The Concept of Regulated Use of Natural Heritage Sites Included in the Tourist Cluster: a Russian Caves Case Study
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On the Quaternary Reptilian Fauna of Bashkortostan (South Urals, Russia)
©Österreichische Gesellschaft für Herpetologie e.V., Wien, Austria, download unter www.biologiezentrum.at HERPETOZOA 19 (3/4): 99 - 110 99 Wien, 30. Jänner 2007 On the Quaternary reptilian fauna of Bashkortostan (South Urals, Russia) Zur Quartären Reptilienfauna von Baschkortostan (Südural, Rußland) VlNER KHABIBULLIN KURZFASSUNG Die Geschichte der quartären Reptilienfauna von Baschkortostan (Südural, Rußland) wird im Zusammen- hang mit einem kurzen Überblick zur Entwicklung des Klimas, der Landschaften und der Vegetation dargestellt. Fünf Reptilienarten {Lacerta agilis, Anguis fragilis, Lacerta vivipara, Natrix natrix, Vipera berus) sind für das Spätquartär des Untersuchungsgebietes anhand von Fossilbelegen nachgewiesen. Die neuzeitliche Herpetofauna des Urals begann sich im späteren Pliozän herauszubilden. Die gegenwärtige Reptilfauna entwickelte sich im mitt- leren Holozän, mit der Rückkehr der Reptilien aus den eiszeitlichen Refugialräumen. Die Gebirgsketten des Urals sowie die Tätigkeit des Menschen hatten auf die Ausbildung der gegenwärtigen Kriechtierfauna der Region keinen bedeutenden Einfluß. ABSTRACT The history of the Quaternary reptilian fauna of Bashkortostan (South Urals, Russia) is described and the development of climate, landscapes and vegetation are briefly reviewed. Five late Quaternary fossil reptile species {Lacerta agilis, Anguis fragilis, Lacerta vivipara, Natrix natrix, Vipera berus) had been identified for the region. The modern herpetofauna of the Urals started to form approximately in the Late Pliocene. In the -
T H E T I M E W O
GEOGRAPHY OF THE WORLD UralsTHE TIMEWORN GEOGRAPHY OF THE WORLD UralsTHE TIMEWORN By Barbara A. Somervill THE CHILD’S WORLD® CHANHASSEN, MINNESOTA Published in the United States of America by The Child’s World® PO Box 326, Chanhassen, MN 55317-0326 800-599-READ www.childsworld.com Content Adviser: Photo Credits: Cover/frontispiece: TASS/Sovfoto. Interior: Bryan & Cherry Alexander: 18; Animals Animals/Earth Scenes: 9 (OSF/O. Mark Williams, Newman), 14 (Bradley W. Stahl), 17 (Darek Kapp); Corbis: 11 (Steve Raymer), 26 Associate Professor, (Dave G. Houser); Wolfgang Kaehler: 6; Wolfgang Kaehler/Corbis: 8, 16, 21; Jacques University of Colorado, Langevin/Corbis Sygma: 22; Novosti/Sovfoto: 4, 24; TASS/Sovfoto: 5, 12, 13. Boulder, Colorado The Child’s World®: Mary Berendes, Publishing Director Editorial Directions, Inc.: E. Russell Primm, Editorial Director; Melissa McDaniel, Line Editor; Katie Marsico, Associate Editor; Judi Shiffer, Associate Editor and Library Media Specialist; Matthew Messbarger, Editorial Assistant; Susan Hindman, Copy Editor; Sarah E. De Capua and Lucia Raatma, Proofreaders; Marsha Bonnoit, Peter Garnham, Terry Johnson, Olivia Nellums, Chris Simms, Katherine Trickle, and Stephen Carl Wender, Fact Checkers; Tim Griffin/IndexServ, Indexer; Cian Loughlin O’Day, Photo Researcher; Linda S. Koutris, Photo Selector; XNR Productions, Inc., Cartographer The Design Lab: Kathleen Petelinsek, Design and Page Production Copyright © 2005 by The Child’s World® All rights reserved. No part of this book may be reproduced or utilized in any form or by any means without written permission from the publisher. Library of Congress Cataloging-in-Publication Data Somervill, Barbara A. The timeworn Urals / by Barbara A. Somervill. p. -
