakes – the Prateletskie and Chui-Kuraipaleovo- doema. This conclusion is confirmed by a series of radiocarbon age determinations of sediments and opto-luminescence dating. Keywords: Altai Mountains, above the floodplain terrace, glacier, moraine, alluvium, catastrophic flooding, radiocarbon dating. Floods in the Altai Mountains were largely Today there is much obtained actual data determined by the climatic conditions of on the terrace sediments in the Upper Priob’ye the region, that in the past was related to the region. Numerous studies of terraces quantity increase in temperature and intensive deglaci- and their age based on common geomorpholog- ation, with subsequent formation of ice-mar- ical observations, groundwater bore data, paly- ginal lakes and their outflow through the nological and paleocarpological materials, small arterial rivers. These were catastrophic flood- mammal fauna justification, molluscan shells, ing phenomena. At the present day the most a number of radiocarbon dates interpreted as important triggering factor for floods is abun- organic deposits of alluvial sediments in the Ob dant precipitation in the mountains succeeded river, lead to contradictory conclusions. -
Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains
geosciences Article Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains Dmitrii A. Ganyushkin 1,* , Sofia N. Lessovaia 1, Dmitrii Y. Vlasov 2, Gennady P. Kopitsa 3,4 ,László Almásy 5 , Kirill V. Chistyakov 1, Elena G. Panova 1, Ekaterina Derkach 1 and Anastasiya Alekseeva 1 1 Institute of Earth Sciences, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, Russia; [email protected] (S.N.L.); [email protected] (K.V.C.); [email protected] (E.G.P.); [email protected] (E.D.); [email protected] (A.A.) 2 Biological Faculty, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, Russia; [email protected] 3 B.P. Konstantinov Petersburg Nuclear Physics Institute NRC KI, Orlova roshcha, d. 1, 188300 Gatchina, Russia; [email protected] 4 I.V. Grebenshchikov Institute of Silicate Chemistry RAS, nab. Adm. Makarova, d. 2, 199155 St. Petersburg, Russia 5 Centre for Energy Research, Institute for Energy Security and Environmental Safety, Konkoly-Thege ut. 29–33, 1121 Budapest, Hungary; [email protected] * Correspondence: [email protected]; Tel.: +7-921-3314-598 Citation: Ganyushkin, D.A.; Abstract: For the Altai Mountains’ region, especially the arid southeastern part of the Russian Altai, Lessovaia, S.N.; Vlasov, D.Y.; Kopitsa, the data on glacier fluctuations in the Pleistocene and Holocene are still inconsistent. The study area G.P.; Almásy, L.; Chistyakov, K.V.; was the Kargy River’s valley (2288–2387 m a.s.l.), a location that is not currently affected by glaciation Panova, E.G.; Derkach, E.; Alekseeva, and the glacial history of which is poorly studied. -
With L European Species .S°U*E™ B * N PV Rj' Ff WJ^F?
