An Unforgettable Trip That Circumnavigates the Tatra Mountains, the Highest Part of the Carpathian Range
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1 Mountains of Slovakia (Hory Slovenska)
MOUNTAINS OF SLOVAKIA (HORY SLOVENSKA) © PIOTR MIELUS, AUGUST 2007 Introduction Slovakia is a small country (it covers an area of 49.000 sq km) and borders on: Austria, Czech Republic, Poland, Ukraine and Hungary. There are 5 million people living there and approx. 10% live in the capital city of Bratislava. Slovakia is one of the most mountainous countries in Europe. The highest point is located in the Tatra Mountains (Gerlachovský štít 2655m) and the lowest point is in the Bodrog valley (94m). The extreme points of the Slovak territory are: in the north: near a top of Mondrálova in Babia hora massiv on the Polish border (49:37) in the south: Donau coast near the village of Patnice on the Hungarian border (47:44) in the west: Morava coast near the village of Záhorska Ves on the Austrian border (16:50) in the east: near a top of Kremenec in Bukovské vrchy on the Ukrainian/Polish border (22:34) Slovakian mountains belong to the Western Carpathians (a tiny part in the east belong to the Eastern Carpathians). The main rivers have estuaries in the Danube: Vah, Hron, Hornad and Torisa. The majority of the Slovak territory belongs to the basin of the Black Sea, but the highest part (High Tatras) belongs to the Baltic Sea (upper Poprad valley). Technical data For the each peak the following information is provided: 1. Peak – official Slovak name, for border peaks alternative name in brackets, distinguishing adjectives (if needed added by the author) in italics. 2. Height – taken from the Source Map. 3. -
Chapter 2 High Mountains in the Baltic Sea Basin
Chapter 2 High mountains in the Baltic Sea basin Joanna Pociask-Karteczka 1, Jarosław Balon 1, Ladislav Holko 2 1 Institute of Geography and Spatial Management, Jagiellonian University in Kraków, Poland, [email protected] 2 Institute of Hydrology, Slovak Academy of Sciences, Slovakia Abstract : The aim of the chapter is focused on high mountain regions in the Baltic Sea basin. High mountain environment has specific features defined by Carl Troll. The presence of timberline (upper tree line) and a glacial origin of landforms are considered as the most important features of high mountains. The Scandianavian Mountains and Tatra Mountains comply with the above definition of the high mountain environment. Both mountain chains were glaciated in Pleistocene : the Fennos- candian Ice Sheet covered the northern part of Europe including the Scandinavian Peninsula while mountain glaciers occurred in the highest part of the Carpathian Mountains. Keywords : U-shaped valleys, glacial cirques, perennial snow patches, altitudinal belts The Baltic Sea and its drainage The Baltic Sea occupies a basin formed by glacial basin – general characteristic erosion during three large inland ice ages. The latest and most important one lasted from 120,000 until ap. The Baltic Sea is one of the largest semi-enclosed seas 18,000 years ago. The Baltic Sea underwent a complex in the world. The sea stretches at the geographic lati- development during last several thousand years after tude almost 13° from the south to the north, and at the the last deglaciation. At present it exhibits a young geographic longitude 20° from the west to the east. -
The Tatra Mts – Rocks, Landforms, Weathering and Soils Tatry – Skały, Rzeźba, Wietrzenie I Gleby
Geoturystyka 2 (13) 2008: 51-74 The Tatra Mts – rocks, landforms, weathering and soils Tatry – skały, rzeźba, wietrzenie i gleby Marek Drewnik1, Ireneusz Felisiak2, Irena Jerzykowska3 & Janusz Magiera2 1Jagiellonian University, Faculty of Biology and Earth Sciences; ul. Gołębia 24, 31-007 Kraków, Poland. (Institute of Geography and Spatial Management) 2AGH University of Science and Technology; Faculty of Geology, Geophysics and Environmental Protection; Al. Mickiewicza 30, 30-059 Kraków, Poland. 