Annual Report 2018

Total Page:16

File Type:pdf, Size:1020Kb

Annual Report 2018 Content Director’s Introduction 1 History of the Czech Geological Survey 2 Geological and thematic maps 9 Regional geological research 13 Research on biodiversity and global changes in the past 17 Mineral resources 21 Groundwater research and evaluation 27 Annual Report 2018 Geoenergy research 31 Geosphere-biosphere-atmosphere interaction 35 www.geology.cz Geohazard research 39 Regional Geological Administration 43 State geological survey agendas of the Geofond Division 47 Mine workings and mining waste 53 Geological Information System 57 Remote sensing 63 International activities and cooperation 67 Laboratories 77 Library and collections 83 Geological documentation 87 CGS Publishing House and promotional activities 91 Selected publications issued by the CGS 98 Selected scientific papers 100 Financial review for 2018 106 Human resources 108 Website of the Czech Geological Survey 110 Principal events in 2018 112 Projects 120 Czech Geological Survey Annual Report 2018 Editor Petr Maděra Executive editor Šárka Sedláčková English translation Robert Alger Strategic research plan 2016–2020 Graphic design Eva Šedinová Photo on the cover Pavel Hanžl Printed by the A.R. Garamond s.r.o., Prague Research on the structure and evolution of the Earth’s crust Research on geosphere-biosphere-atmosphere interaction Published by the Czech Geological Survey, Prague 2019 Research on the biodiversity and global changes in the past Research on geohazards 03/9 446-412-19 ISBN 978-80-7075-964-6 Research on and use of natural resources Research on and development of geochemical and mineralogical methods © Czech Geological Survey, 2019 _Vyrocni_zprava_CGS_2018_OBALKA_EN.indd 1 06.09.2019 13:52:37 Content Director’s Introduction 1 History of the Czech Geological Survey 2 Geological and thematic maps 9 Regional geological research 13 Research on biodiversity and global changes in the past 17 Mineral resources 21 Groundwater research and evaluation 27 Annual Report 2018 Geoenergy research 31 Geosphere-biosphere-atmosphere interaction 35 www.geology.cz Geohazard research 39 Regional Geological Administration 43 State geological survey agendas of the Geofond Division 47 Mine workings and mining waste 53 Geological Information System 57 Remote sensing 63 International activities and cooperation 67 Laboratories 77 Library and collections 83 Geological documentation 87 CGS Publishing House and promotional activities 91 Selected publications issued by the CGS 98 Selected scientific papers 100 Financial review for 2018 106 Human resources 108 Website of the Czech Geological Survey 110 Principal events in 2018 112 Projects 120 Czech Geological Survey Annual Report 2018 Editor Petr Maděra Executive editor Šárka Sedláčková English translation Robert Alger Strategic research plan 2016–2020 Graphic design Eva Šedinová Photo on the cover Pavel Hanžl Printed by the A.R. Garamond s.r.o., Prague Research on the structure and evolution of the Earth’s crust Research on geosphere-biosphere-atmosphere interaction Published by the Czech Geological Survey, Prague 2019 Research on the biodiversity and global changes in the past Research on geohazards 03/9 446-412-19 ISBN 978-80-7075-964-6 Research on and use of natural resources Research on and development of geochemical and mineralogical methods © Czech Geological Survey, 2019 _Vyrocni_zprava_CGS_2018_OBALKA_EN.indd 1 06.09.2019 13:52:37 Organizational Structure Situation as of 31 December, 2018 Management Principal O ces of the Czech Geological Survey Advisory bodies Directorate Advisory bodies Scienti c Board Management Zdeněk Venera Human Resources Section Editorial Board of the Bulletin Review Board Project Management Director Internal Audit of Geosciences Editorial Board Management and Administration CGS Portal Board CGS Map Approbation Committee of the Brno Branch [email protected] CGS Library Board Geochemical Division Economic Division Geological