DRAFT 8/8/2013 Updates at Chapter 40 -- Karstology
Chapter 40 -- Karstology Characterizing the mechanism of cavern accretion as "force" tends to suggest catastrophic attack, not a process of subtle persistence. Publicity for Ohio's Olentangy Indian Caverns illustrates the misconception. Formed millions of years ago by the tremendous force of an underground river cutting through solid limestone rock, the Olentangy Indian Caverns. There was no tremendous event millions of years ago; it's been dissolution at a rate barely discernable, century to century. Another rendition of karst stages, this time in elevation, as opposed to cross-section. Juvenile Youthful Mature Complex Extreme 594 DRAFT 8/8/2013 Updates at http://www.unm.edu/~rheggen/UndergroundRivers.html Chapter 40 -- Karstology It may not be the water, per se, but its withdrawal that initiates catastrophic change in conduit cross-section. The figure illustrates stress lines around natural cavities in limestone. Left: Distribution around water-filled void below water table Right: Distribution around air-filled void after lowering water table. Natural Bridges and Tunnels Natural bridges begin as subterranean conduits, but subsequent collapse has left only a remnant of the original roof. "Men have risked their lives trying to locate the meanderings of this stream, but have been unsuccessful." Virginia's Natural Bridge, 65 meters above today's creek bed. George Washington is said to have surveyed Natural Bridge, though he made no mention it in his journals. More certain is that Thomas Jefferson purchased "the most sublime of nature's works," in his words, from King George III. Herman Melville alluded to the formation in describing Moby Dick, But soon the fore part of him slowly rose from the water; for an instant his whole marbleized body formed a high arch, like Virginia's Natural Bridge. -
Argus Nefte Transport
Argus Nefte Transport Oil transportation logistics in the former Soviet Union Volume XVI, 5, May 2017 Primorsk loads first 100,000t diesel cargo Russia’s main outlet for 10ppm diesel exports, the Baltic port of Primorsk, shipped a 100,000t cargo for the first time this month. The diesel was loaded on 4 May on the 113,300t Dong-A Thetis, owned by the South Korean shipping company Dong-A Tanker. The 100,000t cargo of Rosneft product was sold to trading company Vitol for delivery to the Amsterdam-Rotter- dam-Antwerp region, a market participant says. The Dong-A Thetis was loaded at Russian pipeline crude exports berth 3 or 4 — which can handle crude and diesel following a recent upgrade, and mn b/d can accommodate 90,000-150,000t vessels with 15.5m draught. 6.0 Transit crude Russian crude It remains unclear whether larger loadings at Primorsk will become a regular 5.0 occurrence. “Smaller 50,000-60,000t cargoes are more popular and the terminal 4.0 does not always have the opportunity to stockpile larger quantities of diesel for 3.0 export,” a source familiar with operations at the outlet says. But the loading is significant considering the planned 10mn t/yr capacity 2.0 addition to the 15mn t/yr Sever diesel pipeline by 2018. Expansion to 25mn t/yr 1.0 will enable Transneft to divert more diesel to its pipeline system from ports in 0.0 Apr Jul Oct Jan Apr the Baltic states, in particular from the pipeline to the Latvian port of Ventspils. -
