Bohemian Switzerland 3.3.2. Regional Analysis Good Practises Collection
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Okres Děčín Okres, Obec, Část Obce (Díl), Výměra Rok Počet Obyvatel Katastrální Území
Okres Děčín Okres, obec, část obce (díl), Výměra Rok Počet obyvatel Katastrální území Poř.č. historická osada / lokalita v ha připojení 1869 1880 1890 1900 1910 1921 1930 1950 1961 1970 a b j k l 1 2 3 4 5 6 7 8 9 10 Okres Děčín 174 262 186 961 197 309 213 629 233 066 213 164 231 859 131 279 131 956 132 429 1. Arnoltice Arnoltice 554 835 867 822 779 762 686 716 308 340 307 2. Benešov nad Ploučnicí 977 2 267 2 496 3 370 3 875 4 089 3 800 4 457 3 265 3 570 3 630 1. Benešov nad Ploučnicí Benešov nad Ploučnicí 531 1 952 2 159 3 080 3 567 3 797 3 507 4 150 3 125 3 471 3 554 2. Ovesná Ovesná 446 1956 315 337 290 308 292 293 307 140 99 76 3. Bynovec Bynovec 636 613 620 625 608 610 523 529 302 286 275 4. Česká Kamenice 3 877 8 243 9 036 9 008 9 308 9 675 8 786 9 284 5 383 5 560 5 477 1. Česká Kamenice Česká Kamenice 562 3 596 4 171 4 400 4 670 4 723 4 311 4 538 3 024 3 144 3 303 2. Dolní Kamenice Dolní Kamenice 508 1947 591 754 786 922 1 064 980 1 025 707 799 793 3. Filipov Dolní Kamenice 1947 289 277 276 271 263 247 279 94 67 77 4. Horní Kamenice Horní Kamenice 535 1947 738 794 849 978 1 197 1 042 1 074 739 794 664 5. -
Saxon-Bohemian Switzerland Transparcnet Meeting Saxon-Bohemian Switzerland
National Park Region Saxon-Bohemian Switzerland TransParcNet Meeting Saxon-Bohemian Switzerland: 7.6.2016 Four protected areas, two countries, NLP-Zentrum Bad Schandau one landscape Handrij Härtel & Jürgen Phoenix National Park Region Saxon-Bohemian Switzerland Saxon-Bohemian Switzerland: Discovery by Romantic painters Adrian Zingg (1734-1816) National Park Region Saxon-Bohemian Switzerland Saxon-Bohemian Switzerland Caspar David Friedrich (1774 Greifswald - 1840 Dresden) National Park Region Saxon-Bohemian Switzerland Saxon-Bohemian Switzerland Caspar David Friedrich (1774 Greifswald - 1840 Dresden) National Park Region Saxon-Bohemian Switzerland Saxon-Bohemian Switzerland: One of the oldest European tourist destinations Protected areas in sandstone rock regions across the world National Park Region Saxon-Bohemian Switzerland TransParcNet Meeting Saxon-Bohemian Switzerland: 7.6.2016 Singularity in European context: NLP-Zentrum Bad Schandau 3 sandstone rock national parks only National Park Region Saxon-Bohemian Switzerland TransParcNet Meeting Saxon-Bohemian Switzerland 7.6.2016 as part of larger geological unit NLP-Zentrum Bad Schandau Bohemian Cretaceous Basin PL D CZ Marine fossils from Cretaceous sandstones Inoceramus labiatus Natica bulbiformis Pecten Inoceramus lamarcky National Park Region Saxon-Bohemian Switzerland TransParcNet Meeting Saxon-Bohemian Switzerland: 7.6.2016 NLP-Zentrum High diversity of morphologic forms at different Bad Schandau spatial scales Saxon-Bohemian Switzerland: Terciary volcanism Růžovský vrch Zlatý vrch National Park Region Saxon-Bohemian Switzerland TransParcNet Meeting Saxon-Bohemian Switzerland: 7.6.2016 geodiversity-biodiversity relations NLP-Zentrum Bad Schandau Saxon-Bohemian Switzerland: role of microclimate Saxon-Bohemian Switzerland: vertebrates Grasshopper Troglophilus neglectus New for Central Europe (Chládek, Benda & Trýzna 2000) Charissa glaucinaria Extremely rare montane species, within CZ in Bohemian Switzerland only L – Phengaris nausithous R – Phengaris telejus Monitoring of the butterflies from the gen. -
Creation of Sustainable Public Transport in the National Park Region Saxon-Bohemian Switzerland
National Park Region Saxon-Bohemian Switzerland Creation of sustainable public transport in the National Park Region Saxon-Bohemian Switzerland Jürgen Phoenix, NPA Saxon Switzerland National Park Region Saxon-Bohemian Switzerland Saxon-Bohemian Switzerland: Protected Landscape Area (D): 287 km² Protected Landscape Area (CZ): 245 km² National Park (D): 93 km² National Park (CZ): 80 km² National Park Region Saxon-Bohemian Switzerland Situation analysis - tourism is the most important economic sector in the region, - but the large number of visitors causes risks for the protected areas, - one problem area is the private vehicle traffic of visitors (although the region