Division Geofond Division Division of Informatics and Central Laboratories Jan Pašava Zdeněk Cilc Petr Mixa Vít Štrupl Dana Čápová Klárov Headquarters Barrandov Laboratories Kostelní Office Brno Branch Kutná Hora Office Jeseník Office Head of Division Head of Division & Deputy Head of Division Head Head of Division & Deputy & Deputy Director for Research Director for Economics & Deputy Director for Geology of Division Director for Informatics Klárov 3, 118 21 Praha 1, Geologická 6, 152 00 Praha 5, Kostelní 26, 170 06 Praha 7, Leitnerova 22, 658 69 Brno, Dačického náměstí 11, 284 01 Erbenova 348, 790 01 Jeseník, [email protected] [email protected] [email protected] [email protected] [email protected] Phone: 257 089 411, Fax: 257 531 376 Phone: 251 085 111, Fax: 251 818 748 Phone: 234 742 111, Fax: 234 742 290 Phone: 543 429 200, Fax: 543 212 370 Kutná Hora, Phone/Fax: 327 512 220 Phone/Fax: 584 412 081 Directorate | Regional and Applied Central Laboratory Geofond | Study Room | Video Archive Regional and Applied Geology, Geofond – Mining Impacts Department Regional O ce | Archive of Geological Environmental General Economics Regional Geology Mineral Raw Materials CGS Publishing House Geology | Library | Archive Collections | (inorganic geochemistry) | Document Archive (part.) | Specialized Geophysics | Geochemistry | Testing Samples | Bookshop Geochemistry of Crystalline Complexes and Biogeochemistry GIS and DB | Publishing House | Bookstore | Geochemistry | Special Laboratories O c e s Laboratory (organic geochemistry) Jana Kuklová Jaroslava Pertoldová Jaromír Starý Patrik Fiferna | Reprographic Centre Martin Novák Head of Department Head of Department Head of Department vedoucí vydavatelství | Library and Archive | Bookshop | Head of Department GIS and DB [email protected] [email protected] [email protected] [email protected] patrik. [email protected] Rock Geochemistry Economics Regional Geology of Mining Impacts Information Services and Administration Sedimentary Formations Anna Vymazalová Head of Department Mirko Vaněček Tomáš Hroch Jolana Šanderová Hana Breiterová Head of Department Head of Department Head of Department Head of Department From the left: Vít Štrupl – Head of the Geofond Division, Dana Čápová – Deputy Director for Informatics, Oldřich Krejčí – Director of the Brno Branch, [email protected] [email protected] [email protected] [email protected] [email protected] Zdeněk Venera – Director of the Czech Geological Survey, Petr Mixa – Deputy Director for Geology, Zdeněk Cilc – Deputy Director for Economics, Jan Pašava – Deputy Director for Research and Head of the Geochemical Division and Central Laboratories. Mineral Resources Applied Geology Geological Exploration Information Systems Research Electron Microprobe and Microanalysis Jílové Regional Museum and Centre Lužná Archive of Material Stratov Archive of Material Kamenná Archive of Material Kovanice Archive of Material and Policy Petr Kycl Zdeňka Petáková Zuzana Krejčí Laboratory, Faculty of Science, MU Brno for Documentation of Gold Deposits Documentation Documentation Documentation Documentation Petr Rambousek Head of Department Head of Department Head of Department Head of Department [email protected] [email protected] [email protected] [email protected] Czech Geological Survey Kotlářská 2, 611 37 Brno, Masarykovo nám. 16, 254 80 270 51 Lužná u Rakovníka, čp. 432, 289 22 Stratov, čp. 184, Kamenná 42, 262 31 Milín, 288 02 Kovanice, čp. 184, Phone: 541 129 496, Fax: 541 211 214 Jílové u Prahy, Phone: 241 950 455 Phone/Fax: 313 537 849 Phone: 234 742 205 Phone: 234 742 205 Phone: 234 742 205 The Czech Geological Survey is a highly respected state organization Mission Electron Microprobe and Microanalysis Archive of Geological Samples and Written Archive of Geological Samples | Collections Archive of Geological Samples Archive of Geological Samples Archive of Written Documentation Central Laboratory Prague Regional Geology Geological Computer that compiles, stores, interprets