Alsonyek-Discussion-Paper Final.Pdf
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Kft. 24741725210 3397 MAKLÁR II. Rákóczi F U.16
Név Adószám Irányítószám Helység Út Hátralék "Aranyküllő Sport" Kft. 24741725210 3397 MAKLÁR II. Rákóczi F u.16. 270757 1 TH STOP KFT 14472037210 3345 MÓNOSBÉL RÓZSA U.16. 117839 1992 KFT."f.a." 11161329210 3300 EGER SZVORÉNYI UT 23. III/2. 171177 2 NZ Kft 11176529210 3300 EGER CIFRAKAPU U. 76. 163205 3 COM-DT KFT "f.a." 12963368210 3300 EGER Sas utca 60/A. 257402 6B TESSO KFT "f.a." 13434346210 3300 EGER Széchenyi I u. 42. 126811 A VÁROS RITMUSA KFT "f.a." 14978928210 3300 EGER Trinitárius utca 1. 120577 ABA AGRIA Bt."kt.a." 26069058110 3300 EGER TÖVISKES TÉR 2. 3.EM. 10 101793 Ablak-Építő Kft 14269505210 3300 EGER Rajner Károly utca 44. 164823 Ablak-Solutions Kft. "f.a." 11162540242 3300 EGER SZARVASKŐI U.18. 1409728 ACHILLES TCS KFT "v.a." 14590102210 1161 BUDAPEST JÓZSEF A U.10.F.ÉP. 160604 ADLER-CASTOR KFT."f.a." 22647883210 3300 EGER Újsor utca 89. 444816 ADÓ-K 2008 Kft. "f.a." 14502196110 3300 EGER Vörösmarty u.26.III/2. 102667 AGÁRDY P.A.G.KFT 23927391210 3300 EGER Meder utca 7. 947716 AGRIA 2004 BT "kt.a." 21855207210 3300 EGER Egészségház u. 31.FSZ.1. 121922 AGRIA CONSULTING Bt 21188624110 3300 EGER DEÁK F. ÚT 27. 342996 AGRIA CSÁRDA KFT 14767292203 6000 KECSKEMÉT CSOKOR U.1. 1950987 Agria Food Kft "f.a." 24287612210 3300 EGER Farkasvölgy utca 39. 184700 AGRIA MOBIL KFT"f.a." 11865157210 3300 EGER KISTÁLYAI ÚT 0653/5.HRSZ. 4394981 AGRIA NUTS POKER Kft."f.a." 23325191110 3300 EGER Törvényház utca 15. 578958 AGRIA SZIVÁRVÁNY KFT"f.a." 10715918210 1144 BUDAPEST XIV VEZÉR U 53/D 2/9 187013 Agria Trend Team Kft. -
Natural Radioactive Element Content of the Old Crystalline Rocks in Southern Transdanubia (Sw Hungary)
Acta Mineralogica-Petrographica, Szeged, XL, 121-138, 1999 NATURAL RADIOACTIVE ELEMENT CONTENT OF THE OLD CRYSTALLINE ROCKS IN SOUTHERN TRANSDANUBIA (SW HUNGARY) E. PÁL MOLNÁR*, I. VADOS**, I. GERZSON**, B. KÓBOR* •Department of Mineralogy, Geochemistry and Pétrology, Attila József University "Mecsekérc Environment Protection Co. ABSTRACT On the basis of systématisation of several thousand radioactive element content analyses made in laboratories since the 50's, U and Th content of old granitoid rocks of Southern Transdanubia proved to be much higher than the average U and Th content of granitoids in the world. This value of rocks from areas west of Mecsek Mountains as well as near Szalatnak village and Pecs city is twice higher than the world average. Areas west of the Mecsek Mountains show higher U and lower Th contents than areas east of these mountains. Uranium accumulation is higher in aplites and hydrothermal formations than in granites. The western and eastern granites are less and highly sensitive to leaching, respectively. The intensive U migration resulted in significant U accumulation in young sediments in some places. INTRODUCTION Study of natural radioactive element (U /Ra1, Th, K) content of the rocks in Hungary was performed by the Mecseki Ércbányászati Vállalat (Mecsek Ore Mining Company) until 1990, when uranium exploration was stopped in Hungary. Aim of the analyses was to research U sources, therefore, rocks supposed to contain perspective U accumulation were mainly studied. The aim of this paper is to elaborate many thousands radiological data of granitoid rocks, gneisses and amphibolite-like metamorphic rocks coming from Southern Transdanubia (south of the Szekszárd-Kaposvár-Kutas line to the state boundary, and east of the Kutas-Csokonyavisonta-Barcs line to the Danube). -
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. -
Royals on the Road. a Comparative Study of the Travel Patterns of Two
