The Moravian Karst and Environs
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Invertebrates of the Macocha Abyss (Moravian Karst, Czech Republic) Nevretenčarji Brezna Macoha (Moravski Kras, Republika Češka)
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by ZRC SAZU Publishing (Znanstvenoraziskovalni center - Slovenske akademije znanosti... COBISS: 1.02 INVERTEBRATES OF THE MACOCHA ABYSS (MORAVIAN KARST, CZECH REPUBLIC) NEVRETENČARJI BREZNA MACOHA (MORAVSKI KRAS, REPUBLIKA ČEŠKA) Vlastimil RŮŽIČKA1, Roman MLEJNEK2, Lucie JUŘIČKOVÁ3, Karel TAJOVSKÝ4, Petr ŠMILAUER5 & Petr ZAJÍČEK2 Abstract UDC 592:551.44(437.32) Izvleček UDK 592:551.44(437.32) Vlastimil Růžička, Roman Mlejnek, Lucie Juřičková, Karel Vlastimil Růžička, Roman Mlejnek, Lucie Juřičková, Karel Tajovský, Petr Šmilauer & Petr Zajíček: Invertebrates of the Tajovský, Petr Šmilauer & Petr Zajíček: Nevretenčarji brezna Macocha Abyss (Moravian Karst, Czech Republic) Macoha (Moravski kras, Republika Češka) The invertebrates of the Macocha Abyss, Moravian Karst, Med vzorčenjem v letih 2007 in 2008 smo v jami Maco- Czech Republic, were collected in 2007–2008 and 222 species ha določili 222 vrst nevretenčarjev. Ovrednotili smo rela- were identified in total. The relative abundance of individual tivno pogostost posameznih taksonov polžev, suhih južin, taxa of land snails, harvestmen, pseudoscorpions, spiders, mil- paščipalcev, pajkov, stonog, kopenskih enakonožcev, hroščev lipedes, centipedes, terrestrial isopods, beetles, and ants was in mravelj. Na mraz prilagojene gorske in podzemeljske vrste evaluated. The cold-adapted mountain and subterranean spe- naseljujejo dno in spodnji del brezna, toploljubne vrste pa cies inhabit the bottom and lower part of the abyss, whereas naseljujejo kamnite površine soncu izpostavljenega roba. V the sun-exposed rocky margins were inhabited by thermophil- Macohi je več ogroženih vrst, ki jih sicer v okoliški pokrajini ne ous species. Macocha harbors several threatened species that najdemo. Kot habitat s specifično mikroklimo je Macoha izje- are absent or very rare in the surrounding habitats. -
Support for the Use of Technology and the Implementation of Research Activities in The
Support for the Use of Technology and the Implementation of Research Activities in the Undergraduate Education of Future Teachers 2018–2020 Editor: 1 Editors: Eduard Hofmann Hana Svobodová Authors: Useful Science – We Study the Landscape around us (Češková, Frýzová) Frýzová Iva, Češková Tereza, Jireček Miroslav Useful Science – A Key to Sustainable Development (lower secondary school) Hofmann Eduard, Svobodová Hana, Durna Radek Healthy Lifestyle and Spring Stays in Nature Trávníček Marek, Vrbas Jaroslav Healthy Lifestyle and Winter Stays in Nature Vrbas Jaroslav, Trávníček Marek Integrated Language and Methodological Course Editors: Světlana Hanušová, Ailsa Randall Autors: Světlana Hanušová, Ailsa Randall, Jaroslav Suchý, Alena Dobrovolná, Pavla Buchtová, Zuzana Kršková, Ondřej Krahulec, Filip Pultar, Ondřej Vitula, Marek Antal Methodology Course on the Development of Personal and Social Education Soják Petr Brno 2018–2020 2 CONTENTS Contents ..................................................................................................................................... 3 Introduction ................................................................................................................................ 6 1. Outdoor education and its inclusion into teaching at PdF MU .............................................. 9 1.1 Examples of Transdisciplinarity within Outdoor Education ........................................... 10 1.2 Bibliography ................................................................................................................... -
Czech Speleological Society 2005–2008
