Pieniny- the Great Little Mountains
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Karpaty Wewnętrzne – Tatry, Podhale, Pieniny
Karpaty Wewnętrzne – Tatry, Podhale, Pieniny Treści zawarte w tym temacie nie występują w obecnej podstawie programowej. Karpaty Wewnętrzne – Tatry, Podhale, Pieniny Karpaty Wewnętrzne w znaczący sposób odróżniają się od Karpat Zewnętrznych. Tatry są najwyższym pasmem w całych Karpatach, wyraźnie górującym nad okolicą. Pieniny również górują nad okolicą, ale tylko dzięki znacznym wysokościom względnym. Z kolei Podhale jest rozległym, wydłużonym obniżeniem terenu o płaskim dnie. Źródło: ToSter (hp://commons.wikimedia.org), licencja: CC BY-SA 3.0. Już wiesz jakie są główne pasma Karpat; w jaki sposób przebiegają fałdowe ruchy górotwórcze; w jaki sposób lodowce górskie ukształtowały rzeźbę terenu; jak odczytywać dane z wykresów klimatycznych; jaki jest układ pięter roślinnych w Tatrach. Nauczysz się opisywać genezę powstania Tatr, Podhala i Pienin; wskazywać różnice między krajobrazami Tatr Wysokich i Tatr Zachodnich; wyjaśniać, co to jest przełom Dunajca; charakteryzować klimat, hydrografię, gleby i roślinność Karpat Wewnętrznych. 1. Położenie, budowa geologiczna i rzeźba Karpat Wewnętrznych Karpaty Wewnętrzne zajmują niewielki obszar na południu Polski i na północy Słowacji. Pasmo Tatr ma około 50 km długości i do 20 km szerokości. Rozciąga się w kierunku wschód‐zachód, wzdłuż granicy państwowej, przy czym większa ich część znajduje się po stronie słowackiej – w Polsce tylko 160 km2 z 715 km2 ogólnej powierzchni gór. Tatry dzielą się na Tatry Zachodnie oraz Tatry Wschodnie, a granicą między nimi jest Przełęcz Liliowe i Dolina Suchej Wody. W skład Tatr Wschodnich wchodzą przede wszystkim Tatry Wysokie, a ponadto Tatry Bielskie leżące w całości na Słowacji. W Tatrach Wysokich po stronie słowackiej znajduje się najwyższy szczyt całych Karpat – Gerlach o wysokości 2655 m n.p.m. -
The Šariš Transitional Zone, Revealing Interactions Between Pieniny
Swiss Journal of Geosciences (2018) 111:245–267 https://doi.org/10.1007/s00015-017-0297-9 (0123456789().,-volV)(0123456789().,-volV) The Sˇarisˇ Transitional Zone, revealing interactions between Pieniny Klippen Belt, Outer Carpathians and European platform Edyta Jurewicz1 Received: 4 January 2017 / Accepted: 21 December 2017 / Published online: 16 January 2018 Ó The Author(s) 2018. This article is an open access publication Abstract The Pieniny Klippen Belt (PKB) is a narrow structure delineating the boundary between the Central and Outer Carpathians. It is built of nappes stacked during the Cretaceous and Paleocene and then re-folded in the Miocene during the formation of the Outer Carpathian overthrusts. The internal structure of the PKB at the Polish/Slovakian border first formed during northward nappe thrusting processes, which were most intense at the turn of the Cretaceous to the Paleocene. A secondary factor is the change in strike of the PKB turning from W–E to WNW–ESE, associated with dextral strike-slip faulting in the Carpathian basement (North-European Platform). These NNW-SSE oriented strike-slip fault zones, broadly parallel to the Teisseyre-Tornquist Zone, are responsible for the segmentation of the down-going plate, which influenced the sub- duction and collision between the North-European Platform and the Central Carpathian Block. Among them, the most important role was played by the Krako´w—Myszko´w Fault Zone separating the Małopolska and Upper Silesian blocks in the Carpathian foreland. Shifts and interactions between the neighboring Pieniny and Outer Carpathian basins—during contemporaneous sedimentation and deformation—resulted in a difficult-to-define, transitional zone. -
They Fought for Independent Poland
