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Metoda Klasifikacije U Istraživanjima Egzonima Classification Method In
HRVATSKI GEOGRAFSKI GLASNIK 79/1, 81−106 (2017.) UDK 811.163.42'373.21 Pregledni članak 911.3:811 Review DOI 10.21861/HGG.2017.79.01.04 Primljeno / Received 28-12-2016 / 2016-12-28 Ivana Crljenko Prihvaćeno / Accepted 11-02-2017 / 2017-02-11 Metoda klasifikacije u istraživanjima egzonima Classification method in exonym studies Egzonimi su udomaćena imena stranih geografskih Exonyms are adapted names of foreign geographical objekata koja se razlikuju od izvornih imena (endonima); features that differ from their original names (endonyms); npr. Azija, Beč, Prag, Rim, Sejšeli. Važan su dio e.g. Azija (Asia), Beč (Vienna), Prag (Prague), Rim (Rome), kulturnog nasljeđa i jezičnog identiteta zajednice koja ih Sejšeli (Seychelles). They are an important part of the je stvorila i održala. Njima se na međunarodnoj razini cultural heritage and linguistic identity of the community bavi Radna skupina za egzonime, koja djeluje unutar that created (and uses) them. They are researched on the Skupine stručnjaka za geografska imena pri Ujedinjenim international level by the Working Group on Exonyms, narodima. U hrvatskoj jezikoslovnoj i geografskoj which operates within the United Nations Group of znanstvenoj zajednici rijetki se istraživači bave Experts on Geographical Names. Only a few researchers proučavanjem egzonima. Osobito su malobrojne analize study exonyms within the Croatian linguistic and koje se temelje na velikom broju egzonima. Svrha je rada geographical scientific communities. Analyses based on a dati prilog njihovu obuhvatnijem proučavanju razvojem large number of exonyms are especially rare. The purpose metode klasifikacije egzonima, a njegov je cilj izložiti of this article is to contribute to a comprehensive study of moguće klasifikacije i uputiti na njihovu primjenu. -
Vodní Útvary Povrchových Vod Podle ORP Stránka 1/22 Název ORP Kód
Tabulka 1 - Vodní útvary povrchových vod podle ORP Stránka 1/22 rizikový vodní název ORP kód ORP ID VÚ název VÚ kategorie VÚ dílčí povodí útvar Blansko 6201 DYJ_0430 Lubě od pramene po ústí do toku Svratka řeka DYJ ano DYJ_0460 Kuřimka od pramene po vzdutí nádrže Brno řeka DYJ ano DYJ_0580 Býkovka od pramene po ústí do toku Svitava řeka DYJ ano DYJ_0590 Svitava od toku Křetínka po tok Punkva řeka DYJ ano DYJ_0600 Punkva od pramene po ponor řeka DYJ ano DYJ_0610 Bílá voda od pramene po Marianínský potok včetně řeka DYJ ano DYJ_0620 Punkva od ponoru po ústí do toku Svitava řeka DYJ ano DYJ_0630 Šebrovka od pramene po ústí do toku Svitava řeka DYJ ano DYJ_0640 Křtinský potok od pramene po ústí do toku Svitava řeka DYJ ano DYJ_0650 Svitava od toku Punkva po ústí do toku Svratka řeka DYJ ano DYJ_0710 Rakovec od pramene po Vážanský potok včetně řeka DYJ ano DYJ_0740 Říčka (Zlatý potok) od pramene po tok Roketnice řeka DYJ ano MOV_0970 Malá Haná od pramene po vzdutí nádrže Opatovice řeka MOV ano Boskovice 6202 DYJ_0360 Hodonínka od pramene po ústí do toku Svratka řeka DYJ ano DYJ_0380 Svratka od hráze nádrže Vír I. po tok Bobrůvka (Loučka) řeka DYJ ano DYJ_0420 Besének od pramene po ústí do toku Svratka řeka DYJ ano DYJ_0500 Svitava od pramene po tok Křetínka řeka DYJ ano DYJ_0510 Křetínka od pramene po vzdutí nádrže Letovice řeka DYJ ano DYJ_0525_J Nádrž Letovice na toku Křetínka jezero DYJ ano DYJ_0530 Křetínka od hráze nádrže Letovice po ústí do toku Svitava řeka DYJ ano DYJ_0540 Bělá od pramene po vzdutí nádrže Boskovice řeka DYJ ano DYJ_0550 Okrouhlý p. -
Causes and Consequences of a Flood Wave on the Lower Reach of the Dyje River Near Břeclav