National Speleologi'c-Al Society
Bulletin Number Five NATIONAL SPELEOLOGI'C-AL SOCIETY n this Issue: CAVES IN WORLD HISTORY . B ~ BERT MORGAN THE GEM OF CAVES' . .. .. • B DALE WHITE CA VE FAUN A, with Recent Additions to the Lit ture Bl J. A. FOWLER CAT ALOG OF THE SOCIETY LJBR R . B)' ROBERT S. BRAY OCTOBER, 1943 PRJ E 1.0 0 . ------------------------------------------- .-'~ BULLETIN OF THE NATIONAL SPELEOLOGICAL SOCIETY Issue Number Five October, 1943 750 Copies. 64 Pages Published sporadically by THE NATIONAL SPELEOLOGICAL SOCIETY, 510 Scar Building, Washington, D. c., ac $1.00 per copy. Copyrighc, 1943, by THE NATIONAL SPELEOLOGICAL SOCIETY. EDITOR: DON BLOCH 5606 Sonoma Road, Bethesda-14, Maryland ASSOCIATE EDITORS: ROBERT BRAY WILLIAM J. STEPHENSON J. S. PETRIE OFFICERS AND COMMITTEE CHAIRMEN *WM. ]. STEPHENSON J. S. PETR'IE *LEROY FOOTE F. DURR President Vice·Prcsidet1l & Secretary Treasurer Pina~iaJ Sect'eIM"J 7108 Prospect Avenue 400 S. Glebe Road R. D. 3 2005 Kansas Avenue Richmond, Va. Arlin-glon, Va. Waterbury, Conn. Richmond, Va. Archeology Fauna Hydrology Programs &. Activities FLOYD BARLOGA JAMES FOWLER DR. WM. M. MCGILL DR. JAMES BENN 202·8 Lee Boulevard 6420 14th Street 6 Wayside Place, University U. S. Nat. Museum Arlington, Va. Washington, D . C. Charlottesville, Va. Washington, D. C. Bibliography &. Library Finance Mapping PubliCity *ROBERT BRAY *l.EROY FOOTB GBORGE CRABB *·Lou KLBWEJ.t R. F. D. 2 R. F. D. 3 P. O. Box 791 Toledo Blade Herndon, Va. Waterbury, Conn. Blacksburg, Va. Toledo, Ohio BuIletin &. Publications Folklore Metnbership DON BLOCH "'CLAY PERRY SAM ALLBN RECORDS 5606 Sonoma Road East Acres 1226 Wel.Jesley Avenue *FLORENCE WHITLI!Y Deorhesda, Md. -
Winter in the Urals 7 Mountain Ski Resort “Stozhok” Mountain Ski Resort “Stozhok” Is a Quiet and Comfortable Place for Winter Holidays
WinterIN THE URALS The Government of Sverdlovsk Region mountain ski resorts The Ministry of Investment and Development of Sverdlovsk Region ecotourism “Tourism Development Centre of Sverdlovsk Region” 13, 8 Marta Str., entrance 3, 2nd fl oor Ekaterinburg, 620014 active tourism phone +7 (343) 350-05-25 leisure base wellness winter fi shing gotoural.соm ice rinks ski resort FREE TABLE OF CONTENTS MOUNTAIN SKI RESORTS 6-21 GORA BELAYA 6-7 STOZHOK 8 ISET 9 GORA VOLCHIHA 10-11 GORA PYLNAYA 12 GORA TYEPLAYA 13 GORA DOLGAYA 14-15 GORA LISTVENNAYA 16 SPORTCOMPLEX “UKTUS” 17 GORA YEZHOVAYA 18-19 GORA VORONINA 20 FLUS 21 ACTIVE TOURISM 22-23 ECOTOURISM 24-27 ACTIVE LEISURE 28-33 LEISURE BASE 34-35 WELLNESS 36-37 WINTER FISHING 38-39 NEW YEAR’S FESTIVITIES 40-41 ICE RINKS, SKI RESORT 42-43 WINTER EVENT CALENDAR 44-46 LEGEND address chair lift GPS coordinates surface lift website trail for mountain skis phone trail for running skis snowtubing MAP OF TOURIST SITES Losva 1 Severouralsk Khanty-Mansi Sosnovka Autonomous Okrug Krasnoturyinsk Karpinsk 18 Borovoy 31 Serov Kytlym Gari 2 Pavda Sosva Andryushino Tavda Novoselovo Verkhoturye Alexandrovskaya Raskat Kachkanar Tura Iksa 3 Verhnyaya Tura Tabory Perm Region Niznyaya Tura Kumaryinskoe Basyanovskiy Kushva Tagil Niznyaya Salda Turinsk 27 29 Verkhnyaya Salda Nitza 4 Nizhny Tagil 26 1 Niznyaya Sinyachikha Chernoistochinsk Visimo-Utkinsk Alapaevsk 7 Verkhnie Tavolgi Irbit Turinskaya Sloboda Ust-Utka Chusovaya Visim Aramashevo Artemovskiy Verkhniy Tagil Nevyansk Rezh 10 25 Chusovoe 2 Shalya 23 Novouralsk -
