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The Election Attitudes Among the Polish Minority Inhabiting the Region of Zaolzie in the Czech Republic (1990-2018)
https://doi.org/10.4316/CC.2020.01.008 THE ELECTION ATTITUDES AMONG THE POLISH MINORITY INHABITING THE REGION OF ZAOLZIE IN THE CZECH REPUBLIC (1990-2018) Radosław ZENDEROWSKI Cardinal Stefan Wyszyński University in Warsaw, Poland E-mail: [email protected] Abstract. The paper analyses the election activity of the Polish inhabitants of the Zaolzie region (the Czech Republic) in the 1990-2018 period referring to national elections (Lower Chamber of Parliament, Senate, President of the Czech Republic) as well as local and regional elections. The theoretical section offers analyses of national and ethnic minorities as (collective) political actors. The empirical part provides an in-depth analysis of the votes in particular elections, taking into consideration the communes with a significant rate of Polish inhabitants as well as those communes there the Polish ethnos was rather scarce. The ethnic affiliation has been considered as a vital independent variable of the choices made; however, other variables explaining election behaviour have also been indicated. Keywords: Zaolzie, Czech Republic, Polish national minority, elections, politics Rezumat. Atitudinile electorale în rândul minorității poloneze din Regiunea Zaolzie a Republicii Cehe (1990-2018). Articolul analizează problema activității electorale a locuitorilor polonezi din regiunea Zaolzie (Republica Cehă) în perioada 1990-2018, refe- rindu-se la alegerile naționale (Camera inferioară a Parlamentului, Senatul, președintele Re- publicii Cehe), precum și la alegerile regionale și locale. Secțiunea teoretică prezintă minorită- țile naționale și etnice ca actori politici (colectivi). Partea empirică oferă o analiză aprofundată a voturilor la anumite alegeri, luând în considerare comunele cu o pondere semnificativă de locuitori polonezi, precum și acele comune unde etnicii polonezi sunt puțini la număr. -
Silesian: from Gwara to Language After 19891 Dr Habil Tomasz
Silesian: From Gwara to Language After 19891 Dr Habil Tomasz Kamusella Reader in Modern History University of St Andrews Scotland, Britain Abstract In the past Silesian was seen to be a dialect of the Polish language (and sometimes of Czech). During the 1990s, following the fall of communism and the establishment of democracy in Poland, most Silesian-speakers decided to treat Silesian as a language in its own right. It became part and parcel of their effort to shed the status of second-class citizens that had been imposed on them in interwar and communist Poland. Warsaw has not recognized this language yet but, despite suffering this (quite humiliating) disadvantage, Silesian-speakers have produced a growing number of articles, books, websites, or radio and television programs in their language, winning a recognition for Silesian as a language abroad and among scholars. It appears that the Polish administration’s rigid stance toward the Silesians and their language is dictated by the logic of ethnolinguistic nationalism, which equates the legitimacy and stability of the nation-state with the full ethnolinguistic homogeneity of its population. This article sketches the trajectory of the main