Bronisław Grąbczewski
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
The Fluvial Geochemistry of the Rivers of Eastern Siberia: I. Tributaries Of
Geochimica et Cosmochimica Acta, Vol. 62, No. 10, pp. 1657–1676, 1998 Copyright © 1998 Elsevier Science Ltd Pergamon Printed in the USA. All rights reserved 0016-7037/98 $19.00 1 .00 PII S0016-7037(98)00107-0 The fluvial geochemistry of the rivers of Eastern Siberia: I. Tributaries of the Lena River draining the sedimentary platform of the Siberian Craton 1, 1 2 1 YOUNGSOOK HUH, *MAI-YIN TSOI, ALEXANDR ZAITSEV, and JOHN M. EDMONd 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA 2Laboratory of Erosion and Fluvial Processes, Department of Geography, Moscow State University, Moscow, Russia (Received June 11, 1997; accepted in revised form February 12, 1998) ABSTRACT—The response of continental weathering rates to changing climate and atmospheric PCO2 is of considerable importance both to the interpretation of the geological sedimentary record and to predictions of the effects of future anthropogenic influences. While comprehensive work on the controlling mechanisms of contemporary chemical and mechanical weathering has been carried out in the tropics and, to a lesser extent, in the strongly perturbed northern temperate latitudes, very little is known about the peri-glacial environments in the subarctic and arctic. Thus, the effects of climate, essentially temperature and runoff, on the rates of atmospheric CO2 consumption by weathering are not well quantified at this climatic extreme. To remedy this lack a comprehensive survey has been carried out of the geochemistry of the large rivers of Eastern Siberia, the Lena, Yana, Indigirka, Kolyma, Anadyr, and numerous lesser streams which drain a pristine, high-latitude region that has not experienced the pervasive effects of glaciation and subsequent anthropogenic impacts common to western Eurasia and North America. -
Ukrainians and Poles Timothy Snyder
8 Ukrainians and Poles timothy snyder Europe’s road to Muscovy passed through Warsaw and Kyiv (Kiev). Despite what one reads in books, the Renaissance and Reformation did reach Muscovy, if by this most indirect route. In the middle of the seventeenth century,Ortho- dox clerics trained in the rhetoric and languages of the Polish Renaissance and Reformation settled in Moscow.As Muscovy’s political power extended across eastern Ukraine and Kiev with Hetman Bohdan Khmelnyts’kyi’s rebellion against Poland ( 1648–54 ) and the Treaty of Eternal Peace between Muscovy and Poland ( 1686), Orthodox clerics came to terms with their new position in a highly backward Orthodox state. Alexis Mikhailovich (r. 1645–76 ) saw them as people capable of improving Muscovite administration, and encouraged the emigration of learned Ukrainians. Iepifanii Slavynets’kyi was an early arrival, in 1649. Symeon Polots’kyi taught Alexis’s children Latin and Polish. The occa- sional Polish Jesuit was allowed to dispute with the Orthodox, as did Andrzej Kwieczynski before he was sent to break rocks in Siberia in 1660. Disputa- tion itself was an import from Poland, and at this time Polish and Latin were understood to be the languages of reason. Latin itself was learned from Polish translations, for example of Ovid’s ‘Metamorphoses’. Ukrainian clerics such as Stepan Iavors’kyi and Teofan Prokopovych were indeed engaged in some fundamental transformations: of themselves as they reoriented Ruthenian Orthodoxy to Moscow, and of Moscow as they reori- ented public life and political thought to the West. Such men introduced the baroque, not only in rhetoric, but in architecture, ceremonial and secu- lar public displays. -
Pdf Aleksander Czekanowski – Odkrywca Trapów Syberyjskich
