DOCSLIB.ORG

Amazing Giants Have Arrived at the Liptov Arena

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text

Load more

Tatry mountain resorts, a.s. Amazing Giants have arrived at the Liptov Arena LIPTOVSKÝ MIKULÁŠ (7th July 2014) – From today, holidaymakers and local people can cool down at the tropical Tatralandia thanks to extinct but realistic Giants from the Ice Age. A unique exhibition of 17 animal models has come to the multipurpose Liptov Arena at Tatralandia again, after a year. From 7th July to the end of August, visitors will have a chance to learn something about the lives of the cave lion, gigantopithecus, giant moa bird or mammoth and see them in full size. There will also be a unique battle scene of 5-metre-tall and 2-metre-long one-horned rhinoceri. An area of 4,000 m2 will introduce creatures that can´t be met anywhere else on our planet. The exposition was prepared in cooperation of scientists and artists and brings back traces of earthly life long forgotten. Each of 17 models is placed into scenery resembling the original natural environment. Learning the oldest and biggest inhabitants of our planet through this exposition will help students, lovers of prehistory, amateur researchers and also the wide public to see them in details and realize their astonishing size and power. The biggest model of a mammoth is 6 metres tall. All models are displayed in dynamic positions so that every visitor can create their own story about them. The exhibition does not only teach visitors how prehistoric animals looked like, but also what they lived on and how they coexisted with man. As part of the Giant exhibition, there will also be an exhibition of 18 oversized mirror and crystal brain teasers, optical illusions, 3D magic and endless labyrinths. The multipurpose Liptov Arena is located only a few metres from Aquapark Tatralandia, with all tourist centres in the Low and Western Tatras easily accessible. For more information, please visit www.liptovarena.sk. A wide choice of leisure time activities, special summer offers at the water park or trips to both sides of Mt. Chopok for children costing 1 EUR attract the attention of all visitors to the best and most popular tourist destination in the region of Liptov. Tatralandia offers 26 water slides and toboggans in the summer, an adrenalin half-pipe, 14 pools with salt sea and clear water, a team of professional animators, a new Medrano restaurant, an entertaining Fun Park, a mini ZOO, a wrecked pirate ship, a special Sports weekend, Polish days or a traditional Summer Beach Party at the end of the summer, which shouldn´t be missed out on. ______________________________________________________________________________ Tatry mountain resorts, a.s. is a top subject in the field of tourism in Central and Eastern Europe, which owns and operates attractive ski resorts and hotels. These include the resort Jasná Low Tatras and the following hotels in the Low Tatras: Wellness hotel Grand Jasná, Boutique Hotel Tri studničky, Chalets Záhradky De Luxe, Mountain Hotel Srdiečko and Million Star Hotel. TMR also owns Aquapark Tatralandia, the largest Slovak water park with all-year operation, which offers a lot of water and other entertainment, a Tropical Paradise – a special tropical hall with sea water, a Fun Park and accommodation in bungalows and suites of the Holiday Village Tatralandia. In the High Tatras, TMR owns and operates resorts Tatranská Lomnica, Starý Smokovec and cooperates the resort of Štrbské Pleso. It also owns the following hotels: Grandhotel Praha Tatranská Lomnica, Grandhotel Starý Smokovec and Hotel FIS Štrbské Pleso. TMR owns 19% of the Melida, a.s. company, which leases and operates the mountain resort Špindlerův Mlýn in the Czech Republic. In Poland, TMR owns the resort of Szczyrk. The company also owns and rents hotels Slovakia, Kosodrevina, Liptov and Ski&Fun Záhradky and Bungalows. More than 190 million Euros were invested by the end of 2013 in the above mentioned resorts, to support development and modernisation. The TMR shares are traded on three European stock exchanges – in Bratislava, Prague and Warsaw. .
Recommended publications
  • Potential and Central Forms of Tourism in 21 Regions of Slovakia

