Rozkład Przestrzenny Ruchu Turystycznego Na Szlakach Pieszych

Total Page:16

File Type:pdf, Size:1020Kb

Rozkład Przestrzenny Ruchu Turystycznego Na Szlakach Pieszych Pieniny – Przyroda i Człowiek 14: 133–143 (2016) Rozkład przestrzenny ruchu turystycznego na szlakach pieszych w Pienińskim Parku Narodowym (Monitoring Studenckiego Koła Naukowego Uniwersytetu Pedagogicznego w Krakowie w latach 2007–2012) Spatial distribution of tourists on walking trails in the Pieniny National Park (Monitoring conducted in the period 2007–2012 by members of the Geography Students Scientific Association of Pedagogical University in Kraków) Gabriela Bołoz, Witold Jucha Instytut Geografii Uniwersytetu Pedagogicznego im. Komisji Edukacji Narodowej w Krakowie ul. Podchorążych 2, 30-084 Kraków Abstract. The Pieniny National Park is one of the most popular protected areas in Poland due to its natural and cultural values and attractive location. The monitoring of tourist traffic was conducted by the Scientific Association of Geography Students. The results showed a great diversity of spatial and temporary distribution of tourists in the Park. The analyzed number of visitors on each part of trails was used to distinguish trails with high concentration of tourists and to show the most and the less popular trails in the Park during the monitoring. Key words: monitoring, tourist traffic, walking trails Wstęp (m.in. bliskość ciekawych miejsc historycz- nych, rekreacyjnych i przyrodniczych: Zbiornika Obszary chronione, w tym zwłaszcza parki naro- Czorsztyńskiego, zamków w Czorsztynie i Nie- dowe, cechują się wynikającym z ich bogactwa dzicy itp.) powodują, że Park ten jest jednym przyrodniczego znacznym potencjałem tury- z najczęściej odwiedzanych parków narodowych stycznym, ocenianym poprzez atrakcyjność dla w Polsce (Warcholik i in. 2010a). Korzystna rekreacji, krajoznawstwa i edukacji (Bolland 1982; lokalizacja większości punktów docelowych Wróbel 2002; Pilis, Szambelan 2009). Pieniński wycieczek (Trzy Korony, Sokolica czy Zamek Park Narodowy (PPN) chroni unikatowe w skali Pieniny) powoduje znaczną koncentrację ruchu kraju dziedzictwo przyrodnicze i kulturowe pasma turystycznego w centralnej i wschodniej części górskiego Pienin (Bolland 1982, Witkowski 2003). Parku. Monitoring przemieszczania się turystów Park, jako instytucja, oprócz działań ochron- na szlakach w Parku był przedmiotem badań kilku nych prowadzi działalność naukową, edukacyjną jednostek naukowych, w tym Studenckiego Koła oraz udostępnia swój teren odwiedzającym. Naukowego Geografów Uniwersytetu Pedago- Wybitne walory turystyczne i atrakcyjne położenie gicznego w Krakowie (SKNG UP). 134 Pieniny – Przyroda i Człowiek 14, 2016 Artykuł przedstawia wybrane problemy zwią- Mohar 2003; Arnberger i in. 2005; Dzioban 2011). zane z przestrzennym i czasowym zróżnicowa- Poniżej przedstawiono cztery sposoby określania niem liczby turystów na szlakach pieszych w PPN. liczby turystów, które są stosowane w polskich Do rozważań wykorzystano dane zebrane podczas parkach narodowych (Warcholik i in. 2010a; monitoringu ruchu turystycznego na terenie Parku, Buchwał, Fidelus 2010): który prowadzili członkowie SKNG UP w latach 1. Obliczenia na podstawie danych ze sprze­ 2007–2012 (Kiszka i in. 2009; Warcholik i in. daży biletów. Metoda stosowana w m.in. 2010b; Ćwiąkała, Gil 2012). Na podstawie badań w Tatrzańskim Parku Narodowym. W Pienińskim wskazano, które odcinki są najrzadziej, a które PN również jest stosowana, lecz w tym przy- najczęściej wykorzystywane podczas sezonu padku może być zawodna z powodów: umiesz- wakacyjnego. Przedstawiono i przeanalizowano czenia kas nie przy wejściach do Parku, lecz zmiany sposobu przemieszczania się turystów, przy galeriach widokowych na Sokolicy i Trzech podczas dnia powszedniego i weekendowego, Koronach; ograniczonego czasu pobierania opłat w czasie pogody deszczowej i słonecznej. za bilety – w okresie od kwietnia do paździer- nika (9.00–17.00); wniesienie opłaty wymagane jest od osób w wieku od 7 lat; w przypadku Cele badań kupna biletu na jednej z platform bilet obowią- W ramach badań sformułowano trzy cele: zuje tego samego dnia także na drugiej (Faron • określenie preferencji poszczególnych kie- i in. 2012). runków wejściowych do Parku 2. Obliczenia na podstawie badania ankie- • określenie rozmieszczenia przestrzennego towego. Metoda stosowana m.in. w Pienińskim i natężenia ruchu turystycznego w PPN i wska- i Gorczańskim PN; turysta podczas wypełnienia zanie najczęściej oraz najrzadziej odwiedza- ankiety deklaruje, jaką trasą pójdzie podczas nych miejsc w Parku wycieczki (Semczuk i in. 2014). • zbadanie zależności między rozmieszczeniem 3. Liczenie turystów przy użyciu czujników przestrzennym ruchu turystycznego a czyn- ruchu. Metoda stosowana w Tatrzańskim i Babio- nikami zewnętrznymi takimi jak: pogoda górskim PN przy użyciu fotokomórek na podczer- i zmiany w infrastrukturze. wień (Buchwał, Fidelus 2010). Metoda wymaga dużych nakładów finansowych (zakup aparatury pomiarowej). Zaletą jest możliwość niemal nie- METODYKA ograniczonego czasu monitorowania szlaków Określenie wielkości ruchu turystycznego na po­ i duża dokładność wyników. szczególnych szlakach wewnątrz parków narodo- 4. Liczenie turystów przez pomiarowych wych ma na celu zbadanie rzeczywistych na punktach kontrolnych. Metodą posłużono się zachowań turystów co do preferencji (co turysta w przypadku zebrania danych do niniejszego zdecydował się zobaczyć), jak również oceny po- artykułu i została opisana w rozdziale doty- ziomu natężenia i oddziaływania na środowisko czącym metod. przez gości odwiedzających te obszary. Można Każda z wymienionych metod ma swoje wady go szacować na wiele różnych sposobów, i zalety. Ponadto wyniki otrzymywane różnymi w związku z tym niżej zamieszczony rozdział za- metodami w tym samym czasie mogą odbiegać wiera przegląd metod stosowanych w polskich od siebie (niejednolita liczba punktów pomiaro- parkach narodowych oraz przyjętą przez SKNG wych, dokładność i czas pomiaru). Tym niemniej UP metodę monitoringu. parki narodowe wykorzystują każdą z tych metod, aby określić wielkość i strukturę ruchu turystycz- Przegląd wybranych metod monitoringu nego na swoim terytorium. ruchu turystycznego w Polsce Dla PPN istnieją co najmniej trzy serie Istnieje wiele metod określania wielkości ruchu badawcze dotyczące monitoringu ruchu turystycz- turystycznego na terenach chronionych (Cessford, nego: 1) dane pochodzące ze sprzedaży biletów G. Bołoz & W. Jucha: Ruch turystyczny na szlakach pieszych w PPN 135 na platformy widokowe (Faron i in. 2012), i in. 2012). Na terenie Parku wyznaczono 2) dane pochodzące z badań ankietowych prowa- 9 miejsc kontrolnych, których nazwy pochodziły dzonych przez wolontariuszy PPN oraz 3) dane od nazw własnych polan, przełęczy lub najbliż- pochodzące z monitoringu prowadzonego przez szych, charakterystycznych szczytów (Tab. I). SKNG UP w latach 2007–2012 (Sprawozdanie… W wyznaczonych punktach rozlokowano dwu- 2012). W związku z tym, że każde z nich zostało nastu pomiarowych, którzy dokonywali obser- opracowane za pomocą innej metody, w innych wacji na skrzyżowaniach szlaków (Ryc. 1). przedziałach godzinowych i okresach czasu, nie- Wyjątek stanowiła Przełęcz Szopka, gdzie pomiar możliwe jest dokonanie ich analizy porównaw- odbywał się na odcinku szlaku w pewnym czej. Dlatego skupiono się na opracowaniu serii dystansie od skrzyżowania szlaków, a do punktu badawczej SKNG UP, przygotowanej m.in. przez przypisane były cztery osoby. autorów tekstu (pkt 3). Pomiar odbywał się w godzinach 9.00–16.00 w ustalone wcześniej dni monitoringowe. Metoda badań Na kartach obserwacyjnych pomiarowi zapi- Materiał badawczy obejmuje informacje o liczbie sywali liczbę turystów przechodzących dany przemieszczających się turystów po PPN na pod- odcinek szlaku, prowadząc zapis w tabeli podzie- stawie serii monitoringowych przeprowadzonych lonej na interwały 15­minutowe. Kolumna zapisu przez SKNG UP. Pomiary odbywały się w sezonie była podzielona na trzy części: w dwóch pierw- wakacyjnym w okresie 2007–2012 (z wyłącze- szych zapisywano kierunek przemieszczania się niem roku 2011). W każdym sezonie pomiary turystów oraz warunki pogodowe. Odnotowy- wykonywano przez 5–7 dni. wano turystów przemieszczających się każdym Badania prowadzono metodą obserwacji z siedemnastu odcinków szlaków turystycznych kontrolowanej w punktach pomiarowych (Faron wewnątrz Parku (Tab. I). 