Features Lifestyle

Total Page:16

File Type:pdf, Size:1020Kb

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. He possibilities and toilets. Zapadne Tatry - Rohace are the paradise bequeathed a valuable collection based on Boat tour is ideal for school trips and as for hikers, cyclists and visitors. Lovers of natural surrounding with rich set of art and an enrichment of programs for corporate hiking like to climb the Rohace Mountain history objects. The last and most complex events, as well as trips for pensioners. It is and to the passes over the west Tatra ridge. renovation of the castle took place as late possible to pre-order meals, snack or folk Walks in environs of Oravice or ascents to as in 1953 -1968. music. The cruise lasts 1.5 hours including a the Babia hora or Velky Choc peaks are 25 minute break to Slanica Island of Art. also among the favorites. Orava Forest Railway Cruises take place from May until the end Oravsky Podzamok - area: Kubinska of October. Hola - region: Orava, Type of interest: National monuments AQUARELAX Dolny Kubin The unique technical monument of Dolny Kubin - area: Kubinska Hola - Orava Forest Railway is one of the very region: Orava Type of interest: few narrow-gauge switchback railways Aquaparks & Thermal swimming pools preserved to this day. Waterpark - AquaRelax Dolny Kubin is Its original purpose was to transport located in the center of Dolny Kubin in minded visitors who can swim here, while AQUARELAX Dolny Kubin timber from inaccessible mountainous ter- Orava region on the north of Slovakia. the second part of the pool with water rain, however, now it is one of the most Near the water park there are stadiums attractions is reserved for relaxing. popular tourist attractions of the Orava (football and winter), a playground with Artificial waves in thermal pool are great region. The sightseeing trains of Orava artificial grass, a ski resort Kubinska hola. water attraction in this thermal resort. Forest Railway depart from Tanecnik The dominant feature of the resort, Other water attractions of the relaxation Station, near the village of Oravska Lesna. Water World comes with water slides, part include the massage jets, massage The station is connected with the village whirlpools, massage showers and other benches and water mushroom. The length by a 6 km asphalt side-road. At the station, water attractions. On a glazed patio there of the swimming pool has a length of 25 free parking is provided. The train depot, is prepared plenty of sun deck chairs. The meters. train ticket office, souvenir shop, exhibition swimming pool area includes a large multi- You can find here also a children’s pool documenting the evolution of the railway, functional swimming pool, children’s pool with water mushroom and two children’s children playground or peacock aviary are with a slide and relaxation pool with slides. Especially in bad weather you surely Orava dam Winter months in Orava are equally also located at the station. wheelchair access. For adrenaline there are appreciate the connection between several charming. Down-hill skiing in Zuberec and After the ticket purchase, passengers 2 slides that are 40 and 71 meters or dou- outdoor pools with the inner ones. There its environs including Kubinska hola or take a seat on a motorized draisine pulled ble slide with a length of 12.7 meters. The are also bubble pools in the inner or cool- cross-country ski tracks through the by a motor locomotive. The train then waterpark Dolny Kubin features also ing pool. CafÈ, bistro, bar and plenty of sun Skorusinske vrchy and Oravska Magura starts a 15 - 20 minute ride to the peak sta- Children’s Paradise Fun Park with inflatable loungers are also part of the thermal park mountains provide an unforgettable expe- tion at the Beskyd Saddle, located 3 km attractions, playgrounds and slides. area. By entry you will get a chip bracelet, rience to skiers of Slovakia and from from the Tanecnik Station. Here, 935 which records how much consumption and abroad. Orava also has architectural mon- meters above the sea level, the train takes a Meander Thermal Park Oravice which serves to open the locker. You pay uments in every commune. The most valu- break and the passengers can enjoy the Oravice - area: Rohace, Thermal bath on departure. able of them is the Castle of Orava tower- magnificent view of Orava nature from a Oravice - region: Orava Type of interest: ing above the eponymous river. scenic tower. Goral Wooden Cottage host- Aquaparks & Thermal swimming pools Orava Village Museum Samples of old popular architecture can ing an exhibition dedicated to the Goral Meander Oravice Thermal Park is situ- Zuberec - area: Rohace, , Western be found in villages of Orava. They are also culture of Orava is also there to visit. Then, ated in the north of Slovakia in the Orava Tatras - region: Orava Type of interest: concentrates in the monument reserve of the train heads back to the valley. Duration region on the north-western outskirts of Open air museums and folk architecture popular architecture in Podbiel and Open- of the whole trip is 1 hour 10 minutes. the Western Tatras. It is located 6 km from Orava Village Museum in Zuberec Air Museum in Zuberec. The most impor- the center of the village Vitanova and 13 located in beautiful natural surroundings of tant samples of old sacral architecture are Sightseeing cruises on km from the Polish border. Rohace Mountains tries to illustrate a living wooden churches in Tvrdosin, Lestiny and Orava dam, Orava ship Water Park, where you can enjoy swim- of people in Orava region in the past. Istebne. The best place for recreation next Namestovo - area: Orava reservoir, ming pools with natural thermal water is Visitors can see more than 50 houses and to water is the dam Oravska priehrada. Orava Beskids, Slanicka Osada - region: open all year. Highly mineralized water ris- several other buildings of folk architecture. Orava, Type of interest: Sightseeing es from a depth of 1,611 meters. Houses are decorated and there are kept Orava Castle Cruises Vacationers can anytime of the year till late pets here and in the summer