    Potential and Central Forms of Tourism in 21 Regions of Slovakia

    Potential and Central Forms of Tourism in 21 Regions of Slovakia Importance and development priorities of regions The following previews list short characteristics of individual regions in terms of their current state, development possibilities and specific needs. The previews include a list of the most important destinations in the individual regions, the infrastructure that needs to be completed and the anticipated environmental impacts on tourism in the region. These lists are not entirely comprehensive and only include the main elements that create the character of the region as a tourist destination. 1. Bratislava Region Category / relevance Medium-term perspective International Long-term perspective International Sub-region, specific Medium-term perspective - Small Carpathians sub-region (viniculture) location - Bratislava - Senec Long-term perspective - Strip along the right bank of the Danube Type of tourism Long-term incoming foreign tourism over 50%; intensive domestic tourism as well Stay tourism – short-term in incoming as well as in domestic tourism Long–stay waterside tourism only in the summer time; one-day visits – domestic as well as foreign tourism. Transit Forms of tourism - Sightseeing tourism - Business tourism - Summer waterside stays Activities with the - Discovering cultural heritage – Business tourism - Congress/conference tourism – highest long-term Visiting cultural and sport events – Stays/recreation near water – Water sports – Boat potential sports and water tourism - Cycle tourism Position on the Slovak Number
  • The Tatra Mts – Rocks, Landforms, Weathering and Soils Tatry – Skały, Rzeźba, Wietrzenie I Gleby

    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.
  • Possibilities of Increasing Territorial Coverage and Operational Performance of the Tatra Electric Railways

    Possibilities of Increasing Territorial Coverage and Operational Performance of the Tatra Electric Railways

    Available online at www.sciencedirect.com ScienceDirect Procedia Engineering 91 ( 2014 ) 441 – 446 XXIII R-S-P seminar, Theoretical Foundation of Civil Engineering (23RSP) (TFoCE 2014) Possibilities of Increasing Territorial Coverage and Operational Performance of the Tatra Electric Railways Libor Ižvolta, Michal Šmaloa* a Department of Railway Engineering and Track Management, FCE, University of Žilina, Univerzitná 8215/1, 010 26 Žilina, Slovak Republic Abstract In the context of requirement of environmental protection in the Tatra National Park (TANAP) and the territorial coverage solution primarily with ecological railway transport becomes current demand of extending the current network of Tatra Electric Railways (TER) and possibly to connect Slovak and Polish side of the mountains. The basic prerequisite for a functional, safe and attractive operation of the Tatra Electric Railways is modernization of existing lines, because current state causes not only high maintenance costs, but also significantly reduces the speed, safety, reliability and operational efficiency. The paper suggests ways to reconstruct the existing network and upgrade it to achieve the required technical parameters in case of attractiveness of rail transport in the High Tatras. ©© 20142014 The The Authors. Authors. Published Published by Elsevier by Elsevier Ltd. ThisLtd. is an open access article under the CC BY-NC-ND license (Peer-reviewhttp://creativecommons.org/licenses/by-nc-nd/3.0/ under responsibility of organizing). committee of the XXIII R-S-P seminar, Theoretical Foundation of Civil PeerEngineering-review under (23RSP). responsibility of organizing committee of the XXIII R-S-P seminar, Theoretical Foundation of Civil Engineering (23RSP) Keywords: infrastructure; railway; territorial coverage; narrow-gauge lines; operational performance.
  • Features Lifestyle

    Features Lifestyle

    22 Established 1961 Tuesday, February 18, 2020 Lifestyle Features Orava Castle Orava Forest Railway Orava Village Museum he region of Orava lies in the north- property of royals and rich squires. The Enjoy a unique cruise on the Orava Dam hours dive in sulphurous-calcium-magne- Twestern part of Slovakia, on the bor- Thurzos turned the castle into a today’s on comfortable boat that has a capacity of sium water with high iron content. From der with the Poland. The border look. Their renovation of the building made 162 persons. Embarkation on Ship Orava is swimming pools as well as from all over the crossing in environs of the village Oravska the castle become one of very important in port No. 1 near Hotel Goral. During the swimming pool, it is a beautiful view of the Polhora is also the northernmost point of edifices of Renaissance period. In 1800 the voyage you will enjoy beautiful views of most beautiful peaks of the Western Tatras Slovakia. The axis of the region is the castle burnt down and was badly damaged. the Western Tatras and Babia Hora and - Rohace mountain ranges. Sports and Orava river. The last owner Jan Palffy had been rebuild- recognize Slanica Island of Art, where the relaxation pool offers a place for sports- Region possesses almost everything a ing the castle until he died. He focused on boat stops a makes a 25 minutes break. On tourist may wish. The mountain ranges collecting activity - he was buying the the boat there is a buffet with refreshments Mala Fatra, Chocske vrchy and above all objects presented in European auctions.
  • The Tatras – Nappes and Landscapes Tatry – Płaszczowiny I Krajobrazy