3Jagiellonian University, Faculty of Biology and Earth Sciences; ul. Gołębia 24, 31-007 Kraków, Poland. (Institute of Geological Sciences) e-mail: [email protected]; [email protected]; [email protected]; [email protected] Chabówka Introduction Nowy Targ The Tatra Mountains are the most prominent, the highest Szczawnica (2,655 m a.s.l.) and presently non-glaciated mountains in the Warszawa Czarny Dunajec Niedzica Central Europe, located approximately halfway between the Baltic Sea and the Adriatic Sea, and between the Atlantic Zakopane Ocean and the Ural Mts. Thus, they occupy a transitional Kraków position between the maritime Western Europe and the con- tinental Eastern European lowland. Field trip leads through the core of the central part of the Tatry Mts: Bystra valley, Kasprowy Wierch Mt, and Sucha Woda valley (Fig. 1). It gives good insight into geological Abstract: The trip gives insight into geology and landforms as well structure, landscape as well as weathering and soil forming as into past and present dynamic geological, geomorphologic and processes. Essential differences between the both main parts soil-forming processes in the central part of Polish Tatra Mts. -
The Tatra Mountains and Zakopane Through the Eyes of Two Artists: Witkacy and Tetmajer
Prairie Perspectives 181 The Tatra Mountains and Zakopane through the eyes of two artists: Witkacy and Tetmajer Ania Holub and Paul Simpson-Housley York University Abstract: An author’s and an artist’s treatment of landscape reflects the categories of perception of the culture and what Thomas Hardy called the “idiosyncratic mode of regard.” Thus, there are both culturally conditioned and personal (or idiosyncratic) aspects of an artist’s mode of perception. We consider how two Polish artists/writers evaluate the Tatra-Podhale region through their perceptual filters. Kazimierz Przerwa-Tetmajer and Stanislaw Ignacy Witkiewicz (Witkacy) provide colourful insights into their regional domain, an area which contrasts dramatically with the lowlands that cover most of the rest of Poland. A writer’s treatment of landscape reflects the categories of perception of the culture and what Thomas Hardy called ‘the idiosyncratic mode of regard’ (Hardy 1928). Thus, there are both culturally conditioned and personal (or idiosyncratic) aspects of an author’s/artist’s mode of perception. Geography has traditionally emphasized the former in its assessment of human/environment relationships. However, the artist’s personal perception conditions his/her geographic evaluation. In the case of D. H. Lawrence, the general values and categories of English Romanticism are reflected in, for example, his rather conventional contrasts between agrarian and industrial landscapes. His most successful descriptions, however, reflect primarily his intensely personal mode of perception. Lawrence was a writer of extraordinarily diverse works, yet a coherent and very quirky personal view colours everything. 182 Prairie Perspectives In other words, his pseudo philosophy provided a filter through which all is seen, and his sheer descriptive power derives to a great extent from the metaphorical energy provided by his personal view. -
Press Release
Press release Bad Kötzting 19 March 2021 Page 1 from 6 The treetop walks of Erlebnis Akademie AG Spring atmosphere at the treetop walk Neuschönau © Erlebnis Akademie AG The treetop walks of the company based in the Bavarian Forest are a tribute to nature. Erlebnis Akademie AG designs, builds and operates treetop walks nationally and internationally. Characteristic of the company's nature experience facilities are a sustainable wooden construction, a low-barrier walkway through the floors of the forest, play and learning stations, as well as an observation tower at each location that provides new and unique perspectives. In addition to providing an experience for visitors of all ages, Erlebnis Akademie AG's self- imposed ecological educational mission is a key component of the concept. As a specialist for tourist highlights in nature, it creatively implements extraordinary facilities, placing great emphasis on sustainable construction and a barrier-free use for all facilities. The overall concept is designed to promote visitors' sensitivity to the unique natural environment and to enable them to experience it in an interactive way. Individual additional offers at each location complete the concept. Treetop Walk Bavarian Forest The treetop walk in Neuschönau in the Bavarian Forest Press release National Park was opened in 2009. The predominantly Bad Kötzting wooden structure is carefully integrated into the mixed 19 March 2021 mountain forest and conveys an unspoiled experience Page 2 from 6 of nature, which is complemented by mobility and learning stations along the barrier-free walkway. The 1,300-meter-long and up to 25-meter-high footbridge ends on the platform of the observation tower, affectionately called the tree-egg by visitors, at a height of 44 meters and promises a magnificent view on the one hand in the direction of Rachel and Lusen of a settlement-free area with forest and wilderness, and on the other hand of the cultivated cultural landscape of the Bavarian Forest all the way to the Alps. -
