Cultural Connections and Interactions of Eastern Transdanubia During the Urnfeld Period
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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. -
És a Balatonf F Ldtana Velencei-Hegység Geology
Gerinc 10 mm ALATONFÕ B THE AND ILLS H ELENCE V THE OF EOLOGY — G MAGYARORSZÁG TÁJEGYSÉGI TÉRKÉPSOROZATA LDTANA Ö REGIONAL MAP SERIES OF HUNGARY F Õ A VELENCEI-HEGYSÉG ALATONF B A S ÉS A ALATONFÕÖF LDTANA B É G É GEOLOGY HEGYS - OF THE ELENCE ILLS V H ELENCEI V AND THE ALATONFÕ B A A Velencei-hegység és a Balatonfő földtana Magyarázó a Velencei-hegység földtani térképéhez (1:25 000) és a Balatonfő–Velencei-hegység mélyföldtani térképéhez (1:100 000) Geology of the Velence Hills and the Balatonfő Explanatory Book of the Geological Map of the Velence Hills (1:25 000) and the Geological Map of Pre-Sarmatian Surface of the Balatonfő–Velence Area (1:100 000) Szerkesztette — Edited by: GYALOG László és HORVÁTH István Írta — Written by: HÁ ORV TH István, DARIDÁNÉ TICHY Mária (†), DUDKO Antonyina, GYALOG László, ÓDOR László Közreműködött — With contribution of: BUDAI Tamás, CSÁSZÁR Géza, CSERNY Tibor, CSILLAG Gábor, KAISER Miklós, KÓKAY József, LELKESNÉ FELVÁRI Gyöngyi, LESS György, Ó. KOVÁCS Lajos, SELMECZI Ildikó, T. DOBOSI Viola Budapest, 2004 © Copyright Magyar Állami Földtani Intézet (Geological Institute of Hungary) 2004 Minden jog fenntartva! — All rights reserved! Lektor — Reviewer: BALLA Zoltán Angol szöveg — English text: BALI Enikő Nyelvi lektor — Linguistic reviewer: Philip RAWLINSON Szakmai nyelvi lektor — Terminology revised by: ÓDOR László Műszaki szerkesztő — Technical editor: SIMONYI Dezső, PIROS Olga Számítógépes nyomdai előkészítés — DTP: SIMONYI Dezső, PIROS Olga Ábrák, térképek — Figures, maps: PENTELÉNYI Antal, SIMONYI Dezső, ALBERT Gáspár, HEGYINÉ RUSZNYÁK Éva Fényképek — Photos: DARIDÁNÉ TICHY Mária, DUDKO Antonyina, GYALOG László, HORÁ V TH István, LESS György Címlapfotó — Cover photo: A pákozdi Kocka (GYALOG László) Kiadja a Magyar Állami Földtani Intézet — Published by the Geological Institute of Hungary H–1143 Budapest, Stefánia út 14. -
34/2017 Sz. Értesítő
MLSZ FEJÉR MEGYEI IGAZGATÓSÁG Cím: 8000 Székesfehérvár, Honvéd u. 3/a. Fszt. Tel.: 06 (22) 312-282, Fax: 06 (22) 506-126 E-mail: [email protected] Web: fejer.mlsz.hu Adószám: 19020848-2-44 Bank: 11707024-20480772 Számlázási cím: 1112 Budapest, Kánai út 2/d. 34/2017. (10.11.) sz. Megyei Hivatalos Értesítő Versenybizottság határozatai VB-72/2017/2018. (10.10.) Az AGÁRDI TERMÁL Megyei II. osztályú U-19 bajnokság 9. fordulójában, a 2017. október 07. 10:00 órára kiírt Pusztaszabolcs – Adony mérkőzésre az Adony csapata 10 fővel jelent meg. (Kódszám: 1262255) A Versenybizottság második létszámhiányos kiállás miatt az Adony U-19 csapatának évi összeredményéből 1 büntetőpontot levon. (MLSZ Versenyszabályzat 42. §. (2) bekezdés c) pontja, 2) alpontja alapján.) A Versenybizottság versenyügyi eljárást kezdeményez az Adony U-19 csapata ellen. (MLSZ Versenyszabályzat 41. §. (5) bekezdés e) pontja alapján. Az Adony U-19 csapata második alkalommal állt ki létszámhiányosan. Felhívjuk a figyelmüket az MLSZ Versenyszabályzat 42. §. (2) bekezdés c) pontjára! VB-73/2017/2018. (10.10.) Az Öregfiúk bajnokság 4. csoportjának 7. fordulójában, a 2017. október 07. 15:00 órára kiírt Lajoskomárom – Sárszentágota mérkőzés elmaradt. (Kódszám: 1263764) A mérkőzés 3 pontját 3:0 gólkülönbséggel a Versenybizottság a Lajoskomárom öregfiúk csapata javára rendeli el jóváírni. (MLSZ Versenyszabályzat 41. §. (4) bekezdés a) pontja) alapján.) A Sárszentágota öregfiúk csapatát írásbeli megrovásban részesítjük. (MLSZ Versenyszabályzat 41. §. (4) bekezdés h) pontja 1) alpontja alapján.) A Versenybizottság megállapítja a Sárszentágota öregfiúk csapatának versenyügyi felelősségét, és fegyelmi eljárást kezdeményez a Sárszentágota öregfiúk csapata ellen. (MLSZ Versenyszabályzat 41. §. (1) bekezdés a), és b) pontja, illetve a 41. §. (3) bekezdés b) pontja alapján. -