    The Tatras – Nappes and Landscapes Tatry – Płaszczowiny I Krajobrazy

    Geoturystyka 2 (13) 2008: 75-87 The Tatras – nappes and landscapes Tatry – płaszczowiny i krajobrazy Ireneusz Felisiak AGH University of Science and Technology; Faculty of Geology, Geophysics and Environmental Protection; Al. Mickiewicza 30, 30-059 Kraków, Poland, e-mail: [email protected] Chabówka porównać papierowe konstrukcje z rzeczywistymi dziełami natury. Zapraszam do lektury i wycieczki w Tatry. Autor. Nowy Targ Słowa kluczowe: płaszczowina, nasunięcie, zapadlisko, półzrąb, Szczawnica Tatry, Karpaty Czarny Dunajec Warszawa Niedzica Introduction Zakopane Kraków The Alpine-type mountain ranges are built of nappes – huge, tabular rock bodies stacked one above the other by tectonic forces during the process of thrusting. Initially, these rock bodies were the successions (series) of sediments laid Abstract: Geological structure of the Tatra Mts is a result down in sedimentary basins, tens of kilometers distant from of long-lasting processes. The key nappes have already been each other. Discovery of nappes proved the shortening of completed some 65 Ma ago. However as a mountain range the Tatras has emerged at the surface only 5 Ma ago, when a piece some fragments of the Earth crust by several hundreds of of continental crust separated from African continent at the kilometers and stimulated the plate tectonics concept. The beginning of Mesozoic era ultimately collided with Europe. Thus, Tatras (Fig. 1) were the second mountain range in the world the crystalline core of the Tatras, which builts also the highest where the nappe structure has been discovered (Maurice crest is a fragment of Africa. This monumental mountains are, Lugeon. Les nappes de recouvrement de la Tatra et l’origine however, not an effect of the overthrusting but they resulted from young, vertical tectonic movements, which are still active and des Klippes des Carpathes.
  • The Natural History of Poland

    The Natural History of Poland

    CORE Metadata, citation and similar papers at core.ac.uk Robert Wiluś Institute of Socio-Economical Geography and Spatial Organization University of Łódź The Natural History of Poland 1. Location Poland is a Central European country that lies at the crossroads of Eastern and Western Europe. Poland shares borders with Lithuania, Bela- rus and Ukraine to the east; Slovakia and the Czech Republic to the south; Germany to the west, and in the north Poland is bordered by Russia and the Baltic Sea. Poland’s surface area of 312.685 sq km ranks eighth in Eu- rope (larger European countries being Russia, Ukraine, France, Germany, Spain, Great Britain and Sweden). Poland is almost an unbroken plain and is roughly circle-like. It measures about 650 km across (both east-west and north-south). Poland is one of nine Baltic Sea States and occupies more than 500 km of the southern Baltic coast. In the south, Poland occupies a strip of the Carpathian and Sudeten Mountains (belonging to the Czech Massif); in the west – the eastern part of the Central European Lowland; and, in the east, the West Russian (or East European) Plain and (North) Ukrainian Upland move in. 2. Topography Poland is a country with varied topography. It can boast almost all Eu- ropean landscape types – the mountains, uplands, lowlands and seacoast. Yet the average elevation of Poland is 173 m, which is more than 100 m 16 Robert Wiluś below the European average. This means that Poland is a markedly flat country. Areas up to 200 m above sea level comprise 75% of the territory, and regions of up to 300 m above sea level – nearly 92%.
  • Hypsometric Factors for Differences in Chemical Composition of Tatra National Park Spring Waters

    Hypsometric Factors for Differences in Chemical Composition of Tatra National Park Spring Waters

    Pol. J. Environ. Stud. Vol. 22, No. 1 (2013), 289-299 Original Research Hypsometric Factors for Differences in Chemical Composition of Tatra National Park Spring Waters Mirosław Żelazny1*, Anna Wolanin1, Eliza Płaczkowska2 1Department of Hydrology, Institute of Geography and Spatial Management, 2Department of Geomorphology, Institute of Geography and Spatial Management, Jagiellonian University, Gronostajowa 7, 30-387 Kraków, Poland Received: 7 May 2012 Accepted: 18 September 2012 Abstract The aim of this study was to verify a hypothesis about the differences in chemical composition of spring waters as determined by hypsometric factors (relief) in the Tatra Mountains. During our research, 1,505 hydro- logical objects were inventoried, but this research was conducted on 872 selected outflows (swamps and springs). Temperature, conductivity, and pH were measured together with discharge in the field. A 0.5 dm3 water sample was taken from each hydrological object. The chemical composition was determined by ion chromatography. The role of hypsometric factors in the formation of chemical composition of spring waters is reflected throughout the TNP as a systematic reduction of the importance of two major hydrochemical class- 2- es of spring waters (HCO3-Ca, HCO3-Ca-Mg) in favor of waters containing a large share of SO4 . The lower and ridge parts of the mountains are characterized by low hydrochemical diversity for the entire Tatra range. Keywords: chemistry, spring, the Tatra Mountains Introduction circulating water, rock-dissolving conditions, and environ- mental elements typical of a given zone, particularly tem- High mountain relief depends on the geological and tec- perature and precipitation regime. The denudation rate in tonic structure and the commonly occurring process of the highest parts of the Tatra Mountains is slow [8].
  • Slovakia 2010 (Lynx & Wolf)