Sverdlovsk Region Sverdlovsk of Resources Natural of Ministry the by Provided Materials *
44, zakaznik-rezh.ru. 44, Mon. to Sun. 10:00-17:00, millennium-tour.ru. 10:00-17:00, Sun. to Mon. the reserve: the town of Rezh, 4 Sovetskaya Street, +7 (34364) 2-25- (34364) +7 Street, Sovetskaya 4 Rezh, of town the reserve: the 1 Vyazovaya Roscha Street, +7-950-547-10-88, +7-950-547-10-88, Street, Roscha Vyazovaya 1 18 item see Administrative department of of department Administrative quarries Lipovskiye to Lipovskoye a rest in summerhouses. in rest a 115 km away from Ekaterinburg through the settlement of of settlement the through Ekaterinburg from away km 115 relax on the beach, go to Russian sauna, have a barbecue party and take take and party barbecue a have sauna, Russian to go beach, the on relax are all open for a visit, including the ‘wild’ Adouiskiy site. site. Adouiskiy ‘wild’ the including visit, a for open all are friendly and easy-going birds, and in summer visitors can go fishing, fishing, go can visitors summer in and birds, easy-going and friendly Hotels of Ekaterinburg. of Hotels +7-912-663-73-97 (Zverev). The main treasure of the reserve is the semi-precious mines – – mines semi-precious the is reserve the of treasure main The (Zverev). varieties are bred on the farm. All the year round tourists can visit the the visit can tourists round year the All farm. the on bred are varieties 15 km away from Ekaterinburg, the village of Medniy Medniy of village the Ekaterinburg, from away km 15 for the settlement of Koltashy – the homeland of Master Danila Danila Master of homeland the – Koltashy of settlement the for different breeds, guinea fowls, quails and other birds – more than 30 30 than more – birds other and quails fowls, guinea breeds, different harness the dogs. -
Fall 2015 Minutes
Lake Ozarks Grotto The Speleograph Volume 45 Issue 2 July-December 2015 Inside this Issue Fantasy World Caverns Hoary Bat Devils Well Kiesewetter Cave Looking back in Time NSS Awards Goodwin Totals Breakdown Christmas Party Soda Straws in Hartwigs Paradise, Kiesewetter Cave The Speleograph is published twice a year by the Lake Ozarks Grotto. All articles and other information is donated by cavers and individuals who have an interest in caving. For more information please visit us on the web: www.lakeozarksgrotto.com The Speleograph Fantasy World Caverns – 2015 The July meeting of Lake Ozarks Grotto was held at Fantasy World Caverns on the 14th. We were to meet at the cave at 6 pm with the cave tour at 7 pm. Gary and I arrived with Travis and Kathy, Derek and Brandon Zumwalt. Chairman Ken Long was already there, visiting with the owner of the cave, Curtis Whitman. It wasn’t long before the rest of the entourage appeared: Cliff Gill, Krista Bartel, Linda Marg, Dwight, Rosie and Karen Weaver. We had a total of eleven members and four guests. The meeting was short and sweaty. So we proceeded into the cave and the coolness. Before we en- tered the cave, Curtis had briefed us on how to behave in the cave. One thing I remember was not to be shining a flashlight all around on the tour in. Well, let me tell you, there were a lot of flashlights shining up walls, down walls and in the water…… But Curtis just kept talking as we were going down the pas- sage. -
Middle-Urals Ring Structure , Ussr