Przegl¹d Geologiczny, vol. 67, nr 10, 2019 Z MINIONYCH CZASÓW Aleksander Czekanowski – odkrywca trapów syberyjskich Grzegorz Racki1 Aleksander Czekanowski – discoverer of Siberian traps. Prz. Geol., 67: 791–798. A b s t r a c t. Flood basalts (traps) and large igneous provinces (LIPs) belong to the hot topics of modern geology, especially due to their causal links with major evolutionary crises and global catastrophes. However, the history of views on volcanic cataclysms, as well as the recognition stages of particular LIPs are still little known. Surpris- ingly, Polish contribution to this expanding topic may be larger than expected, as exemplified by the issue of field exploration of the largest continental LIP in Siberia. The first exhaustive data were provided in 1873 by Aleksander Czekanowski (1833–1876), a Polish geologist, educated at the universities of Kiev and Dorpat (Tartu),who was exiled by the Russian authorities to Siberia for participation in organizing the Polish January Uprising in 1863. He G. Racki led several large expeditions to distant parts of Siberia, also in the Ni¿nyja (Lower) Tunguska basin. In the summer of 1873, he discovered numerous exposures of basalt lava floods in the tableland along this river, starting from the area between Preobrazhenka and Jerbogachyan. The observations were announced by letters systematically pub- lished in “Izvestiya Imperatorskogo Russkogo Geograficheskogo Obshchestva”. As the most important result of the expedition, he quoted in 1876: “the discovery of previously unknown area of igneous rocks of so large extent that it exceeds the size of any other of its kind”. In his diaries, published posthumously in 1896, Czekanowski described the trap locations in detail, documented in many sketches and cross-sections. -
Debris Flow Hazards for Mountain Regions of Russia: Regional Features
Nat Hazards (2017) 88:S199–S235 DOI 10.1007/s11069-017-2841-3 ORIGINAL PAPER Debris flow hazards for mountain regions of Russia: regional features and key events 1 1 1 Veniamin Perov • Sergey Chernomorets • Olga Budarina • 1 1 Elena Savernyuk • Tatiana Leontyeva Received: 10 December 2016 / Accepted: 21 March 2017 / Published online: 29 March 2017 Ó Springer Science+Business Media Dordrecht 2017 Abstract The total area of debris flow territories of the Russian Federation accounts for about 10% of the area of the country. The highest debris flow activity areas located in Kamchatka-Kuril, North Caucasus and Baikal debris flow provinces. The largest debris flow events connected with volcano eruptions. Maximum volume of debris flow deposits per one event reached 500 9 106 m3 (lahar formed during the eruption of Bezymyanny volcano in Kamchatka in 1956). In the mountains of the Greater Caucasus, the maximum volume of transported debris material reached 3 9 106 m3; the largest debris flows here had glacial reasons. In the Baikal debris flow province, the highest debris flow activity located in the ridges of the Baikal rift zone (the East Sayan Mountains, the Khamar-Daban Ridge and the ridges of the Stanovoye Highland). Spatial features of debris flow processes within the territory of Russia are analyzed, and the map of Debris Flow Hazard in Russia is presented. We classified the debris flow hazard areas into 2 zones, 6 regions and 15 provinces. Warm and cold zones are distinguished. The warm zone covers mountainous areas within the southern part of Russia with temperate climate; rain-induced debris flows are predominant there. -
GEOMORPHIC ASPECT of HYDRAULIC ENGINEERING Dr
GEOMORPHIC ASPECT OF HYDRAULIC ENGINEERING Dr. N.L. Dongre, IPS Omkareshwar Dam on The Narbada River rift valley ABSTRACT- To explain the geomorphic aspects, examples are given from well known Jaypee Groups Dam and hydraulic constructions and Worlds important river project. Morphology may be defined as the science of structure or form "and fluvial may be defined as produced by the action of flowing water." Since rivers can hardly be said to have structure, fluvial morphology is therefore, the science of the form as produced by the action of flowing water. It is a branch of geomorphology, the science of the form of the earth's surface. Geomorphology has also been called physiography. Fluvial morphology is particularly important to the hydraulic engineering because many of his greatest problems arise because of the form of streams brought about by the transportation and deposition of sediment by them. For the proper solution of these problems, knowledge of the principles of fluvial morphology is often necessary. Among the problems in which fluvial morphology is a very important factor are many of those