events and probes into the state of the discourse on the issue of Silesian language and culture during the quarter of a century after the fall of communism in 1989. Keywords: democracy, Einzelsprache, ethnolinguistic nationalism, Germany, language corpus planning, language status planning, multilingualism, Poland, Silesian language, Upper Silesia Na pamiōntka Roztomiłych Ylternōw, Mutry Anny a Fatra Stephana [N]aród to nie jest sprawa doczesna, tylko ideologia! Którą sobie ludzie wymyślili z głowy. -
Understanding Language Death in Czech,Moravian
x Research in Language 2007, vol. 5 x DOI: 10.2478/v10015-007-0006-2 Kevin Hannan Understanding Language Death in Czech-Moravian Texas Kevin Hannan*1 University of Đo´dz´ UNDERSTANDING LANGUAGE DEATH IN CZECH-MORAVIAN TEXAS1 Abstract: Based on several decades of personal interaction with Texas speakers of Czech, the author’s article attempts to correlate social change with some specific stages of language obsolescence and language death. Many instances of language change in that community, as well as cultural and social change, may be explained by the linguistic model known as the wave theory. One hundred and fifty years passed between the introduction of Czech and the death of that language in Texas. From the mid-nineteenth through the mid-twentieth century, the Czech-Moravians represented a closed community in which individuals defined their identity primarily by the Czech language, ethnicity, and culture. In the final five decades of the twentieth century, as the social template representing Texas speakers of Czech disintegrated, spoken Czech ceased to function as a living language, and much of the ancestral culture connected with the language was lost. Today some among the elderly, described as semi-speakers, terminal speakers, or ‘‘rememberers’’ of language, retain a limited knowledge, but the ancestral language now has only a symbolic function. Keywords: language change, language death, language obsolescence, sociolinguistics, Czech. 1. Introduction Despite the intense and systematic study of language change since the nineteenth century, the ‘‘logic’’ of language change remains poorly understood. Even in comparing certain languages which have similar structures, the results of language change experienced in one linguistic community often differ radically from the reflexes observed in another. -
The Political and Symbolic Importance of the United States in the Creation of Czechoslovakia
Graduate Theses, Dissertations, and Problem Reports 2014 Drawing borders: the political and symbolic importance of the United States in the creation of Czechoslovakia Samantha Borgeson West Virginia University Follow this and additional works at: https://researchrepository.wvu.edu/etd Recommended Citation Borgeson, Samantha, "Drawing borders: the political and symbolic importance of the United States in the creation of Czechoslovakia" (2014). Graduate Theses, Dissertations, and Problem Reports. 342. https://researchrepository.wvu.edu/etd/342 This Thesis is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. DRAWING BORDERS: THE POLITICAL AND SYMBOLIC IMPORTANCE OF THE UNITED STATES IN THE CREATION OF CZECHOSLOVAKIA Samantha Borgeson Thesis submitted to the Eberly College of Arts And Sciences at West Virginia University in partial fulfillment of the requirements for the degree -