2019 Special edition PISMO CODZIENNE Independence Day, November 11, 2019 FREE AGAIN! THEY FOUGHT FOR INDEPENDENT POLAND Dear Readers, The day of November 11 – the National Independence Day – is not accidentally associated with the Polish military uni- form, its symbolism and traditions. Polish soldiers on almost all World War I fronts “threw on the pyre their lives’ fate.” When the Polish occupiers were drown- ing in disasters and revolutions, white- and-red flags were fluttering on Polish streets to mark Poland’s independence. The Republic of Poland was back on the map of Europe, although this was only the beginning of the battle for its bor- ders. Józef Piłsudski in his first order to the united Polish Army shared his feeling of joy with his soldiers: “I’m taking com- mand of you, Soldiers, at the time when the heart of every Pole is beating stron- O God! Thou who from on high ger and faster, when the children of our land have seen the sun of freedom in all its Hurls thine arrows at the defenders of the nation, glory.” He never promised them any bat- We beseech Thee, through this heap of bones! tle laurels or well-merited rest, though. On the contrary – he appealed to them Let the sun shine on us, at least in death! for even greater effort in their service May the daylight shine forth from heaven’s bright portals! for Poland. And they never let him down Let us be seen - as we die! when in 1920 Poland had to defend not only its own sovereignty, but also entire Europe against flooding bolshevism. -
Geodynamical Studies of the Pieniny Klippen Belt in 1994 – 2011
Geophysical Research Abstracts Vol. 14, EGU2012-2528, 2012 EGU General Assembly 2012 © Author(s) 2012 Geodynamical studies of the Pieniny Klippen Belt in 1994 – 2011 J Walo, A. Pachuta, D. Próchniewicz, T. Olszak, R. Szpunar, and M. Barlik Faculty of Geodesy and Cartography, Warsaw University of Technology, Poland ([email protected]) The Pieniny Klippen Belt (PKB), which is situated in Southern Poland, is one of the main fault zones on the boundary of the outer and inner Carpathians. The geodynamical investigations which have been carried out since 1960s indicate that PKB demonstrates neo-tectonic activity. In 1994, the GPS measurements were included in the horizontal network and this epoch was used as a reference epoch for the further studies. In 1995-2001, when the measurements were interrupted, the Dunajec river dam and the water reservoirs in Czorsztyn and Sromowce Wyzne˙ have been built. This has created a new aspect in investigations related to the effect of tectonic movements on the dam. Taking that into account, the study was revived and the geodynamical investigations, which contain GPS, relative gravimetric and leveling observations, have been carried out annually, at the beginning of September, from 2001. In 2008, also the absolute gravity measurements (using FG-5 gravimeter) at three stations located in PKB and adjacent geological structures were included in the study. In this paper the result of horizontal displacement in the PKB area obtained from GPS measurement as well as gravity changes obtained from relative and absolute measurements in 1994-2011 period are presented and yields linear trend of horizontal displacement in north-east direction less than 1 mm/year.. -
Early Stages of Structural Evolution of the Carpathian Klippen Belt (Slovakian Pieniny Sector)
Mineralia Slovaca, 44 (2012), 1 – 16 Web ISSN 1338-3523, ISSN 0369-2086 Early stages of structural evolution of the Carpathian Klippen Belt (Slovakian Pieniny sector) DUšan Plašienka Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University, Mlynská dolina, SK-842 5 Bratislava, Slovak Republic; [email protected] Abstract The Pieniny Klippen Belt (PKB) is a distinctive, suture-like tectonic zone that separates the External Carpathian Tertiary accretionary wedge (Flysch Belt) and the Cretaceous thrust stack of the Central Western Carpathians. Whereas the lithostratigraphy of various PKB units is fairly well-known, its tectonic evolution and development of the peculiar “klippen tectonic style” is a subject of very different opinions. We present structural data from the Pieniny sector of the PKB in NE Slovakia, which indicate that: ) distinction should be made between the “blocky” klippen and the “ribbon” klippen, since locally considerable reorientation of the original attitudes of structural elements is