dealing with water resources development and include some of the most important river problems in the world. Among these is flood control on the Ganga, Brahmaputra, Mahanadi, Krishna, Godavari, Periyar, Kaveri, Sutlaj, Narmada, Kosi, Tawa and Chambal (India), lower Mississippi and lower Colorado Rivers (USA). The development of the Hydraulic resources all over the world are ensured and commissioned. The Yellow and Huai River flood problems are solved by China. As streams become highly developed, and changes in sediment movement due to stream developments slowly become evident, the importance of the morphological aspect of river control problems will be increasingly appreciated. -
Mitochondrial Genome Diversity in the Central Siberian Plateau with Particular
bioRxiv preprint doi: https://doi.org/10.1101/656181; this version posted May 31, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Mitochondrial Genome Diversity in the Central Siberian Plateau with Particular Reference to Prehistory of Northernmost Eurasia S. V. Dryomov*,1, A. M. Nazhmidenova*,1, E. B. Starikovskaya*,1, S. A. Shalaurova1, N. Rohland2, S. Mallick2,3,4, R. Bernardos2, A. P. Derevianko5, D. Reich2,3,4, R. I. Sukernik1. 1 Laboratory of Human Molecular Genetics, Institute of Molecular and Cellular Biology, SBRAS, Novosibirsk, Russian Federation 2 Department of Genetics, Harvard Medical School, Boston, MA 02115, USA 3 Broad Institute of Harvard and MIT, Cambridge, MA 02142, USA 4 Howard Hughes Medical Institute, Harvard Medical School, Boston, MA 02115, USA 5 Institute of Archaeology and Ethnography, SBRAS, Novosibirsk, Russian Federation Corresponding author: Rem Sukernik ([email protected]) * These authors contributed equally to this work. bioRxiv preprint doi: https://doi.org/10.1101/656181; this version posted May 31, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Abstract The Central Siberian Plateau was last geographic area in Eurasia to become habitable by modern humans after the Last Glacial Maximum (LGM). -
PLNY TEXT (2.432Mb)
Faculty of Electrical Engineering Department of Economics, Management and Humanities Hybrid electric supply system for Baikalskoe village Study program: Electrical engineering, power engineering and management Field of study: Economics and management of power engineering Scientific adviser: Sherzod Tashpulatov, Ph.D. Aleksei Pliusnin Prague 2017 2 Declaration: I hereby declare that this master’s thesis is the product of my own independent work and that I have clearly stated all information sources used in the thesis according to Methodological Instruction No. 1/2009 – “On maintaining ethical principles when working on a university final project, CTU in Prague. Date Signature 3 Abstract At present time a conventional solution for electricity supply is to set up an overhead transmission line from the nearest substation. Baikalskoe village is connected to centralized electricity grid via single- circuit transmission line with length of more than 35 km and nominal voltage of 10 kV. However, in order to avoid high power and voltage losses which do affect quality of electricity supplied, recommended voltage class for such a length should be at least 35 kV. To follow the conventional solution it is necessary to switch to a higher voltage power line. Considering the fact that there are two main types of line supports, it falls into alternatives with application of either steel or reinforced concrete poles. There are some exceptions which require nonconventional solutions like a construction of a hybrid electric power supply system which. In this particular case such a system should combine centralized power supply with local generation based on renewables. In this work, the conventional and nonconventional solutions for electricity supply in Baikalskoe village are compared. -
Geoima.Com Physical Geography and Mineral Resources of Russia