Logo černobílé (lze použít i při barevném tisku) 1 Před použitím loga pro tisk zkontroluj nastavení přetisku černou. Před finálním tiskem zkontroluj separace! Černá Podle mého názoru, může být toto logo tištěno i v jiných barvaách než v černé. CMYK: K=100 Záleží na účelu a kontextu použití. Také černá nemusí být 100% černá „K“, CMYK Pantone process: BlackK ale může to být černá teplejší či studenější - podle vkusu a chuti. Pantone Solid: 329-1 Tuto verzi doporučuji nejvíce - barevná ve CMYKu je poněkud nevkusná a CMYK + zlatá jako pátá barva není úplně častý případ. MP Barevnost: CMYK = prostá definice barev. CMYK Pantone process = procesní tiskový vzorník Pantone pro čtyřbarevný ofsetový tisk (CMYK). Pantone solid = vzorník přímých barev pro vícebarevný ofsetový tisk (nejdou přesně vytisknout ve CMYKu či vůbec - metalické, reflexní atp.) U žluté je hodnota 5-3 u Pantone process vzorníku (CMYK) jen orientační - barva není ve vzorníku. Martin Přibil mob: 721515248 CZEemai: [email protected] CH SPELEOLOGICAL SOCIETY 2005–2008 2 CZECH SPELEOLOGICAL SOCIETY 2005–2008 Title: Czech Speleological Society 2005-2008 Edited by: Zdeněk Motyčka, Veronika Vlčková Layout, typography: www.trivia.cz Print: www.dhtiskarna.cz © Czech Speleological Society, Praha 2009 ISBN 978-80-254-4928-8 Contacts: Czech Speleological Society Kališnická 4/6 130 00 Praha Tel. 00420 722 651 110 Office e-mail: [email protected] Board e-mail: [email protected] Web page: www.speleo.cz CZECH SPELEOLOGICAL SOCIETY 2005–2008 3 Dear colleagues, Let me present you this report on activities of the Czech Speleological Society in 2005 – 2008 period. On the following pages you can find a short information about activities of all caving clubs, commissions and bureau of CSS. -
Development of Karst Phenomena for Geotourism in the Moravian Karst (Czech Republic) Udostępnianie Geoturystyczne Form Krasowych W Krasie Morawskim (Republika Czeska)
Geotourism 3–4 (26–27) 2011: 3–24 Development of karst phenomena for geotourism in the Moravian Karst (Czech Republic) Udostępnianie geoturystyczne form krasowych w Krasie Morawskim (Republika Czeska) Piotr Migoń University of Wroclaw, Department of Geography and Regional Development, pl. Uniwersytecki 1, 50-137 Wrocław; e-mail: [email protected] Highland, the Moravian Karst is an example of upland karst. Niemcy Liberec Polska Hradec The caves have been developed for tourism as early as in the Praga Kralove beginning of the 20th century. Recently, more attention is paid to other aspects of the Earth heritage: evolution of geo- logical structure, operation of karst systems and/or exploita- Brno tion and processing of karst-related mineral raw-materials. An increasing number of educational trails and dense network Austria Słowacja of tourist trails make the Moravian Karst particularly attrac- tive tourist destination. The author aims to present the karst relief of the area to- Abstract: The Moravian Karst in the south-eastern part of the gether with the main stages of its evolution and to point out Czech Republic has considerable potential for the development of geotourism. It is characterized by outstanding geodiversity, the most important geotourist attractions along with their revealed in abundant, surface and subterranean karst landforms, development for tourism. Finally, the problem is highlighted as well as protracted history of karst evolution which can be how the acquaintance with the geodiversity of the Moravian traced back to the Mesozoic. An additional value is provided Karst can supplement the picture of karst forms and pro- by the presence of cultural heritage, related to exploitation and cesses available in Poland. -
Moravian Karst, the Czech Republic)
FOSSIL IMPRINT • vol. 73 • 2017 • no. 3–4 • pp. 515–532 (formerly ACTA MUSEI NATIONALIS PRAGAE, Series B – Historia Naturalis) THE MAMMALIAN FAUNA OF BAROVÁ CAVE (MORAVIAN KARST, THE CZECH REPUBLIC) MARTINA ROBLÍČKOVÁ1,*, VLASTISLAV KÁŇA2, MIRIAM NÝVLTOVÁ FIŠÁKOVÁ3 1 Moravian Museum, Historical Museum, Anthropos Institute, Zelný trh 6, 659 37 Brno, the Czech Republic; e-mail: [email protected]. 2 Muzeum Blanenska p. o., Zámek 1, 678 01 Blansko, the Czech Republic; e-mail: [email protected]. 3 Institute of Archaeology of the CAS, Brno, v. v. i., Čechyňská 363/19, 602 00 Brno, the Czech Republic; e-mail: [email protected]. * corresponding author Roblíčková, M., Káňa, V., Nývltová Fišáková, M. (2017): The mammalian fauna of Barová Cave (Moravian Karst, the Czech Republic). – Fossil Imprint, 73(3-4): 515–532, Praha. ISSN 2533-4050 (print), ISSN 2533-4069 (on line). Abstract: Barová Cave is located in the central part of the Moravian Karst (the Czech Republic), on the right slope of Josefovské Valley; it is the outfl ow part of Rudické propadání (Rudice Sink) – Býčí skála (Bull Rock) cave system. Even since its discovery by A. Sobol in 1947, Barová Cave has been known as important palaeontological site, with well-preserved fauna of the Late Pleistocene. In the summer of 2011, a landslide of sediments revealed yet unexamined fossiliferous positions, and started the current research activity. There were discovered skeletal remains of these 21 taxa of vertebrates between 2011 – 2017 in Barová Cave: bear from the cave bear group (Ursus ex gr. spelaeus), cave lion (Panthera spelaea), wolf (Canis lupus), cave hyena (Crocuta crocuta spelaea), brown bear (Ursus arctos), lynx (Lynx lynx), wolverine (Gulo gulo), fox, probably red (Vulpes cf. -