presumed for the former ones; 2) bedding poles of the “ribbon” klippen (Jurassic to Neocomian limestones and radiolarites) plot in a girdle in NWN–SES to N–S direction, while those of the klippen matrix (mid-Cretaceous to Lower Eocene marlstones, shales and sandstones) are shifted clockwise; 3) occasionally, the bedding-perpendicular cleavage and buckle folds record an early layer-parallel shortening, which are clearly older than brittle transpression-related faults and fractures – therefore they are interpreted as initial detachment and thrusting deformation elements that are likely related to the nappe-forming processes in the PKB; 4) fold axes, β-intersections of mesoscopic fold limb pairs, as well as a part of the bedding/ cleavage intersections are all oriented in the SW–NE direction (mean 55°), i.e. -
XVIII INTERNATIONAL MYELOMA WORKSHOP KRAKÓW 2021, POLAND (Proposed Term 14 – 19.09.2021)
APPLICATION FOR ORGANIZATION OF: XVIII INTERNATIONAL MYELOMA WORKSHOP KRAKÓW 2021, POLAND (proposed term 14 – 19.09.2021) Local Congress Organizers MD PhD, Prof. Aleksander B. Skotnicki Head of the Chair and Departament of Hematology Jagiellonian University Collegium Medicum MD PhD, Assoc. Prof . Artur Jurczyszyn Ms. Agnieszka Grzesiak President of the Myeloma Treatment Fundation Centre JORDAN Congress Bureau Chairman of the Krakow Branch Polish Society of Haematology and Blood Transfusion Address: 22/2 Sobieskiego St, 31-136 Krakow Jagiellonian University Medical College Department of Hematology (PCO Professional Congress Organiser) Address: 17, Kopernika St, 31-501 Krakow Address: 22/2 Sobieskiego St, 31-136 Krakow T: + 48 601 53 90 77 T: + 48 341 46 40 , e-mail: [email protected] e-mail: [email protected], http://szpiczak.org/en/ http://kongres.jordan.pl/en International Myeloma Workshop 2021 1 Table of Contents: Kraków 2021 ? Yes, of course ! …………………………..pages 3-4 Traveling to Cracow…………………………..………………..page 5 Scientific Committee and Partners………………………pages 6-7 Congress Venue ICE …………………………………………….page 8 Hotels in Krakow …………………………………………………pages 9-10 Opening and Closing Ceremony…………………………..page 11 Exhibition Space ………………………………………………… pages 12-13 Welcome Reception…………………………………………… page 14 Gala Dinner……………………………………………………….. .pages 15-17 Social Programme……………………………………………….pages 18-22 General Information about Poland…………………….pages 23-25 International Myeloma Workshop 2021 2 Kraków 2021 ? Yes, of course ! KRAKÓW is the second largest and one of the oldest cities in Poland situated on the Vistula river in the south of Poland. For many years Krakow was the royal capital of Poland until 17 th c. Krakow - an architectural pearl amongst Polish cities on the UNESCO World Cultural Heritage list with its architectural complex of the Old City which has survived unchanged since the Middle Age It is still the city where, like ages ago, one can walk along the Royal Route , starting from the city gates and arriving at the Royal Castle Hill . -
Improved Tools for River Flood Preparedness Under Changing Risk - Poland
7th Study Conference on BALTEX, Borgholm, Sweden, 10-14 June 2013 Improved tools for river flood preparedness under changing risk - Poland Zbigniew W. Kundzewicz Institute of Agricultural and Forest Environment, Polish Academy of Sciences, Poznań, Poland and Potsdam Institute for Climate Impact Research, Potsdam, Germany - Changing flood risk in Poland - Improved tools for river flood preparedness - Changing flood risk in Poland - Improved tools for river flood preparedness River flooding in Poland River flooding is the most destructive natural peril in the Baltic Sea Basin in general and in Poland in particular. Flood risk and preparedness became matters of broad concern, following the dramatic floods in Poland in 1997 and 2010, when dozens of people were killed, national flood losses reached the level of billions of Euros and the topic made it to cover stories. Floods in PL, May-June 2013 IAHS Special Publication 10 (April 2012) ISBN ISBN 978-1- 907161-28-5 (Paperback); 516 + xvi pages 10 12 14 0 2 4 6 8 Dartmouth Flood Observatory. Source: et al. (2012) Kundzewicz Dartmouth Flood Observatory. Increasing number of large floods, according tothedata in 1985 1986 1987 1988 1989 1990 1991 1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004 2005 2006 2007 2008 2009 y = 0.3123x + 2.46 y = 0.2608x + 0.33 R R 2 2 = 0.4339 = 0.6012 Magnitude=>5 Severity=>1.5 Trend in number of days with precipitation in excess of 30 mm, and (b) trend in maximum 5-day precipitation, 1971–2002 (after Lorenc & Olecka, 2006). Catastrophic floods of regional extent in Poland: from 1946 to 1970; from 1971 to 1990; from 1991 to 2010; from 1946 to 2010. -
