– – Medieval Novgorod in Its Wider Context
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Review and Updated Checklist of Freshwater Fishes of Iran: Taxonomy, Distribution and Conservation Status
Iran. J. Ichthyol. (March 2017), 4(Suppl. 1): 1–114 Received: October 18, 2016 © 2017 Iranian Society of Ichthyology Accepted: February 30, 2017 P-ISSN: 2383-1561; E-ISSN: 2383-0964 doi: 10.7508/iji.2017 http://www.ijichthyol.org Review and updated checklist of freshwater fishes of Iran: Taxonomy, distribution and conservation status Hamid Reza ESMAEILI1*, Hamidreza MEHRABAN1, Keivan ABBASI2, Yazdan KEIVANY3, Brian W. COAD4 1Ichthyology and Molecular Systematics Research Laboratory, Zoology Section, Department of Biology, College of Sciences, Shiraz University, Shiraz, Iran 2Inland Waters Aquaculture Research Center. Iranian Fisheries Sciences Research Institute. Agricultural Research, Education and Extension Organization, Bandar Anzali, Iran 3Department of Natural Resources (Fisheries Division), Isfahan University of Technology, Isfahan 84156-83111, Iran 4Canadian Museum of Nature, Ottawa, Ontario, K1P 6P4 Canada *Email: [email protected] Abstract: This checklist aims to reviews and summarize the results of the systematic and zoogeographical research on the Iranian inland ichthyofauna that has been carried out for more than 200 years. Since the work of J.J. Heckel (1846-1849), the number of valid species has increased significantly and the systematic status of many of the species has changed, and reorganization and updating of the published information has become essential. Here we take the opportunity to provide a new and updated checklist of freshwater fishes of Iran based on literature and taxon occurrence data obtained from natural history and new fish collections. This article lists 288 species in 107 genera, 28 families, 22 orders and 3 classes reported from different Iranian basins. However, presence of 23 reported species in Iranian waters needs confirmation by specimens. -
Characteristics of the Regime and Structure of Water Masses in the Volga Reservoirs
Characteristics of the regime and structure of water masses in the Volga reservoirs N. V. Butorin Abstract. The characteristics of the hydrological regime of reservoirs is shown in peculiarities of the water balance, water circulation, level, wave, temperature and ice regimes. The peculiarities of the hydrological regime lead to heterogeneity in the physical and chemical characteristics of the water. Detailed analysis of these characteristics makes it possible to identify distinct water masses with different properties in reservoirs. Resume. Los traits spécifiques du regime hydrologique des reservoirs se manifestent dans les particularités du bilan hydrologique, de la circulation de l'eau et dans les particularités des régimes des vagues, des températures et des glaces. Ces particularités du régime hydrologique conduisent à l'hétérogénéité physique et chimique de la masse d'eau. L'analyse complexe des champs de ces caractéristiques nous permet d'établir la présence dans les réservoirs des masses d'eau présentant des particularités différentes. The use of natural water resources under modem technological progress is limited by the peculiarities of their geographical distribution, their seasonal and yearly fluctuations and also by considerable water pollution from domestic and industrial waste. One of the most effective means of controlling water resources is by creating reservoirs. Reservoirs are becoming an essential feature of the landscape. Each of them is a complex geographical object. Reservoirs differ from other water bodies in their bed morphology, in the interaction of the water mass with the bottom and the shores, in the physical and chemical properties of the waters and their dynamics, The main characteristic feature of a reservoir is its slow water exchange and the possibility of regulating it. -
The German 290Th Infantry Division at Demyansk by Henning Nagel and Vance Von Borries