is very well connected by public transport). keeping the situation in balance takes a lot of communication and cooperation between the different stakeholders. National Park Region Saxon-Bohemian Switzerland Traffic calming - a never-ending story? Traffic calming is a long-term task, don´t let any failures discourage you, after defeat get back on your feet again. National Park Region Saxon-Bohemian Switzerland Experiences from 25 years involvement in traffic calming Traffic regulation and public transport don´t fall within the jurisdiction of the National Park administration. Its possibilities are limited: - to chair processes, - to provide ideas, - to support projects and plannings with (limited) finances. Changes in the main points 1990 – 2000 the stakeholders gave a lukewarm reaction to the topic, the activities focused on the private vehicle traffic of the visitors. since -
Abecední Přehled Sídelních Jednotek Podle Stavu Územní Struktury K 1
Abecední přehled sídelních jednotek podle stavu územní struktury k 1. lednu 2019 - Děčín KOD_ZSJ_D NAZZSJD VYMERU OB91 OB01 OB11TRV OB11OBV UO KOD_CAST NAZCOBE Počet Počet Počet Počet Výměra obyvatel obyvatel obyvatel obyvatel Kód základní Kód v ha k 3.3.1991 k 1.3.2001 k 26. 3. 2011 k 26. 3. 2011 sídelní jednotky Název dílu základní sídelní jednotky urbanistického Kód části obce Název části obce (odhad dle (včetně dílů) obvodu GIS) podle podle trvalého bydliště obvyklého pobytu 3100260 Aloisov 152 307 331 368 386 016 407763 Rumburk 1 3100340 Antonínovo Údolí 60 210 208 215 220 017 407747 Rumburk 3-Dolní Křečany 0004340 Arnoltice 554 261 285 359 371 000434 Arnoltice 1653870 Babětín 195 34 31 57 55 165417 Těchlovice 3280570 Bechlejovice 124 - 146 192 190 078 407348 Děčín XXVI-Bechlejovice 0252410 Bělá 85 1 040 1 134 1 050 1 023 033 407313 Děčín X-Bělá 0024530 Benešov nad Ploučnicí-střed 11 462 457 557 440 001 407577 Benešov nad Ploučnicí 0386360 Blankartice 454 31 36 43 42 038636 Blankartice 0071610 Boletice nad Labem 134 5 238 5 175 4 893 4 675 052 407526 Děčín XXXII-Boletice nad Labem 0269210 Borek 132 37 44 30 27 026921 Borek 0272860 Brložec 220 17 27 41 46 027286 Brložec 0129800 Brtníky 1 046 272 257 250 251 012980 Brtníky 0141920 Březiny 310 2 224 2 212 1 961 1 872 048 407356 Děčín XXVII-Březiny 0252320 Bynov 101 4 897 4 476 4 114 3 932 032 407305 Děčín IX-Bynov 0004420 Bynovec 637 215 223 295 287 000442 Bynovec 1435370 Cihelna 32 374 146 150 151 003 407763 Rumburk 1 3101740 Císařský-horní část 387 36 54 69 83 012 407798 Císařský 1628410 -
District Heating in Lusatia
Brandenburg University of Technology Cottbus-Senftenberg District Heating in Lusatia Status Quo and Prospects for Climate Neutrality Fernwärme in der Lausitz Status quo und Perspektiven für Klimaneutralität Thesis for the degree of Master of Science in Environmental and Resource Management submitted by Jan Christian Bahnsen 1st Examiner: Prof. Dr. Bernd Hirschl 2nd Examiner: Katharina Heinbach Submitted: 29th May 2020 Statement of Authentication I hereby declare that I am the sole author of this master thesis and that I have not used any other sources other than those listed in the bibliography and identified as references. I further declare that I have not submitted this thesis at any other institution in order to obtain a degree. The content, either in full or in part, has not been previously submitted for grading at this or any other academic institution. ________________________________ _____________________________________ (Place, Date) (Signature) Abstract The master thesis at hand examines the potential of district heating in Lusatia. The thesis follows the approach of first identifying technical and economic potentials in general and then transferring them to the study region. For the quantitative determination of district heating potential in Lusatia, the status quo is determined and a GIS-based analysis is carried out with regard to minimum heat demand densities. The extent to which district heating is suitable for climate-neutral heat supply will be investigated using the potential of renewable and waste heat energy sources. Furthermore, the regional economic effects of developing these potentials are examined. The results show that despite an overall decline in heat demand, there is potential to increase the relative share of district heating in Lusatia. -