    Slovakia 2010 (Lynx & Wolf)

    PROJECT REPORT Expedition dates: 30 January – 19 February 2010 Report published: March 2011 White wilderness: winter wolf and lynx tracking in the Tatra mountains of Slovakia. BEST BEST FOR TOP BEST WILDLIFE BEST IN ENVIRONMENT TOP HOLIDAY VOLUNTEERING GREEN-MINDED RESPONSIBLE VOLUNTEERING SUSTAINABLE AWARD FOR NATURE ORGANISATION TRAVELLERS HOLIDAY HOLIDAY TRAVEL Germany Germany UK UK UK UK USA PROJECT REPORT White wilderness: winter wolf and lynx tracking in the Tatra mountains of Slovakia Expedition dates: 30 January – 19 February 2010 Report published: March 2011 Authors: Robin Rigg Slovak Wildlife Society Matthias Hammer (editor) Biosphere Expeditions Cover page courtesy of Robin Rigg 1 © Biosphere Expeditions www.biosphere-expeditions.org Abstract Many hunters consider wolves and other carnivores such as lynx as competitors, because they prey on valuable game animals such as red deer and wild boar. As a result hunters tend to overestimate carnivore numbers and cull them intensively. While official game statistics list more than 1,500 wolves in Slovakia, others claim that the annual winter hunting season leaves fewer than 150 individuals. Are wolves being hunted to extinction, as the environmentalists say, or too numerous, as hunters claim? The dispute shows the clear need for reliable, objective methods to estimate numbers of predators. The work of this project aimed to answer that need by designing and testing a methodology for indexing wolf and lynx abundance. In doing so it brought together international volunteers and local people, nature conservationists, foresters, landowners and hunters. This report deals with the 2010 field season, which was conducted in collaboration between Biosphere Expeditions and the Slovak Wildlife Society.
  • Bukowska Janiszewska Mordw

    Bukowska Janiszewska Mordw

    Potentials of Poland Introduction to Socio-Economic Geography of Poland for Foreigners Łódź 2012 citation: Rosińska-Bukowska M., Janiszewska A., Mordwa S. (eds), 2012, Potentials of Poland. Introduction to socio-economic geography of Poland for foreigners, Dep. of Spatial Economy and Spatial Planning, ISBN 978-83937758-1-1, doi: 11089/2690. Review Izabela Sołjan Editors Magdalena Rosińska-Bukowska Anna Janiszewska Stanisław Mordwa Managing editor Ewa Klima (If you have any comments to make about this title, please send them to: [email protected]) Text and graphic design by Karolina Dmochowska-Dudek Cover design by Karolina Dmochowska-Dudek Książka dostępna w Repozytorim Uniwersytetu Łódzkiego http://hdl.handle.net/11089/2690 ISBN: 978-83-937758-1-1 © Copyright by Department of Spatial Economy and Spatial Planning, University of Łódź, Łódź 2012 TABLE OF CONTENTS 1. INTRODUCTION ......................................................................................................... 9 (Editors) 2. POTENTIAL OF THE POLISH ENVIRONMENT ................................................. 10 (Sławomir Kobojek) 2.1. Location – area – spatial resources .............................................. 10 2.2. Resources of the Polish land – geological composition – minerals12 2.2.1. Geological structures in Poland – tectonic units ................... 12 2.2.2. The Quaternary and the Pleistocene – the Polish ice age ... 18 2.3. Diversity of geomorphological landscape – topographic relief of Poland ..........................................................................................
  • Preliminary Palaeomagnetic Study of the High Tatra Granites, Central Western Carpathians, Poland

    Preliminary Palaeomagnetic Study of the High Tatra Granites, Central Western Carpathians, Poland