and provides objective expert • Geological mapping and regional research within the territory of Moravia Documentation Administration Laboratory Documentation | Publications and Maps and Written Documentation geological information for the state administration, the private sector of the Czech Republic Věra Zoulková Jan Vít Milada Hrdlovicsová Richard Binko and the public. It is a state-funded body, the departmental research • Basic and applied research on geohazards, mineral resources, Head of Department Head of Department Head of Department Head of Section institute of the Ministry of the Environment responsible for functioning groundwater sources, rock environments and environmental [email protected] [email protected] [email protected] [email protected] as the state geological survey in the Czech Republic. It is the only protection institution tasked with the systematic investigation of the geological • Serves as the state geological survey in accordance Central Laboratory Brno Environmental Geology structure of the entire Czech Republic. with Act No. 62/1988 Coll. (on geological work) and Geophysics • Gathering, compilation and interpretation of data on the Juraj Franců Jan Šikula The well-established reputation of the Czech Geological Survey is geological structure, mineral resources and geohazards Head of Department Head of Department based on the optimum combination of services to society with of the CR [email protected] [email protected] top-ranking research in
Recommended publications
  • Early Paleozoic Life & Extinctions (Part 1)
    NJU Course Extinctions: Past, Present & Future Prof. Norman MacLeod School of Earth Sciences & Engineering, Nanjing University Extinctions: Past, Present & Future Extinctions: Past, Present & Future Course Syllabus (Revised) Section Week Title Introduction 1 Course Introduction, Intro. To Extinction Introduction 2 History of Extinction Studies Introduction 3 Evolution, Fossils, Time & Extinction Precambrian Extinctions 4 Origin of Life & Precambrian Extionctions Paleozoic Extinctions 5 Early Paleozoic World & Extinctions Paleozoic Extinctions 6 Middle Paleozoic World & Extinctions Paleozoic Extinctions 7 Late Paleozoic World & Extinctions Assessment 8 Mid-Term Examination Mesozoic Extinctions 9 Triassic-Jurassic World & Extinctions Mesozoic Extinctions 10 Labor Day Holiday Cenozoic Extinctions 11 Cretaceous World & Extinctions Cenozoic Extinctions 12 Paleogene World & Extinctions Cenozoic Extinctions 13 Neogene World & Extinctions Modern Extinctions 14 Quaternary World & Extinctions Modern Extinctions 15 Modern World: Floras, Faunas & Environment Modern Extinctions 16 Modern World: Habitats & Organisms Assessment 17 Final Examination Early Paleozoic World, Life & Extinctions Norman MacLeod School of Earth Sciences & Engineering, Nanjing University Early Paleozoic World, Life & Extinctions Objectives Understand the structure of the early Paleozoic world in terms of timescales, geography, environ- ments, and organisms. Understand the structure of early Paleozoic extinction events. Understand the major Paleozoic extinction drivers. Understand
    [Show full text]
  • Bakalarska Prace
    ZÁPADOČESKÁ UNIVERZITA V PLZNI FAKULTA EKONOMICKÁ Bakalářská práce Vyhodnocení dostupnosti zdravotních služeb v jednotlivých oborech poskytování péče pro oblasti Karlovarského kraje Evaluation of availability of health services in individual fields of care provision for areas of the Karlovy Vary Region Lenka Šebková Plzeň 2020 Čestné prohlášení Prohlašuji, že jsem bakalářskou práci na téma „Vyhodnocení dostupnosti zdravotních služeb v jednotlivých oborech poskytování péče pro oblasti Karlovarského kraje“ vypracoval/a samostatně pod odborným dohledem vedoucí/vedoucího bakalářské práce za použití pramenů uvedených v přiložené bibliografii. Plzeň dne 11. května 2020 .............................................. podpis autora/autorky Poděkování Tímto bych ráda poděkovala vedoucímu své bakalářské práce panu RNDr. Davidovi Vogtovi, Ph.D. za odborné vedení práce, užitečné rady, ochotu a čas věnovaný při konzultacích. Obsah Úvod ............................................................................................................................... 