Árpád Bebes Royals on the road. A Comparative study of the travel patterns of two Hungarian kings Sigismund of Luxemburg and Matthias Corvinus MA Thesis in Medieval Studies Central European University CEU eTD Collection Budapest May 2015 Royals on the road. A Comparative study of the travel patterns of two Hungarian kings Sigismund of Luxemburg and Matthias Corvinus by Árpád Bebes (Hungary) Thesis submitted to the Department of Medieval Studies, Central European University, Budapest, in partial fulfillment of the requirements of the Master of Arts degree in Medieval Studies. Accepted in conformance with the standards of the CEU. ____________________________________________ Chair, Examination Committee ____________________________________________ Thesis Supervisor ____________________________________________ Examiner ____________________________________________ CEU eTD Collection Examiner Budapest May 2015 Royals on the road. A Comparative study of the travel patterns of two Hungarian kings Sigismund of Luxemburg and Matthias Corvinus by Árpád Bebes (Hungary) Thesis submitted to the Department of Medieval Studies, Central European University, Budapest, in partial fulfillment of the requirements of the Master of Arts degree in Medieval Studies. Accepted in conformance with the standards of the CEU. ____________________________________________ External Reader CEU eTD Collection Budapest May 2015 Royals on the road. A Comparative study of the travel patterns of two Hungarian kings Sigismund of Luxemburg and Matthias Corvinus by Árpád Bebes -
Adatok a Baranyai-Dombság Flórájához -..:::: Kitaibelia
17 KITAIBELIA XIII. évf. 1. szám pp.: 17-28. Debrecen 2008 Adatok a Baranyai-dombság flórájához PURGER Dragica Pécsi Tudományegyetem, TTK, Biológiai Intézet, Állatökológia Tanszék, H-7624 Pécs, Ifjúság útja 6. [email protected] Bevezetés A Mecseken és környékén végzett botanikai kutatások több mint kétszáz éves történetét HORVÁT Adolf Olivér munkái foglalják össze (HORVÁT 1942, 1958, 1975, 1976, 1977). Az elmúlt évtizedekben végzett florisztikai felmérések eredményei számos adattal gazdagították ismereteinket a Baranyai-dombság növényvilágáról (KEVEY 1986, 1988, 1995, 2001, KEVEY & HORVÁT 2000, DÉNES 1997, TÓTH 1998, 1999, 2000). Az utóbbi öt évben országszerte intenzív terepbotanikai kutatások folytak, és a legújabb eredmények (K EVEY 2004, PÁL 2002 a, b, 2003, PURGER 2002 a, 2002 b, CSIKY et al. 2005) arról tanúskodnak, hogy a vizsgált terület még sok feltáratlan botanikai értéket rejt. A vizsgált terület és módszerek A Baranyai-dombság a Mecsekt ől délre-délkeletre terül el. Négy részre tagolódik. Délen a Pécsi-síkság, attól északkeletre, pedig a Geresdi-dombság helyezkedik el. Legnagyobb részét a Dél-Baranyai dombság kistáj teszi ki. A Baranyai-dombság negyedik részét, mint egy sziget a Villányi hegység képezi (MAROSI & SOMOGYI 1990). Ez utóbbi tájegységet azonban e munkában mell őzzük, tekintettel arra, hogy a növényföldrajzi dolgozatokban a Villányi-hegységet általában külön (pl. MOLNÁR 1999), vagy a Mecsekkel együtt tárgyalják (pl. BORHIDI 2006). A félreértések elkerülése végett itt jegyzem meg, hogy az el őző cikkemben (PURGER 2002 a) a „Baranyai-dombság” név alatt a Dél-Baranyai dombságot értettem. Mindazonáltal, az egész térséget, és ezt a területet is, a geográfusok és a botanikusok több néven tárgyalyák: pl.: Mecsekalja (HORVÁT 1942), Tolna-Baranyai dombvidék (BORHIDI 2006, PÁL 2003). -
8 Book Review.Indd
88 Chronicle – Hungarian Geographical Bulletin 66 (2017) (1) 88–89. CHRONICLE György Lovász (1931–2016) A prominent representative of Hungarian physical channel erosional geography, one of the last of his generation, passed processes, trig- away on 3 October 2016. Professor György Lovász gered by river was born on 23 May 1931 in Budapest. He studied regulation works. geography and history at the Budapest University, He also pointed where he gathered rich experience in fieldwork out the impact of under the guidance of Professor Sándor Láng. recent tectonics While he worked as a