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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. -
Knowledge and Development of Modern Military Structures
Dipartimento di Progettazione dell’Architettura (DPA) KNOWLEDGE AND DEVELOPMENT OF MODERN MILITARY STRUCTURES Luoghi e architetture della transizione: 1919 – 1939. I sistemi difensivi di confine e la protezione antiaerea nelle città. Storia, conservazione e riuso Sites and architectural structures of the transition period: 1919 – 1939. Border defense systems and air raid protection in the cities. History, conservation and reuse II Congresso Internazionale a cura di Maria Antonietta Breda 2nd International Congress by Maria Antonietta Breda 27 – 28 Novembre 2012 – ore 9.00 – 18.30 Politecnico di Milano – via Durando 10 Milano – Campus Bovisa – Aula Castiglioni edificio PK November 27-28, 2012 – 9:00 AM – 6:30 PM Politecnico di Milano – Via Durando 10, Milan –Bovisa Campus – Castiglioni Room PK building Diretta video: Napoli Underground Channel – Live video: Napoli Underground Channel http://www.napoliunderground.org/it/component/content/article/58-nug-channel.html PRESENTAZIONE 1919 – 1939. La Grande Guerra si è conclusa, ma i trattati per la pace non diminuiscono le disparità economiche preesistenti tra gli Stati. La storiografia dell’epoca riconosce che proprio in quei patti vi è la genesi del secondo conflitto mondiale. Nonostante da più parti si invochi la pace e si confidi nelle capacità diplomatiche per risolvere le crisi tra gli stati, sul territorio europeo tutte le nazioni rafforzano e completano i propri sistemi difensivi di confine. Inoltre, coscienti che l’arma aerea, già usata durante il primo conflitto, potrebbe trasformare le città in campi di battaglia, si impongono provvedimenti per la protezione collettiva della popolazione civile delle grandi città e dei centri vitali. La guerra chimica è definita “arte demoniaca dei veleni sottili e silenziosi” (Djalma Juretigh 1932). -
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. -
On the Rapallo Border
foto: jana jocif STORY WITH A VIEW – ON THE RAPALLO BORDER Soriška planina, mountain beauty, surounded with spectacular views, offers all year round activities for all generations. Rapallo Border Over the peaks of the Soriška planina highland once ran the old border – the Rapallo border, which marked the lives of the locals and cut nearly a third of Slovenians from their motherland. On the theme tourist trail you can have a look at many remains of the Italian defensive fort system – the Alpine wall, well-preserved barracks, a mule track and an observation dome. Only a week or so after the end of the Great War and the signing of the cease-fire between the Austro-Hungarian Empire and Italy (4 November 1918), the first Italian soldiers settled in the Upper Bača Valley and the neighbouring Sorica community. Without any resistance whatsoever, they occupied the majority Slovenian territory and stayed there until the capitulation of Italy in 1943. But the border between the Kingdom of Italy and the newly founded Kingdom of SHS (Kingdom of Serbs, Croats and Slovenes) was finalized more than two years later (12 November 1920), when the long awaited peace treaty was signed in the Italian city of Rapallo following lengthy negotiations. The towns on the Primorska side or in the valley of the river Bača thus went to Italy, while Sorica and the surrounding villages were annexed to the Kingdom of SHS. foto: jana jocif How does a guided Rapallo border tour look like? With our experienced guides you will ascent to Soriška planina peaks with chair- lift Lajnar and than walk on mountain tops and see the remains of military baracks, mule tracks and observation domes. -
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. -
Of Napoleon 100 Years After His Downfall
