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Act Cciii of 2011 on the Elections of Members Of
Strasbourg, 15 March 2012 CDL-REF(2012)003 Opinion No. 662 / 2012 Engl. only EUROPEAN COMMISSION FOR DEMOCRACY THROUGH LAW (VENICE COMMISSION) ACT CCIII OF 2011 ON THE ELECTIONS OF MEMBERS OF PARLIAMENT OF HUNGARY This document will not be distributed at the meeting. Please bring this copy. www.venice.coe.int CDL-REF(2012)003 - 2 - The Parliament - relying on Hungary’s legislative traditions based on popular representation; - guaranteeing that in Hungary the source of public power shall be the people, which shall pri- marily exercise its power through its elected representatives in elections which shall ensure the free expression of the will of voters; - ensuring the right of voters to universal and equal suffrage as well as to direct and secret bal- lot; - considering that political parties shall contribute to creating and expressing the will of the peo- ple; - recognising that the nationalities living in Hungary shall be constituent parts of the State and shall have the right ensured by the Fundamental Law to take part in the work of Parliament; - guaranteeing furthermore that Hungarian citizens living beyond the borders of Hungary shall be a part of the political community; in order to enforce the Fundamental Law, pursuant to Article XXIII, Subsections (1), (4) and (6), and to Article 2, Subsections (1) and (2) of the Fundamental Law, hereby passes the following Act on the substantive rules for the elections of Hungary’s Members of Parliament: 1. Interpretive provisions Section 1 For the purposes of this Act: Residence: the residence defined by the Act on the Registration of the Personal Data and Resi- dence of Citizens; in the case of citizens without residence, their current addresses. -
Geological Analysis of the Kis-Alföld Based on Satellite-Photos L
GEOLOGICAL ANALYSIS OF THE KIS-ALFÖLD BASED ON SATELLITE-PHOTOS L. JAKUCS The research introduced only in its main results in this study is a part óf a five-year scientificic program which was carried out by the Institute of Physical Geography of Attila József University of Sciences within the frame of the theme "Satellite Research of Natural Resources of Hungary" at the commission of the Central Institute of Geology. The members of the team lead by dr. prof László Jakucs are as follows: reader dr. Mihály Andó, senior lecturer dr. József Fehér, Senior lecturer dr. Mrs Ferenc Kevei, lecturer candidate dr. Gábor Mezősi and senior lec- turer dr. Imre Tóth. The available LANDSAT longdistance survaillances show that defining the Kis-Alföld as a physical geographical region is a simple task only with a cursory examination because its margins protrude deeply into the wide valley-plains of the bordering Carpathian and Transdanubian rivers. On the satellitephotos of the LANDSAT-satellites (I; II; III.) these marginal regions, which are quastionable and subjectively treatable, too, stand out clearly and this fact helps making a more exact genetic limitation. Yet during our work of interpretation we overstepped the actual borders of the Kis-Alfpld for we saw comparation standing out at all points which says that the regionmargins drawn on geomorphological or soilgeographycal basis are not at the same time the margins of the natural factors determining the development of a region. For quality and quantityration óf past and recens hydro- logical, climatological, sedimentational and structural many times determinant) factors determining and directing the geographycal and sedimentological develop- ment of the Kis-Alföld are controlled far from the frontier, mainly from the direction of the Alps and the Carpathians. -