Soil & Water Res., 5, 2010 (4): 121–127 Causes and Consequences of a Flood Wave on the Lower Reach of the Dyje River Near Břeclav Milan PALÁT 1, Alois PRAX1, Milan PALÁT jr.1 and Jaroslav ROžNOVSKÝ 2 1Mendel University in Brno, Brno, Czech Republic; 2Czech Hydrometeorological Institute, Brno, Czech Republic Abstract: The settlements situated on broad flat floodplains of rivers are threatened by floods during increased water flows in the rivers. The floodplain of the Dyje river situated in the area between the Nové Mlýny water reservoir and Břeclav has been protected from former annual floods since the 70s of the last century due to the water-management measures. The realised measures including the construction of the new floodway protect the town of Břeclav as well. A long-term research into the soil water regime of the floodplain forest is underway in the region. The results obtained document its historical evolution and current status. Only in the early April of 2006 (i.e. after 34 years), an unexpected “flash flood” occurred again due to a specific climatic situation. The combination of the high snow cover in higher parts of the basin and a rapid warming up caused an intensive runoff. The so-called dry polder (floodplain forests, meadows and fields) above Břeclav protected the town and its infrastructure from potential catastrophic consequences. Keywords: basin; climatic characteristics; dry polder; floodplain forest; floods; sewerage; soil water regime Urban agglomerations including the costly infra- example, spring floods in 1941 had catastrophic structures situated in the broad floodplain valleys consequences (Figure 1). of rivers are often threatened by increased water The data of the National Water Management flows. -
Tourmalinites in the Metamorphic Complex of the Svratka Unit (Bohemian Massif): a Study of Compositional Growth of Tourmaline and Genetic Relations
Journal of Geosciences, 54 (2009), 221–243 DOI: 10.3190/jgeosci.048 Original paper Tourmalinites in the metamorphic complex of the Svratka Unit (Bohemian Massif): a study of compositional growth of tourmaline and genetic relations Renata ČOpJakOvá1,2*, David BuRIánek1, Radek ŠkODa1,2, Stanislav HOuzaR3 1 Czech Geological Survey, Leitnerova 23, 658 59 Brno, Czech Republic; [email protected] 2 Institute of Geological Sciences, Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic 3 Department of Mineralogy and Petrography, Moravian Museum, Zelný trh 6, 659 37 Brno, Czech Republic * Corresponding author Tourmalinites (rocks with an association Tu + Qtz + Ms ± Grt ± Bt ± Ky ± Sil ± Pl ± Kfs) from the Svratka Unit form stratiform layers hosted in mica schists. The chemical composition of tourmaline from tourmalinites varies from Al- rich schorl to dravite. The tourmaline usually exhibits three compositional domains, which are, from centre to the rim: a chemically inhomogeneous brecciated core (zone I), a volumetrically minor internal rim zone II, and a dominant outermost zone III. X Y W X Y W The compositional variability of tourmaline in all the zones is controlled by the ( Al OH) ( Na Mg F)-1 and Y Y Fe Mg-1 substitutions. The tourmaline of the zone I corresponds to highly vacanced X-site, Al-rich schorl with lower F (up to 0.43 apfu), which is interpreted as an older, low-temperature hydrothermal tourmaline. Tourmaline of the zone II corresponds to dravite rich in F (reaching up to 0.66 apfu) crystallizing during the prograde metamorphism. Lastly, the Al-rich schorl–dravite of the zone III grew most likely during retrograde metamorphism. -
Opinions/Opinions – Standard Reference
01 April 1999 ACFC/SR(1999)006 ______ REPORT SUBMITTED BY THE CZECH REPUBLIC PURSUANT TO ARTICLE 25, PARAGRAPH 1 OF THE FRAMEWORK CONVENTION FOR THE PROTECTION OF NATIONAL MINORITIES ______ ACFC/SR(1999)006 TABLE OF CONTENTS The Czech Republic Information about Compliance with Principles set forth in the Framework Convention for the Protection of National Minorities according to Article 25, Paragraph 1 of this Convention PART I Population of the Czech Republic according to National Identity and Mother Tongues8 (according to the 1991 public census) PART II SECTION I Article 1 Article 3 SECTION II Article 4 Article 5 Article 6 Article 7 Article 8 Article 9 Article 10 Article 11 Article 12 Article 13 Article 14 Article 15 Article 16 Article 17 Article 18 Article 19 Article 30 APPENDICES I. Charter of Fundamental Rights and Freedoms (paper version only) Appendix No.II Statistical Overview of Racially Motivated Prosecuted Crimes(1998) Appendix No.IIIa Appendix No. IIIb Appendix No. IIIc 2 ACFC/SR(1999)006 The Czech Republic Information about Compliance with Principles set forth in the Framework Convention for the Protection of National Minorities according to Article 25, Paragraph 1 of this Convention The Czech Republic signed the Framework Convention for the Protection of National Minorities (hereinafter referred to as the Convention) in Strasbourg on April 28, 1995. The Convention was approved by the Czech Parliament in accordance with Article 39, paragraph 4 of the Constitution of the Czech Republic as an international treaty on human rights and fundamental freedoms pursuant to Article 10 of the Czech Constitution. -