geoima.com Physical Geography and Mineral Resources of Russia INTRODUCTION:-- Russia is the largest country in the world by area (twice the size of Canada). It has coastlines along the Baltic, Black, Caspian, and Pacific. It stretches 9650 km east to west and 4500 km north to south. The chief regions of Russia and their physical features are briefly discussed below. The European Plain: This is part of the Great European Plains. It is on top of the Russian Platform and its southern edge terminates in the Caucasus Mountains and the Caspian Sea lowlands. Its average height is about 180 meters above the mean sea level_ The European.Plains are drained by Volga, N_Dvina,-the Pechora and other rivers_ It includes the lakes of Onega and Ladoga in the northwest The Volga basin and Pechora basin within the region are rich in oil and gas. The Ural Mountains: These stretch for 2400 Kms and are part of the Hercynian folds. The Urals extend from Arctic Circle to Kazakhstan. Mt. Narodnaya is the highest peak. The Urals region is mineral-rich and is heavily industrialized with large industrial cities like Chelyabinsk and YeTaierinberg. The Urals are an Asia-Europe Divide. The West SiberianPlain: This is part of the Siberian Plateau (a Volcanic Plateau). The average elevation of the plain is 150 meters above the Mean Sea Level. It is the largest level tract of land in Russia. I l as fertile glacial soils in the north_ It is drained by river Ob and its tributary Irtysh. It is very rich in natural gas. -
The Functioning of Erosion-Channel Systems of the River Basins of the South of Eastern Siberia
geosciences Article The Functioning of Erosion-channel Systems of the River Basins of the South of Eastern Siberia Olga I. Bazhenova 1,*, Aleksandr V. Bardash 1, Stanislav A. Makarov 1, Marina Yu. Opekunova 1, Sergei A. Tukhta 1 and Elizaveta M. Tyumentseva 2 1 V.B. Sochava Institute of Geography SB RAS, Irkutsk 664033, Russia; [email protected] (A.V.B.); [email protected] (S.A.M.); [email protected] (M.Y.O.); [email protected] (S.A.T.) 2 Geographical Department, Pedagogical Institute of Irkutsk State University, Irkutsk 664033, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-3952426920 Received: 23 March 2020; Accepted: 6 May 2020; Published: 11 May 2020 Abstract: We revealed the regional features of the functioning of the erosion-channel systems of the Angara, Upper Lena, Selenga, and Upper Amur basins in the south of Eastern Siberia and examined the action of sloping non-channel, temporary, and permanent channel water flows, and presented the patterns of the spatial distribution of soil and gully erosion belts. The development conditions and factors of fluvial processes are considered and the role of cryogenic processes in the increasing activity of water flows is emphasized. The interdecadal dynamic cycles of the erosion-accumulative processes are revealed. A quantitative assessment of soil loss from erosion on agricultural land in the forest-steppe basins was carried out. We made an assessment of the plane deformation of the upper course of the Lena river (Siberian platform) and Irkut (Baikal rift zone and the Irkutsk-Cheremkhovo plain) using cartographic sources of different times, aerial photographs, and satellite imagery. -
INHIGEO Annual Record No
ISSN 1028-1533 International Commission on the History of Geological Sciences INHIGEO ANNUAL RECORD I No. 46 Covering activitiesI generally in 2013 Issued in 2014 INHIGEO is A Commission of the International Union of Geological Sciences & An affiliate of the International Union of the History and Philosophy of Science and Technology Compiled and Edited by Wolf Mayer INHIGEO Editor Printed in Canberra on request Available at www.inhigeo.org 1 | Page 2 | Page CONTENTS INHIGEO Annual Record No. 46 (Published in May 2014 covering events generally in 2013) INHIGEO BOARD 7 MESSAGES TO MEMBERS President‘s Message: Kenneth L. Taylor 8 Secretary-General‘s Report: Barry Cooper 9 Editor’s Message: Wolf Mayer 10 INHIGEO 2014 – Asilomar, California, United States 12 INHIGEO 2015 – Beijing 13 INHIGEO 2016 – Cape Town 13 LATER INHIGEO CONFERENCES 14 OTHER INHIGEO BUSINESS NOTICES Liaison with other IUGS Commissions and Task Groups 14 INHIGEO Affiliated Association category 15 INHIGEO Virtual Bibliography 16 A message encouraging INHIGEO members to join HESS 18 INHIGEO CONFERENCE AND EXCURSION REPORTS Report on the INHIGEO Meeting, Manchester, United Kingdom, 22-27 July 2013 19 Pre-congress Field Trip: The Silurian of ‘Siluria’ and the Idea of a Palaeozoic Era 24 Intra-congress trip: Buxton Spar and Buxton Spa 28 Post-congress fieldtrip: Ruskin’s Geology 30 International Congress of the History of Science, Technology and Medicine – Manchester 2013 34 MANCHESTER MANIFESTO 36 3 | Page OTHER CONFERENCE REPORTS Past, present and future of human connections to the Antarctic 37 CONFERENCES OF INTEREST The BSHS Annual Conference, 6 July 2014, at the University of St Andrews. -