Školení Pracovníků IS
TransParcNet European network of transboundary areas Case studies: Saxon-Bohemian Switzerland Krkonoše/Karkonosze National Parks Kari Lahti, Handrij Härtel, Jakub Kašpar http://www.europarc.org/what-we-do/transboundary-parks From DURBAN to SYDNEY From DURBAN to SYDNEY From DURBAN to SYDNEY http://www.europarc.org/what-we-do/transboundary-parks TransParcNet: Certified parks 1. Neusiedler See National Park (Austria) and Fertö-Hansag National Park (Hungary) 2. Krkonoše National Park (Czech Republic) and Karkonosze National Park (Poland) 3. Oulanka National Park (Finland) and Paanajärvi National Park (Russia) 4. Maas-Schwalm-Nette Nature Park (Germany/Netherlands) 5. Thayatal National Park (Austria) and Podyjí National Park (Czech Republic) 6. Vätsäri Wilderness Area (Finland), Øvre-Pasvik National Park (Norway), Øvre-Pasvik Landscape Protection Area (Norway), Pasvik Nature Reserve (Norway) and Pasvik Zapovednik (Russia) 7. Prealpi Giulie Nature Park (Italy) and Triglav National Park/ Julian Alps Biosphere Reserve (Slovenia) 8. Bavarian Forest National Park (Germany) and Sumava National Park (Czech Republic) 9. Saxon Switzerland National Park (Germany), Bohemian Switzerland National Park (Czech Republic) and Elbe Sandstones Protected Landscape Area (Czech Republic) 10.Escaut Plaines Nature Park (Belgium) and Scarpe-Escaut Regional Nature Park (France) TB PAs Europe: historical background First TB area: 1932 Pieniny Nature Reserve (today National Park) between Czechoslovakia (today Slovakia) and Poland TB PAs Europe: historical background Challenging time: 90th of the 20th century Political changes: End of the iron-curtain Splitting to smaller countries (Czechoslovakia, Yugoslavia) Saxon-Bohemian Switzerland synonym: Elbe Sandstones The largest sandstone rock landscape in Europe 3 pillars of cooperation (i) Nature and Landscape, (ii) Formal basis of cooperation, (iii) Personal basis 31.08.2007 1. -
Fungal Diversity in Sandstone Gorges of the Bohemian Switzerland National Park (Czech Republic): Impact of Climatic Inversion
CZECH MYCOL. 63(2): 243–263, 2011 Fungal diversity in sandstone gorges of the Bohemian Switzerland National Park (Czech Republic): impact of climatic inversion 1 2,3 JAN HOLEC , JAN WILD 1National Museum, Mycological Department, Václavské nám. 68, 115 79 Praha 1, Czech Republic; [email protected] 2Institute of Botany of the ASCR, v. v. i., CZ-252 43 Průhonice, Czech Republic; [email protected] 3Faculty of Environmental Sciences, Czech University of Life Sciences Prague, Kamýcká 129, Praha 6 – Suchdol, 165 21, Czech Republic Holec J., Wild J. (2011): Fungal diversity in sandstone gorges of the Bohemian Switzerland National Park (Czech Republic): impact of climatic inversion. – Czech Mycol. 63(2): 243–263. The diversity of macrofungi in 8 sandstone gorges (narrow valleys bordered by sandstone walls, mostly covered by Picea forests with admixed Fagus, alt. 170–390 m) was assessed with respect to microclimatic data from 235 stations measuring temperature and soil moisture along the elevation gra- dient. In total, 253 species of macrofungi were found including some boreal-montane species, species preferring moist habitats and/or species of more or less natural vegetation. Microclimatically, the bot- toms of gorges are significantly colder than their slopes and slope crests during the vegetation period (climatic inversion) and show higher soil moisture throughout the year. However, they are not signifi- cantly colder during the winter period and even show a higher average minimal temperature than the rest of gorges. Generally, bottoms of sandstone gorges function as „buffers“ maintaining a stable, hu- mid and rather cold microclimate and enabling the occurrence of some boreal-montane fungi and spe- cies requiring humid conditions. -
The City of Corinth and Its Domestic Religion