The Glaciofluvial Terrace in the Moravian Gate (Czech Republic)
Journal of Anthropozoic Pages 8 – – Czech Geological Survey ISBN 978-80-7075-761–1 Geological Sciences 27 51–61 figures table plate Prague 2011 ISSN 0036-5270 The glaciofluvial terrace in the Moravian Gate (Czech republic) Glacifluviální terasa v Moravské bráně Jaroslav Tyráček † TyráČek, J. (2011): The glaciofluvial terrace in the Moravian Gate (Czech Republic). – Sbor. geol. Věd, Antropozoikum, 27, 51–61. Praha. Key words: northern Moravia, Pliocene, Pleistocene, continental glaciation Abstract: The sediments exotic to local geological setting that occur close to the European water-divide in the Moravian Gate have been primarily interpreted as glacial since the end of the 19th century. Because the Scandinavian ice sheet advanced twice into the Moravian Gate, the age of its maximum extent, level and direction of the meltwater drainage were the most important topics. The term glaciofluvial terrace, introduced into the literature by Hassinger (1914) is intimately linked with the maximum glaciation, which is here dated to the Elsterian Stage glacial. In fact, however, the Elsterian glacier halted far from the divide and no traces of its having crossed this barrier have been identified. Nor has the drainage via the Moravian Gate during the Elsterian times been confirmed. Two gravel occurrences at Nad dolama and Horecko about 70–80 m above the Bečva River have been proposed as the representatives of the glaciofluvial terrace. They are composed of local lithologies derived from the Nízký Jeseník upland. No exotic rocks have been identified in these sediments not even those from the flysch conglomerates, which occur in the upper Carpathian part of the Bečva River course. -
TD 4.1C Obce S Navrženou Protipovodňovou Ochranou V Rámci
Tabelární přílohy Plán oblasti povodí Dyje D. Ochrana před povodněmi a vodní režim krajiny TD 4.1c Obce s navrženou protipovodňovou ochranou v rámci krajských studií protipovodňových opatření Pracovní Obec s rozšířenou Správce číslo Obec, lokalita Kraj Vodní tok Název vodního útvaru působností toku vodního útvaru Obce na tocích Povodí Moravy, s. p. Dačice JHC Dačice Moravská Dyje PM D006 Moravská Dyje po státní hranici Staré Město pod Landštejnem JHC Jindřichův Hradec Pstruhovec PM D007 Pstruhovec po státní hranici Adamov JHM Blansko Svitava PM D061 Svitava po ústí do toku Svratka Bílovice nad Svitavou JHM Šlapanice Svitava PM D061 Svitava po ústí do toku Svratka Blansko JHM Blansko Svitava PM D055 Svitava po soutok s tokem Punkva Blížkovice JHM Znojmo Jevišovka PM D020 Jevišovka po soutok s tokem Ctidružický potok Borač JHM Tišnov Svratka PM D037 Svratka po soutok s tokem Bobrůvka Boskovštejn JHM Znojmo Jevišovka PM D026 Jevišovka po ústí do toku Dyje Brankovice JHM Bučovice Litava (Cézava) PM D067 Litava po soutok s tokem Rakovec Brno JHM Brno Svratka PM D047 Svratka po soutok s tokem Svitava Brno JHM Brno Svitava PM D061 Svitava po ústí do toku Svratka Brno-Řečkovice JHM Brno Ponávka PM D046 Ponávka po ústí do toku Svratka Brno-Židenice JHM Brno Svitava PM D061 Svitava po ústí do toku Svratka Břeclav JHM Břeclav Dyje PM D124 Dyje po soutok s tokem odlehčovací rameno -061/2 Bučovice JHM Bučovice Litava (Cézava) PM D067 Litava po soutok s tokem Rakovec Černvír JHM Tišnov Svratka PM D037 Svratka po soutok s tokem Bobrůvka Doubravice nad -
ÆTHELMEARC Ásta Vagnsdóttir. Name and Device. Azure, Two Bars