International Commission on the History of Geological Sciences
ISSN 1028-1533 International Commission on the History of Geological Sciences INHIGEO ANNUAL RECORD I No. 46 Covering activitiesI generally in 2013 Issued in 2014 INHIGEO is A Commission of the International Union of Geological Sciences & An affiliate of the International Union of the History and Philosophy of Science and Technology Compiled and Edited by Wolf Mayer INHIGEO Editor Printed in Canberra on request Available at www.inhigeo.org 1 | P a g e INSIDE COVER (Please scroll down) 2 | P a g e CONTENTS INHIGEO Annual Record No. 46 (Published in May 2014 covering events generally in 2013) INHIGEO BOARD 7 MESSAGES TO MEMBERS President‘s Message: Kenneth L. Taylor 8 Secretary-General‘s Report: Barry Cooper 9 Editor’s Message: Wolf Mayer 10 INHIGEO 2014 – Asilomar, California, United States 12 INHIGEO 2015 – Beijing 13 INHIGEO 2016 – Cape Town 13 LATER INHIGEO CONFERENCES 14 OTHER INHIGEO BUSINESS NOTICES Liaison with other IUGS Commissions and Task Groups 14 INHIGEO Affiliated Association category 15 INHIGEO Virtual Bibliography 16 A message encouraging INHIGEO members to join HESS 18 INHIGEO CONFERENCE AND EXCURSION REPORTS Report on the INHIGEO Meeting, Manchester, United Kingdom, 22-27 July 2013 19 Pre-congress Field Trip: The Silurian of ‘Siluria’ and the Idea of a Palaeozoic Era 24 Intra-congress trip: Buxton Spar and Buxton Spa 28 Post-congress fieldtrip: Ruskin’s Geology 30 International Congress of the History of Science, Technology and Medicine – Manchester 2013 34 MANCHESTER MANIFESTO 36 3 | P a g e OTHER CONFERENCE REPORTS Past, present and future of human connections to the Antarctic 37 CONFERENCES OF INTEREST The BSHS Annual Conference, 6 July 2014, at the University of St Andrews. -
CONTENTS INHIGEO Newsletter No. 43
1 CONTENTS INHIGEO Newsletter No. 43 (Published in May 2011 covering events generally in 2010) INHIGEO BOARD 4 REPORTS President‟s Message: Silvia Figueirôa 5 Secretary-General‟s Report: Barry Cooper 5 INHIGEO 2011, TOYOHASHI, JAPAN 7 INHIGEO BUSINESS NOTICES Minutes of 2010 INHIGEO Business Meeting, Almadén, Spain 9 Agenda INHIGEO Business Meeting, Toyohashi, Japan, August 2011 13 CONFERENCE REPORTS INHIGEO 2010, Spain 13 IUGS 50th Anniversary Event, Paris 2011 22 “History of polar exploration, co-operation, research and logistics”, Oslo, 2010 23 “History of Antarctica and scientific research”, Buenos Aires, 2010 24 First Symposium: History of Geology of Chile 25 CONFERENCE ANNOUNCEMENTS 34th International Geological Congress, Brisbane, Australia 2012 (37th INHIGEO conference) 26 24th International Congress for the History of Science, Technology and Medicine, Manchester, England 2013 (38th INHIGEO conference) 28 OTHER FORTHCOMING ACTIVITIES 28 AWARDS GSA History of Geology Award (2010) to Gabriel Gohau 30 Reinhard Süring Medal to Cornelia Lüdecke 33 Prix Jubilé 2010 Award to Andrea Westermann 33 OBITUARIES Evgeny Alekseyevich Baskov (1925–2010) 33 Masae Omori (1919- 2011) 35 Alexander Meier Ospovat (1923–2010) 36 Manuel Carlos Serrano Pinto (1936 –2011) 39 Wang Hongzhen (1916- 2010) 40 2 INTERVIEW Interview with Yusheng Zhai, Beijing, China, 21 December 2010, Jiuchen Zhang and Yufeng Zhou 42 ARTICLES IUGS 50th Anniversary History Project, Susan Turner 46 Investigations by the German geologist, H. von Abich, in Armenia, Hayk H. Melik-Adamyan & Christophor V. Khachanov 49 Staszic Fascicules, Andrzej J. Wójcik & Wojciech Narębski 52 Early Geological Maps from Central Europe, Alena Čejchanová 54 Mexican geologic cartography: an exhibition marking the centennial of the UNAM, Lucero Morelos Rodríguez 57 NOTES A special historical gem from Hungary 59 International Year of Crystallography – 2013 60 BOOK REVIEWS Stephen K.