The German 290th Infantry Division at Demyansk By Henning Nagel and Vance von Borries During September 1941 the summer advance into the Soviet Union by German Army Group North had largely ended. In the north, units of the Army Group’s 18th Army laid siege to Leningrad while to the east and south they stood against Soviet efforts to relieve the great siege. To the south, 16th Army entered the Valday Hills region, taking Demyansk on September 8th thereby securing Army Group North’s southern flank and establishing a link with its neighbor, Army Group Center. By the end of November the 16th Army conducted little more than local actions and the campaign in the area settled in to static warfare. The main German effort had shifted south to Army Group Center in front of Moscow. Yet, as Army Group Center began to close around Moscow, it too lost momentum and shifted to the defensive. Then the Soviets struck. What began as a limited counter-offensive against Army Group Center in December grew by January 1942 into a general strategic offensive that threatened to expel the Germans from much of the Soviet Union. Practically all German divisions in Russia were caught up in the winter campaign and at times each would find itself thrown back on its own resources. Little else would be available. In the Demyansk/Valday area all German divisions worked together and each played an important role, sometimes critical, in withstanding the Soviet tide. The story of the 290th illustrates how these divisions held together. The 290th Infantry Division (ID), part of 16th Army’s X.Army Corps in the Valday region, had been formed in March and April 1940 in the Munsterlager Troop Maneuver Area from newly trained north German personnel. -
Surface Runoff to the Black Sea from the East European Plain During Last Glacial Maximum–Late Glacial Time
Downloaded from specialpapers.gsapubs.org on September 18, 2012 The Geological Society of America Special Paper 473 2011 Surface runoff to the Black Sea from the East European Plain during Last Glacial Maximum–Late Glacial time Aleksey Yu. Sidorchuk Andrey V. Panin Geographical Faculty, Moscow State University, Vorob’evy Gory, Moscow 119991, Russia Olga K. Borisova Institute of Geography, Russian Academy of Sciences, Staromonetny per., Moscow 119017, Russia ABSTRACT Hydromorphological and hydroclimatic methods were used to reconstruct the former surface runoff from the East European part of the Black Sea drainage basin. Data on the shape and dynamics of the last Fennoscandian ice sheet were used to cal- culate meltwater supply to the headwaters of the Dnieper River. The channel width and meander wavelength of well-preserved fragments of large paleochannels were measured at 51 locations in the Dnieper and Don River basins (East European Plain), which allowed reconstruction of the former surface runoff of the ancient rivers, as well as the total volume of fl ow into the Black Sea, using transform functions. Studies of the composition of fossil fl oras derived from radiocarbon-dated sediments of vari- ous origins and ages make it possible to locate their modern region analogues. These analogues provide climatic and hydrological indexes for the Late Pleniglacial and Late Glacial landscapes. Morphological, geological, geochronological, and palyno- logical studies show that the landscape, climatic, and hydrologic history of the region included: -
Revised Draft Experiences with Inter Basin Water
REVISED DRAFT EXPERIENCES WITH INTER BASIN WATER TRANSFERS FOR IRRIGATION, DRAINAGE AND FLOOD MANAGEMENT ICID TASK FORCE ON INTER BASIN WATER TRANSFERS Edited by Jancy Vijayan and Bart Schultz August 2007 International Commission on Irrigation and Drainage (ICID) 48 Nyaya Marg, Chanakyapuri New Delhi 110 021 INDIA Tel: (91-11) 26116837; 26115679; 24679532; Fax: (91-11) 26115962 E-mail: [email protected] Website: http://www.icid.org 1 Foreword FOREWORD Inter Basin Water Transfers (IBWT) are in operation at a quite substantial scale, especially in several developed and emerging countries. In these countries and to a certain extent in some least developed countries there is a substantial interest to develop