Rigorózní Práce
MASARYKOVA UNIVERZITA PŘÍRODOV ĚDECKÁ FAKULTA Ústav geologických v ěd & Ústav fyziky Země Rigorózní práce Brno 2012 Miroslav Halló MASARYKOVA UNIVERZITA PŘÍRODOV ĚDECKÁ FAKULTA ÚSTAV GEOLOGICKÝCH V ĚD & ÚSTAV FYZIKY ZEM Ě CHARAKTERISTIKA AKTIVNÍ STRUKTURY V SEISMICKY AKTIVNÍ ZÓN Ě NOVÝ KOSTEL (ZÁPADNÍ ČECHY ) NA ZÁKLAD Ě PROSTOROVÉHO A ČASOVÉHO ROZMÍST ĚNÍ SEISMICKÝCH JEV Ů Rigorózní práce Miroslav Halló Brno 2012 MASARYK UNIVERSITY FACULTY OF SCIENCE DEPARTMENT OF GEOLOGICAL SCIENCES & INSTITUTE OF PHYSICS OF THE EARTH CHARACTERISTIC OF THE ACTIVE STRUCTURE IN THE SEISMO -ACTIVE ZONE NOVÝ KOSTEL (WESTERN BOHEMIA ) BASED ON THE SPATIAL AND TIME DISTRIBUTION OF SEISMIC EVENTS Rigorosum thesis Miroslav Halló Brno 2012 Bibliografický záznam Autor: Miroslav Halló, Mgr. Charakteristika aktivní struktury v seismicky aktivní zón ě Nový Kostel (západní Čechy) na Název práce: základ ě prostorového a časového rozmíst ění seismických jev ů Studijní program: Geologie Studijní obor: Geologie Vedoucí práce: - Akademický rok: 2012/2013 Po čet stran: 53+6 Klí čová slova: zem ětřesení; seismicita; Nový Kostel; hypocentrum; zlom; Chebská pánev; Mariánsko Láze ňský zlom Bibliographic Entry Author: Miroslav Halló, Mgr. Characteristic of the Active Structure in the Seismo-active zone Nový Kostel (western Title of Thesis: Bohemia) Based on the Spatial and Time Distribution of Seismic Events Degree Geology programme: Field of Study: Geology Supervisor: - Academic Year: 2012/2013 Number of Pages: 53+6 Keywords: earthquake; seismicity; Nový Kostel; hypocentre; fault; Cheb Basin; Mariánské Lázn ě Fault Prohlášení (Statement of authorship) Prohlašuji, že jsem svoji rigorózní práci vypracoval samostatn ě s využitím informa čních zdroj ů, které jsou v práci citovány. Brno 26. zá ří 2012 ……………………………… Miroslav Halló Prolog Tato studie vznikla výrazným rozší řením autorovi diplomové práce “Studium geometrie seismicky aktivní struktury v epicentrální oblasti Nový Kostel (západní Čechy).„ úsp ěšn ě obhájené na P řírodov ědecké fakult ě Masarykovy univerzity v roce 2011 s výborným hodnocením. -
Computing Hydrological Balance in the Medard Mining Pit with the Help
nvironm E en & ta Kovar, et al., J Civil Environ Eng 2016, 6:5 il l iv E C n f g i o n DOI: 10.4172/2165-784X.1000250 l e a e Journal of Civil & Environmental n r r i n u g o J ISSN: 2165-784X Engineering Research Article Open Access Computing Hydrological Balance in the Medard Mining Pit With the Help of the Water Balance Conceptual Model (WBCM) Pavel Kovar*, Jana Kalibova and Hana Bacinova Department of Land Use and Improvement, Faculty of Environmental Sciences, Czech University of Life Sciences Prague, The Czech Republic Abstract A positive water balance is the main prerequisite for successful hydro-reclamation of residual mining pits. Under the current conditions of climate change, long dry periods occur more frequently, which may have a negative impact on the water supply to fill the pit lakes. This study deals with the hydrological balance of the Medard mining pit, which has been computed with the help of the Water Balance Conceptual Model (WBCM). The purpose of this study is to test the feasibility of the WBCM model for water balance estimation in endorheic catchments. The water