11 1 Cíle práce ............................................................................................................... 12 2 Metodika a data .................................................................................................... 13 3 Vymezení teoretických pojmů ............................................................................. 15 3.1 Zdraví ............................................................................................................... 15 3.2 Systém
    [Show full text]
  • Tentaculites of the Upper Silurian and Lower Devonian of Poland
    ACT A PAL A EON T 0 LOG ICA POLONICA Vol. XIX 1974 No. 4 BARBARA HAJI..ASZ TENTACULITES OF THE UPPER SILURIAN AND LOWER DEVONIAN OF POLAND Abstract. - The tentaculites, described in the present paper, come from the Upper Silurian deposits of the Baltic coastal region and the Lower Devonian deposits of the Radom-Lublin region. The Upper Silurian assemblage of tentaculites allows one to compare and correlate the Upper Silurian deposits of Northern Europe. The Lower Devonian tentaculites are' indicative of the Gedinnian and Siegenian age of the deposits under study and of their close correlations primarily with Podolia. PART I INTRODUCTION In Poland, the tentaculites have not so far been described in detail. Giirich (1895) was the first to take an interest in the tentaculites occurring in this country. He described the following species from the Holy Cross Mountains: Tentaculites sp. d. intermedium Barr., T. multiformis Sandb., T.ornatus? Sow., T. schlotheimi Koken., T. polonicus Gurich., T. sand­ bergeri Gurich, T. tenuicinctus Sandb., Styliolites sp. From the same region, the following species were identified by Paj­ chlowa (1957): Tentaculites schlotheimi Koken., Tentaculites sp., Styliolina laevis Richter and Styliolina sp. The tentaculites of the species Homoc­ tenus tenuicinctus (Roem.), Homoctenus sp., Styliolina laevis Richter and Styliolina sp. were distinguished by Koscielniakowska (1962-1967) in the Frasnian deposits of these region. The present writer described the following Eifelian tentaculites from the Holy Cross Mts and the Cracow-Cz~stochowaUpland (Hajlasz, 1967): Tentaculites schlotheimi Koken., T. subconicus Geinitz, T.sp., and Dicri­ coconus mosolovicus (Ljasch.). Next, a list of species from Lower Devonian of the Lublin area was published (Hajlasz, 1968).
    [Show full text]
  • S.No Cities / Towns Districts 1 Abertamy 2 Adamov Blansko District
    S.No Cities / Towns Districts 1 Abertamy 2 Adamov Blansko District 3 Aš 4 Bakov nad Jizerou 5 Bavorov 6 Bechyně 7 Bečov nad Teplou 8 Bělá nad Radbuzou 9 Bělá pod Bezdězem 10 Benátky nad Jizerou 11 Benešov 12 Benešov nad Ploučnicí 13 Beroun 14 Bezdružice 15 Bílina 16 Bílovec 17 Blansko 18 Blatná 19 Blovice 20 Blšany 21 Bochov 22 Bohumín 23 Bohušovice nad Ohří 24 Bojkovice 25 Bor Tachov District 26 Borohrádek 27 Borovany České Budějovice District 28 Boskovice 29 Boží Dar 30 Brandýs nad Labem-Stará Boleslav 31 Brandýs nad Orlicí 32 Břeclav 33 Březnice Příbram District 34 Březová Sokolov District 35 Březová nad Svitavou 36 Břidličná 37 Brno 38 Broumov 39 Brtnice 40 Brumov-Bylnice 41 Bruntál 42 Brušperk 43 Bučovice 44 Budišov nad Budišovkou 45 Budyně nad Ohří 46 Buštěhrad www.downloadexcelfiles.com 47 Bystré Svitavy District 48 Bystřice Benešov District 49 Bystřice pod Hostýnem 50 Bystřice nad Pernštejnem 51 Bzenec 52 Čáslav 53 Čelákovice 54 Černošice 55 Černošín 56 Černovice Pelhřimov District 57 Červená Řečice 58 Červený Kostelec 59 Česká Kamenice 60 Česká Lípa 61 Česká Skalice 62 Česká Třebová 63 České Budějovice 64 České Velenice 65 Český Brod 66 Český Dub 67 Český Krumlov 68 Chabařovice 69 Cheb 70 Chlumec nad Cidlinou 71 Choceň 72 Chodov Sokolov District 73 Chomutov 74 Chotěboř 75 Chotětov 76 Chrast Chrudim District 77 Chrastava 78 Chřibská 79 Chropyně 80 Chrudim 81 Chvaletice 82 Chýnov 83 Chyše 84 Cvikov 85 Dačice 86 Dašice 87 Děčín 88 Desná Jablonec nad Nisou District 89 Deštná Jindřichův Hradec District 90 Dětřichov Svitavy District