Origin of Eocene-Covered Karst Bauxites of the Transdanubian Central Range (Hungary) Evidence for Early Eocene Volcanism
Eur. J. Mineral. 1992, 4, 581-595 Origin of Eocene-covered karst bauxites of the Transdanubian Central Range (Hungary) evidence for early Eocene volcanism ISTVÁN DUNKL Hungarian Academy of Sciences, Laboratory for Geochemical Research, H-1112, Budapest, Budaörsi üt 45, Hungary Abstract : Fission track (FT) ages measured in detrital zircon crystals from Eocene-covered bauxites of the Transdanubian Central Range (TCR) appear to reflect the cooling age of the source rock(s). Thus, by means of FT-dating of zircons new information could be obtained to explain the problem of source rocks debated so far. Since the majority of the detrital zircon crystals proved to be euhedral, their typologic analysis permitted conclu sions regarding the petrographic character of the source rocks as well. (1) In the light of the age results it is clear that the pyroclastics of a Pre-Middle Eocene volcanism contributed to the bauxite material which was deposited on the exposed karstified carbonate terrain. Andesitic tuffite layers intercalated in the upper part of the overlying Eocene sequence are traces of younger explosions of the same Paleogene volcanic event. Zircon grains found in the bauxite are morphometricaHy identical to those found in the younger Eocene pyroclastics of andesitic character. (2) A euhedral zircon population of 210 to 260 million years was also identified in some of the bauxite deposits studied. These crystals derive most probably from Middle Triassic trachyandesite tuffs of the Central Range, though anatectic granitic sources cannot be excluded. (3) Those zircon grains which are the oldest and fairly well rounded are thought to derive from the parametamor- phic of Hercynian age of the surrounding areas. -
Regional Geology Reviews
Regional Geology Reviews Series Editors Roland Oberh€ansli Maarten de Wit Francois M. Roure For further volumes: http://www.springer.com/series/8643 . Ja´nos Haas Editor Ja´nos Haas • Ge´za Ha´mor{ •A´ ron Ja´mbor • Sa´ndor Kova´cs{ • Andra´s Nagymarosy • Tibor Szederke´nyi Geology of Hungary Editor Ja´nos Haas Eotv€ os€ Lora´nd University Geological, Geophysical and Space Science Research Group Budapest Hungary ISBN 978-3-642-21909-2 ISBN 978-3-642-21910-8 (eBook) DOI 10.1007/978-3-642-21910-8 Springer Heidelberg New York Dordrecht London Library of Congress Control Number: 2012936971 # Springer-Verlag Berlin Heidelberg 2012 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. Exempted from this legal reservation are brief excerpts in connection with reviews or scholarly analysis or material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Duplication of this publication or parts thereof is permitted only under the provisions of the Copyright Law of the Publisher’s location, in its current version, and permission for use must always be obtained from Springer. Permissions for use may be obtained through RightsLink at the Copyright Clearance Center. -
Karszt És Barlang
Karszt es Barlang, Special Issue 1989. p. 17— 30. Budapest THE CAVES OF HUNGARY Kata lin Takdcs-Bolner — Istvan Eszterhas — Mart on Juhasz — Sandor Kraus Young clastic sediments constitute a large share the travertine deposited by large karst springs is of the geological composition of Hungary; car enhanced by their rarity. bonate rocks suitable for karstification only amount The oldest known karstic phenomena in Hun to a mere 1.5% of the surface of the country (Fig. gary are the 70—100 million year old karstic sur I). Despite the limited expanse of karstic regions, faces of the Cretaceous period which were exposed there are more than 2,400 caves