contribution of the Medard mining pit’s own catchment was quantified, in order to determine if an external supply of water is necessary to fill the pit within several years. The outcomes of the study have shown that the internal water sources of the Medard catchment can hardly provide sufficient water supply, either during a normal, or during a dry hydrological year. Thus, an external water supply from the Ohre River is needed in addition to the water from the mining pits (the quality of the water from the mining pits must of course be carefully monitored). -
Later and Different: the Development of Czech National Institutions in Moravia, 1848-1905
LATER AND DIFFERENT: THE DEVELOPMENT OF CZECH NATIONAL INSTITUTIONS IN MORAVIA, 1848-1905 BY JESSICA ANNE PRESTLEY THESIS Submitted in partial fulfillment of the requirements for the degree of Master of Arts in Russian, East European, and Eurasian Studies in the Graduate College of the University of Illinois at Urbana-Champaign, 2010 Urbana, Illinois Adviser: Assistant Professor David L. Cooper ABSTRACT The Czech national movement in Moravia has been ignored by historians as a topic for inquiry. Although Bohemia and Moravia have shared a similar historical trajectory and close ties, there remains a lack of English-language scholarship on the dissemination of the Czech national identity in Moravia. While the establishment of cultural and political institutions was delayed, the case of Moravia is not a simple carbon copying and implementing of Bohemian-style institutions without consideration of the special regional environment. This work will attempt to provide the reader with an overview of the Czech national movement in Moravia between 1848 and 1905 by analyzing institutional and political development. ii ACKNOWLEDGMENTS First and foremost, I would like to extend my gratitude to my adviser, Professor David Cooper, for his guidance, support, and patience throughout this project. His assistance during the writing process and correcting numerous Czech translations were invaluable. He provided encouragement on my endeavor to learn more about the unexplored history of Moravia during the nineteenth century. Without his support, this thesis would not have been possible in its end form. I would also like to thank Professor Maria Todorova for conducting an independent study course, allowing me to more closely examine the Czech national movement in Bohemia. -
S.1 Supplementary Materials
S.1 Supplementary materials 1 Table S1: River stations analyzed over the period 1950 - 2009. The column elev denotes the mean basin elevation in meters above sea level, area denotes catchment area in km2, forest gives the relative coverage of forest land use (%) based on Corine 1990 data. Forest damage in percent is given in the “damage” column, using the Corine class 324. The columns P , E0, Q and P − Q denote average annual water balance components for the basins in mm/yr. miss gives the number of missing months. station / river major basin elev area forest damage PE0 QP -Q miss Buschmuehle/Kirnitzsch Upper Elbe 397 98 78 1 853 686 298 563 264 Kirnitzschtal/Kirnitzsch Upper Elbe 379 154 77 0 847 687 290 557 0 Porschdorf/Lachsbach Upper Elbe 378 267 39 0 845 687 360 485 0 Sebnitz/Sebnitz Upper Elbe 422 102 47 1 870 686 449 426 264 Markersbach/Bahra Upper