new IBWTs. IBWTs are being applied or developed not only for irrigated agriculture and hydropower, but also for municipal and industrial water supply, flood management, flow augmentation (increasing flow within a certain river reach or canal for a certain purpose), and in a few cases for navigation, mining, recreation, drainage, wildlife, pollution control, log transport, or estuary improvement. Debates on the pros and cons of such transfers are on going at National and International level. New ideas and concepts on the viabilities and constraints of IBWTs are being presented and deliberated in various fora. In light of this the Central Office of the International Commission on Irrigation and Drainage (ICID) has attempted a compilation covering the existing and proposed IBWT schemes all over the world, to the extent of data availability. The first version of the compilation was presented on the occasion of the 54th International Executive Council Meeting of ICID in Montpellier, France, 14 - 19 September 2003. -
2018 FIFA WORLD CUP RUSSIA'n' WATERWAYS
- The 2018 FIFA World Cup will be the 21st FIFA World Cup, a quadrennial international football tournament contested by the men's national teams of the member associations of FIFA. It is scheduled to take place in Russia from 14 June to 15 July 2018,[2] 2018 FIFA WORLD CUP RUSSIA’n’WATERWAYS after the country was awarded the hosting rights on 2 December 2010. This will be the rst World Cup held in Europe since 2006; all but one of the stadium venues are in European Russia, west of the Ural Mountains to keep travel time manageable. - The nal tournament will involve 32 national teams, which include 31 teams determined through qualifying competitions and Routes from the Five Seas 14 June - 15 July 2018 the automatically quali ed host team. A total of 64 matches will be played in 12 venues located in 11 cities. The nal will take place on 15 July in Moscow at the Luzhniki Stadium. - The general visa policy of Russia will not apply to the World Cup participants and fans, who will be able to visit Russia without a visa right before and during the competition regardless of their citizenship [https://en.wikipedia.org/wiki/2018_FIFA_World_Cup]. IDWWS SECTION: Rybinsk – Moscow (433 km) Barents Sea WATERWAYS: Volga River, Rybinskoye, Ughlichskoye, Ivan’kovskoye Reservoirs, Moscow Electronic Navigation Charts for Russian Inland Waterways (RIWW) Canal, Ikshinskoye, Pestovskoye, Klyaz’minskoye Reservoirs, Moskva River 600 MOSCOW Luzhniki Arena Stadium (81.000), Spartak Arena Stadium (45.000) White Sea Finland Belomorsk [White Sea] Belomorsk – Petrozavodsk (402 km) Historic towns: Rybinsk, Ughlich, Kimry, Dubna, Dmitrov Baltic Sea Lock 13,2 White Sea – Baltic Canal, Onega Lake Small rivers: Medveditsa, Dubna, Yukhot’, Nerl’, Kimrka, 3 Helsinki 8 4,0 Shosha, Mologa, Sutka 400 402 Arkhangel’sk Towns: Seghezha, Medvezh’yegorsk, Povenets Lock 12,2 Vyborg Lakes: Vygozero, Segozero, Volozero (>60.000 lakes) 4 19 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 30 1 2 3 6 7 10 14 15 4,0 MOSCOW, Group stage 1/8 1/4 1/2 3 1 Estonia Petrozavodsk IDWWS SECTION: [Baltic Sea] St. -
Материалы Совещания Рабочей Группы INQUA Peribaltic
САНКТ-ПЕТЕРБУРГСКИЙ ГОСУДАРСТВЕННЫЙ УНИВЕРСИТЕТ Материалы совещания рабочей группы INQUA Peribaltic Из сборника материалов совместной международной конференции «ГЕОМОРФОЛОГИЯ И ПАЛЕОГЕОГРАФИЯ ПОЛЯРНЫХ РЕГИОНОВ», симпозиума «Леопольдина» и совещания рабочей группы INQUA Peribaltic, Санкт-Петербург, СПбГУ, 9 – 17 сентября 2012 года Санкт-Петербург, 2012 SAINT-PETERSBURG STATE UNIVERSITY Proceedings of the INQUA Peribaltic Working Group Workshop From the book of proceeding of the Joint International Conference “GEOMORPHOLOGY AND PALАEOGEOGRAPHY OF POLAR REGIONS”, Leopoldina Symposium and INQUA Peribaltic Working Group Workshop, Saint-Petersburg, SPbSU, 9-17 September, 2012 Saint-Petersburg, 2012 УДК 551.4 Ответственные редакторы: А.И. Жиров, В.Ю. Кузнецов, Д.А. Субетто, Й. Тиде Техническое редактирование и компьютерная верстка: А.А. Старикова, В.В. Ситало Обложка: К.