Environmental Geography Ofthe Semi-Arid Regions Ofthe

Total Page:16

File Type:pdf, Size:1020Kb

Environmental Geography Ofthe Semi-Arid Regions Ofthe “Environmental Geography ofthe Semi-arid Regions ofthe Hungarian Great Plains and Arizona: Comparative Changes for Sustainable Productivity” by Kimberly Taylor A Dissertation Presented in Partial Fulfiilment of the Requirements for the Degree Doctor of Philosophy Janus Pannonius University December 1996 “Environmental Geography of the Semi-arid Regions of the Hungarian Great Plains and Arizona: Comparative Changes for Sustainable Productivity” by Kimberly Taylor has been approved December 1996 APPROVED: Supervisory Committee ACCEPTED: Supervising Professor Chair, Doctorate Committee ABSTRACT A comparative study ofthe Great Plains ofHungary and the Basin area of Phoenix, Arizona was performed. Both of these regions are experiencing increasing semi-arid conditions via the desertification process taking place in various regions across the giobe. The environmental, geographical, and physical aspects arc discussed and analyzed with the goal of developing new environrnental policies. The main emphasis is to be placed on the fact that the key to sustainable development is proper land use. Through analysis ofthe antbropogenic influences ofagricultural production, urbanization, and industrialization, recommendations are given to decrease the negative effects of human influence in the wake of significant ciimate changes. The effects of these ciimate changes are predicted for each region, and recommendations presented to either prevent or reverse the ecological changes that have been induced. ACKNOWLEDGMENTS I wish to thank Dr. István Fodor and Dr. George Halasi-Kun for their guidance, encouragement and support. Their interest in this project and critical comments regarding the preparation ofthis dissertation were most valued. I extend gratitude to Dr. Ferenc Schweitzer for Kis professional support and provision of valuable information. I would also like to thank Dr. Jozsef Toth for his professional support ofthis project. I am grateful to Dr. Botond Sinóros-Szabó, without whom the initiation ofthis project would not have been possible. In addition, I would like to thank Dr. Erdie Morris, whose support, encouragement, advice and smile made the process easier. Thanks are also due to Dr. Phil Fernandez, Dr. David Wing, and Dr. Jim Witherspoon for their personal and professional support. A major thanks John Holleman for Kis technical assistance, and to Joyce Holleman for her heip on the manuscript. Thank you to my friend Alicia Doyle for her professional photographic assistance. I would also like to thank Dr. Jerry Justus who lectured for me numerous times, reviewed papers and always said “we just want you to know you’re doing a good job and we appreciate you”. I would like to personaily thank the Szabó family for being there for me every time I have been in Hungary. A special word ofthanks goes to my husband, my mother, and my sister. Mark, tharik you for being understanding, patient, supportive, and my best friend. Mom and Keily, thank you for your constant love, support and patience with this entire time frame. Most ofall, I would like to thank Jehovah for everything He has biessed me with. This dissertation is dedicated to Him. TABLE OF CONTENTS Chapter 1: Environmental, Physical and Geographical Background of Hungary and Arizona 1 Introduction 1 Hungary: The General Facts 7 The General Physical Geography of Flungary 7 The Physical Geography of the Great Plain 13 The General Ciimate of Hungary 19 The Ciimate ofthe Great Plains 22 The Soils ofHungary 26 The Soils ofthe Great Plain 29 Natural Vegetation of Hungary 31 The Vegetation of the Great Plain 33 Hydrological Conditions in Hungary 35 Water Reserves ofthe Great Plain 42 Arizona: The General Facts 44 General Physical Geography of Arizona 44 Physical Geography ofthe Basin and Range Province of Arizona 50 General Ciimate of Arizona 53 The Ciimate ofthe North Basin and Range Province 59 The Soils of Arizona 63 . Soils ofthe North Basin and Range Province 64 The Vegetation of Arizona 65 Vegetation ofthe North Basin and Range Province 70 Hydrological Conditions in Arizona 75 Water Resources in the North Basin and Range Province . 