Elbe 545 49 45 10 819 678 374 431 267 Bischofswerda/Wesenitz Upper Elbe 363 69 30 0 819 689 362 452 264 Elbersdorf/Wesenitz Upper Elbe 315 227 17 0 789 690 295 496 1 Dohna/Müglitz Upper Elbe 557 198 35 6 848 677 408 440 9 Geising/Rotes Wasser Upper Elbe 780 26 53 35 956 667 559 389 216 Kreischa/Lockwitzbach Upper Elbe 380 44 23 0 779 684 254 531 187 Klotzsche/Prießnitz Upper Elbe 261 40 60 0 724 693 267 454 244 Rehefeld/Wilde Weißeritz Upper Elbe 808 15 91 61 974 666 783 188 140 Ammelsdorf/Wilde Weißeritz Upper Elbe 734 49 64 20 963 671 605 368 18 Beerwalde/Wilde Weißeritz Upper Elbe 663 81 53 12 940 674 527 413 84 Baerenfels/Pöbelbach Upper Elbe 742 6 75 12 976 670 808 194 244 Freital/Poisenbach Upper Elbe 295 12 42 0 720 690 222 493 336 Piskowitz/Ketzerbach Upper Elbe 214 157 0 0 665 696 122 547 336 Seerhausen/Jahna Upper Elbe 178 153 0 0 635 698 63 570 219 Merzdorf/Döllnitz Upper Elbe 167 211 7 0 623 699 136 489 1 Zescha/Hoyersw. -
Groundwater Level Variations in the Seismically Active Region of Western Bohemia in the Years 2005–2010
Acta Geodyn. Geomater., Vol. 8, No. 1 (161), 17–27, 2011 GROUNDWATER LEVEL VARIATIONS IN THE SEISMICALLY ACTIVE REGION OF WESTERN BOHEMIA IN THE YEARS 2005–2010 Renata GAŽDOVÁ *, Oldřich NOVOTNÝ, Jiří MÁLEK, Jan VALENTA, Milan BROŽ and Petr KOLÍNSKÝ Institute of Rock Structure and Mechanics, Academy of Sciences of the Czech Republic, v.v.i., V Holešovičkách 41, 182 09 Prague, Czech Republic *Corresponding author‘s e-mail: [email protected] (Received December 2010, accepted February 2011) ABSTRACT The western part of the Bohemian Massif (Vogtland/West-Bohemia region at the Czech-German border) is characterized by relatively frequent intraplate earthquake swarms and by other manifestations of current geodynamic activity, such as mofettes, mineral and thermal springs. In this study we analyze variations of groundwater level in four hydrological wells in the region during the years 2005–2010. Monitoring during the previous time interval of 2000–2004 is also mentioned and used for comparison. Two of the wells are located in the epicentral region of Nový Kostel, and the other wells are more distant. The time interval includes the 2008 earthquake swarm when all the wells displayed a noticeable drop in the water level. This effect was observed up to epicentral distances of nearly 30 km, which exceeds the distances of hydrological changes observed during previous earthquake swarms. Moreover, it seems that a small rise in the water level preceded the intervals of increased seismic activity, which could represent a certain precursory phenomenon. On the other hand, the hydrological changes in the Nový Kostel area were relatively small, indicating that this epicentral area is not hydrologically linked with the seismically active fault at depth. -
Kraslice – Zwotental Výlukový Jízdní Řád, Platí: 13