SLOVAKIA Caves-Of-Demanova-Valley Slovakia RIS 2006 En
Information Sheet on Ramsar Wetlands (RIS) – 2006-2008 version Available for download from http://www.ramsar.org/ris/key_ris_index.htm. Categories approved by Recommendation 4.7 (1990), as amended by Resolution VIII.13 of the 8 th Conference of the Contracting Parties (2002) and Resolutions IX.1 Annex B, IX.6, IX.21 and IX. 22 of the 9 th Conference of the Contracting Parties (2005). Notes for compilers: 1. The RIS should be completed in accordance with the attached Explanatory Notes and Guidelines for completing the Information Sheet on Ramsar Wetlands. Compilers are strongly advised to read this guidance before filling in the RIS. 2. Further information and guidance in support of Ramsar site designations are provided in the Strategic Framework and guidelines for the future development of the List of Wetlands of International Importance (Ramsar Wise Use Handbook 7, 2 nd edition, as amended by COP9 Resolution IX.1 Annex B). A 3 rd edition of the Handbook, incorporating these amendments, is in preparation and will be available in 2006. 3. Once completed, the RIS (and accompanying map(s)) should be submitted to the Ramsar Secretariat. Compilers should provide an electronic (MS Word) copy of the RIS and, where possible, digital copies of all maps. 1. Name and address of the compiler of this form: Mgr. Dagmar Haviarova, Slovak Caves Administration, FOR OFFICE USE ONLY . DD MM YY Hodzova 11, 031 01 Lipt. Mikulas, Slovakia Tel.: +421/(0)44/5536201, Fax: +421/(0)44/5536311 e-mail: [email protected] RNDr. Zuzana Visnovska, Slovak Caves Administration, Designation date Site Reference Number Hodzova 11, 031 01 Lipt. -
The Tatra Mountains Stretch Across Poland and Slovakia Offering a Rich Tapestry of Scenery to Explore by Bike
Discover Hidden Europe Come and share in our passion for exploration. Podiaventures are fully supported cycling adventures across Hidden Europe. The Tatra Mountains stretch across Poland and Slovakia offering a rich tapestry of scenery to explore by bike. Tatra Mountains Roadventure, Poland & Slovakia 12th - 16th June 2019 11th - 15th September 2019 Start: Base location: Duration: Avg Distance: Avg Elevation: Difficulty: Kraków Niedzica 4 days riding / 4 nights 100km 1300m 3/5 The Podia Way Roadventures are fun, social rides with a chance to meet new people with the same interests. They are not about performance, but the joys of adventure. If you want to test yourself up a climb, we have the guides to go with you, but if you want to ride it at the back at your own pace, we also accommodate that. BOARS PASS 120km 1,680m WARM UP 42km 630m POLAND SLOVAKIA ROMA ROADS 105km 1,630m GIANT’S SHADOW 92km 1,700m TATRA MOUNTAINS Location The Tatra Mountains make up the highest part of the Carpathian range that stretches in an arc from Czech Republic, through Slovakia, Poland, Hungary and the Ukranie all the way down to Romania. The Tatra’s are rugged mountains with high cols and precipitous faces. The wall-like nature of them forms a natural border between Poland and Slovakia with only a few places to pass through them. "The experience turned out to be much more than just beautiful roads and spectacular scenery, I also got to meet and ride with a group of exceptional cycling enthusiasts from all over Europe." Eric, Hong Kong Roadventure includes.. -
Geological Framework of the Tatra Mountains- Podhale Geothermal System (Carpathians)