77 Chapter 2: Environmental Geography of Water Resources in Hungary and Arizona 100 Introduction 100 The Hungarian Enviroimient: Past to Present 106 Arizona from an Environmental Perspective 111 Chapter 3: Potential Ramifications oflncreasing Desertification in Hungary and Arizona 118 Introduction 118 Possible Outcomes of Increasing Desertification in Hungary 119 Possible Outcomes oflncreasing Desertification in Arizona 128 Chapter 4: Agriculture and the Environment in Hungary and Arizona 131 Hungary and Agriculture 131 Agriculture and Arizona 146 Chapter 5: Urbanization and the Environment in Hungary and Arizona 154 Hungary and Urbanization 154 Arizona and Municipal Water Demand 162 Chapter 6: Industrialization in Hungary and Arizona 168 11 L . Industrialization in Hungary 168 Industrialization in Arizona 172 Chapter 7: Water Resource Policy Analysis in Hungary and Arizona 176 Water Resource Policy Analysis in Hungary 176 Water Resource Policy Analysis in Arizona 179 Chapter 8: New Results 187 Chapter 9: Recommendations for Sustainable Future Productivity 190 Introduction 190 Hungary 191 Arizona 192 References 194 Ui. LIST OF FIGURES Figure 1.1: States in South Eastern Europe, 950-1990 8 Figure 1.2: Hungary’s Present-Day Position in Europe 9 Figure 1.3: Basin Orientation of }{ungary 10 Figure 1.4: Geomorphological Regions of Hungary 12 Figure 1.5: The Great Hungarian Plains 15 Figure 1.6: Political Map ofHungary 23 Figure 1.7: Topography and Hydrography ofthe Danube Basin 36 Figure 1.8: Passage by Land to California 45 Figure 1.9: Three Macroregions of Arizona 46 Figure 1.10: Generalized ReliefofArizona 48 Figure 1.11: Physiographic Diagram of Arizona 49 Figure 1.12: Biogeographic Provinces ofthe Southwest 51 Figure 1.13: Population Distribution 54 Figure 1.14: Koppen Ciimate Regions 55 Figure 1.15: Annual Rainfall in Arizona 61 Figure 1.16: Vegetation in Arizona 66 Figure 1.17: Interior Chaparall of Arizona 68 Figure 1.18: Vegetational Subregions of the Sonoran Desert 71 Figure 1.19: Desert Scrub ofthe Lower Colorado River Valley 72 Figure 1.20: Vegetation ofthe Arizona Upland Desert 74 Figure 1.21: Arizona’ s Ancient Irrigation Network 76 Figure 1.22: Arizona’s Planning Areas and Groundwater Basins 78 Figure 1.23: Regional Map 79 Figure 1.24: Regional Map 81 Figure 1.25: Regional Map 83 Figure 1.26: Regional Map 85 Figure 1.27: Earth Fissure in Arizona 89 Figure 2.1: The Water Cycle 102 Figure 2.2: Reduction ofthe Ozone Layer 105 Figure 2.3: Satellite Photo Map of Arizona 115 Figure 2.4: River Flow in Arizona 116 Figure 3.1: Areal Distribution of the “Days of heat” in 1993 121 Figure 3.2: Areal Distribution ofthe Longest Precipitation-Poor Period in the Summer of 1993 122 Figure 3.3: Actual and Potential Salt Effected Soils in Hungary 126 Figure 3.4: Areal Position ofthe Largest Droughts of 1990-93 127 Figure 4.1: Drought Index: H = Evaporation per year/Precipitation per year 136 Figure 4.2: Water Use According to Sector 137 4 3 Quality of Surface Waters 140 Figure lv L Figure 4.4: Groundwater Quality in Various Hungarian Hydrogeological Areas 143 Figure 5.1: Quotient of Inhabitants with Public Water Supply and those with Public Sewerage 158 Figure 5.2: Anzona Population Distribution, 1994 163 / V. LIST OF TABLES Table 4.1: Land Under Cultivation by Area 132 Table 4.2: Supply ofFertilizers 14 Table 4.3: Irrigation by Type ofLand 135 Table 4.4: Sampiing Sites of Surface Water Grouped According to River System and Sampiing Frequency 139 Table 4.5: Mean Values ofNitrate and Orthophosphate Ions During the Fourth, Fifth, and Sixth Five-year Plan Periods (1976-80, 1981-85, 1986-90) 139 Table 4.6: Total Water