In the Path of Napoleon 100 Years After His Downfall * \ ^ Crossing the Alps by the Great St. Bernard Bv JAMES MORGAN Napoleon’s secret passage of the Alps six months after he became the first consul of France and his un- heralded descent from the clouds upon the rear of an Austrian army as it was about to invade France, was not only one of the boldest feats of his military career, but also one of his most important and decisive move- ments. Mr. Morgan tells today the dra- matic story of the celebrated march of more than 30,000 men over the Al- pine heights and sketches his own journeys :n “The Path of Napoleon” through the pass of the great St. Bernard. A visit to the house Napo- *' leon gave his guide and to the famous hospice on the summit of the lofty mountain, where, amid eternal snows, the good monks and their faithful dogs after a thousand years still keep watch over the storm-beaten way- fa rers. DATES AND EVENTS—AGE 30. April 5. 1880—Austrian army under Me* las opened its campaign in Italy. April 10. 1800—Mclas shut French army tinder Massena within the walls of J -r) 1 Genoa. 25. 1880—Austrian under de April army or rzzr y^zrs, Kray opened its campaign in Germany. *~Zzrr Snvrrs fjj May 0, 1800—De Kray driven across JV/7VZ Sr/irczr or Sr. 23rz?Mnrz> ■ the Danube by French rnder Moreau. May 6, 1800—Napoleon left Paris, desti- nation unknown. May 13, 1800—Reviewed his army at Lau- sanne. -
The Tatra National Parks
Profoundly National Yet Transboundary: The Tatra National Parks Bianca Hoenig The Tatra Mountains are situated on the Polish-Slovak border and form the highest part of the Carpathian arc. They are protected by two neighboring national parks, established in 1949 and 1954 in Czechoslovakia and Poland respectively. The location of these mountains within an empire and on a national borderland shaped the history of these parks. The lake Morskie Oko (Eye of the Sea) was the subject of a long-lasting dispute over property rights, giving rise to a national struggle for the Poles. It was finally settled by an international court of arbitration in Graz in 1902, in favor of the Polish side. This work (Morskie Oko Pond in Tatra Mountains, Poland, by Tamerlan ), identified by Wikipedia , is free of known copyright restrictions. This work is licensed under a Creative Commons Public Domain Mark 1.0 License . The lake Morskie Oko (Eye of the Sea) was the subject of a long-lasting dispute over property rights, becoming a focal point of the Polish national struggle. An international court of arbitration in Graz settled the conflict in favor of the Polish side in 1902. In 1888, the priest Bogusław Królikowski urged for the creation of a national park in the Polish Tatras, named after the distinguished Polish poet Adam Mickiewicz. The former Polish Commonwealth had been partitioned by the Central European empires at the end of the eighteenth century. Since that time, the whole Tatra Mountains belonged to the Habsburg Empire as Slovakia was part of the Kingdom of Hungary. -
Stable Isotopes in Lakes of the High Tatra Mountains, Western Carpathians, Slovakia
STABLE ISOTOPES IN LAKES OF THE HIGH TATRA MOUNTAINS, WESTERN CARPATHIANS, SLOVAKIA J. MICHALKO*, D. BODIS*, P. MALIK, K. MARHEVKOVA**, S. SCHERER* * Geological Survey of Slovak Republic, ** Faculty of Natural Sciences, Comenius University Bratislava, Slovakia XA0100612 Abstract Data of oxygen, hydrogen and sulphate sulphur stable isotopes from the lakes of the Vysoke Tarry Mts., acquired in the framework of IAEA No. 8675/RB project "Stable isotopes in lakes of High Tatra mountains, Western Carpathians, Slovakia" represent the first set of this kind information on the territory of Slovakia. Moreover a complete set of chemical composition of waters was taken and compared to preceding results and contemporary state of acidification was evaluated. Values of studied chemical compounds respond to their source - initial precipitation waters and bedrock character with influence of biochemical processes. Acidification is due to inactive geological background (granites), high contribution of SOX and NOX from atmospheric deposition and low buffering ability of soil. Acidification of lakes is lowered from 1980 and is approaching to level before acidification, probably as consequence of industry crisis in Eastern Europe after 1989. Water samples from the Furkotska dolina valley water system follow the MWL with natural trend of increasing content of heavy isotopes with lowering altitude. In depth profiles of single lakes' isotope composition does not change - due to natural conditions during sampling campaigns (spring and fall homothermy?), all waters are meteoric in origin without signs of evaporation. Water of the Strbske pleso lake is enriched to heavy isotopes, all samples fit an evaporation line. This could be explained by longer residence time of water, or by the recharging from the last phases of the snowmelt.