Magyarországi Nevek Magyar-Angol Névmutatója Névmutató Névváltozatok
Bradlo, Szl., 543, C2 Déda, Rom., J4 Feketebalog, Szl., E2 Gutin-hágó, Rom., I3 Istállós-kő, Ma., 959, F2 Szerb., E5 Kurjantó-tó, Ma., E4 Máriafalva, Rom., L4 Nagy (Ferenc)-csatorna, Oláhlápos, Rom., I3 Podgorac, Horv., D5 Ruszkova, Rom., J3 Szászorbó, Rom., I5 Taktaköz, Ma., G2 Újbázos, Rom., G5 Vulkán-hg., Rom., H5-I5 Branyiszkó-hágó, Szl., F1 Dél-bácskai-teraszvidék, Fekete-Cseremos, Ukr., J2 Gutin Tomnatek, Ukr., 2016, Isten dombja, Ma., 338, B4 Kishartyán, Ma., E2 Kurói (Tilicsi)-hágó, Len./Szl., Máriafölde, Rom., F5 Szerb., E5 Oláhszentgyörgy, Rom., J3 Podolin, Szl., F1 Ruszt, Au., B3 Szászrégen, Rom., J4 Talabor, Ukr., I2 Újbezdán, Horv., D5 Vurpód, Rom., J5 Ez a névmutató csak azon Kőlyuk-galya = Kőlyuk-galya forest . 8. A személyneveket nem fordítjuk. geographical names in English- complete them by a generic term Névmutató Brassó, Rom., K5 Szerb., E5 Fekete-Dunajec, Len., E1 J2 Isten széke, Rom., 1380, J3 Kis-havas, Rom., H5 G1 Márianosztra, Ma., D3 Nagyfödémes, Szl., C2 Ólom-hegy, Ma., 174, E4 Podságai-szoros, Rom., I4 Rybotycze, Len., H1 Szászsebes, Rom., I5 Taliándörögd, Ma., C4 Újegyház, Rom., J5 Vysoká, Cs., 1024, D1 Magyarországi nevek magyar-angol névmutatója természetföldrajzi nevek angol Pl.: János-hegy = János Hill . language publications. The main written in lower case: Bükkalja = Oszágnév rövidítések: Len. Lengyelország Brassói-havasok, Rom., K5 Delelő-hegy, 1549, E1 Fekete-h., Ukr., 565, I2 Guvno, BH., 363, B5 Istenmezeje, Ma., F2 Kis-havas, Rom., 1802, H5 Kutina, Horv., B5 Máriapócs, Ma., G3-H3 Nagy-Galla, Ma., 479, D3 Olt, Rom., K4-J5 Podu Calului, Rom., 1439, L5 Rymanów-Zdrój, Len., G1 Szásztyukos, Rom., K5 Tállya, Ma., G2 Újfehértó, Ma., G3 Watkowa, Len., 846, G1 4. -
Geology of Hungary
Regional Geology Reviews Geology of Hungary Alter und Altern: Wirklichkeiten und Deutungen Bearbeitet von Janós Haas 1. Auflage 2012. Buch. xxii, 246 S. Hardcover ISBN 978 3 642 21909 2 Format (B x L): 17,8 x 25,4 cm Weitere Fachgebiete > Geologie, Geographie, Klima, Umwelt > Geologie > Geologie: Allgemeines Zu Leseprobe schnell und portofrei erhältlich bei Die Online-Fachbuchhandlung beck-shop.de ist spezialisiert auf Fachbücher, insbesondere Recht, Steuern und Wirtschaft. Im Sortiment finden Sie alle Medien (Bücher, Zeitschriften, CDs, eBooks, etc.) aller Verlage. Ergänzt wird das Programm durch Services wie Neuerscheinungsdienst oder Zusammenstellungen von Büchern zu Sonderpreisen. Der Shop führt mehr als 8 Millionen Produkte. Contents Introduction ......................................... ix Ja´nos Haas History of Geologic Research ............................ xi Ja´nos Haas Geography and Outline of Geologic Framework .............. xvii Ja´nos Haas Structural Units and Main Stages of the Structural Evolution . xxi Ja´nos Haas 1 Geology and History of Evolution of the ALCAPA Mega-Unit 1 1.1 Austroalpine Units . ........................... 1 Tibor Szederke´nyi 1.1.1 Lower Austroalpine Nappe System ............. 1 1.1.2 Upper Austroalpine Nappe System . 6 1.1.3 Penninic Unit . 6 1.2 Central and Internal Western Carpathian Units . 9 Sa´ndor Kova´cs and Ja´nos Haas 1.2.1 Veporic Unit . ........................... 9 1.2.2 Zemple´nic Unit . 10 1.2.3 Internal Western Carpathian Nappe-Stack ........ 11 1.2.3.1 Bo´dvaNappe...................... 12 1.2.3.2 Torna Nappe ...................... 14 1.2.3.3 Telekesoldal Nappe ................. 15 1.2.3.4 Szo˝lo˝sardo´ Unit . ................. 16 1.2.3.5 Silica–Aggtelek Nappe . -