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. -
Neotectonics of the Polish Carpathians in the Light of Geomorphic Studies: a State of the Art
Acta Geodyn. Geomater., Vol. 6, No. 3 (155), 291-308, 2009 NEOTECTONICS OF THE POLISH CARPATHIANS IN THE LIGHT OF GEOMORPHIC STUDIES: A STATE OF THE ART Witold ZUCHIEWICZ Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, A. Mickiewicza 30, 30-059 Kraków, Poland *Corresponding author‘s e-mail: [email protected] (Received January 2009, accepted March 2009) ABSTRACT Neotectonics of the Carpathians used to be studied extensively, particular attention being paid to the effects of large-scale domal uplifts and open folding above marginal zones of thrusts and imbricated map-scale folds, and rarely to the characteristics of young faulting. Neotectonic faults tend to be associated with the margins of the Orava-Nowy Targ Basin, superposed on the boundary between the Inner and Outer Western Carpathians, as well as with some regions within the Outer Carpathians. The size of Quaternary tilting of the Tatra Mts. on the sub-Tatric fault were estimated at 100 to 300 m, and recent vertical crustal movements of this area detected by repeated precise levelling are in the range of 0.4-1.0 mm/yr in rate. Minor vertical block movements of oscillatory character (0.5-1 mm/yr) were detected along faults cutting the Pieniny Klippen Belt owing to repeated geodetic measurements performed on the Pieniny geodynamic test area. In the western part of the Western Outer Carpathians, middle and late Pleistocene reactivation of early Neogene thrust surfaces was suggested. Differentiated mobility of reactivated as normal Miocene faults (oriented (N-S to NNW-SSE and NNE-SSW) in the medial portion of the Dunajec River drainage basin appears to be indicated by the results of long-profile analyses of deformed straths, usually of early and middle Pleistocene age. -
Floods in Poland from 1946 to 2001 — Origin, Territorial Extent and Frequency
Polish Geological Institute Special Papers, 15 (2004): 69–76 Proceedings of the Conference “Risks caused by the geodynamic phenomena in Europe” FLOODS IN POLAND FROM 1946 TO 2001 — ORIGIN, TERRITORIAL EXTENT AND FREQUENCY Andrzej DOBROWOLSKI1, Halina CZARNECKA1, Janusz OSTROWSKI1, Monika ZANIEWSKA1 Abstract. Based on the data concerning floods on the territory of Poland during the period 1946–2001, the reasons generating floods, the number of regional floods in the rivers catchment systems, and sites of local floods occurrence, were defined. Both types of floods: caused by riverbank overflows, and land flooding by rain or snow-melt water, were considered. In the most cases, the floods were caused by rainfall. They were connected with changes in the rainfall structure within Po- land. In each season of the year floods of various origin were observed. When the flood initiating factors appeared simulta- neously, the flood grew into a catastrophic size. In present analysis, for the first time in Poland, a large group of local floods has been distinguished. A special attention has been paid to floods caused by sudden flooding of the land (flash flood), including floods in the urban areas — more and more frequent during the recent years. The results of the analyses have provided important data for the assessment of the flood hazard in Poland, and for the creation of a complex flood control strategy for the whole country and/or for selected regions. Key words: flood, classification of floods, floods territorial extent, frequency of floods occurrence, torrential and rapid rain- fall, threat of life, material losses. Abstrakt. Na podstawie zbioru danych z lat 1946–2001 okreœlono przyczyny wystêpowania powodzi w Polsce, liczbê powodzi re- gionalnych w uk³adzie zlewni rzecznych oraz miejsca wyst¹pieñ powodzi lokalnych. -