teacher in a vocational school on riverbed inci- of Nagykanizsa and in a primary school of Gyál, sion and subsid- Professor Béla Bulla encouraged him to start with ence of the afore- scientific research. mentioned three In 1956 his first academic paper appeared in print rivers (published on the origin of the ’meridional valleys’ of the Zala in the Journal of Hills, an issue which is still a subject of heated de- Hydrology and bates among Hungarian geomorphologists. He him- Hydromechanics self also returned to this topic and summarised his in 2007). opinion in a paper published in 1970. The thesis written for obtaining the university Working in the Transdanubian Institute of the doctorate in 1959 was concerned with the evolution Hungarian Academy of Sciences in Pécs, his favourite of the Lenti Basin. He also studied the evolution of topics encompassed the geomorphological issues of the Drava floodplain and concluded that the basin, the Mecsek Mountains, such as the planated surfaces, originally thought to be uniform was dissected into the evolution of the Pécs Basin and the karst and loess subbasins during the Holocene. -
Kompolt: the Divided Village
PÉTER VÁRKONYI Kompolt: The Divided Village Pro&Contra 1 (2018) 81-95. DOI: 10.33033/pc.2018.1.81 KOMPOLT: THE DIVIDED VILLAGE 83 Abstract This paper discusses the history of modern Kompolt, a village in Heves County, Hunga- ry, with a particular emphasis on its social history. During the 19th and 20th centuries, the society of Kompolt was split along a number of lines and this essay focuses on just one of these divisions, that between the Swabians and the Hungarians. Keywords: Kompolt, identity, Germans, Swabians, Hungarians, society, 19th century, 20th century, immigrants, agriculture, material culture, demography I. Hypothesis This research is grounded in a paradox.1 Swabians have resided in Kompolt since the 18th century but the statistics (for example, the censuses from the 20th century) do not reflect this ethnic reality. A detailed examination can uncover the reason for this paradox. The settlement structure and material culture (on maps and in today’s reality), the sources of Kompolt’s economic status, and the self-reflections of the inhabitants (in the personal papers of both the town’s inhabitants and the community, as well as in interviews) confirm that Kompolt was indeed divided in the past and thus brings the accuracy of the censuses into question. It is this disconnect between reality and bureaucracy that supplies the hypothesis for this study. The prime importance of source criticism for the result of censuses is widely ac- cepted. The methodology2 adopted, the assessors and external factors (politics3, indiscre- tion4, and beliefs5) affect the comparability and usability of the results of censuses. -
Pécs Várad, a Keleti-Mecsek Kapuja PÉCSVÁRADI
Hírmondó PÉCSVÁRADI Az önkormányzat lapja* 1993. május •III; évfolyam 5. szám*Ára; 20,-Ft Természeti környezetünk Pécs várad, a Keleti-Mecsek kapuja Szeretettel é s tisztelettel köszöntünk minden Édesanyát é s Nagym am át! Látkép a Zengő oldalról. Fotó: Qörbics János í. ■* A község a Mecsek hegység egység, tiszta patakokkal, forrá csak itt, vag5fc=nagyobb számban déli peremén, a Zengő (682 ni) sokkal. Éghajlata szintén össze csak itt található, mint hazánk védelmében húzódik meg. tett. A tavaszi - őszi csapa egyik legszebb vadon termő vi A Mecsek szigetszerűen emel dékcsúcs szubmediterrán, a júni rágos növénye, a szubmediter kedik ki környezetéből. Hajdan usi, általában jégesővel kísért rán flóraelem, a bánáti bazsaró két tömbje ténylegesen is sziget záporok kontinentális hatást zsa: peónia banatica. Az Önkormányzat volt - a Keleti Mecsekben a mutatnak. Jelentősen befolyá Állatvilága is gazdag, sok vé Zengő-Dobogó 450 tszfm feletti solja a klímát a domborzat - a dett fajjal (törpesas, békászó és része. A hegység a mélyre Zengő