registered in Hun during bauxite and manganese mining in the Bakony gary today. Even so, only 77 of them reach 200 m, Mountains. The fossils found in the cave fills prove and a mere 24 stretch to 1 km. Since our karstic that our oldest cave was created at the end of the regions are mostly of medium height, the vertical Miocene period; several caves can be dated back extent of the caves is not great: sixty-nine extend to the lower Pleistocene era, while most of our to a depth of 50 m, and only 3 are deeper than known caves were formed over the past one and a 200 m. half million years during the middle and upper The number of known caves has increased con Pleistocene periods. siderably during the past decade due to systematic field-work and new explorations: compared to the Aggtelek Karst 1,314 known caves in 1977 the present figure is up One of the most typical karstic area of Hungary 85%. -
Cretaceous Sediments of the Transdanubian Range
Cretaceous sediments of the Transdanubian Range Geological excursion 14–16 May 2009 Organized by the Sedimentological Subcommission of the Hungarian Academy of Sciences and the Hungarian Geological Society Field guide Leaders: Géza CSÁSZÁR1, János HAAS2, Andrea MINDSZENTY3, Attila ŐSI4, Márton PALOTAI5, Tamás POCSAI6, Ágoston SASVÁRI6, Ottilia SZIVES7 1Geological Institute of Hungary 2Geological Research Group of the Hungarian Academy of Sciences, Eötvös University 3Eötvös Loránd University, Department of Applied Geology 4Hungarian Academy of Sciences – Hungarian Natural History Museum, Research Group for Paleontology 5 Eötvös Loránd University, Department of Geology 6MOL (Hungarian Oil and Gas Company) 7Hungarian Natural History Museum Department of Palaeontology Budapest, 2009 Cretaceous sediments of the Transdanubian Range, 14–16 May 2009 Field guide Programme May 14 Gerecse Mountains Stop 1. Geological Open Air Museum, Tata Stop 2. Grindstone quarry, Lábatlan Stop 3. Marl Yard, Bersek Hill, Lábatlan 2 Cretaceous sediments of the Transdanubian Range, 14–16 May 2009 Field guide May 15 Bakony Mountains Stop 1. Eperjes Hill, Olaszfalu Stop 2. Abandoned quarry between villages Zirc and Borzavár Stop 3. A quarry of Jásd Stop 4. Iharkút, Dinosaur-bearing alluvial complex of the Csehbánya Formation May 16 Bakony Mountains Stop 1. Sümeg, Mogyorós Hill Stop 2. Sümeg, Sintérlap quarry Stop 3. Manganese slurry reservoir, Úrkút Stop 4. A quarry on the south-western side of the road between Úrkút and Ajka 3 Cretaceous sediments of the Transdanubian Range, 14–16 May 2009 Field guide Introduction Introduction to the geology of the Transdanubian Range Cretaceous Géza CSÁSZÁR The Jurassic history of the Transdanubian Range were characterized by disintegration of the long lasting (Middle to Late Triassic) carbonate platform thanks to the separation of Africa and North America and as a consequence Africa and Europe. -
Magyarország Közigazgatási Helynévkönyve, 2014. Január 1
Magyarország közigazgatási helynévkönyve 2014. január 1. Gazetteer of Hungary 1st January, 2014 Központi Statisztikai Hivatal Hungarian Central Statistical Office Budapest, 2014 © Központi Statisztikai Hivatal, 2014 © Hungarian Central Statistical Office, 2014 ISSN 1217-2952 Felelős szerkesztő – Responsible editor: Waffenschmidt Jánosné főosztályvezető – head of department További információ – Contact person: Nagy Ferenc Andrásné szerkesztő – editor (tel: 345-6366, e-mail: [email protected]) Internet: http://www.ksh.hu [email protected] 345-6789 (telefon), 345-6788 (fax) Borítóterv – Cover design: Nyomdai kivitelezés – Printed by: Xerox Magyarország Kft. – Táskaszám: 2014.076 TARTALOM ÚTMUTATÓ A KÖTET HASZNÁLATÁHOZ ............................................................................................................... 5 KÓDJEGYZÉK ..................................................................................................................................................................... 