Additional Material Ecosystem Services Hydrological Values: the Hydrography and Hydrology of the Site Differ Substantially From
Ramsar Site: 1413 - Punkva subterranean stream Ramsar Information Sheet March 2004 Additional material Ecosystem services Hydrological values: The hydrography and hydrology of the site differ substantially from those of the surrounding area. Streams originating in non-karst area of Drahanská Uplands sink below the ground immediately after entering the limestone area. Hydrography and hydrology of the area is rather complicated - some sinks and springs function depending on the water dynamics, subterranean streams cross each other at differing levels, a sink may become a spring and vice versa, etc. Surface streams are almost non-existent, subterranean streams and their catchments do not correspond with the surface relief. In the area of sinkholes, valleys with abrupt dead-ends, or partially so, have been created and streams are periodical. This karst area has its own, mainly subterranean, hydrographic systems with single erosion base being the drainage system of the Punkva stream. Detailed hydrology of the area is highly complicated and not yet fully understood. Sloupský potok and Bílá voda streams are the sources for the Punkva stream, that has a catchment area of 170 km2 and average discharge of 0.96 m3.s-1. Before reaching a cave, the waters of Sloupský stream, during the period of low water level, disappear down about 20 sinkholes or infiltrate into the bottom substrate at the time of low water discharge. Thus, part of the stream is periodical. The stream disappears finally underground at Staré skály (rocks) near Sloupsko-šošůvské Caves. At a depth of 70-100m it creates the Sloupský corridor that belongs to the Amateur Cave complex. -
FRIENDS of SOQOTRA 19Th International Conference and Annual General Meeting
1st Announcement FRIENDS OF SOQOTRA 19th International Conference and Annual General Meeting 24 – 27 September 2020, Mendel University, Brno, Czech Republic Conference Aim The “Friends of Soqotra” (or Friends of Socotra, both spellings are possible) meet every year gathering naturalists, botanists, marine biologists, geographers, sociologists, linguists, archeologists, explorers, writers, travellers interested in Socotra from all over the world. Presentations and discussions occur for ongoing projects and scientific research about Socotra. Attendees actively promote awareness for the conservation of the unique culture and nature of the Archipelago and its sustainable development. The aim is to create an event that brings together all people with a heart for the Socotra Archipelago, its biodiversity, its myths and traditions, its history and future. Conference Venue The conference will be held from September 24th to 27th, 2020, Mendel University in Brno (Zemědělská 1, Brno, http://www.mendelu.cz), Czech Republic. Call for Papers Participants are kindly invited to submit abstracts of papers and posters related to the themes of the conference. Each submitted abstract will be subject to peer review and the conference organizers reserve the right to allocate the appropriate means of presentation to submitted contributions. Preliminary Programme Thursday 24th September 2020 Registration, Welcome excursion Vila Tugendhat Friday 25th September 2020 Registration, Conference, Conference dinner Saturday 26th September 2019 Conference, Brno guided -
The Updated Record of Cave Bear and Other Members of the Genus Ursus