Availability and Use 141 Table 4.7: Stream Sediment Sampies Collected by the U.S. Fish aiid Wildlife Service, 1985-87 152 Table 5.1: Urban and Rural Population (in percent) 155 Table 5.2: Housing Stock by Numbers ofRooms and Services (in percent) 156 Table 5.3: Soil Degradation Processes, Acidification 161 Table 6.1: Historical Industrial Sectors 169 Table 6.2: Industrial Generation of Wastewater 171 Table 6.3: Industries in Arizona 173 Vi. CHAPTER1: ENVIRONMENTAL, PHYSICAL, AND GEOGRAPHICAL BACKGROUND OF HUNGARY AND ARIZONA INTRODUCTION Earth, one ofthe nine planets within our solar system, is 510 million square kilometers ard contains a human population of 5 billion. Earth can be discussed in terms ofbeing a system, as a system is an interrelated set ofthings linked by flows of energy and matter. The nature of the organization of a system can be either open or ciosed. Earth has characteristics of both. In terms of energy, our planet can be ciassified as an open system. Analogous to this lack of self-containment is the functioning of a green leaf. Water, carbon dioxide, and sunlight represent inputs of energy which effect matter (via carbohydrates) while energy outputs inciude oxygen aud water transpiration. The Earth, energeticaily speaking, functions in the same manner. Solar energy enters the system and heat energy leaves the system freely, while some energy is temporarily stored in various states. Theoretically, the amounts of energy input and energy output are ultimately equal and in a fixed amount, therefore the Earth is in a relatively steady-state equilibrium in regards to fixed, dependent events. It is when either the input is greater than the output or the output remains in a stored capacity for 2 too long ofa period oftime that the dynamic equilibrium ofthe Earth’s geosystems change. These changes tend to be gradual over time and space, but do have cumulative effects on the operation of the system. This is currently the situation in the case of increasing atmospheric and ocean temperatures, as well as in the fluctuating weather patterns that are occurring across the giobe.
Recommended publications
  • 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.
    [Show full text]
  • Cultural Connections and Interactions of Eastern Transdanubia During the Urnfeld Period
    Dissertationes Archaeologicae ex Instituto Archaeologico Universitatis de Rolando Eötvös nominatae Ser. 3. No. 1. Budapest 2013 Dissertationes Archaeologicae ex Instituto Archaeologico Universitatis de Rolando Eötvös nominatae Ser. 3. No. 1. Editor-in-chief: Dávid Bartus Editorial board: László Bartosiewicz László Borhy István Feld Gábor Kalla Pál Raczky Miklós Szabó Tivadar Vida Technical editors: Dávid Bartus Gábor Váczi András Bödőcs Proofreading: ZsóFia Kondé Szilvia Szöllősi Available online at htp://dissarch.elte.hu Contact: [email protected] © Eötvös Loránd University, Institute of Archaeological Sciences Budapest 2013 Contents Articles Melinda Torbágyi – István Vida 7 Te coin hoard of Abasár Anikó Bózsa 21 Roman mirrors from a private collection in the Hungarian National Museum Lajos Juhász 45 Te Biesheim cameo – a reinterpretation Methods Péter Csippán 53 Az állatcsont, mint információhordozó leletanyag Kata Dévai 85 Terminológiai alapfogalmak régészeti korú üvegtárgyak elemzéséhez Lőrinc Timár – Zoltán Czajlik – Sándor Puszta – Balázs Holl 113 3D reconstructions using GPR data at the Mont Beuvray Field reports Zsolt Mester 121 Excavation at a new Upper Palaeolithic site of the Eger region (Northern Hungary) László Borhy – Dávid Bartus – Emese Számadó 129 Short report on the excavations at Brigetio (Szőny-Vásártér) in 2013 Dénes Hullám – Zsófa Rácz 141 Report on the participation of the Eötvös Loránd University at the Wielbark Archaeological Field School in Malbork-Wielbark, Poland Gábor Váczi – Dávid Bartus 147 Short report
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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%.