11 I. ÖSSZEFOGLALÓ ADATOK 1. A helységek száma a helység jogállása szerint ............................................................................................................................................................ 21 2. A főváros és a megyék területe, lakónépessége és a lakások száma ........................................................................................................................... 22 3. A települési önkormányzatok főbb adatai .................................................................................................................................................................. -
Ministry of Agriculture and Rural Development PROGRAMME
Ministry of Agriculture and Rural Development PROGRAMME-COMPLEMENT (PC) to the AGRICULTURE AND RURAL DEVELOPMENT OPERATIONAL PROGRAMME (ARDOP) (2004-2006) Budapest June 2009 ARDOP PC modified by the ARDOP MC on 7 March 2006 and by written procedures on 18 August, 29 September 2006 and on 14 August 2007, revised according to the comments of the European Commission (ref.:AGRI 004597of 06.02.2007, AGRI 022644 of 05.09.07 and AGRI 029995 of 22.11 07.) 2 TABLE OF CONTENTS I. INTRODUCTION .............................................................................................................. 5 I.1 PROGRAMME COMPLEMENT....................................................................... 5 I.2 THE MANAGING AUTHORITY for ARDOP.................................................. 6 I.2.1 General description......................................................................................... 6 I.2.2 The MANAGING AUTHORITY in Hungary................................................ 6 I.2.3 Monitoring ...................................................................................................... 6 I.2.4 Financial Management and Control Arrangements ........................................ 6 I.2.5 Monitoring the capacities................................................................................ 6 I.3 THE PAYING AUTHORITY............................................................................. 6 I.4 THE INTERMEDIATE BODY .......................................................................... 6 I.5 THE FINAL BENEFICIARIES......................................................................... -
Beiskolázási Körzetek 2 20 2 Település Iskola
Fejér megye településeinek beiskolázási körzetei 2020/2021. tanév Település A kötelező felvételt biztosító iskola OM Irsz. Település Cím Atilla Király Gimnázium, Általános Iskola és Alapfokú Művészeti Iskola Aba 200963 8127 Aba Szent István király tér 7. Aba Sámuel Általános Iskolája Alcsútdoboz Alcsútdobozi József Nádor Általános Iskola 201310 8087 Alcsútdoboz Szabadság u. 105. Bakonycsernye Bakonycsernyei Általános Iskola és Alapfokú Művészeti Iskola 201028 8056 Bakonycsernye Rákóczi utca. 37. Bakonykúti Iszkaszentgyörgyi Általános Iskola 030117 8043 Iszkaszentgyörgy Kastély utca 8. Balinka 1 Bodajki Általános Iskola 201027 8053 Bodajk Bányász ltp. 21-22. Balinka 2 Bakonycsernyei Általános Iskola és Alapfokú Művészeti Iskola 201028 8056 Bakonycsernye Rákóczi utca 37. Bicske Bicskei Csokonai Vitéz Mihály Általános Iskola 030072 2060 Bicske Szent István u. 42. Bodajk Bodajki Általános Iskola 201027 8053 Bodajk Bányász ltp. 21-22. Bodmér Vértesboglári Nyelvoktató Német Nemzetiségi Általános Iskola 030146 8085 Vértesboglár Alkotmány u. 14. Csabdi Csabdi Petőfi Sándor Általános Iskola 202962 2064 Csabdi Szabadság u. 37. Móri Radnóti Miklós Általános Iskola Nádasy Tamás Tagiskolája Csákberényi Telephelye Csákberény 201026 8073 Csákberény Kossuth L. u. 15. (1-4. osztály) Csákberény Móri Radnóti Miklós Általános Iskola Nádasy Tamás Tagiskolája (5-7. osztály) 201026 8074 Csókakő Petőfi u. 5. Csákberény Móri Dr. Zimmermann Ágoston Általános Iskola (8. osztály) 030042 8060 Mór Kodály Z. u. 28. Csákvár Esterházy Móric Nyelvoktató Német Nemzetiségi Általános Iskola 030136 8083 Csákvár Szabadság tér 8. Csókakő Móri Radnóti Miklós Általános Iskola Nádasdy Tamás Tagiskolája 201027 8074 Csókakő Petőfi S. u. 5. Csór Csóri Mátyás Király Általános Iskola 030114 8041 Csór Fő tér 1. Csősz Gorsium Általános Iskola Csőszi Telephelye (1-4. osztály) 030132 8122 Csősz Kossuth L. -