    [Show full text]
  • Report on Extremism and Manifestations of Racism and Xenophobia on the Territory of the Czech Republic in 2011
    Report on Extremism and manifestations of racism and xenophobia on the territory of the Czech Republic in 2011 Ministry of Interior Security Policy Department Prague 2012 Report on Extremism on the territory of the Czech Republic in 2011, Evaluation of the implementation of the Policy for the fight against extremism for 2011 and the Policy for the fight against Extremism for 2012 were approved by the Czech Government on May 9th 2012 by Resolution No 328. This text was not subject to a linguistic or stylistic editing. Contents Contents...................................................................................................................................... 2 1. Introduction ............................................................................................................................ 4 2. The challenge posed by definition of extremism ................................................................... 5 3. Report on Extremism in the Czech Republic in 2011............................................................ 6 3.1. Summary ......................................................................................................................... 6 3.2. Major trends in extremism .............................................................................................. 8 3.3. Right-wing extremism (PEX)........................................................................................ 10 3.3.1. Elements of the extreme-right scene ...................................................................... 11
    [Show full text]
  • PALEOZOIC (CAMBRIAN THROUGH DEVONIAN) Anoxltropic BIOTOPES
    Palaeogeography, Palaeoclimatology, Palaeoecology, 74 (1989): 3-13 3 Elsevier Science Publishers B.V., Amsterdam -- Printed in The Netherlands PALEOZOIC (CAMBRIAN THROUGH DEVONIAN) ANOXlTROPIC BIOTOPES W. B. N. BERRY, P. WILDE and M. S. QUINBY-HUNT Marine Sciences Group, Department of Paleontology, University of California, Berkeley, CA 94720 (U.S.A.) (Received April 27, 1989) Abstract Berry, W. B. N., Wilde, P. and Quinby-Hunt, M.S., 1989. Paleozoic (Cambrian through Devonian) anoxitropic biotopes. Palaeogeogr., Palaeoclimatol., Palaeoecol., 74:3 13. The oxygen-poor to denitrified waters of modern oceans provide an analog for open ocean conditions which contained the Early Paleozoic "graptolite" biotope. Certain euphausiids, other zooplankton and fish, as demonstrated in the Eastern Tropical Pacific, are found concentrated in and about denitrified waters. The boundary zone between oxic and denitrified waters show intense organismal growth due to the increased chemical availability of nutrients as reduced nitrogen compounds. Such waters are areally limited in the present cold and well-ventilated modern ocean. The distribution patterns showing attraction to low or oxygen-depleted waters (anoxitropy) in these modern open marine faunas suggest that Early Paleozoic plankton and nekton, preserved in lithofacies formed under low oxygen or anoxic coditions, could have been similarly attracted to the more extensive ancient denitrified and anoxic waters. The major Paleozoic faunal groups, in order of their occupation of the niche, include agnostid and olenid trilobites, graptoloid graptolites, styliolinids, thin-shelled bivalves, small orthocone nautiloids, and early ammonoids. The expansion of low-oxygen to anoxic waters across the shelves during warm climates in the Early Paleozoic may be correlated with major evolutionary radiations in the graptolites and possibly in the early ammonites.