Expressway M 86, Szombathely - Csorna Section Environmental Performance Assessment
Expressway M86, Szombathely– Csorna Section Msz: 43.036 Environmental Performance Assessment Executive Summary EXPRESSWAY M 86, SZOMBATHELY - CSORNA SECTION ENVIRONMENTAL PERFORMANCE ASSESSMENT EXECUTIVE SUMMARY Made by: „UTIBER – UNITEF ’83” Consortium Employer: 2013. 1 Expressway M86, Szombathely– Csorna Section Msz: 43.036 Environmental Performance Assessment Executive Summary SENIOR DESIGNER Szakály Krisztina 13 -12295 Certified Environmental Engineer Environmental Expert UTIBER Kft. DESIGNERS: Design preliminaries, base technical data Coordination, documentation UTIBER Kft. UTIBER Kft. Protection of groundwaters and sub-surface waters Protection of surface waters Veresné Sz. Hortenzia Szakály Krisztina Veresné Sz. Hortenzia Szakály Krisztina 13-1908 13 -12295 13-1908 13 -12295 UNITEF’83 Zrt. UTIBER Kft. UNITEF’83 Zrt. UTIBER Kft. Air protection Noise control Silló Szabolcs 13-13573 Silló Szabolcs 13-13573 COACHING TEAM Kft. COACHING TEAM Kft. Wildlife protection Landscape protection Tölgyesi Magdolna Mogyorós Péter Mogyorós Péter SZ-015/2012. 13-13547 SZ-015/2012. MOTT MACDONALD MAGYARORSZÁG Kft. MOTT MACDONALD MAGYARORSZÁG Kft. Built environment Waste management Veresné Sz. Hortenzia Szakály Krisztina Veresné Sz. Hortenzia Szakály Krisztina 13-1908 13 -12295 13-1908 13 -12295 UNITEF’83 Zrt. UTIBER Kft. UNITEF’83 Zrt. UTIBER Kft. 2 Expressway M86, Szombathely– Csorna Section Msz: 43.036 Environmental Performance Assessment Executive Summary Contents 1. Introduction ........................................................................................................................ -
Éves Jelentés 2019
ÉVES JELENTÉS 2019 A GYSEV CSOPORT WWW.GYSEV.HU TARTALOMJEGYZÉK VEZETŐINK Vezetőink 3 Tulajdonosi struktúra és 4 vonalhálózat Küldetés 5 Személyszállítás 6 Szolgáltatásaink 8 Dávid Ilona Kövesdi Szilárd István Boda János Utazóközönségünk 9 elnök, vezérigazgató, vezérigazgató, GYSEV Zrt. GYSEV Zrt. GYSEV CARGO Zrt. Pályavasút 10 Gépészet 12 GYSEV CARGO Zrt. és RAABERBAHN CARGO GmbH 14 Humán erőforrás 16 Beruházások, fejlesztések 18 Hotel Sopron 25 Beszámoló 26 2 GYSEV ÉVES JELENTÉS 2019 WWW.GYSEV.HU WWW.GYSEV.HU GYSEV ÉVES JELENTÉS 2019 3 TULAJDONOSI STRUKTÚRA ÉS VONALHÁLÓZAT KÜLDETÉS Bratislava Bratislava Wien Wien RajBkratislava Neusiedl am See Wien Wien Rajka Wien Wien Wien Neusiedl aRmaj Skeae Wien Hegyeshalom Ebenfurth Neusiedl am See Wien Hegyeshalom Ebenfurth Hegyeshalom Ebenfurth Wulkaprodersdorf 16 1 Wulkaprodersdorf Bratislava Wiener 16 1 WulkapNroedusetrasdodt rf Pamhagen Wiener 16 1 Pamhagen Neustadt Budapest Wien Wiener Sopron Neustadt FertőbozPamhagen Wien Rajka 9 Budapest Sopron Győr Fertőboz 9 Budapest Neusiedl am See Sopron Fertőszentmiklós Csorna Deutschkreutz 8 Győr Fertőboz 9 Wien Nagycenk Fertőszentmiklós Csorna Győr Deutschkreutz Kapuvár 8 Hegyeshalom Nagyc1e5nk Fertőszentmiklós Csorna Deutschkreutz 8 Kapuvár Ebenfurth Nagycenk Pápa 15 Kapuvár Pápa 15 16 Pápa 16 Kőszeg 16Répcelak Wulkaprodersdorf Bük Kőszeg Répcelak 16 1 Bük Kőszeg 18 Répcelak Bük Wiener 18 Neustadt Pamhagen 18 Celldömölk Porpác GYSEV-vasútvonal (villamosított) Szombathely 20 Celldömölk STRABAG SE Budapest GYSEV-vasGútYvoSnEaVl- v(asneúmtv voinllalm -
An Annotated Checklist of the Springtail Fauna of Hungary (Hexapoda: Collembola)