145 Sokolov – Kraslice – Zwotental Výlukový jízdní řád, platí: 13. 12. 2020 – 12. 2. 2021 km 17000 17002 17004 17006 17008 17010 20810 17012 17014 17016 20818 17018 17020 17022 17024 GW Train Regio, a.s. 0 Karlovy Vary dolní nádraží Informace o návazných vlacích ČD E F 12:09 Informace o návazných vlacích ČD 3 Karlovy Vary v úseku Karlovy Vary – Sokolov: n 12:14 v úseku Karlovy Vary – Sokolov: 26 Sokolov www.cd.cz E F 12:30 www.cd.cz 0 Sokolov 140 W 4:53 EX# 5:05 W 5:53 E X 6:33 W 6:55 E X 7:26 8:34 W ! 9:30 E X 10:32 W ! 11:15 12:32 13:26 W 13:50 E X 14:34 W 14:36 2 Svatava n 4:55 n 5:07 n 5:55 n 6:35 n 6:57 n 7:28 8:36 n 9:32 n 10:34 n 11:17 12:34 13:28 n 13:53 n 14:36 n 14:38 3 { Svatava zastávka n 4:58 n 5:10 n 5:58 n 6:38 n 7:00 n 7:31 8:39 n 9:35 n 10:37 n 11:20 12:37 13:31 n 13:56 n 14:38 n 14:40 6 { Luh nad Svatavou n 5:02 n 5:14 n 6:02 n 6:42 n 7:04 n 7:35 8:43 n 9:39 n 10:41 n 11:24 12:41 13:35 n 14:00 n 14:42 n 14:44 8 { Hřebeny n 5:04 n 5:16 n 6:04 n 6:44 n 7:06 n 7:37 8:45 n 9:41 n 10:43 n 11:26 12:43 13:37 n 14:03 n 14:44 n 14:46 13 Oloví n 5:13 n 5:24 n 6:13 n 6:51 n 7:14 n 7:43 8:52 n 9:48 n 10:50 n 11:33 12:50 13:43 n 14:14 n 14:51 n 14:53 18 Rotava n 5:20 n 5:31 n 6:22 n 6:59 n 7:21 n 7:49 9:00 n 9:55 n 10:59 n 11:40 12:59 13:49 n 14:21 n 15:00 n 15:03 21 { Kraslice předměstí n 5:24 n 5:35 n 6:26 n 7:03 n 7:25 n 7:53 9:04 n 9:59 n 11:03 n 11:44 13:03 13:53 n 14:25 n 15:03 n 15:06 24 Kraslice W 5:29 EX# 5:40 W 6:31 E X 7:08 W 7:30 E X 7:57 9:09 W ! 10:04 E X 11:08 W ! 11:49 13:08 13:57 W 14:31 E X 15:09 W 15:11 km GW Train Regio, a.s. -
145 Sokolov - Kraslice - Zwotental IDOK Sokolov - Kraslice-Pod Vlekem Km PDV RAILWAY A.S
145 Sokolov - Kraslice - Zwotental IDOK Sokolov - Kraslice-Pod vlekem km PDV RAILWAY a.s. / Vlak 20802 17000 17002 20804 17004 17006 20806 17008 17010 20808 20810 17012 20812 GW Train Regio a.s. + Die Länderbahn - GmbH Ze stanice 0 Sokolov 140 1 4 53 5 05 5 53 6 33 6 55 7 26 8 34 9 32 2 Svatava 1 4 55 5 07 5 55 6 35 6 57 7 28 8 36 9 34 3 Svatava zastávka 1,6 4 58 5 10 5 58 6 38 7 00 7 31 8 39 9 37 6 Luh nad Svatavou 6 5 02 5 14 6 02 6 42 7 04 7 35 8 43 9 41 8 Hřebeny 6 5 04 5 16 6 04 6 44 7 06 7 37 8 45 9 43 13 Oloví 6,7 5 13 5 24 6 13 6 51 7 14 7 43 8 52 9 50 18 Rotava 7 5 20 5 31 6 22 6 59 7 21 7 49 9 00 9 57 21 Kraslice předměstí 7 5 24 5 35 6 26 7 03 7 25 7 53 9 04 10 01 24 Kraslice 7 5 29 5 40 6 31 7 08 7 30 7 57 9 09 10 06 Kraslice 7 5 10 6 10 7 10 8 10 9 10 10 10 25 Kraslice-Pod vlekem 7 5 11 6 11 7 11 8 11 9 11 10 11 28 Klingenthal 5 16 6 16 7 16 8 16 9 16 10 16 36 Zwotental 5 29 6 29 7 29 8 29 9 29 10 29 Do stanice Zwickau Zwickau Mehltheuer Zwickau Mehltheuer Zwickau km PDV RAILWAY a.s. -
145 Sokolov - Kraslice - Zwotental IDOK Sokolov - Kraslice-Pod Vlekem Km PDV RAILWAY A.S
145 145 Sokolov - Kraslice - Zwotental IDOK Sokolov - Kraslice-Pod vlekem km PDV RAILWAY a.s. / Vlak 20802 17000 17002 20804 17004 17006 20806 17008 17010 20808 20810 17012 20812 GW Train Regio a.s. + Die Länderbahn - GmbH Ze stanice 0 Sokolov 140 1 4 54 5 05 5 53 6 33 6 55 7 26 8 34 9 32 2 Svatava 1 4 56 5 07 5 55 6 35 6 57 7 28 8 36 9 34 3 Svatava zastávka 1,6 4 59 5 10 5 58 6 38 7 00 7 31 8 39 9 37 6 Luh nad Svatavou 6 5 03 5 14 6 02 6 42 7 04 7 35 8 43 9 41 8 Hřebeny 6 5 05 5 16 6 04 6 44 7 06 7 37 8 45 9 43 13 Oloví 6,7 5 13 5 24 6 11 6 51 7 14 7 43 8 52 9 50 18 Rotava 7 5 20 5 31 6 20 6 59 7 21 7 49 9 00 9 57 21 Kraslice předměstí 7 5 24 5 35 6 24 7 03 7 25 7 53 9 04 10 01 24 Kraslice 7 5 29 5 40 6 29 7 08 7 30 7 57 9 09 10 06 Kraslice 7 5 10 6 10 7 10 8 10 9 10 10 10 25 Kraslice-Pod vlekem 7 5 11 6 11 7 11 8 11 9 11 10 11 28 Klingenthal 5 16 6 16 7 16 8 16 9 16 10 16 36 Zwotental 5 29 6 29 7 29 8 29 9 29 10 29 Do stanice Zwickau Zwickau Mehltheuer Zwickau Mehltheuer Zwickau km PDV RAILWAY a.s.