А. Смыкова «ГЕОМОРФОЛОГИЯ И ПАЛЕОГЕОГРАФИЯ ПОЛЯРНЫХ РЕГИОНОВ»: Материалы совместной международной конференции «ГЕОМОРФОЛОГИЯ И ПАЛЕОГЕОГРАФИЯ ПОЛЯРНЫХ РЕГИОНОВ», симпозиума «Леопольдина» и совещания рабочей группы INQUA Peribaltic. Санкт-Петербург, СПбГУ, 9 – 17 сентября 2012 года / Отв. ред. А.И. Жиров, В.Ю. Кузнецов, Д.А. Субетто, Й. Тиде. – СПб., 2012. – 475 с. ISBN 978-5-4391-0029-3 Сборник содержит материалы совместной международной конференции "Геоморфологические и палеогеографические исследования полярных регионов", симпозиума «Леопольдина» и совещания рабочей группы INQUA Peribaltic. Обсуждается целый ряд актуальных вопросов, связанных с изучением проблем теоретической -
Russia and Siberia: the Beginning of the Penetration of Russian People Into Siberia, the Campaign of Ataman Yermak and It’S Consequences
The Aoyama Journal of International Politics, Economics and Communication, No. 106, May 2021 CCCCCCCCC Article CCCCCCCCC Russia and Siberia: The Beginning of the Penetration of Russian People into Siberia, the Campaign of Ataman Yermak and it’s Consequences Aleksandr A. Brodnikov* Petr E. Podalko** The penetration of the Russian people into Siberia probably began more than a thousand years ago. Old Russian chronicles mention that already in the 11th century, the northwestern part of Siberia, then known as Yugra1), was a “volost”2) of the Novgorod Land3). The Novgorod ush- * Associate Professor, Novosibirsk State University ** Professor, Aoyama Gakuin University 1) Initially, Yugra was the name of the territory between the mouth of the river Pechora and the Ural Mountains, where the Finno-Ugric tribes historically lived. Gradually, with the advancement of the Russian people to the East, this territorial name spread across the north of Western Siberia to the river Taz. Since 2003, Yugra has been part of the offi cial name of the Khanty-Mansiysk Autonomous Okrug: Khanty-Mansiysk Autonomous Okrug—Yugra. 2) Volost—from the Old Russian “power, country, district”—means here the territo- rial-administrative unit of the aboriginal population with the most authoritative leader, the chief, from whom a certain amount of furs was collected. 3) Novgorod Land (literally “New City”) refers to a land, also known as “Gospodin (Lord) Veliky (Great) Novgorod”, or “Novgorod Republic”, with its administrative center in Veliky Novgorod, which had from the 10th century a tendency towards autonomy from Kiev, the capital of Ancient Kievan Rus. From the end of the 11th century, Novgorod de-facto became an independent city-state that subdued the entire north of Eastern Europe. -
The Research History of Long Barrows in Russia and Estonia in the 5Th –10Th Centuries
Slavica Helsingiensia 32 Juhani Nuorluoto (ed., ., Hrsg.) Topics on the Ethnic, Linguistic and Cultural Making of the Russian North , Beiträge zur ethnischen, sprachlichen und kulturellen Entwicklung des russischen Nordens Helsinki 2007 ISBN 978–952–10–4367–3 (paperback), ISBN 978–952–10–4368–0 (PDF), ISSN 0780–3281 Andres Tvauri (Tartu) Migrants or Natives? The Research History of Long Barrows in Russia and Estonia in the 5th –10th Centuries Introduction The central problem in the history of North-Western Russia is how the area became Slavic. About 700–1917 AD Finno-Ugric and Baltic heathen autochthons turned into Orthodox Russians speaking mostly Slavic languages. Scholars have up to now been unable to clarify when, how, and why that process took place. Archaeologists have addressed the question of how Slavicization began in South-Western Russia by researching primarily graves, which represent the most widespread type of sites from the second half of the first millennium AD. During the period from the 5th to the 10th century, the people of North-Western Russia, South-Eastern Estonia, Eastern Latvia, and North-Eastern Belarus buried part of their dead in sand barrows, which were mostly erected in groups on the banks of river valleys, usually in sandy pine forests. Such barrows are termed long barrows. The shape of the barrows and burial customs vary considerably in their distribution area. Both round and long barrows were erected. The barrows are usually dozens of metres in length, in exceptional cases even a hundred metres, and their height is most often between 0.5–1 m. In such cemeteries, the cremation remains of the dead were buried either in a pit dug in the ground beneath the later barrow, placed on the ground below the barrow, or in the already existing sand barrow. -