    Geological Quarterly, 1999, 43 (3): 263-276 Preliminary palaeomagnetic study of the High Tatra granites, Central Western Carpathians, Poland Jacek GRABOWSKI, Aleksandra GA WI;;DA Grabowski J., Gaw\1da A. (1999) - Preliminary palaeomagnetic study of the High Tatra granites, Central Western Carpathians, Poland. Geo!. Quart., 43 (3): 263-276. Warszawa. Variscan granitoids ofthe High Tatra Mts. in Poland were the subject of palaeomagnetic, petrographical and rock magnetic investigations. The sampled rocks were granodiorites, rarely tonalites showing weak hydrothermal alterations (chloritisation, epidotisation). 3 I hand samples from 7 localities were palaeomagnetically investigated. Stable palaeomagnetic directions of Late Palaeozoic age were isolated in four localities (mean direction: D = 193", I = IT, U95 = 12, k = 59, palaeopole: 4"E, 31 OS). The stable magnetisation resides in hematite. This mineral occurs in hematite-ilmenite intergrowths that exsolved in high temperatures (670-720"C) and as secondary hematite of hydrothermal origin. Because of heterogeneity of magnetic carriers it is possible that the characteristic magnetisation is shifted in time between localities. Question of tectonic tilt of the High Tatra granite is discussed. The age of characteristic magnetisation based on palaeoinclination estimations apparently fits the isotopic cooling age of the intrusion (330-300 Ma) iftectonic correction is not applied. The palaeopole is situated between the European and African Apparent Polar Wander Paths (APWP) and could be matched with both reference curves. After tectonic correction the palaeopole could be matched only with the African APWP at the point ca. 360 Ma. In this case the magnetisation related to the high temperature hematite would preceed the cooling ages recorded by Ar-Ar method.
  • Tying Together Textures, Temperatures, and Timing in the Western Tatra Mountains, Slovakia

    Tying Together Textures, Temperatures, and Timing in the Western Tatra Mountains, Slovakia

    TYING TOGETHER TEXTURES, TEMPERATURES, AND TIMING IN THE WESTERN TATRA MOUNTAINS, SLOVAKIA A thesis submitted to the Kent State University Graduate College in partial fulfillment of the requirements for the degree of Master of Science by Jenna C. Hojnowski December, 2010 Thesis written by Jenna C. Hojnowski B.A. State University of New York at Geneseo, 2008 M.S. Kent State University, 2010 Approved by , Advisor Daniel Holm , Chair, Department of Geology Daniel Holm , Dean, College of Arts and Sciences John R.D. Stalvey ii Table of Contents List of Figures ...................................................................................................................vii List of Tables, Equations, and Appendices………………………………………..…..viii Acknowledgments ..............................................................................................................x Abstract . .............................................................................................................................1 1. Introduction ...................................................................................................................3 Tectonic Background of the Western Tatra Mountains...........................................5 Structural Features……………………………………………………………….10 P-T-t Paths……………………....................................................................…….11 Geochronology Data…………………………………………………………....13 2. Petrographic Fabrics.....................................................................................................14 Optical
  • Preliminary Palaeomagnetic Study of the High Tatra Granites, Central Western Carpathians, Poland

    Preliminary Palaeomagnetic Study of the High Tatra Granites, Central Western Carpathians, Poland

    Geological Quarterly, 1999, 43 (3): 263-276 Preliminary palaeomagnetic study of the High Tatra granites, Central Western Carpathians, Poland Jacek GRABOWSKI, Aleksandra GA WI;;DA Grabowski J., Gaw\1da A. (1999) - Preliminary palaeomagnetic study of the High Tatra granites, Central Western Carpathians, Poland. Geo!. Quart., 43 (3): 263-276. Warszawa. Variscan granitoids ofthe High Tatra Mts. in Poland were the subject of palaeomagnetic, petrographical and rock magnetic investigations. The sampled rocks were granodiorites, rarely tonalites showing weak hydrothermal alterations (chloritisation, epidotisation). 3 I hand samples from 7 localities were palaeomagnetically investigated. Stable palaeomagnetic directions of Late Palaeozoic age were isolated in four localities (mean direction: D = 193", I = IT, U95 = 12, k = 59, palaeopole: 4"E, 31 OS). The stable magnetisation resides in hematite. This mineral occurs in hematite-ilmenite intergrowths that exsolved in high temperatures (670-720"C) and as secondary hematite of hydrothermal origin. Because of heterogeneity of magnetic carriers it is possible that the characteristic magnetisation is shifted in time between localities. Question of tectonic tilt of the High Tatra granite is discussed. The age of characteristic magnetisation based on palaeoinclination estimations apparently fits the isotopic cooling age of the intrusion (330-300 Ma) iftectonic correction is not applied. The palaeopole is situated between the European and African Apparent Polar Wander Paths (APWP) and could be matched with both reference curves. After tectonic correction the palaeopole could be matched only with the African APWP at the point ca. 360 Ma. In this case the magnetisation related to the high temperature hematite would preceed the cooling ages recorded by Ar-Ar method.