Cadernos Lab. Xeolóxico de Laxe ISSN: 0213-4497 Coruña. 2001. Vol. 26, pp. 447-455 The updated record of cave bear and other members of the genus Ursus on the territory of Czech Republic Registro actualizado de Oso de las Cavernas y otras especies del género Ursus en la República Checa WAGNER, J. AB S T R A C T During the 2nd half of 20th century, a succession of new Pleistocene localities was dis- covered and some classical paleontological sites were revised. From many of those pla- ces also bear remains were recorded. Nine localities provided large material of bear remains in good stratified layers. Bear record from Moravian localities were studied in details by Prof. R. MUSIL from Brno. This paper presents a review of updated kno- wledge on this localities - especially about their stratigrafical position (based on micro- mammalian evidence) and basic information on bear remains studied. Key words: Pleistocene, Ur s u s , cave bear, brown bear, Czech Republick, Bohemian karst, Moravian Karst Charles University. Faculty of Sciences. Department of Palaeontolog. Albertova 6.12843 Praha 2. CZECH REPUBLIC 448 WAGNER, J. CAD. LAB. XEOL. LAXE 26 (2001) INTRODUCTION The most important informations are given by new discovered sites with both Palaeontological investigation of fossil large and small mammals together, which cenozoic mammals has a tradition in the allows morphometric studies of bears territory of the Czech Republic. Already combined with their exact stratification. from the begining of this investigations The most importent are as follows: remains of bears were among the most fre- 1) Holstejn (Moravian karst) quent finds. -
Speleological Mapping in the Northern Part of Moravian Karst
Moravian Karst • Surface: 92 km2 Speleological Mapping in the • South Moravia, Nord NorthernPart of Moravian Karst of Brno • Largest cave system Jan Sirotek, Josef Weigel – Amatérská cave Czech Republic • Tourist caves: Punkevní with Macocha Abyss, Czech Speleological Society Sloupsko-šošuvské, Institute of Geodesy FAST, Brno University of Technology Katerínská, Balcarka Long tradition of speleological mapping in „Cave which was not surveyed MK – Kríž, Wankel, Absolon was not explored!“ Cooperation between FAST and CSS Speleological mapping course • Training of cavers from CSS • Manual on cave mapping • Education on speleological mapping during surveying master degree as a voluntary course • Cooperation on mapping projects in Amatérská cave and Býcí skála cave 1 Controlpoints network on the surface Surface karst phenomenas mapping Sloup 8017 8016 8022 8014 8021 8015 8020 8019 8018 8001 b e l z y 8011 t us P 8013 8012 Skalni mlyn Practical application of speleological Amatérská cave mapping – Amatérská cave • Main corridors were surveyed by total station using fixed tripods • Some parts were surveyed by mining compass, clinometer and tape • The rest – geological compass, clinometer, tape • Underwater survey – marked line, compass, gauge Classical speleological mapping Main corridors were surveyed by total station 2 Under water surveying equipment Device „COMBI“ especially developped for cave survey Special map key Microstation Karsologic digital map map Sloupský corridor original 1 : 10 000 Original 1:500 3 Parts ? 5. sifon Stará Amatérská Practical jeskyne between application sumps Vintocká odbocka Amatérská cave ? Sloupský koridor Belovodská vetev ? S Šošuvská odbocka Krematorium S Bludište 4. sifon 3. sifon Milana Šlechty 0 500 m 2. sifon 0 50 m Podzemn í Punkva Západní macošská vetev Východní macošská vetev Vstupní štola Predmacošský sifon Chodba mezi 1 a 2. -
Hydrogeochemistry of Dripwaters in Selected Caves of Moravian Karst Ph D Dissertation
MASARYK UNIVERSITY FACULTY OF SCIENCE DEPARTMENT OF GEOLOGICAL SCIENCES Hydrogeochemistry of Dripwaters in Selected Caves of Moravian Karst Ph D Dissertation Pavel. Pracný SUPERVISOR: DOC. ING. JIŘÍ FAIMON, DR. BRNO 2017 BIBLIOGRAPHIC ENTRY Author Mgr. Pavel Pracný Faculty of Science, Masaryk University Department of Geological Sciences Title of Dissertation Hydrogeochemistry of Dripwaters in Selected Caves of Moravian Karst Degree Programme Geology Field of Study Geological Sciences Supervisor doc. Ing. Jiří Faimon, Dr. Faculty of Science, Masaryk University, Department of Geological Sciences Faculty of Science, Palacký University, Department of Geology Academic Year 2016/2017 Number of Pages 53+65 Keywords Cave dripwater; Moravian Karst; Anomalous drip; Car- bon dioxide; Mg/Ca ratio; Kinetic modeling; Limestone dissolution; Degassing; Mg-calcite BIBLIOGRAFICKÝ ZÁZNAM Autor Mgr. Pavel Pracný Přírodovědecká fakulta, Masarykova univerzita Ústav geologických věd