MIDDLE-URALS RING STRUCTURE , USSR: DEFINITION, DESCRIPTION, POSSIBLE PLANETARY ANALOGUXS; G.A.Burba, Vernadsky Institute, Moscotx, 117975, USSR The general straight linear position of Ural Mountains North to South along 60°E meridian is interrupted in the middle part of the range with an eastward facing semicircular curvatu- re. This arc is considered here as an eastern part of a large ring structure, We called it Middle-Urals Ring Structure(Pm~) The structure is located between 54/5g0N, and 52/6z0~. The mi- nimal diameter of its rim is 400 km. The eastern half of the rim is a part of Ural Range: from Ym~aatauMountain on the South to the area of Kachkanar Moun- tain on the North. NW part of the rim is Okhanskaya Vozvyshen- nost (~ighland)North of Kama River, western part is presented by Sarapulskaya Vozv., and SW part - by Bugulminsko-Belebeyevs- kaya Vozv.(South of Belaya River). There are two uprises within the central part of WURS both elongated N to S - Tulvinskaya Vozv, and Sylvbsky Kryazh (~ange). SE part of the PmRS bottom is occupied by Ufimskoye Plateau. The ring structure is outlined with a general pattexn of the large river valleys (~ig,l,position 2): Chusovaya, Belaya, and Kama Rivers (a part of Kama Revalley between the mouths of Chusovaya R. and Belaya R,). A net of a smaller (intermediate- sized) river valleys also outlines a MURS concentric pattern (~ig.1,position 3). The general straight directions of the small-sized river valleys are mainly radial to NURS (J?ig,l, po- sition 4), The hypsometric level of the eastern part of NURS rim is up to 1000-1500 m, NW part - up to 300 m, W - up to 220-250 rn, SW - up to 300-350 m. -
Bulletin Number Seven
~1t==~======:=====, BULLETIN NUMBER SEVEN of the In this Issue: FROM MY CAVE NOTEBOOKS By ALEXANDER WETMORE TECHNIQUE OF CAVERN PHOTOGRAPHY By GEORGE F. JACKSON COMPOSITE OBSER VA TIONS ON CAVE LIFE By JAMES H. BENN CACAHUAMILPA CAVE OF MEXICO By VICTOR S. CRAUN • WASHINGTON, D. C. ~-I -~----~ BULLETIN OF THE NATIONAL SPELEOLOGICAL SOCIETY Issue Number Seven December. 1945. 1000 Copies. 88 Pages Published intermittently by The NatioI].al Speleological Society, 510 Star Building, Washington, D. C., at $1.00 per copy. Copyright, 1945, by The National Speleological Society. EDITOR: DON BLOCH 654 Emerson St., Denver 3: Colorado ASSOCIATE EDITORS: DR. R. W. STONE, . DR. MARTIN H. Mm~1A" FLOYD BARL~GA OFFICERS AND COMMiTTEE CHAIRM.EN *WM. J. STEPHENSON *DR. MAR TIN H. MUMA LEROY \VI. FOOTE J. S. PETRIE President Vice-President TreaS1lrer Correspondillg Secretary 7108 Prospect Avenue 1515 N. 32 St. R. D. 1 400 S. Glebe Road Richmond. Va • . Lincoln. Neb. Middlebury. Conn. Arlington. Va. MRS. KATHARINE MUMA FRANK DURR W. S. HILL R ecording Secretary Financial Secretary The NEWSLETTER 1515 N. 32 St. 2005 Kansas Ave. 2714-A Garland Ave. Lincoln. Neb. Richmond. Va. Richmond. Va. Archeology Fauna Hydrology Publicity *ELOYD BARLOGA • JAMES FOWLER DR. ALFRED HAWKINS GEORGE M. BADGER 2600 Nash St. 6420 14th St. 208 Boscaron St. 1333!.f:z Ohio Ave. ArIing~on. Va. Washington, D. C. Winchester, Va. Long Beach, Cal. Records Bibliography ~ Library Finance Mapping ROBERT MORGAN MRS. BETTY BRAY LERoy W. FOOTE E. EARL PORTER 5014 Caledonia Road R. D. 2 R. D. 1 2602-3rd Ave. Richmond, Va. Herndon, Va. -
Speleothem Samples Collected for Dating Palaeolithic Cave Art in Shulgan-Tash Cave and for Paleoclimate Research in Southern Ural in 2013-2017