Bulletin d’Hydrogiologie No 17 (1999) Centre d’Hydrogiologie, Universiti de Neuchdtel ED~IONSPET ERLwc Geological framework of the Tatra Mountains- Podhale geothermal system (Carpathians) by J6zef Wieczorek GEOCONSULTMG, Smoluchowskiego4/1,30-083 Krak6w, Poland, in cooperation with PEC Geotermia Podhalanska S. A. Zakopane ABSTRACT The Podhale (Western Carpathians) region lying between the Tatra Mts. and the Pieniny Klippen Belt is known as an area rich in thermal water exploited for heating purposes as well as recreation (swimming pools). The thermal springs at the foot of the Tatra Mts. (Jaszczurowka, Oravice) are the surhce manifestations of an active geothermal system. Numerous drilling data have cohedthe existence of low-enthalpy geothermal reservoir under the entire Podhale basin. The thermal waters are associated with carbonates of highly fractured Nummulite Eocene and with Mesozoic rocks (carbonates of Middle Triassic, sandstones of Lower Jurassic).Two geothermal doublets were completed for themal water exploitation in the northern part of Podhale basin where thermal waters of 80-90°C occur at the depth -2000-3000m. KEVWORDS Thermal waters, geothermal system, geology, Carpathians 1. Entroduction The Podhale (Western Carpathians) region lying between the Tatra Mts. and the Pieniny Klippen Belt is known as an area rich in low-enthalpy thermal water (SOKOLOWSKI, 1992, CHOWANJEC & POPRAWA 1998). The Tatra Mts. massif elevated in Miocene and mainly in post-Miocene period form a recharge area of 350 km2however, the Pieniny Klippen Belt is considered an impermeable barrier for fluid flow. The Tatra Mts.-Podhale segment of the Inner Carpathians form an alpine-type artesian geothermal system, which is only a part of a much larger Inner Carpathian geothemml region, situated on both sides of Poland-Slovakian border around the Tatra Mts. -
Female Messages from the High Altar Kristina Potuckova
Female Messages from the High Altar Kristina Potuckova Mlynica,1 now a small village nested under the High Tatra Mountains in the Spiš region of present-day Slovakia, was once a small town of some importance. First mentioned in 1268, Mlynica was inhabited by German settlers and their descen- dants and remained largely German until World War II.2 The town is listed as a member of the League of 24 Spiš towns and its parish priest as a member of the fraternity of Spiš parish priests, although probably at a lower rank than the priest of the prosperous trading town of Levoča.3 In a situation typical of medieval Hungary’s small towns and villages, the written sources are silent on any details of Mlynica’s life or indeed Mlynica itself. The scattered mentions here and there are, however, complemented by a remarkable work of art, the late medieval high altar of St. Margaret of Antioch (around 1515-1520), the patron saint of the par- ish church. The altar was donated by Hedwig of Teschen from the Silesian branch of the Polish Piast dynasty, widow of the influential Hungarian magnat Stephen Szapolyai. In the central shrine of the altarpiece looms the statue of St. Margaret (159 cm; fig. 1) flanked by panel paintings of four female saints. The most easily re- cognizable is St. Barbara holding a chalice. Her counterpart is most likely St. Elisabeth of Thuringia feeding the poor. The other two saints have not been iden- tified so far. They obviously do not belong to the virgin martyr type. -
Contemporary Geomorphic Processes in the Polish Carpathians Under Changing Human Impact
21 by Adam Lajczak1, Wlodzimierz Margielewski2, Zofia Raczkowska3 Jolanta Swiechowicz4 Contemporary geomorphic processes in the Polish Carpathians under changing human impact 1 Pedagogical University, Institute of Geography, 2 Podchorazych Str., 30-084 Cracow, Poland. E-mail: [email protected] 2 Polish Academy of Sciences, Institute of Nature Conservation, 33 A. Mickiewicza Ave., 31-120 Cracow, Poland 3 Polish Academy of Sciences, Institute of Geography and Spatial Organization, 22 Sw. Jana Str., Cracow, Poland 4 Jagiellonian University in Krakow, Institute of Geography and Spatial Management, 7 Gronostajowa Str., 30-387 Cracow, Poland The paper presents activity of contemporary The Polish Carpathians are relatively densely populated (127 2 geomorphic processes in the Polish Carpathians, taking persons/km ), and more than 65% of the population live in rural areas (Dlugosz and Soja, 1995). For this reason man exerts a strong into account human impact on relief transformation in influence on the course of geomorphic