    [Show full text]
  • The Oldest Ammonoids of Morocco (Tafilalt, Lower Emsian)
    Swiss Journal of Palaeontology (2019) 138:9–25 https://doi.org/10.1007/s13358-019-00189-1 (0123456789().,-volV)(0123456789().,- volV) REGULAR RESEARCH ARTICLE The oldest ammonoids of Morocco (Tafilalt, lower Emsian) 1 2 1 3 1 Ralph Thomas Becker • Christian Klug • Till So¨ te • Sven Hartenfels • Zhor Sarah Aboussalam • Ahmed El Hassani4 Received: 11 December 2018 / Accepted: 18 February 2019 / Published online: 5 April 2019 Ó Akademie der Naturwissenschaften Schweiz (SCNAT) 2019 Abstract During a fieldtrip of the 10th International Cephalopod Symposium to the Tafilalt (SE Morocco), a fauna with the so far oldest ammonoid of the region was discovered at the top of the basal Emsian Deiroceras Limestone of Jebel Mech Irdane. The new material confirms the record of a single, poorly preserved specimen of the same age from Ras El Kebbar in the northwestern Tafilalt. All specimens are assigned within the Chebbitinae n. subfam. (Mimosphinctidae) to Praechebbites debaetsi n. gen. n. sp., which differs from the slightly younger Chebbites reisdorfi mostly in the lack of a dorsal lobe and dorsal imprint zone. In the conodont succession, the new species and genus falls in the top of the Eolinguipolygnathus excacatus M114 Zone, which has been proposed to define in future the base of the Emsian. Since the new taxon is morphologically already advanced, it is likely that even older ammonoids with loosely coiled conchs will be discovered in the future. A block from a Lower Carboniferous olistostrome of the adjacent Tinerhir region contained the gyroconic Ivoites n. sp. only. The global comparison of oldest ammonoid faunas shows the rarity of assemblages assigned to Lower Devonian (LD) III-B, often dated by conodonts and dacryoconarids.
    [Show full text]
  • Devonian Tentaculitoidea of the Malvinokaffric Realm of Brazil, Paraná Basin
    Palaeontologia Electronica palaeo-electronica.org Devonian Tentaculitoidea of the Malvinokaffric Realm of Brazil, Paraná Basin Jeanninny Carla Comniskey and Renato Pirani Ghilardi ABSTRACT The Tentaculitoidea is represented by extinct invertebrates characterized by small, conic, carbonate shells of animals that inhabiting exclusively marine environ- ments. The tentaculitoids occur from the Ordovician to Devonian, with diversity peak- ing in the Middle Devonian. The Tentaculitoidea has three orders: Tentaculitida (benthic habit), Homoctenida, and Dacryoconarida (planktonic habit). In Brazil, the old- est tentaculitoids occur in strata of the early Silurian, with the genus Tentaculites. Spec- imens of the Dacryoconarida and Homoctenida orders were only found in the Lower Devonian strata. In this study, we conducted taxonomic analyses of specimens in col- lections from various research institutions, including samples used in the last system- atic study with this group, in mid-1991. The present study aims to review the systematic aspects of the tentaculitoids of the Devonian strata, Paraná basin, Brazil. Seven species of tentaculitoids were identified: two species previously described, Ten- taculites jaculus and Tentaculites crotalinus and five news species: Tentaculites kozlo- wskii, Tentaculites paranaensis, Uniconus ciguelii, Homoctenus katzerii, and Styliolina langenii. This is the first known occurrence of the genus Uniconus in Devonian strata from Brazil. The analyzed species of homoctenids and dacryoconarids are larger than those previously described in the specialized literature. This study demonstrated that the tentaculitoids of the Paraná Basin have a stratigraphic distribution from the end of the Pragian to the early Givetian. Jeanninny Carla Comniskey. Faculdade de Filosofia, Ciências e Letras de Ribeirão Preto, Pós-Graduação em Biologia Comparada, Universidade de São Paulo-USP.