European Bison in Russia – Past, Present and Future
European Bison Conservation Newsletter Vol 2 (2009) pp: 148–159 European bison in Russia – past, present and future Taras P. Sipko Institute of Problems Ecology and Evolution RAS, Moscow, Russia Abstract The area of the European bison during historical time Holocene is discussed with addition of new information published in last years. Northern border of an area corresponds 60 0 N. The area included average and southern Urals Mountains, the south of Western Siberia. On the east the European bison lived up to the Altay Mountains and Lake Baikal. The same area at a red deer having similar ecological needs. Increase of inbreeding level considerably and negatively influences adaptable and reproductive opportunities of a bison. This circumstance is especially shown in case of its reintroduction in mountain areas. The basic projects on cultivation of the European bison in Russia are discussed. Keywords : European bison, geographical range, inbreeding, reintroduction Bison Habitat The studies on historical changes of European bison habitat are important both theoretically and practically. Historical geographical range of a species is the most favorable area for reintroduction and creation new free populations. In Pleistocene, the European bison range covered the most part of Eurasia (Flerov 1979). From the beginning of Holocene natural conditions changed (especially in the western part of the region). Glacier shield and vast pre-glacier lakes shortened and disappeared. Forest boundary migrated to the North. Humans occupied the area. Snow cover became deeper and lasted longer and become a limiting factor of European bison distribution at the Russian plain. All factors mentioned above served in drawing of northeastern boundary of European bison range in historic time (Heptner et al. -
Journal American Historical Society of Germans from Russia
Journal of the American Historical Society of Germans from Russia Winter 1998 Volume 21. No. 4 Editor JO ANN KUHR AHSGR Headquarters, Lincoln, Nebraska Editorial Board IRMGARD HEDM ELLINGSON PETER J.KLASSEN Bukovina Society, Ellis, K.S California State University, Fresno ARTHUR E.FLEGEL TIMOTHY KLOBERDANZ Certified Genealogist, Menio Park, CA North Dakota State University, Fargo ADAM GIESINGER GEORGE KUFELDT University of Manitoba, Canada, emeritus Anderson University, Indiana, emeritus CHRIS LOVETT NANCY BERNHARDT HOLLAND Emporia State University, Kansas Trinity College, Burlington, VT LEONAPFEIFER WILLIAM KEEL Fort Hays State University, Kansas, emeritus University of Kansas, Lawrence On the cover: Wearing a traditional Russian fur hat, en- tertainer John Denver stands outside the U.S. Embassy in Moscow, Russia, 1984. He The Journal of the American Historical Society of Germans from Russia is published quarterly by AHSGR. was one of the first American recording Members of the Society receive a quarterly Journal and Newsletter. Members qualify for discounts on artists to be allowed to do a public concert in material available for purchase from AHSGR. Membership categories are: Individual, $50; the former USSR. John Denver used this Family, $50; Contributing. $75; Sustaining. $100; Life, $750. Memberships are based on a calendar year, due each January I. Dues in excess of $50 may be tax-deductible as allowed by law. Applications for membership photo for a Christmas card that he sent out should be sent to AHSGR, 631 D Street, Lincoln, NE 68502-1199. to friends and relatives. (Picture by Norman The Journal welcomes the submission of articles, essays, family histories, anecdotes, folklore, book Gershman. -
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.