ACCEPTANCES Page 1 of 19 January 2007 LoAR THE FOLLOWING ITEMS HAVE BEEN REGISTERED: ÆTHELMEARC Ásta Vagnsdóttir. Name and device. Azure, two bars Or, overall an owl displayed argent. The use of an owl displayed is a step from period practice. Creature Twyne Dragon. Device. Per pale argent and sable all semy of fishhooks bendwise counterchanged. Please see the Cover Letter for a discussion on fishhooks. Desiderata Drake. Name. Maol Duín Ó Duinn. Name. Submitted as Máel-dúin O’Duinn, the submitter requested a name authentic for 15th C Ireland. As submitted, the name is unregisterable since the byname mixes the English patronymic marker O’ with the Irish patronym Duinn in violation of RfS III.1.a. This can be fixed by changing the marker to the Irish Ó. This change was specifically allowed by the submitter. The given name Máel-dúin is documented to before the 13th C; it is a Middle Irish form of the name inappropriate for use in the 15th C. The Annals of the Four Masters has a Magnus mac Maoile Duin in an entry for 1486. Irish bynames that use mac in this period are typically true patronymics; Magnus’s father almost certainly bore the given name Maol Duin. The normalized Early Modern Irish form of this name is Maol Duín; precedent holds that accents in Gaelic names must either be used consistently or dropped consistently. We have changed the name to Maol_Duín Ó Duinn, a fully Early Modern Irish form appropriate for the 15th C, in order to register it and to fulfill the submitter’s request for authenticity. -
UNITED NATIONS Working Paper GROUP of EXPERTS on No. 67 GEOGRAPHICAL NAMES
UNITED NATIONS Working Paper GROUP OF EXPERTS ON No. 67 GEOGRAPHICAL NAMES Twenty-third Se ssion Vienna, 28 March – 4 April 2006 Item 14 of the Provisional Agenda: Activities relating to the Working Group on Exonyms 4th Meeting of the Working Group on Exonyms Ljubljana, Slovenia, 19 th – 20th May 2005 Prepared by Peter Jordan (Austria), Working Group on Exonyms Two items deserve to be highlighted among the activities conducted by the Working Group on Exonyms since it 3rd Meeting in the framework of the 22nd Session of UNGEGN in New York in 2004: (1) 4 th Meeting of the Working Group on Exonyms in Ljubljana (2) preparation of a book on exonyms This two-day meeting was arranged by the UNGEGN Working Group (WG) on Exonyms and hosted by the Anton Melik Geographical Institute of the Scientific Research Centre of the Slovenian Academy of Sciences and Arts in Ljubljana, Slovenia. Papers were presented by Mr Woodman on the relationship between man and his terrain, and how the geographical name provided the point of reference between them, Mr Jordan on the relative definition of exonym and endonym, Mr Raukko on the linguistic classification of exonyms, Mr Kadmon on the history of the definitions of endonym and exonym in UNGEGN and the current definitions as recorded in the “Glossary of Terms for the Standardisation of Geographical Names”, Mr Pokoly on the history of the usage of Hungarian language geographical names and the current status of exonyms in Hungary, Mrs Burgess and Miss Cheetham on the planned creation of an UNGEGN toponymic database of country and major city names, Mr Kladnik on the historical usage of Slovene geographical names in texts and cartography, Mr. -
Report of the Working Group on Exonyms Conference
Eleventh United Nations Conference on the Standardization of Geographical Names New York, 8-17 August 2017 Item 11 of the provisional agenda Exonyms Report of the Working Group on Exonyms Submitted by the Working Group on Exonyms Prepared by Peter Jordan (Austria), Convenor, Working Group on Exonyms - 1 - Summary The report highlights the activities of the UNGEGN Working Group on Exonyms (WGE) since the 10th United Nations Conference on the Standardization of Geographical Names (UNCSGN) in 2012. In this period, the Working Group held three business meetings and four workshops and published four books of proceedings. The WG met on August 6, 2012 during the 10th Conference on the Standardization of Geographical Names in the UN Headquarters in New York and discussed the endonym/ exonym divide and new definitions of the endonym and the exonym as well as the question whether a third term for international waters is needed. At