    [Show full text]
  • 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.
    [Show full text]
  • 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 .........................................................................................
    [Show full text]
  • Historical Review of the Tourism Development of Lake Velence
    TURIZAM Volume 20, Issue 4 192–211 (2016) ORIGINAL SCIENTIFIC PAPER Historical Review of the Tourism Development of Lake Velence Wirth GáborA Received: January 2016 | Accepted: November 2016 DOI: 10.18421/TRZ20.04-03 Abstract Nowadays the development and future of the well-known Hungarian bathing resort, Lake Vel- ence, have been put to focus by professionals and the media since „Historia est magistra vitae”. Even experts must learn from the mistakes and successes of the past. This study is trying to show the tourism development of Lake Velence by analyzing this settlement’s functions. Liter- ature, statistics and research deal with this issue. These sources cover actual questions as for the tourism development of Lake Velence. Historical databases of Hungarian Central Statis- tical Office (KSH) and System of Settlement Data (TeIR) have been used as well as the sketch- map of Geomarket software, which gives a chronological contrast. The advantageous transport-geographical state and the nearness of Budapest influenced the tourism development of Lake Velence. The development of tourist attractions, prima- ry and secondary suprastructure deepened the differences between the examined settlements. Improvements can be achieved only if a complex regional development is put through in the area of Lake Velence. Keywords: Tourism development, settlement development, functions of settlements, Lake Vel- ence. Introduction The proper mapping of a certain area to be developed, or the lack of this mapping, can deter- mine the results of a whole development project. For this reason it is essential to examine the function and state of a given settlement from a chronological point of view – not only from the area’s spatial features.
    [Show full text]
  • Plenary Session of Carpatho-Balkan Geomorphological Commission
    GEOGRAPHICAL RESEARCH INSTITUTE HUNGARIAN ACADEMY OF SCIENCES PLENARY SESSION OF CARPATHO-BALKAN GEOMORPHOLOGICAL COMMISSION BUDAPEST 7-10 SEPT. 1975 Guide Compiled by 9 Pecsi,M -Juhasz, A BUDAPEST 1 9 7 5 Geographical Kosoaroh Institute, Hungarian Academy of Sciences PLENARY SESSION OF CARPATIIO-DAUCAN GEOMORPHOLOGICAL COMMISSION BUDAPEST 7-10. SEPT. 1975. GUIDE Compiled by P6osi, M, - Juhdsz, A. Budapest 1975 Contents p£c s i ,m . Evolution of the mountain and basin structures 1 VEIN)GY. Zusammenfassung dor vornoogenen Entnioklung Ungems 3 p£c s i ,m . The Transdanubian Mountains 7 VEIN > GY. Tectonics of the Duda Mountains 15 p6c s i ,m . GeomorfologicoskaJa ovoljuoija ploskogor'ja Duda 20 SC11EUER, GY. - SCHWEITZER,F. Ne* aspeots in the formation of i the fresh-vater limestone series of the environs of Duda Mountains 26 PfcCSIi M. North Hungarian or Intra-Carpathian Mountains 28 SZEKELY»A. Die ftitstehung und der Formonsohatz dea vestlichen M&tragebirges 31 m ezCs i , j . Teotonioa of the nortlrwestern slope of tho M&tra Mountains 36 IIAHN> G Y , Pliysioo—geographioal observations in the surroundings of Istenmezeje 44 juhAs z .X. Geomorphologipal study of the Budakoszi Dasin 46 p £ c s i , m . Prinoipal types of slope deposits of dissected pediments 51 P i ' C S I , M. I. EVOLUTION OF THK MOUNTAIN AND BASIN STKUCTUKES Hungary is situated in the middle of a basin1 surrounded by tin* Alpine. Carpathian and Dinuric mountain ranges, The roundish Pannonian Basin is a relatively recent form, due to the Tertiary subsidence of the Variscan basement, concurrently with the uplifting of the encircling mountains.