typical crops Oravsky Podzaamok - area: Kubinska are grown here, too. Hola - region: Orava, Type of interest: The museum is divided into five parts, Castles, chateaus, National monuments Meander Thermal Park Oravice which the form of settlements and villages Large and well-preserved castle is tow- are presented in. Towering above the ering on a steep limestone hill right by the whole village, the wooden Gothic church village at 112 meters over the level of the from the early 15th century is a real gem of river Orava, about 10 kilometers from the open-air museum. Orava Village Dolny Kubin. The castle is a national cul- Museum is open to visitors year round. ture heritage. During the tourist season (summer and Orava Castle, before the center of Orava winter) various interesting programs are area, was founded in the 13th century on held in its area. the place of older settlement. The oldest historical notes of it come back to the year before 1235 when it had been the king’s property. Orava Castle together with the surrounded Orava lands were alternately in Xin and Shuan Shuan are the main vulnerable species. Xattractions at the Chapultepec zoo in As Ying Ying and Pe Pe arrived in Xin Xin, a female giant panda (Ailuropoda melanoleuca) born in captivity in Mexico City but what makes them Mexico before China changed its policy, Mexico, rests at the Chapultepec zoo in Mexico City. — AFP photos truly unique, zoo officials say, is that Xin Xin and Shuan Shuan will stay in they’re the only giant pandas in the world Mexico. “With that, Mexico became the not owned by China. They were born in first country outside of China to have had captivity in Mexico and although they have a successful natural reproduction of pan- Chinese names, “they belong to Mexico,” das outside their natural habitat, in cap- Rafael Tinajero, a manager at the zoo, told tivity conditions,” said Tinajero.
Recommended publications
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Chapter Ii the Development of China Panda Diplomacy A
    CHAPTER II THE DEVELOPMENT OF CHINA PANDA DIPLOMACY This chapter discusses the development of China Panda Diplomacy. The researcher will explain the symbolism of Panda. In the other hand, the researcher will explore the stages of Panda Diplomacy and mentioning the step of the giant Panda loan breeding process. Last but not least, the writer will mention the countries that received the Panda. A. THE SYMBOLISM OF PANDA China was known as one of the oldest ancient in the earth. Besides its famous landmark of the Great Wall, China owns a cute animal named the Giant Panda, Ailuropoda Melanoleuca (Xianmeng Qiu, Susan A. Mainka, 1993). From the Chinese perspective, Panda is a symbol of peace and friendship. They have a gentle temperament and aren’t known for attacking others. This animal is also believed to have powers to combat evil spirits (Wang, 2017). There some province in China assumes that giant panda is a symbol of luck. The color contrast of giant panda equated as the mythology of Yin and Yang or means as equality that reflected the equality of life. The Pandas are seen as a symbol of co- operation between China and the receiving countries (Hinderson, 2017). Scholars acknowledge that culture is as important a politics, military, and economic as an element in influencing the development of a nation’s foreign policy (Hu, 2013). Buckingham, et al. (2013) stated that the Panda represents a fascinating soft-power resource. The panda offers a softer animal symbol for China compared to those of its past – the red dragon- and it is dealing with the natural beauty of the country.
    [Show full text]
  • 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.
    [Show full text]
  • 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%.
    [Show full text]
  • 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].
    [Show full text]
  • 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.
    [Show full text]
  • 2019 Breeding and Management Recommendations and Summary of the Status of the Giant Panda Ex Situ Population
    Report to: Chinese Association of Zoological Gardens (CAZG) Giant Panda Office, Department of Wildlife Conservation, State Forestry Administration Giant Panda Conservation Foundation (GPCF) 2019 Breeding and Management Recommendations and Summary of the Status of the Giant Panda Ex Situ Population 8 - 9 November 2018 Chengdu, China Submitted by: Kathy Traylor-Holzer, Ph.D. IUCN SSC Conservation Planning Specialist Group Jonathan D. Ballou, Ph.D. Smithsonian Conservation Biology Institute/ Species Conservation Toolkit Initiative Chinese translation provided by: Yan Ping, Giant Panda Conservation Foundation Sponsored by: Chengdu Research Base of Giant Panda Breeding Chinese Association of Zoological Gardens Executive Summary This is a report on the meeting held 8-9 November 2018 in Chengdu, China to update the analysis of the ex situ population of giant pandas and develop breeding recommendations for the 2019 breeding season. This is the 17th annual set of genetic management recommendations developed for giant pandas. The current ex situ population of giant pandas consists of 548 animals (249 males, 299 females) located in 93 institutions worldwide. As of 8 November181 animals were transferred in 2018, including 4 from China to institutions outside of China and 4 between institutions in Canada. The genetic status of the population is currently healthy (gene diversity = 97.59%), with 58 founders represented and another 4 that could be genetically represented if they were to produce living offspring. There are 9 living inbred animals with estimated inbreeding coefficients > 6% and another 39 animals with lower levels of inbreeding. There are 66 giant pandas in the studbook that are living or have living descendants with sires that are uncertain (due to natural mating and/or artificial insemination with multiple males).
    [Show full text]
  • 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 ..........................................................................................
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]