the same occasion, Peter JORDAN was confirmed as WG convenor by elections. The WG met again for its 14th meeting in Corfu, Greece, 23-25 May 2013. It had the character of a workshop and was organized in conjunction with a meeting of the UNGEGN Working Group on Toponymic Terminology (Convenor: Staffan NYSTRÖM). The meeting of the WGE was attended by 33 experts from 20 countries and saw 17 paper presentations on the endonym/exonym divide as well as on use and documentation of exonyms in various countries. This sequence of paper presentations was followed by an intensive discussion on new definitions of the endonym and the exonym. Proceedings of the 14th Meeting have been published as Vol. -
Characterization of PM10 Sampled on the Top of a Former Mining Tower by the High-Volume Wind Direction-Dependent Sampler Using INNA
atmosphere Article Characterization of PM10 Sampled on the Top of a Former Mining Tower by the High-Volume Wind Direction-Dependent Sampler Using INNA Irena Pavlíková 1,2,* , Daniel Hladký 1,3, OldˇrichMotyka 4 , Konstantin N. Vergel 2, Ludmila P. Strelkova 2 and Margarita S. Shvetsova 2 1 Department of Environmental Protection in Industry, Faculty of Materials Science and Technology, VSB–Technical University of Ostrava, 708 00 Ostrava-Poruba, Czech Republic; [email protected] 2 Sector of Neutron Activation Analysis and Applied Research, Frank Laboratory of Neutron Physics, Joint Institute for Nuclear Research, 141980 Dubna, Russia; [email protected] (K.N.V.); [email protected] (L.P.S.); [email protected] (M.S.S.) 3 Czech Hydrometeorological Institute, 708 00 Ostrava-Poruba, Czech Republic 4 Nanotechnology Centre, VSB–Technical University of Ostrava, 708 00 Ostrava-Poruba, Czech Republic; [email protected] * Correspondence: [email protected] or [email protected]; Tel.: +420-604-636-041 Abstract: The PM10 concentrations in the studied region (Ostravsko-karvinská agglomeration, Czech Republic) exceed air pollution limit values in the long-term and pose a significant problem for human health, quality of life and the environment. In order to characterize the pollution in the region and identify the pollution origin, Instrumental Neutron Activation Analysis (INAA) was employed for determination of 34 elements in PM10 samples collected at a height of 90 m above ground level. From April 2018 to March 2019, 111 PM10 samples from eight basic wind directions and calm and two smog situations were sampled. The elemental composition significantly varied depending on season and sampling conditions. -
The German National Attack on the Czech Minority in Vienna, 1897
THE GERMAN NATIONAL ATTACK ON THE CZECH MINORITY IN VIENNA, 1897-1914, AS REFLECTED IN THE SATIRICAL JOURNAL Kikeriki, AND ITS ROLE AS A CENTRIFUGAL FORCE IN THE DISSOLUTION OF AUSTRIA-HUNGARY. Jeffery W. Beglaw B.A. Simon Fraser University 1996 Thesis Submitted in Partial Fulfillment of The Requirements for the Degree of Master of Arts In the Department of History O Jeffery Beglaw Simon Fraser University March 2004 All rights reserved. This work may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. APPROVAL NAME: Jeffery Beglaw DEGREE: Master of Arts, History TITLE: 'The German National Attack on the Czech Minority in Vienna, 1897-1914, as Reflected in the Satirical Journal Kikeriki, and its Role as a Centrifugal Force in the Dissolution of Austria-Hungary.' EXAMINING COMMITTEE: Martin Kitchen Senior Supervisor Nadine Roth Supervisor Jerry Zaslove External Examiner Date Approved: . 11 Partial Copyright Licence The author, whose copyright is declared on the title page of this work, has granted to Simon Fraser University the right to lend this thesis, project or extended essay to users of the Simon Fraser University Library, and to make partial or single copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. The author has further agreed that permission for multiple copying of this work for scholarly purposes may be granted by either the author or the Dean of Graduate Studies. It is understood that copying or publication of this work for financial gain shall not be allowed without the author's written permission.