1 2 3 4 5 6 7 8 9 10 11 Ryc. 1. Piesze szlaki turystyczne w Pienińskim Parku Narodowym (PPN) oraz lokalizacja punktów pomiarowych: 1 – lokalizacja punktu pomiarowego (numery rzymskie), 2 – lokalizacja punktów pomiarowych przy Przełęczy Szopka (numer rzymski II), 3 – szlak czerwony, 4 – szlak niebieski, 5 – szlak zielony, 6 – szlak żółty, 7 – obszar Parku, 8 – zabudowa miejscowości wokół Parku (nazwy na mapie kursywą), 9 – zbiorniki wodne, 10 – rzeki, 11 – ważniejsze drogi; numeracja arabska – odcinki szlaków Fig. 1. Walking tourist trails in the Pieniny National Park (PNP) and location of monitoring points: 1 – location of monitoring point (roman numerals), 2 – location of monitoring points near Przełęcz Szopka (roman numeral II), 3 – red trail, 4 – blue trail, 5 – green trail, 6 – yellow trail, 7 – PNP area, 8 – towns and villages near the PNP (names on the map written in italic), 9 – water reservoirs, 10 – rivers, 11 – main roads; Arabic numerals – sections of trails, Tab. I. Source: own study 136 Pieniny – Przyroda i Człowiek 14, 2016 Tabela I. Odcinki szlaków wewnątrz Pienińskiego Parku Narodowego Table I. Sections of trails inside Pieniny National Park Lp. Kolor szlaku Punkt początkowy Punkt końcowy (patrz Ryc. 1) Colour of the trail Starting point Ending point Nr (Fig. 1) 1. niebieski
Recommended publications
  • 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.
    [Show full text]
  • 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..
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Environmental Properties of Soils in the Pieniny National Park of Slovakia
    Pieniny – Przyroda i Człowiek 7: 97–98 (2002) Environmental properties of soils in the Pieniny National Park of Slovakia Charakterystyka gleb Pienin´skiego Parku Narodowego na Słowacji JOZEF KOBZA Soil Science and Conservation Research Institute, 974-04 Banska Bystrica, Mládežnícka 36, Slovakia Abstract. This study examines environmental properties of agricultural soils in the Pieniny National Park of Slovakia. Excluding the present status of basic soil properties and heavy metal content, the development tendency of evalu- ated properties is described between 1993 and 1997. One of the most important environmental properties is the susceptibility of ag- ricultural soils to pH value decrease, soil organic matter decrease, available P and K loss and to soil contamination, which has been mostly slight, resp. not determined during short-term compared period. INTRODUCTION MATERIAL AND METHODS Soil is a very important part of the environment. The results were obtained from the 10 monitoring The original properties of soil cover depend on sites in agricultural land (arable land and grass- geological composition. Geologically, the pale- land) of Pieniny National Park in Slovakia. The ocene flysch is most extended. On this geological soil samples from the surface have been analysed substra occur Cambisols which are mostly for pH/KCl, Cox, fractional composition of soil covered with grassland. The haligov region organic matter (humic acids and fulvoacids), (mostly forest) is composed of mesozoic rocks content of available nutrients – phosphorus and carbonateous sediments including dolomites (Egner’s method) and potassium (Schachtschabel’s and limestones (Vološcˇuk 1992). These substrates method). The heavy metals have been extracted are covered with Rendzinas and Cambic Rendzi- with 2M HNO3 and 0.05 M EDTA.