    [Show full text]
  • Földtani Közlöny
    Felelős kiadó BAKSA Csaba, a Magyarhoni Földtani Társulat elnöke Főszerkesztő CSÁSZÁR Géza Főszerkesztő-helyettes SZTANÓ Orsolya Műszaki szerkesztők PIROS Olga PENTELÉNYI Gábor Nyelvi lektor Philip RAWLINSON Szerkesztőbizottság Elnök: BAKSA Csaba CSERNY Tibor, FODOR László, KLEB Béla, PALOTÁS Klára, PAPP Gábor, VÖRÖS Attila Főtámogató Mol Nyrt. Támogatók Colas Északkő Kft.,Elgoscar 2000 Kft., Geoproduct Kft., Mecsekérc Zrt., Mineralholding Kft., OMYA Kft., OTKA, Perlit-92 Kft., TXM Olaj- és Gázkutató Kft., Wildhorse Energy Hungary Kft. A kéziratokat az alábbi címre kérjük küldeni PIROS Olga, 1442 Budapest, Pf. 106. e-mail: [email protected] Tartalom — Contents * * * BAKSA Csaba: Elnöki megnyitó 113 Editor-in-charge CSERNY Tibor: Főtitkári jelentés 115 Csaba BAKSA, 123 President of the Hungarian Geological BAKSA Csaba: Közhasznúsági jelentés Society HAAS János, BUDAI Tamás: A Dunántúli-középhegység felső-triász képződmé- Editor-in-chief nyeinek rétegtani- és fácieskérdései. Régi problémák újragondolása újabb Géza CSÁSZÁR ismeretek alapján. — Stratigraphic and facies problems of the Upper Vice editor-in-chief Triassic in the Transdanubian Range. Reconsideration of old problems on Orsolya SZTANÓ the basis of new results. 125 Technical editors HORVÁTH Réka, HAAS János: A Dachsteini Mészkő szedimentológiai jellegei és Olga PIROS PENTELÉNYI Gábor képződésének körülményei a Budai-hegységben. — Sedimentological char- Language editor acteristics and genetic conditions of the Dachstein Limestone of oncoidal Philip RAWLINSON facies, based on studies in the Buda Hills, Hungary. 143 Editorial board NÉMETH Norbert, SZAKÁLL Sándor, KRISTÁLY Ferenc, FEHÉR Béla, ZAJZON Chairman: Csaba BAKSA Norbert: A vincepáli (Répáshuta, Bükk hegység) karsztvasérc mangán- és Tibor, CSERNY, László FODOR, Béla vasásványai. — Manganese and iron minerals of the Vincepál karst iron ore KLEB, Klára PALOTÁS, Gábor PAPP, Attila VÖRÖS (Répáshuta, Bükk Mts).