processes, but recent processes the past several centuries. and their effects also pose a threat to man. According to Slaymaker Landsliding in the flysch Carpathians is a principal (2010), human activity is a key driver in present-day landscape process in slope transformation, posing the most serious evolution in mountain areas. threat to man, both in the mountains and the foothills. The aim of this paper is to present such mutual relationships within areas showing four types of relief, indicating the most important On the other hand, unsuitable housing on slopes initiates process, type of geomorphic hazard and type and effect of human mass movements, frequently with catastrophic influence on relief transformation, as well as tendencies in these consequences. -
1.Assessing Sustainability in Mountain Tourism of Demanovska Valley
European Journal of Geography Volume 8, Number 2:6 - 23, February 2017 ©Association of European Geographers ASSESSING SUSTAINABILITY IN MOUNTAIN TOURISM OF DEMANOVSKA VALLEY, SLOVAKIA Iveta Rakytova Catholic University, Faculty of Education, Department of Geography, Ruzomberok, Slovakia [email protected] Ivana Tomcikova Catholic University, Faculty of Education, Department of Geography, Ruzomberok, Slovakia [email protected] Abstract: Demanovska Valley belongs to the most beautiful and the most valuable territories of Slovakia. It is a source of interest for its high country aesthetic and natural value not only from the scientific and professional point of view, but also from the touristic and recreational point of view. The aim of this paper is to evaluate the natural potential of Demanovska Valley, to analyze the development of tourism over the past 10 years, the current state of the cable cars, ski lifts and slopes, as well as accommodation facilities in the valley. Also to point to the growing interest in Demanovska Valley and the growing share of visitors within the district, country and Slovakia. We use the Intensity Index of Tourism Development to assess the attractiveness of Demanovska Valley, but also to point out how the development of tourism impacts the environment, as the monitored area is located in the Low Tatra National Park. Keywords: Resort Jasna Nizke Tatry, environment, protected areas, amenity, the intensity of tourism. 1. INTRODUCTION Slovakia offers a very interesting and varied landscape from the tourism point of view. The development of tourism in Slovakia is one of the potential accelerators of economic development and factors in the standard of living. -
LOGO Basic Region Characteristic: LAG Identification
LOGO Basic region characteristic: LAG identification: Population: 10 771 Statutory agent: Name: Ivan Nomilner Area in km2: 30374 Population density (people / km2): 36,1 LAG office: Residence: Number of municipalities: 10 Mýto pod Ďumbierom 64 List of LAG region municipalities: 976 44 Mýto pod Ďumbierom Nemecká, Podbrezová, Predajná, Horná Lehota, Dolná Lehota, Mýto pod Ďumbierom, Bystrá, Ráztoka, Jasenie, LAG manager: Jarabá, Brezno - town Name: Mgr. Vivien Kohútová Tel.: - Cities: 0 Mob.: 00421-948 074 741 Fax: - Administrative classification: E-mail: [email protected] District: Brezno LAG web site address: www.maschopokjuh.eu Region: Banská Bystrica Self-Governing Region Communication in: Slovak, English Map of LAG region Map of Banská Bystrica Self-Governing Region with LAGCHJ area designation LAG Chopok Juh brief description: LAG Chopok Juh region (hereinafter LAGCHJ) is geographically situated in the central Slovakia. The Hron River flows through its axis and drains almost the entire region (except Mýto pod Ďumbierom). Low Tatras are situated in the north of the region (Ďumbier – 2 043 m is the highest mountain of the Brezno district). In the east and south-east, Spišskogemerský Karst (Kľak – 1 409 m) and Stolické vrchy (Kyprov – 1 391 m) touch the region and Veporské vrchy (Fabova hoľa – 1 439 m) in the south. LAGCHJ settlement structure is significantly influenced by the landscape environment, which limited its full-area development. In the territory of the Brezno city live 34.7% inhabitants of the whole district. Settlements of the higher size category create a nodular-band structure with the economic base - Nemecká, Predajná, Podbrezová on the west from the settlement centre.