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Braueria Jahr/Year: 2007 Band/Volume: 34 Autor(en)/Author(s): Ivanov Vladimir D., Melnitsky Stanislav I. Artikel/Article: New data of the Trichoptera of Siberia 31-35 © Hans Malicky/Austria; download unter www.biologiezentrum.at 31 BRAUERIA (Lunz am See, Austria) 34:31-35 (2007) Hydropsychidae Curtis, 1835 New data of the Trichoptera of Siberia Cheumatopsyche lepida (PICTET, 1834) Chita Region, Makkaveevka (60 KM SE from Chita), r. Ingoda, Vladimir D.IVANOV&Stanislav I. MELNITSKY 04.06^02, numerous adults. First record for Eastern Siberia; the easternmost point in the areal Abstract. Recent collections made in South Siberia yielded of this species. 109 species from 16 families; some of them are new for Hydropsyche angustipenn^ (CURTIS, 1834) certain regions in this territory: 10 for Siberia, 2 for East „J^. ™ayma (6 ^ N from Gorno-Altaysk), r. Zemiyanaya, Siberia, 21 for the Altai Mts, 5 for Pribaikalie, 3 for the Chita ^Ö.UÖ.UJ I. region, 1 for Buryatia. The distributions of some species are nrst record tor Altai. discussed. The fauna of river Ingoda (upper Amur Basin) has Hydropsyche contubernali* MACLACHLAN, 1865 S U e B spring and summer component! with L European species R . ° * ™ *n PV rJ' f f WJ^f? nrevailinp in snrinp Region, Makkaveevka (60 KM SE from Chita), r. Ingoda, 4.06.02, 5 f; prevailing in spring. Novosibirsk, r. Ob1, 28.08.03, 9 m, 7 f; Southern Buryatia, vie. ..... Gusinoe Ozero, small lakes south to the Gusinoe Lake, 12.08.05, If; Southern Buryatia, lake Tsaidam, 1 km south of the Gusinoe Lake, c-u • • -r .u n • -. -
Recurrence Interval of Strong Earthquakes in the Se Altai, Russia Revealed by Tree-Ring Analysis and Radiocarbon Dating
GEOCHRONOMETRIA 45 (2018): 20–33 DOI 10.1515/geochr-2015-0083 Available online at http://www.degruyter.com/view/j/geochr Conference Proceedings of the 12th International Conference “Methods of Absolute Chronology” May 11-13th, 2016, Gliwice-Paniówki, Poland RECURRENCE INTERVAL OF STRONG EARTHQUAKES IN THE SE ALTAI, RUSSIA REVEALED BY TREE-RING ANALYSIS AND RADIOCARBON DATING ROMAN K. NEPOP1, 2 and ANNA R. AGATOVA1, 2 1Sobolev Institute of Geology and Mineralogy, Koptyuga av., 3, Novosibirsk, 630090 Russia 2Ural Federal University, Yekaterinburg, Mira str., 19, 620002 Russia Received 28 June 2016 Accepted 23 October 2017 Abstract: This paper presents the results of paleoseismogeological investigations including tree-ring analysis and radiocarbon dating in pleistoseist zone of the 2003 Chuya earthquake, SE Altai, Russia. Twenty-five radiocarbon dates of previously unknown evidences of prehistoric earthquakes along the fault bounders of the Chagan-Uzun massif, North Chuya and South Chuya ranges are reported. Per- spectives of applying dendroseismological approach within the high mountainous seismically active southeastern part of Russian Altai are demonstrated. In addition to estimating the germination ages of trees growing on the bare surfaces of seismically triggered landslides, analysis of wood penetrating injuries in the individual tree ring series was applied for dating paleorock-falls. Analysis of distribu- tion patterns of tree-ring anomalies and injured trees suggests a criterion of recognizing seismic origin of past rock-falls. Dendrochronologically obtained dates of abrupt intensifications of rock-falls can be considered as supposed dates of past earthquakes, which should be verified by alternative proxy data. Obtained results argue for the high regional seismicity in the second half of the Holocene. -
FLOOD and MEGAFLOOD PROCESSES and DEPOSITS: RECENT and ANCIENT EXAMPLES IFAA01 9/12/08 4:26 PM Page Ii IFAA01 9/12/08 4:26 PM Page Iii