Rekreacyjne Walory Rzeki Dunajec W Obszarze Pienińskiego Parku Narodowego
PRACE NAUKOWE Akademii im. Jana Długosza w Częstochowie Seria: Kultura Fizyczna 2009, z. VIII Wiesław Pilis∗ Marek Szambelan* Rekreacyjne walory rzeki Dunajec w obszarze Pienińskiego Parku Narodowego Streszczenie W 1932 roku utworzono Park Narodowy w Pieninach, a po kilkunastu latach przekształcono go w Pieniński Park Narodowy. Główną atrakcją turystyczną te- goż parku jest przełom Dunajca i spływ tratwami odbywający się po nim. Ta forma rekreacji jest dobrze znana nie tylko w Polsce, ale i w Europie. Trwający kilka godzin spływ urzeka bogactwem i różnorodnością natury. Podczas trzech godzin spływu turyści mogą podziwiać przełom i najbliższe szczyty, tj. Faci- miech, Grabczychę, Trzy Korony, Sokolicę. Te niezwykłe atrakcje powodują, że udział w spływie wzrasta z roku na rok i w roku 1967 liczba uczestników osią- gnęła 200 000 osób. Obecnie obserwuje się jej stabilizację na niższym poziomie. Wszystkie te „cuda” natury i turystyczne atrakcje przyciągały w to miejsce zna- nych ludzi, takich jak Marię Konopnicką czy Adama Asnyka, co było czynni- kiem promującym. Chociaż podobne imprezy są organizowane w Europie na większych rzekach, spływ na Dunajcu ma swoją specyficzną atmosferę i okre- ślony rodzaj wielbicieli. Słowa kluczowe: turystyka, rzeka Dunajec, park narodowy, spływ. 1. Wstęp Dnia 23 maja 1932 roku, na wniosek Państwowej Rady Ochrony Przyrody pod przewodnictwem prof. dr. Władysława Szafera, minister rolnictwa podpisał ∗ ALMAMER, Wyższa Szkoła Ekonomiczna w Warszawie. 242 Wiesław Pilis, Marek Szambelan rozporządzenie o utworzeniu z dniem 1 czerwca 1932 roku „Parku Narodowego w Pieninach” (PNP) o powierzchni 7,36 km2. Działania te poprzedzone były utworzeniem prywatnego rezerwatu o powierzchni 0,75 km2 założonego wokół ruin zamku w Czorsztynie, a następnie wykupywaniem na własność Skarbu Pań- stwa gruntów prywatnych, głównie w masywie Trzech Koron, pod utworzenie w Polsce pierwszego parku narodowego. -
Environmental Protection of the Gorce Mountains by The
ENVIRONMENTAL PROTECTION OF THE AND GORCE MOUNTAINS BY THE USE OF GEOTHERMAL ENERGY KRZAN National Park Zakopane. POLAND SOKOLOWSKI Polish Academy of Science Mineral and Energy Economy Research Centre, POLAND Key words: Doublet, Ecology, Air pollution, Defoliatian Tatra are an important center of popular and winter sports. The TNP research station coordinates 100 scientific programs annually, and the naturc museum presents natural values of the park. 1992 Tatra Park Poland one of most polluted countries. This became a MAB Biosphere et 1993). also applies to that of high touristic Podhale basin, where geothermal waters have Pieniny National Park discovered, is national parks. A large The total area of the park is 2328 of which 25% are scale ecological degradation is observed due to atmospheric pol- strictly nature reservation. 'The highest peak, lution some of which is due t o emissions from lo- crowns) is 982 Park is covered cal sources. Geothermal water fur and farmland. climatic zones encompass a moderately in settlements (Zakopane, Nowy Biaty Dunajec, w a r m zone cool zone There etc.) can beneficially influence state of are species of vascular planrs with many endemics and rare health of population and the environment in national parks l'he whole area is located in a low mountain forcst aonc, as well as area's numerous nature reservations. with a forest dominant. The very the park contains 45 specics of t70 species of birds, and numerous fauna Pieniny National is also an historical site. Tourist totaling 28 NATIONAL PARKS Canyon boat, well as many other tourist facilities make the park The southern part of Poland is a very popular lor visitors.