déli oldalán 600 mm az sas, fekete gólya... ). A vadász a Szerkesztőség süllyedt variszkuszi hegység- évi csapadék, az északi lejtón ható fajok bősége eredményes rendszer felszínen maradt 100 mm-rel több. vadgazdálkodást tesz lehetővé. dombja, melyre többszörösen Besugárzásnál 60 % -kai na A védett déli oldal kedvező tengeri üledék rakódott. gyobb a déli lejtő többlete. (A körülményeket biztosított az Szerkezetét, felszínét gyűrő Zengő déli lépcsőjének és Afri emberi életnek is. A közelben dések, vetődések, és - főleg a ka E-i peremének klímája közel kőkori települést tártak fel Keleti Mecsekben - a vulkáni megegyezik.) (Dombay, 1960), kőszerszámo tevékenység is erősen befolyá Szeged után az országban itt kat ma is fordít ki eke. -
The Karpatian (Late Early Miocene) Flora of the Mecsek Area
Acta Palaeobotanica 60(1), 51–122, 2020 e-ISSN 2082-0259 https://doi.org/10.35535/acpa-2020-0003 ISSN 0001-6594 The Karpatian (late early Miocene) flora of the Mecsek area LILLA HABLY Botanical Department, Hungarian Natural History Museum, H-1431 Budapest, P.O. box 137, Hungary; e-mail: [email protected] Received 9 September 2019; accepted for publication 28 January 2020 In remembrance of the beautiful summers spent collecting with my family in the Mecsek Mountains ABSTRACT. A rich macroflora has been collected from Karpatian (late early Miocene) layers of the Mecsek Mts during recent decades. The bulk of the fossil assemblage consists of leaves and also fruits of angiosperms. Among the more than a hundred taxa, several endemic species were described: Leguminocarpum mecsekense Andreánszky, Ailanthus mecsekensis Hably, Nyssa gyoergyi sp. nov., Nyssa gergoei sp. nov., Nyssa sp. 1, Clematis csabae sp. nov., Gordonia sp. and Carpolithes gergoei Hably et Erdei sp. nov. Many taxa were last recorded in the Carpathian Basin, e.g. Cedrelospermum, Ziziphus. Other taxa appeared in this flora, e.g. Quercus kubinyii, Podocarpium podocarpum, Liquidambar europaea and Populus populina, and later became dominant in the middle Miocene (Sarmatian) floras or even in the late Miocene (Pannonian) floras. Four main vegetation types were determined. The most significant types are subxerophytic vegetation showing high diversity, swamp veg- etation, riparian vegetation, and a vegetation type growing in habitats with higher rainfall. Thermophilous flora elements are dominant in the assemblage, although “arctotertiary” species also appear. The floristic character of the flora supports the results of an earlier quantitative climate analysis of the Magyaregregy flora, accord- ing to which mean annual temperature was 15.6–16.6°C and coldest-month and warmest-month temperatures were 5–6.2°C and 24.7–27.9°C, respectively. -
A Millennium of Migrations: Proto-Historic Mobile Pastoralism in Hungary
Bull. Fla. Mus. Nat. Hist. (2003) 44(1) 101-130 101 A MILLENNIUM OF MIGRATIONS: PROTO-HISTORIC MOBILE PASTORALISM IN HUNGARY Ldsz16 Bartosiewiczl During the A.D. 1st millennium, numerous waves of mobile pastoral communities of Eurasian origins reached the area of modern- day Hungary in the Carpathian Basin. This paper reviews animal exploitation as reconstructed from animal remains found at the settlements of Sarmatian, Avar/Slavic, and Early ("Conquering") Hungarian populations. According to the historical record, most of these communities turned to sedentism. Archaeological assemblages also manifest evidence of animal keeping, such as sheep and/or goat herding, as well as pig, cattle, and horse. Such functional similarities, however, should not be mistaken for de facto cultural continuity among the zooarchaeological data discussed here within the contexts of environment and cultural history. Following a critical assessment of assemblages available for study, analysis of species frequencies shed light on ancient li feways of pastoral communities intransition. Spatial limitations (both geographical and political), as well as a climate, more temperate than in the Eurasian Steppe Belt, altered animal-keeping practices and encouraged sedentism. Key words: Central European Migration, environmental determinism, nomadism, pastoral animal keeping Zoarchaeological data central to this paper originate from Data used in this study represent the lowest common settlements spanning much of the A.D. 1st millennium denominator of the three different -