IFAA01 9/12/08 4:26 PM Page i FLOOD AND MEGAFLOOD PROCESSES AND DEPOSITS: RECENT AND ANCIENT EXAMPLES IFAA01 9/12/08 4:26 PM Page ii IFAA01 9/12/08 4:26 PM Page iii SPECIAL PUBLICATION NUMBER 32 OF THE INTERNATIONAL ASSOCIATION OF SEDIMENTOLOGISTS Flood and Megaflood Processes and Deposits: Recent and Ancient Examples EDITED BY I. PETER MARTINI, VICTOR R. BAKER AND GUILLERMINA GARZÓN IFAA01 9/12/08 4:26 PM Page iv © 2002 International Association of Sedimentologists distributors and published for them by Marston Book Services Ltd Blackwell Science Ltd PO Box 269 Editorial Offices: Abingdon, Oxon OX14 4YN Osney Mead, Oxford OX2 0EL (Orders: Tel: 01235 465500 25 John Street, London WC1N 2BS Fax: 01235 465555) 23 Ainslie Place, Edinburgh EH3 6AJ 350 Main Street, Malden The Americas MA 02148-5018, USA Blackwell Publishing 54 University Street, Carlton c/o AIDC Victoria 3053, Australia PO Box 20 10, rue Casimir Delavigne 50 Winter Sport Lane 75006 Paris, France Williston, VT 05495-0020 (Orders: Tel: 800 216 2522 Other Editorial Offices: Fax: 802 864 7626) Blackwell Wissenschafts-Verlag GmbH Kurfürstendamm 57 Australia 10707 Berlin, Germany Blackwell Science Pty Ltd 54 University Street Blackwell Science KK Carlton, Victoria 3053 MG Kodenmacho Building (Orders: Tel: 3 9347 0300 7–10 Kodenmacho Nihombashi Fax: 3 9347 5001) Chuo-ku, Tokyo 104, Japan Iowa State University Press A catalogue record for this title A Blackwell Science Company is available from the British Library 2121 S. State Avenue Ames, Iowa 50014-8300, USA ISBN 0-632-06404-8 The right of the Authors to be Library of Congress identified as the Authors of this Work Cataloging-in-Publication Data has been asserted in accordance with the Copyright, Designs and Flood and megaflood processes and deposits: Patents Act 1988. -
Case Study of Katun River and Lake Teletskoye, Altai (Siberia)
NATURAL MERCURY LEVELS IN GEOLOGICAL ENRICHED AND GEOLOGICAL ACTIVE AREAS: CASE STUDY OF KATUN RIVER AND LAKE TELETSKOYE, ALTAI (SIBERIA) W. BAEYENS1*, B. DEHANDSCHUTTER2, M. LEERMAKERS1, V. A. BOBROV3, R. HUS4 and D. BAEYENS-VOLANT5 1 Analytical and Environmental Chemistry (ANCH), Vrije Universiteit Brussel (VUB), BRUEGEL, Brussels, Belgium; 2 Department of Geology, Vrije Universiteit Brussel (VUB), Brussels and Department o f Geology, Royal Museum o f Central Africa (KMMA), Tervuren, Belgium; 3 United Institute of Geology, Geophysics and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Novosibirsk, Russia; 4 Renard Centre of Marine Geology, Universiteit Gent (UG), Gent, Belgium; 5 General Chemistry, Faculty of Medicine, Université Libre de Bruxelles (ULB), Brussels, Belgium (* author for correspondence, e-mail:[email protected] , fax: 32 2 629 3274) (Received 6 September 2001; accepted 23 May 2002) Abstract. Natural geological Hg deposits control the Hg levels in the upper Katun river. Very high levels of total Hg are observed in the watercolumn (up to 20 ng L_1) and the sediments (up to 244 /xg g_1) close to the deposit area, but almost normal levels (1.8 ng L_1 in the water column and 0.14 /xg g_1 in the sediments) are reached 60 km downstream of that zone. In general, low dissolved methylmercury (MMHg) concentrations were found (0.04-0.05 ng L_1) due to unfavour able méthylation conditions. The MMHg concentrations in the sediments vary from 23.3 ng g_1, in the vicinity of the geological Hg deposits, to 0.17 ng g_1 60 km downstream. Total Hg levels in Lake Teletskoye (a geological active area) are slightly increased (1.1-1.8 ng L_1) compared to Lake Baikal and fairly constant alover the Lake, suggesting multiple sources. -
The Altai Flood
THE ALTAI FLOOD OVERVIEW The Altai Mountains lie in the center of the largest landmass on Earth, the area most distant from any ocean [Fig.1]. The Altai Mountains straddle the common borders of Russia, Kazakhstan, China, and Mongolia. The north slopes of this range in southern Siberia are drained by the headwaters of the Ob River, which flows north to the Arctic Ocean. Toward the end of the last glacial period, about 11,000 to 13,000 years ago, surging alpine and outlet glaciers in the Altai dammed montane rivers, creating large glacial lakes. These ice dams subsequently failed, causing catastrophic floods. The largest of these floods resulted from emptying two interconnected lakes on the Chuya River; this flood is referred to here as the Altai