    [Show full text]
  • Of the Environmental Impact Assessment
    EVERNIA s.r.o. DOCUMENTATION OF CONSTRUCTION’S ENVIRONMENTAL IMPACT ASSESSMENT R6 JENIŠOV – KAMENNÝ DVŮR Responsible researcher: Illegible signature RNDr. Petr Anděl, CSc. Professional Competence Certificate Ref. No. 7248/1155/OPV/93 Liberec 1997 E.I.A. Documentation R6 Jenišov – Kamenný Dvůr C.IX. NON-TECHNICAL SUMMARY EXPRESSWAY R6 JENIŠOV – KAMENNÝ DVŮR (non-technical summary of documentation pursuant to Act No. 244/1992 Coll.) 1. CONSTRUCTION IDENTIFICATION • Name: R6 Jenišov – Kamenný Dvůr • Construction type: New construction, reconstruction • Location: Karlovy Vary, Sokolov, Cheb districts • Investor: Road & Motorway Directorate Prague, Na Pankráci 56, 145 05 Prague 4 workpace Praha 8 – Čimická 319 • Responsible ministry: Ministry of Transport and Communications of the CR • Design: R6 Karlovy Vary – Sokolov, August 1995 Pragoprojekt a.s., K. Vary Design Studio Vítězná 26, 360 01 Karlovy Vary Chief Designer: Ing. Olga Havlíková R6 Sokolov – Cheb, study revision, May 1996 Valbek a spol. v.o.s. Vaňurova 505/17, 460 02 Liberec 1 Responsible of project: Ing. Milan Koloušek • Documentation prepared pursuant to Act No. 244/1992 Coll. by: EVERNIA s.r.o. Tř. 1. máje 97, 460 01 Liberec 1 Authorized person: RNDr. Petr Anděl, CSc. • Competent governmental agency pursuant to Act No. 244/1992 Coll.: Ministry of the Environment of the CR • Communities involved: Karlovy Vary, Jenišov, Sokolov, Březová, Dolní Rychnov, Kynšperk nad Ohří, Nové Sedlo, Staré Sedlo, Šabina, Odrava, Tuřany EVERNIA s.r.o., Liberec page 194 E.I.A. Documentation R6 Jenišov – Kamenný Dvůr 2. APPLICATION OF ACT NO. 244/1992 COLL. Act No. 244/1992 Coll. on environmental impact assessment stipulates that extensive constructions with a potentially great impact on the environment must be assessed in a way guaranteeing evaluation completeness and optional involvement of the public.