THE CITY OF CORINTH AND ITS DOMESTICRELIGION (PLATES 87-90) A LTHOUGH much attention has been devoted to Greek religion, most of the em- phasis has been upon majorgods and goddesses. Informationis readily availablein ancient official or state records and inscriptions, or by interpretationof sanctuaryarti- facts and architecture.Much less information is available for the understandingof the humbler aspects of religion as practicedalong the byways and in the neighborhoodsof the urbancenters of Greece. To judge by such descriptionsas Pausanias'enumeration of the hero shrines found throughout the city of Sparta,1by such archaeologicalremains as the street shrines and altars at the entrances of houses in Delos2 and by Wycherley's study for Athens,3 to use three examples, one suspects that small neighborhoodshrines were commonly scattered throughout many Greek cities, even though they appearin different forms in different places. Little literarytestimony and even less epigraphicalevidence exist for neighborhood and domestic religion at Corinth, as contrasted with official or public religion. Still one is able by examinationof the archaeologicalremains to present a reasonablepicture of a pre-RomanCorinth studded with numerous neighborhood shrines of various sorts and with still others within the houses themselves. One type of shrine is that set in the open, along a roadwayor in a small open-air temenos, picturedcommonly on reliefs of the Hellenistic period.4The sacred areas are marked by statues raised high on tall shafts. Such shrines appear not to have been uncommon in Corinth. Two tall shafts with cuttings on their tops for statues are pre- I Pausanias,III. 12-16. 2p. Bruneau,Recherches sur les cultesde Delos a l'epoquehellenistique et a l'epoqueimperiale, Paris 1970. -
Sídla Od Samot Aţ Po Města, Včetně Církevních Staveb
Sídla od samot aţ po města, včetně církevních staveb (mimo vodní mlýny, které jsou uvedené v Hydronymech Ústecka – dále mimo tvrze, tvrziště, hrady, hradiště, komendy, zámky a zámečky, které jsou uvedené jako samostatný soubor) Zkratky okresů: CV = Chomutov, DC = Děčín, LN = Louny, LT = Litoměřice, MO = Most, TP = Teplice, UL = Ústí nad Labem. Václavice (= Ves Sv. Václava) – MO (PK) 5447 – 2,4 km SSV od Nového Mostu (www.stránky). Václavov – DC (ČS) 5250 – 3,2 km JZ od DC (obec V od Krásného Studence, mezi Chrochvicemi a popovicemi a JJV od Popovického vrchu – prvá zmínka o obci je z r. 1787, nyní je XXII část DC) (JK, ODC, P-4, P-5, PP, SOALT, Š, VK. www.stránky+mapy). Syn.: Wenzelsdorf. Vacovice – LN (?) ? – podle P-4 je to ves „?někde― na Ţatecku a podle P-5 se jedná o sídliště, které není po 1945 osadou (P-4, P-5). Vadkovice – CV (?) 5646 – 13,5 km JJZ od CV (JZ od Vikletic, SZ od Přeskak, S od Libědic – první zpráva o obci je z r. 1384, nyní část obce Chbany) (BTM, JK, OCV, OLN, P-4, P-5, SOALT, UK, www.stránky+mapy). Syn.: Wadkowitz, Wakowitz. Valdek – DC (ŠP) 5053 – 30 km SV od DC (SZ od Rumburka, JV od Šluknova, SSV od Starých Křečan – prvá zpráva o obci je z r. 1787, nyní je její jiţní část částí ob. Staré Křečany a severní část /= Harta-Valdek/ je částí Šluknova) (JK, ODC, SOALT, UK, V, V-1, www.stránky+mapy). Syn.: Waldecke. Valencie (hostinec) – TP (PK) 5349 – 2,5 km S od TP (hostinec v Proboštorském lesíku v severní části TP, JZ od Krupky, J od Přítkova, Z od Sobědruh) (KP2). -
Plánu Pokrytí Území Kraje Výjezdovými Základnami Zdravotnické
OBSAH Úvod ......................................................................................................................................................................................... 3 Dokumentace Plánu pokrytí .......................................................................................................................................... 4 Stanovení rizikových parametrů ................................................................................................................................. 4 Dostupnost místa poskytnutí přednemocniční neodkladné péče ................................................................. 5 Struktura výjezdových základen ................................................................................................................................. 5 Vyhodnocení stávající situace ....................................................................................................................................... 6 Opatření k zajištění dostupnosti .................................................................................................................................. 6 Aktualizace Plánu pokrytí .............................................................................................................................................. 8 Seznam příloh ...................................................................................................................................................................... 8 Přílohová část ..................................................................................................................................................................... -