Hungarian National Seismological Bulletin
K¨ovesligethy Rad´oSeismological Observatory HUNGARIAN NATIONAL SEISMOLOGICAL BULLETIN 2011 MTA CSFK GGI - BUDAPEST - HUNGARY Hungarian National Seismological Bulletin 2011 Authors: Zolt´anGr´aczer Tibor Czifra M´artaKiszely P´eterM´onus Tibor Zs´ıros MTA CSFK GGI K¨ovesligethy Rad´oSeismological Observatory Budapest, Hungary 2012 Reference: Gr´aczer,Z., Czifra, T., Kiszely, M., M´onus, P., Zs´ıros,T., 2012. Hungarian National Seismological Bulletin 2011, K¨ovesligethy Rad´oSeismological Observatory, MTA CSFK GGI, Budapest, 357pp. Publisher: Dr. J´ozsefZ´avoti ISSN 2063-8558 This work is licensed under a Creative Commons License. cbed http://creativecommons.org/licenses/by-nc-nd/3.0/ Contents 1 Local earthquakes 9 2 Focal mechanisms 129 3 Macroseismic data 131 4 Regional and teleseismic earthquakes 143 5 References 355 5 Foreword This publication reports the results of the seismological routine work performed at the K¨ovesligethy Rad´oSeismological Observatory. The Observatory belongs to the Geodetical and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungar- ian Academy of Sciences (MTA CSFK GGI). Until the beginning of the year 2012 the Observatory was part of the Geodetical and Geophysical Research Institute of Hungarian Academy of Sciences (MTA GGKI), but because of the structural reform at the Hungarian Academy of Sciences the Institute joined to the new research center, MTA CSFK and has changed its name to MTA CSFK GGI. The Institute will be referred as GGI throughout the Bulletin. The main objectives of the Observatory are operating the Hungarian National Seismo- logical Network and conducting seismological research for the better understanding of the seismicity and structure of the Pannonian basin. -
Hungary Geographical Studies.Pdf
HUNGARY GEOGRAPHICAL STUDIES HUNGARY GEOGRAPHICAL STUDIES Edited by MARTON P6CSI GYORGY ENYEDI SANDOR MAROSI Hungary Geographical Studies INTERNATIONAL GEOGRAPHICAL UNION EUROPEAN REGIONAL CONFERENCE BUDAPEST 1971 f Translotion revised by MARY VOLGYES Title-page designed by L. Ballonyi 704314 MTA KESZ Sokszorosito. F. v.: Szabo Gyula CONTENTS Preface ................................................................................................................................................ 7 Part One . Physical Geography Pecs/, M „ Somogyi, S. and Jakucs, P. Landscape units and their types in Hungary ..................................................................... 11 Bacso, N. The climate of Hungary .......................................... ............................................................... 65 Pecs/', M. and Somogyi. S. The hydrography of Hungary ................................................................................................. 85 Pecsi, M. and Jakucs, P. The natural vegetation of Hungary ........................................................................................ 109 Pecs!, M. and Goczan, L. The soils of Hungary .............................................................................................................. 125 Part two Economic Geography Enyedi, Gy. Regional development of the Hungarian national economy ........................................ 137 Krajkd, Gy. The economic regions of Hungary .........................................................................................