Speleothem samples collected for dating Palaeolithic cave art in Shulgan-Tash cave and for paleoclimate research in Southern Ural in 2013-2017 6/20/2018 Technical report Yuri Dublyansky* and Yuri Lyakhnitsky** * Institute of Geology, Innsbruck University, Innrain 52, 6020 Innsbruck, Austria ** A.P. Karpinsky Russian Geological Research Institute (VSEGEI), Sredny prospect 74, 199106 St.-Petersburg, Russia Aknowledgment Work described in this report was partly funded by a grant of the Head of Government of Republic of Bashkortostan R. Khamitov through the State Organization “Scientific-Production Centre for Protection and Use of Objects of Cultural Heritage”, Ministry of Culture of the Republic of Bashkortostan. Additional funding was provided through FWF (Austria) grants P257160 and I027070 to YD. Cite this dataset Dublyansky, Yuri; Lyakhnitsky, Yuri (2018), “Description of speleothem samples collected for U- series dating of Paleolithic cave art in Shulgan-Tash cave, Southern Ural, Russia”, Mendeley Data, v1 http://dx.doi.org/10.17632/c85nth69rb.1 Fig. 1. Google Earth satellite image showing locations of caves from which samples were collected. Coordinates of the center of this map are: 53.03 N, 57.05 E. All caves are located in Southern Ural, Russia. 1. INTRODUCTION Location of caves is shown in Fig. 1. In this report we document: (a) sampling of flowstonein Shulgan- 2. SAMPLING PURPOSES Tash cave for the purpose of dating AND STRATEGIES Palaeolithic parietal art; (b) sampling of stalagmites in Shulgan- 2.1. Sampling flowstone for Tash, Kulyurtamak, Victoria, and dating Palaeolithic Gryoz caves for paleoclimate and cave art paleoenvironmental studies 230 (c) sampling of cryogenic cave calcite The Th-U method has recently emerged as (CCC) in Shulgan-Tash and Victoria a unique tool for accurately and precisely caves for paleoclimate and paleo- dating cave art in the presence of calcite permafrost studies. -
Origin and Evolution of River Systems - V.I
FRESH SURFACE WATER – Vol. I - Origin and Evolution of River Systems - V.I. Babkin ORIGIN AND EVOLUTION OF RIVER SYSTEMS V.I. Babkin Doctor of Geographical Science, State Hydrological Institute, St. Petersburg, Russia Keywords: Geological epochs, formation, hydrography, Earth, river, lakes, sea, ocean, land, erosion, glaciation, runoff, valley, channel. Contents 1. Introduction 2. Primary stage of the occurrence of river systems 3. Development of rivers in the Paleozoic 4. Change of hydrography in the Mesozoic 5. Modification of river systems in the Cenozoic 6. Water balance change of the river basins in the Mesozoic-Cenozoic 7. Features of dynamics of the hydrographic network and channel deformations 8. Hydrography and water resources of the rivers of Eurasia during the period of the last Ice Age and in the Holocene 9. Processes of the formation and development of rivers 10. Conclusion Glossary Bibliography Biographical Sketch Summary The origin of rivers at Earth has a long history. It is related to the appearance and development of the continents and islands as a result of tectonic-magmatic processes as well as to the formation of the Earth’s hydrosphere in the process of juvenile water inflow to the Earth’s surface. A large role in its formation belonged to the processes of complicating global water exchange and erosion development as well as changing climatic conditions. In the processes of their development, rivers changed the direction of their currents and had different water content during the different geological epochs. Their