Název práce Hydrogeochemie skapových vod ve vybraných jeskyních Moravského krasu Studijní program Geologie Studijní obor Geologické vědy Školitel doc. Ing. Jiří Faimon, Dr. Přírodovědecká fakulta, Masarykova univerzita, Ústav geologických věd Přírodovědecká fakulta, Univerzita Palackého, Katedra geologie Akademický rok 2016/2017 Počet stran 53+65 Klíčová slova Skapové vody; Moravský kras; Anomální skap; Oxid uhličitý; Poměr Mg/Ca; Kinetické modelování; Rozpouštění vápenců; Odplyňování; Mg-kalcit ABSTRACT Karst dripwaters are an important factor of speleothem formation. These cave precipitates provide various proxy data (e.g. stable isotopes, minor and trace elements or grow laminae) about paleoenvironment. To better under- stand the interrelationship between proxies and environment, an investigation of recent karst processes is important. A dripwater hydrogeochemistry and cave PCO2 were studied in the dry part of Punkva Caves (Moravian Karst). -
Moravian Karst, Czech
International Journal of Speleology 46 (3) 345-358 Tampa, FL (USA) September 2017 Available online at scholarcommons.usf.edu/ijs International Journal of Speleology Off icial Journal of Union Internationale de Spéléologie The impact of door opening on CO2 levels: A case study from the Balcarka Cave (Moravian Karst, Czech Republic) Marek Lang1*, Jiří Faimon1,2, and Sandra Kejíková1 1Department of Geological Sciences, Faculty of Sciences, Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic 2Department of Geology, Faculty of Science, Palacký University Olomouc, 17. listopadu 1192/12, 771 46 Olomouc, Czech Republic Abstract: The impact of door opening on cave carbon dioxide (CO2) levels was studied in the Entrance Chamber and the Gallery Chamber of the Balcarka Cave (Moravian Karst, Czech Republic). The effect of door opening differed with cave ventilation modes. Under upward airflow mode, the cave door opening led to the increase of output advective CO2 fluxes from the cave and to the decrease of CO2 levels. This effect was evident especially in the Entrance Chamber near the cave entrance and then suppressed in the Gallery Chamber situated deeper in the cave. Under the downward airflow mode, the cave door opening changed airflow paths and main CO2 sources/fluxes. This resulted in the increase of CO2 level in the Entrance Chamber while the levels in the Gallery Chamber decrease. Modeling indicates that the increase could -2 -1 be result of input advective CO2 fluxes from epikarst (up to 5.9 × 10 mol s ). To reduce the impact on cave microclimate, a careful control of the visiting regime without overlapping of individual doors’ openings is recommended. -
Ve Sloupu Na Blanensku a Jeho Okolí 26. Května 2003
Český hydrometeorologický ústav pobočka Brno Zpráva o povodni ve Sloupu na Blanensku a jeho okolí 26. května 2003 Zpráva o povodni ve Sloupu na Blanensku a jeho okolí 26. května 2003 Zpracovali: Ing. Ivo Dostál, Ing. Eva Soukalová, CSc. a kolektiv oddělení hydrologie RNDr. Milan Šálek a kolektiv RPP Předkládá: RNDr. Ing. Jaroslav Rožnovský, CSc. ředitel ČHMÚ P-Brno V Brně dne 23.7.2003 tel: 5 41421022 e-mail: [email protected] fax: 541421018 Úvod Dne 26. května zasáhla obce na Blanensku v odpoledních hodinách přívalová srážka, která zničila komunikace, mosty a ploty. Přívalem vody byl nejvíce poškozen Sloup, který podobnou situaci, i když v menším měřítku, zažil již před dvěma týdny dne 13. května 2003. Voda a bahno se valila na obec ze západu, z polí od Petrovic, Žďáru a Němčic. Přívalové deště zatopily jen ve Sloupu osmdesát domů, garáže, obecní úřad, restauraci, poštu, hřiště i provozní budovy Sloupsko-šosůvských jeskyní. Na druhou stranu rozvodnice do údolí Svitavy způsobily tyto deště škody i v obcích Doubravice, Kuníčky. Z jiného bouřkového centra se přehnala menší přívalová voda obcí Lažánky a okolí. 1. Popis území Celé území Sloupska náleží k povodí řeky Svitavy. Říční síť je zde především tvořena řadou ponorných toků vtékajících do řeky Punkvy, která ústí z levého břehu v městě Blansku do řeky Svitavy. Punkva vzniká v podzemí spojením několika vodních větví. Na západní straně Sloupu je hlavním tokem potok Luha, na východě, u Holštejna, je to Bílá voda. Luha pramení ve výši 700 m n.m. na úbočí nejvyšší hory Drahanské vrchoviny, zvané Skály. Přítoky Luhy jsou potok Protivanský, Hartmanický, Novodvorský a malý potůček Olejnický.