Les Carnets De L'acost, 19
Les Carnets de l’ACoSt Association for Coroplastic Studies 19 | 2019 Varia Édition électronique URL : http://journals.openedition.org/acost/1696 DOI : 10.4000/acost.1696 ISSN : 2431-8574 Éditeur ACoSt Référence électronique Les Carnets de l’ACoSt, 19 | 2019 [En ligne], mis en ligne le 11 juin 2019, consulté le 29 septembre 2020. URL : http://journals.openedition.org/acost/1696 ; DOI : https://doi.org/10.4000/acost.1696 Ce document a été généré automatiquement le 29 septembre 2020. Les Carnets de l'ACoSt est mis à disposition selon les termes de la licence Creative Commons Attribution - Pas d'Utilisation Commerciale - Pas de Modification 4.0 International. 1 SOMMAIRE The Study of Figurative Terracottas: A Cautionary Tale from a Personal Perspective Jaimee P. Uhlenbrock Early Iron Age Terracottas from Southern Portugal: Towards the Definition of a Regional Coroplastic Tradition Francisco B. Gomes Works in Progress Archaic Votive Figurines from the Sanctuary of Demeter at Corinth Susan Langdon News and notes « Quand on a la terre sous l’ongle » : Le modelage dans le monde grec antiqueColloque international, 3-5 avril 2019, Aix-en-Provence. Hélène Aurigny et Laura ROHAUT Terracottas in the News Seizure: An Etruscan Hare Alabastron, circa 580-560 B.C.E. Reprinted from ARCA Blog, Friday, June 29, 2018. At the Museums Alt oder jung? Den Fälschungen im RPM auf der Spur Martina Prante Recent Books Simbolo e gesto. La determinazione di genere nelle statuette fittili del Mondo Greco Marina Albertocchi, Nicola Cucuzza et Bianca Maria Giannattasio Terrakotten aus Akraiphia und ihr Fundkontext. Beiträge zur Chronologie der archaischen böotischen Koroplastik Angeliki K Andreiomenou Bodies of Clay: On Prehistoric Humanised Pottery Heiner Schwarzberg and Valeska Becker (eds.) Les Carnets de l’ACoSt, 19 | 2019 2 A Wayside Shrine in Northern Moab. -
Jurassic Pebbles in the Cretaceous Sandstones of the Bohemian Basin As a Possible Tool for Reconstruction of the Late Jurassic and Late Cretaceous Palaeogeography
Volumina Jurassica, 2019, XVii: 17–38 Doi: 10.7306/VJ.17.2 Jurassic pebbles in the Cretaceous sandstones of the Bohemian Basin as a possible tool for reconstruction of the Late Jurassic and Late Cretaceous palaeogeography Jaroslav Valečka1 Key words: Bohemian Massif, Jurassic relics, Jurassic pebbles, Bohemian Cretaceous Basin, Late Jurassic and Late Cretaceous palaeogeography. Abstract. a new find of pebbles of Jurassic silicites in the Coniacian sandstones of the Bohemian Cretaceous Basin in N Bohemia has permitted analysis of the stratigraphic extent of Jurassic sediments in the NW part of the Bohemian Massif. The studied silicites are domi- nated by the rhax microfacies, while bioclastic and oolitic microfacies are less common. The thickest section of Jurassic sediments in the NW part of the Bohemian Massif has been obtained from the Doubice borehole. It is represented by basal clastics overlain by a 70 m thick succession of silicite-free carbonate rocks which range in age from Callovian to lower kimmeridgian. These deposits are dominated by the bioclastic microfacies whereas the rhax and oolitic microfacies are missing. The studied silicite-bearing sequence is younger than the carbonate rocks in Doubice borehole and was deposited mostly in a deeper zone probably during the late kimmeridgian transgression, much like in the Upper Frankenalb in Se Germany. The extensive Jurassic basin in the Bohemian Massif was connected with the S part of the Polish and German basins and – via the Hessian (Saxonian) Seaway – with the Jurassic basin in Se Germany. The Jurassic sediments were mostly eroded from the Bohemian Massif during the early Cretaceous with the exception of small relics.