Opusc. Zool. Budapest, (2007) 2008, 38: 3–82. An annotated checklist of the springtail fauna of Hungary (Hexapoda: Collembola) 1 2 L. DÁNYI and GY. TRASER Abstract. A checklist of the species of springtails (Hexapoda: Collembola) hitherto recorded from Hungary is presented. Each entry is accompanied by complete references, and remarks where appropriate. The present list contains 414 species. he Collembola fauna of several countries in critical review of the literature data of Collembola T the world was already overwied in the recent referring to Hungary. past (e.g. Babenko & Fjellberg 2006, Culik & Zeppelini Filho 2003, Skidmore 1995, Waltz & HISTORY Hart 1996, Zhao et al. 1997). The importance of such catalogues was stressed by several authors The first records of Collembola referring to (e.g. Csuzdi et al, 2006: 2) and their topicality is Hungary are some notes on the mass occurrence indicated also by the fact that several cheklists of certain species (Frenzel 1673, Mollerus 1673, referring even to European states were published Steltzner 1881), which however, are without any most recently (e.g. Fiera (2007) on Romania, taxonomical or faunistical value, as it has already Juceviča (2003) on Latvia, Kaprus et al. (2004) on been pointed out by Stach (1922, 1929). The next the Ukrain, Skarzynskiet al. (2002) on Poland). In springtail reference to Hungary is to be found in spite of these facts, the last comprehensive article the zoological book of János Földy (1801), which on the Hungarian springtail fauna was published was the first time the group was mentioned in about 80 years ago (Stach 1929), eventhough such Hungarian language in the scientific literature, critical reviews have a special importance in the eventhough this work doesn’t contain relevant case of this country because of the large changes faunistical records of the taxon. -
Construction of Csorna Bypass Section, Motor Road M86-M85
Transport Study for the Danube Macro-Region – Annex II of the Final Report Construction of Csorna bypass section, motor road M86-M85 General information This project regards the construction of the second stage of the Csorna bypass, which is part of the development project of road M85. The road M85 Győr-Csorna-Nagycenk is the East-West axis of the Győr-Moson-Sopron County and crosses the road M86 Rédics-Szombathely-Rajka in the town of Csorna (see Figure 4-1). Figure 4-1: Localisation of the Csorna bypass Source: Ministry of National Development (2017) The objectives of this project are presented in general terms. It is expected that, once completed, the Csorna bypass could generate benefits in terms of: time savings, safety levels, environmental impact and vehicle operating costs. The project could improve the accessibility of the region enhancing the mobility of both passengers and freight. As regards its relevance, the project is in line with the EU transport policy, the National Transport Development Strategy of Hungary and with the National Land Use Framework Plan. The project promoter is the National Infrastructure Developing Private Company Limited (i.e., NIF), the rail and road infrastructure manager of Hungary. Technical description The second stage of the Csorna bypass is 5,9 km long. It joins two adjacent sections. The first section is 4,4 km long with two lanes per carriageway. The second section is 1,5 km long with one lane per carriageway. The project includes 4 civil structures, but it is not specified the typology. The total estimated investment cost is equal to € 47,6 million. -
ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE Rolai'h)O E01VOS Nolvllnajae .I V
ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLAi'H)O E01VOS NOlvllNAJAE .i V. S c i. Budapest. Sect. Geol. 26 /1986/ S&P,\R,ITU;n SECTIO GEOLOGICA TOlIUS X:tVL TECTONIC UNITS OF HUNGARY: THEIR B01JNDARIES AND STRATIGRAPHY ~) (A BIBLIOGRAPHIC GUIDE) nUDAPEST 1936 M.KAzMER E6tv6s University, Department of Palaeontology, H-lOS3 Budapest, Kun Bela tel' 2, Hungcuy ABSTRACT This review pa,per presents a brief description ofpre-N eogene tectonic units of Hungary. Their boundaries are defined, stratigraphic cohm1ns are described and possible palaeogeog raphie relationships are outlined. Bibliographic references for descriptive papers (stratig raphy, palaeontology, sedimentology, petrology, geochemistry, metamorphic grade, radio metric ages, etc) are included. Data for igneous activity, metamorphism, deformation, tec tonic position and eeonomic geology are supplied. N eogene and Q.uaternarybasin evolution and volcanism are discussed. Appendices list books on the geology ofHungary, review papers of each periods, available maps and periodicals publishing geological information. Introduction This paper presents a brief review of fundamental geological infor mation on Hungary. The style is concise, similar to that used by PALFREY MAN (1984) in his treatise on Australia. First, boundaries of tectonic units are defined. Then each unit is short ly characterized, followed by a more detailed treatment (rocks, fossil content, c1epositional environment, magmatism, metamorphic grade, racliometTic age. etc) with references to the latest relevant publications, wTitten or having summaries in English, French or German. Our aim is that the interested rea,der would find the last paper on his problem to start with. The review of pre-Neogene units is followed by the outlines of Neo gene and Quaternary sedimentation, volcanism and tectonics. -
Soproni Szemle 47. Évf. 2. Sz. (1993.)
1993. XLVII. ÉVFOLYAM 2. SZÁM 97 1993. XLVII. ÉVFOLYAM 2. SZÁM Alapította: Heimler Károly Kiadja: a Soproni Szemle Alapítvány Fıszerkeszt ı: MOLLAY KÁROLY Szerkeszt ıbizottság: ASKERCZ ÉVA, BIRCHER ERZSÉBET, CSAPODY ISTVÁN, DOMONKOS OTTÓ, GRÜLL TIBOR, HÁRS JÓZSEF titkár, olvasó- és technikai szerkeszt ı, HORVÁTH ZOLTÁN, KÖRNYEI ATTILA, KUBINSZKY MIHÁLY, METZL JÁNOS, SARKADY SÁNDOR, TURBULY ÉVA 1993. XLVII. ÉVFOLYAM 2. SZÁM / Karakai Gy ızı: Az 1945. évi földreform, a földosztás eredményei, problémái Nagycenken Karakai Gy ızı: Az 1945. évi földreform, a földosztás eredményei, problémái Nagycenken 1993. XLVII. ÉVFOLYAM 2. SZÁM / Karakai Gy ızı: Az 1945. évi földreform, a földosztás eredményei, problémái Nagycenken / I. A község földrajzi helyzete, fekvése I. A község földrajzi helyzete, fekvése Nagycenk község Gy ır-Moson-Sopron megyében Soprontól délkeletre, 13 km távolságra fekszik. Nagycenk és Kiscenk 1893. október 1-jén egyesült, az egyesítést a belügyminiszter rendelte el. Nagycenk nevének hivatalos megállapítása 1906-ban történt. 1(1) A nyugat-magyarországi peremvidék a Sopron–Vas-i síkságon helyezkedik el. A határ délnyugati része dombos és a soproni hegység nyúlványaihoz kapcsolódik. Keleti része alföldies jelleg ő, kavicstakarós síkság. A felszín magassága és talaja szerint két tájat különböztetünk meg: az Arany-pataktól DNY-ra fekv ı táj dombvidék. Középs ı részén az Agghegy emelkedik. Új tagnak nevezik a nyugati erd ı melletti tájat, mióta a kiirtott erd ıterületen szántóm ővelést folytatnak . A táj déli részén, a Dombháti-d őlınél van a község legmagasabb pontja, 234 m-es magassággal. A terület talaja nehezen m ővelhet ı, agyagos márga. 1 A másik tájegység alacsonyabb, alföldi jelleg ő terület, ami a mez ıgazdaság szempontjából kedvez ıbb. -
Thermochronologic Constraints on the Late Cenozoic Exhumation Along the Alpine and West Carpathian Margins of the Pannonian Basin