Flood. Floodwaters rushed into paleo-Lake Mansi, causing the lake level to rise enough to overtop the Turgay Spillway and flow southwest into the Aral Sea. This, in turn, spilled into the Caspian Sea, then the Black Sea, and eventually into the Mediterranean Sea [Fig. 2]. The Chuya Basin is the most distal part of the Ob River drainage, at the Mongolian border [Fig. 3]. This basin was dammed by a surging glacier from the Chagan Uzun River, creating Lake Chuya. Figure 1—Altai area and the Eurasian landmass. Just downstream, surging glaciers from the Aktash and Maashay Valleys coalesced to dam the lower end of the Kuray Basin, creating Lake Kuray. Lake Kuray probably spilled over local divides upstream into Lake Chuya and established a common level for the lake system. This lake system stored 3500 km3 of water, deeper than 900 m at the lower ice dam. -
The Affected Areas and Zonation by the Degree of Mud Flow Hazard. On
the affected areas and zonation by the degree of mud flow hazard. On developed and undeveloped territories of Arshan and its environs, hazardous, potentially hazardous and non- hazardous areas have been distinguished. A map of mudflow hazard is necessary for sound management of the territories and for further sustainable development. Availability of large- scale charts (maps, plans) of mudflow hazard zones of the territory will allow to work out full measures that contribute to protection of the population and infrastructure from mudflow processes. The works are intended to prevent and or reduce economic losses by development of natural hazards. In the future, there is need to develop limitation plan schemes to the general plans of Arshan village, which allows to determine the impact of mud flow on economic facilities, to select the location for reliable and safe facilities. In conclusion, it should be noted that the mud flows in Arshan village on June 28, 2014 may serve an example of natural disasters that should be considered when selecting and evaluating engineering construction sites by the degree of hazard. The caused economic damage from the mudslides in the village is conditioned by the geographical location (Arshan settlement is situated at the altitude of 893 m at the exit point of the Kyngarga River on the northern outskirts of the Tunka valley at the foot of the southern slope of Tunka bold mountains) as well as by geological and geomorphological features (the village occupies a part of ancient alluvial fan of the Kyngarga River and the streams, flowing into it from the east and originating from the kar valleys filled with moraine sediments). -
Come Hell Or High Altai Water Eugene Kaspersky
Eugene Kaspersky Come Hell or High Altai Water Eugene Kaspersky Come Hell or High Altai Water From the author In my piggy bank of mind-blowing places on In 2016 I was lucky enough to spend a full three Briefly, our route went like this: the planet I’ve been to, Altai ranks up there weeks in Altai with the group of like-minded as one of the most fascinating and magical adventurers I often go away on an extreme In all we walked around 70 kilometers to Lake of them all. vacation with. We trekked, we choppered, Akkem and then round it; we flew around we rafted (down the Katun River), and – of Mount Belukha in a helicopter; and we flew But that’s not only because Altai is off-the- course – we snapped lots of pics, which fill out up to the headwaters of the Katun and rafted scale beautiful; there’s something else about most of this book you’re now holding, if you down to the lower reaches of the river – the place. It might be some sort of special haven’t already guessed. almost 400km (four HUNDRED kilometers!!) energy in the rocks, something in the air, in all and descending over a kilometer on the something in the water, or something else vertical axis. And that was how I spent the we’ll never fathom. It’s just that here the summer that year. colors are brighter, the water is tastier, the grass is greener, and the mountains contrast all the more against their surroundings.