    [Show full text]
  • Download (15MB)
    Tájökológiai Lapok 3 (1): 1–17. (2005) 1 A GYÜMÖLCSFAISKOLÁK TÁJFORMÁLÓ SZEREPE A RÉGI MAGYARORSZÁGON SURÁNYI DEZSÕ Ceglédi Gyümölcstermesztési Kutató-Fejlesztõ Intézet Kht. 2700 Cegléd, Pf. 33. e-mail: [email protected] Kulcsszavak: alkalmazott ökológia, faiskolák, géntartalékok, gyümölcsfajták, tájváltozások, történeti gyümölcs- termesztés Összefoglalás: Már a 16. században a korabeli források gyakran említik a híres fajtákat és általában a gyü- mölcsfákat. I. Ferdinánd (1526–1564), I. Miksa (1564–1576) és I. Rudolf (1576–1608) királyok Magyarország- ról kértek s kaptak is gyümölcsfákat. Batthyány Ferenc (1497–1566) pl. I. Ferdinánd király új kertjébe 1558- ban (Német) Újvárról küldött oltványokat. Sokáig csak sporadikus adatok találhatók oltványokról, oltóágakról, fõleg a magánlevelezésekben, vagy másfajta dokumentumokban. A faiskolák létét az is jelzi, hogy a régi hagyatéki leltárak, inventáriumok hangsúlyosan említik azokat, mint értékes ingatlan formát. A két legérdekesebb adat a következõ. Este-i Hippolit, esztergomi érsek a szobi fais- kolából 400 db csemetét vásárolt a visegrádi kertjének gazdagítására 1489-ben; a másik pedig Szigeti István jobbágyai az óbudai Kandé nevezetû határban a klarisszák faiskoláját feldúlták és elvitték az össze oltványt, még ugyanebben az évben. Történeti áttekintés és elemzés Oltványnevelés és fajtamegõrzés Egykor az oltásról még az volt a vélemény, hogy a nemesfajta általa nemcsak gyümöl- csét, hanem „minemûségét” is képes megváltoztatni. Ezzel együtt sok más babonás tév- hit is élt az emberekben. Figyelembe vették – amúgy helyesen – az oltás idején a válta- kozó idõjárást, de a csillagászati körülményeket is. Sõt a közelmúltig az amatõr kerté- szek hitték, a vadfák többszöri átültetésével „megnemesülnek”. LIPPAY (1667) már rész- letesen leírta az oltási módokat, így a hasítékoltást, „a fa közé- a héj alá miként kell olta- ni”, a szemre oltást, úgyszintén a sípolást, oldaloltást és még egyéb használatos oltási módokat ismertetette (LIPPAY 1667).
    [Show full text]
  • Geologica Hungarica. Series Geologica
    Geologica Hungarica Series Geologica (1999), Tomus 24: 179-196 Carlin gold in Hungary GEOLOGICAL SETTING AND TECTONIC EVOLUTION OF HUNGARY Já n o s H a a s ', G éza H á m o r 2 and Lá s zló K o r p á s 3 1 Hungarian Academy of Sciences-Eötvös Loránd University, Geological Research Group, H-1088 Budapest, Múzeum krt. 4a., Hungary 2 Eötvös Loránd University, Department of Regional Geology, H -l 143 Budapest, Stefánia út 14., Hungary 3 Geological Institute of Hungary, H -l 143 Budapest, Stefánia út 14., Hungary ABSTRACT Hungary is located in the central part of the Pannonian Basin filled up with a thick clastic sedimentary cover Neogene to Quaternary in age. Its basement is made up by Paleozoic to Early Tertiary formations representing the Austroalpine-Tatro-Veporic, the Pelso and the Tisza Megaunits, which are separated by major lineaments from each another. At the end of the Variscan cycle the polymetamorphic complexes of the Tisza Megaunit belonged to the Variscan Foldbelt forming the southern margin of the European plate. Metamorphic formations of the Pelso Megaunit and the Austroalpine nappes may have formed in the Prototethys existed between the Eurasian and Af­ rican plates. Closure of the Prototethys in the Middle Carboniferous led to accretion of the Variscan Foldbelt. Middle Carboniferous flysch and Late Carboniferous to Middle Permian continental molasse deposits indicate stages of this process. Low to high level gold anomalies were detected in some of the pre-Alpine formations of the Pelso Megaunit. The Alpine evolution may be characterized by multiphase opening (Permian to Jurassic), closure of the Tethys (Cretaceous to Paleogene) and which was followed by the formation and filling up of the Pannonian Basin (Neogene to Quaternary).
    [Show full text]