EGU Stephan Mueller Special Publication Series, 3, 135–147, 2002 c European Geosciences Union 2002 Thermochronologic constraints on the Late Cenozoic exhumation along the Alpine and West Carpathian margins of the Pannonian basin I. Dunkl1,2 and W. Frisch1 1Institute of Geology, University of Tubingen,¨ Sigwartstrasse 10, Tubingen,¨ D-72076, Germany 2Laboratory for Geochemical Research, Hungarian Academy of Sciences, Budaorsi¨ u´ 45, Budapest, H-1112, Hungary Received: 1 May 2000 – Accepted: 16 July 2001 Abstract. The uplifted and partly re-exhumed basement of prove the much broader extent of the sedimentary cover in the Neogene Pannonian basin was investigated by the ap- Miocene time. The elevation of these sediment remnants ex- atite fission track thermochronometer along the marginal belt ceed 800 m a.s.l. reflecting young faulting with significant to the Eastern Alps and the Western Carpathians. In some vertical displacement (Tari, 1988). This fault generation was zones the reset Late Miocene apatite FT ages and the high also found in the internal part of the Pannonian basin (Cson- organic maturation of the Neogene sediments give evidences tos, 1995; Tari et al., 1999). The inversion is a widespread on the high magnitude of the post-Middle Miocene sediment phenomenon and the young flank uplift of the basin system removal. Thermal modeling of the fission track data allows was also reported from the eastern margin in the Apuseni to quantify this removal and to conclude that its magnitude in mountains and along the Eastern and Southern Carpathians the investigated sites was in the range of 1–1.5 km. In this pa- (Sanders, 1998; Bojar et al., 1998; Willingshofer, 1999). -
Bükk Faanyag Ragaszthatósági Vizsgálata Egykomponensű
DOI: 10.1515/aslh-2016-0012 Acta Silv. Lign. Hung., Vol. 12, Nr. 2 (2016) 135–143 Bondability of Beech Wood with One-component Polyurethane Structural Adhesive a* b Norbert HORVÁTH – Csilla CSIHA a Institute of Wood Science, University of West Hungary, Sopron, Hungary b Institute of Wood Products and Technologies, University of West Hungary, Sopron, Hungary Abstract – The bondability of beech (Fagus sylvatica L.) wood with a one-component polyurethane (1K PUR) structural (load-bearing) adhesive has been investigated at the Simonyi Károly Faculty at the University of West Hungary. Our trial is considered a preliminary investigation in order to set the convenient parameters of bonding for the structural gluing of beech wood. Wood samples were characterized by their oven dry density, and the surfaces to be bonded were characterized by their surface roughness and surface tension after machining. Based on our measurements, we have made a suggestion on the value of the ensemble of open time, applied quantity and pressure, pressing time, and surface preparation/surface roughness parameters which result in good bonding and a shear strength higher than 10 N/mm2. Furthermore, we investigated the penetration of the adhesive into the surface and state that one-sided adhesive application results in differing levels of penetration. In order to check the suitability of beech wood for glued laminated timber production, further investigations according to EN standards are necessary. Based upon the considerations noted above, delamination tests are already under evaluation. Fagus sylvatica / load-bearing glued laminated timber / bondability / penetration Kivonat – Bükk faanyag ragaszthatósága egykomponensű poliuretán szerkezeti ragasztóval. Bükk (Fagus sylvatica L.) faanyag ragaszthatósági vizsgálatait egykomponensű poliuretán (1K PUR) szerkezeti ragasztóval a Nyugat-magyarországi Egyetem Simonyi Károly Karán végeztük.