    [Show full text]
  • Distribution of Sweet Chestnut Castanea Sativa Mill. in the Czech Republic
    JOURNAL OF FOREST SCIENCE, 49, 2003 (6): 259–272 Distribution of sweet chestnut Castanea sativa Mill. in the Czech Republic P. HALTOFOVÁ, L. JANKOVSKÝ Mendel University of Agriculture and Forestry, Faculty of Forestry and Wood Technology, Brno, Czech Republic ABSTRACT: Sweet chestnut Castanea sativa Mill. is an introduced species in the Czech Republic. It is recorded roughly from 300 localities. To the end of 2002, the occurrence of chestnut was verified at about 140 macrolocalities. The most northern locality recorded so far was Choustníkovo Hradiště in the region of Hradec Králové. Chestnuts occur generally to an altitude of 500 m (80% of all examined localities), at higher altitudes they suffer from climatic extremes particularly late frosts. The occurrence of chestnut was recorded at 27 localities (ca. 20% localities under investigation) where altitudes exceed 500 m. The highest location of chestnut is locality Nejdek, Karlovy Vary District where chestnut trees thrive at an altitude of 678 m. At altitudes over 600 m, two other localities were recorded. The health condition of chestnut is relatively good. At some localities, however, crown drying occurs as a result of not quite ideal climatic conditions. Within our research, quarantine Cryphonectria parasitica (Murr.) Barr. was determined for the first time in the Czech Republic at the only examined locality. Keywords: Castanea sativa; chestnut; distribution; Czech Republic; Cryphonectria parasitica; ecology Sweet chestnut Castanea sativa Mill. is an old-time cul- by Romans to the whole Mediterranean and across France tivated tree species in Europe. Fruits of relative species to western Europe (VILLANI et al. 1994; OOSTERBAAN of chestnut were already used in ancient China.
    [Show full text]
  • Sepkoski, J.J. 1992. Compendium of Fossil Marine Animal Families
    MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. Department of the Geophysical Sciences University of Chicago Chicago, Illinois 60637 Milwaukee Public Museum Contributions in Biology and Geology Rodney Watkins, Editor (Reviewer for this paper was P.M. Sheehan) This publication is priced at $25.00 and may be obtained by writing to the Museum Gift Shop, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Orders must also include $3.00 for shipping and handling ($4.00 for foreign destinations) and must be accompanied by money order or check drawn on U.S. bank. Money orders or checks should be made payable to the Milwaukee Public Museum. Wisconsin residents please add 5% sales tax. In addition, a diskette in ASCII format (DOS) containing the data in this publication is priced at $25.00. Diskettes should be ordered from the Geology Section, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Specify 3Y. inch or 5Y. inch diskette size when ordering. Checks or money orders for diskettes should be made payable to "GeologySection, Milwaukee Public Museum," and fees for shipping and handling included as stated above. Profits support the research effort of the GeologySection. ISBN 0-89326-168-8 ©1992Milwaukee Public Museum Sponsored by Milwaukee County Contents Abstract ....... 1 Introduction.. ... 2 Stratigraphic codes. 8 The Compendium 14 Actinopoda.
    [Show full text]
  • CHARACTERISTICS of the REGION the Karlovarský Region Is in Particular Famous for Its Spas
    CHARACTERISTICS OF THE REGION The Karlovarský Region is in particular famous for its spas. There are not only one of our most famous spas Karlovy Vary but also Mariánské Lázně, Františkovy Lázně, Lázně Kynžvart and Jáchymov in the Region. The spa in Kyselka is not currently in operation. Along with mineral springs the region is rich with its natural mineral waters of which the most famous is Mattoni. In connection with spas what is also very popular are the spa wafers loved not only by local inhabitants but predominantly by spa guests from all over the world. Karlovy Vary apart from this are also famous for its herbal liquor Becherovka and the art of glassmakers from the Moser Company. The city Chodov was made famous by peach-blow, exported to the whole world. Among the cultural aspects it is mainly the International Film Festival Karlovy Vary that offers the meeting of domestic and foreign creators. The Karlovarský Region is located in the west of the Czech Republic and was formed by the split of the Západočeský Region to form the Karlovarský and Plzeňský Region. In the north and west there is the state border with Germany, in the east its neighbour is the Ústecký Region and in the south the Plzeňský Region. Along with the Ústecký Region it forms the Northwest cohesion area, the so-called NUTS 2. The mountains Krušné hory are stretching along the national borders across these two regions. The highest point is Klínovec (1 244 m above sea level) in the Karlovy Vary District as well as the lowest point of the region (320 m above sea level), which is on the river Ohře on the borders of the region.
    [Show full text]