BARANYA Megye Autóbusz-Hálózata
Jelmagyarázat / Legend 5707 Lengyel Országos autóbuszjáratok útvonala Mekényes BARANYA megye autóbusz-hálózata 5707 Route of long-distance bus services Dombóvár 5707 Nagyhajmás Regionális autóbuszjáratok útvonala Bus network of Baranya county 5707 Route of regional bus services 5611 Pécs 5707 Komló 2021. április 11-től Dombóvár 1652 5924 Mohács térségi központtal Dombóvár 5611 5707 Siklós és Harkány with regional hub Pápa Szárász 1564 Sásd 5706 Mágocs 1652 Vajszló és Sellye Veszprém 1740 5623 5708 5611 5611 Szigetvár Siófok 5608 5623 5707 Magyaregregy 5702 5706 1134 Budapest Egyéb (szomszédos megyék gócpontjairól induló) vonalak Dombóvár Dombóvár 5708 5707 Egyházaskozár 1566 Kecskemét Other services (of the neighbouring counties) 5516 5702 Budapest 50 Bikal 5924 1568 Kiskőrös A vastagabb vonallal jelölt szakaszon az autóbuszok sűrűbben, 1652 1707 Győr a vékonyabb vonallal jelölt jelölt szakaszon ritkábban közlekednek az autóbuszok 5708 5611 1843 Tatabánya Thicker line represents more frequent services, Vásárosdombó Hegyhátmaróc Tófű 1136 Budapest Alsómocsolád 5623 5625 Bonyhád Thinner line represents less frequent services Jágónak Gerényes 1652 Szeged 5706 5626 Siófok 5605 5740 Vásárosdombó 5710 5707 5434 5624 Szekszárd 5887 Autóbuszvonal száma Keszthely 1576 5702 Mágocs- 5630 Szekszárd Kiskeresztúr 5702 Köblény 5924 5485 5710 Bonyhád Bus line number Kaposvár 5606 5930 5931 5932 40 Alsómocsolád Szalatnak 5631 Nagydorog Gödre 5924 Mohács Autóbuszvonal száma a járat végállomásánál 1578 Meződ 1652 Ág Szászvár 5634 Paks 5887 Kárász- 5856 -
Sideritic–Kaolinitic and Green Clay Layers in the Mecsek Mountains (SW Hungary): Indicators of Middle Triassic Volcanism–Myth Or Reality?
Central European Geology, Vol. 58/4, 334–355 (2015) DOI: 10.1556/24.58.2015.4.4 Sideritic–kaolinitic and green clay layers in the Mecsek Mountains (SW Hungary): Indicators of Middle Triassic volcanism–Myth or reality? Georgina Lukoczki1, 2, 3*, Tamás Budai2, 4, Tibor Németh5, 6 1Boone Pickens School of Geology, Oklahoma State University, Stillwater, USA 2Department of Geology and Meteorology, University of Pécs, Pécs, Hungary 3Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Pécs, Hungary 4Geological and Geophysical Institute of Hungary, Budapest, Hungary 5Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budapest, Hungary 6Department of Mineralogy, Eötvös Loránd University, Budapest, Hungary Received: January 31, 2016; accepted: February 1, 2016 Sideritic–kaolinitic and green clay layers were previously reported from the Mecsek Mountains (SW Hungary) as indicators of Tethyan volcanism in the otherwise germanotype Middle Triassic succession. The aim of the present study is to provide a review and a critical re-evaluation of the previously pub- lished data on both the sideritic–kaolinitic layers (the so-called “Mánfa Siderite”) and the green clay layers. New results of mineralogical investigation of the green clay layers are also presented. The Middle Triassic volcanic origin of the “Mánfa Siderite” cannot be confirmed. In addition to a possible volcanic contribution, the sideritic–kaolinitic layers were probably formed in a freshwater swamp under humid, tropical climatic conditions, whereby weathering in an organic-rich, acidic environment led to the for- mation of “underclays” and siderite in the coal-bearing formations of Late Triassic to Early Jurassic age.