    [Show full text]
  • 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.
    [Show full text]
  • Diptera) Along an Elevational Diversity Gradient in a Low Mountain Range: an Example from Central Europe
    insects Article Distributional Patterns of Aquatic Empididae (Diptera) along an Elevational Diversity Gradient in a Low Mountain Range: An Example from Central Europe Iwona Słowi ´nska* and Radomir Jaskuła Department of Invertebrate Zoology and Hydrobiology, Faculty of Biology and Environmental Protection, University of Lodz, Banacha 12/16, 90-237 Łód´z,Poland; [email protected] * Correspondence: [email protected] Simple Summary: The insect distribution and diversity depend on many different abiotic and biotic factors, which is especially well documented in the high mountains but has not been studied in detail in the low mountain massifs. We studied 17 different macro and microhabitat factors that influence the altitudinal distribution of 40 Hemerodromiinae and Clinocerinae species in the Pieniny Mts., Poland. This is the first such study in Central Europe and one of only a few in the world. The results clearly show that species richness and distribution of Hemerodromiinae and Clinocerinae species are changing with the elevational gradient, with a monotonic decline in species richness with increasing elevation observed for the first subfamily and the hump-shaped distribution pattern noted for the second subfamily, as well as the size of the stream/river and the surrounding area in species distribution in the Pieniny Mts. Abstract: The two subfamilies Hemerodromiinae and Clinocerinae, also known as aquatic dance Citation: Słowi´nska,I.; Jaskuła, R. flies, are a group of small predatory insects occurring mainly in mountainous areas and the northern Distributional Patterns of Aquatic temperate. However, very little is known about distribution patterns for most of the species.
    [Show full text]
  • Pieniny- the Great Little Mountains
    Pieniny- The Great Little Mountains JERZY W. GAJEWSKI On the map of Poland, the Pieniny Mountains are over-shadowed by other mountains situated in the south of the country, along the Czechoslovakian border. However, the Pieninys with their pointed rocky hills provide a contrast to the landscape of the surrounding Flysch Beskidy Mountains. The landscape and natural beauty of the Pieninys have brought about their great popularity with tourists, especially ramblers, resulting in the establishment of the first Polish National Park there. In general, the Pieniny Mountains cover the area between the BiaTka River in the west (its source is situated above the White Water Valley on the Slovak side of the Tatra Mountains), and the Rozdziele Pass in the east, where they border on the Beskid Sadecki Mountains. The western part of the Pieninys, which culminate on Zar (879m), is called Pieniny Spiskie, because the surrounding territory - with its interesting villages, architecture, costumes and cusroms of the people - is joined to the Spisz region (part of this area is situated on the Slovak side, roo). This is where Dt;bno, the village with the famous St Michael's Church, is situated. This wooden church was built in the 15th century and its interior is covered with unusual and rare wall-paintings. 0 wonder Dt;bno church is a goal for most tourists who go to the Pieniny Mountains. The eastern part of the Pieninys, although being the highest, is called MaTe Pieniny (Little Pieniny). It culminates on the Wysoka (105 2m), at the foot of which are four conservation areas with short but beautiful gorges (the most famous is called Homole).
    [Show full text]
  • Western Carpathians, Poland)
    Geological Quarterly, 2006, 50 (1): 169–194 Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland) Nestor OSZCZYPKO Oszczypko N. (2006) — Late Jurassic-Miocene evolution of the Outer Carpathian fold-and-thrust belt and its foredeep basin (Western Carpathians, Poland). Geol. Quart., 50 (1): 169–194. Warszawa. The Outer Carpathian Basin domain developed in its initial stage as a Jurassic-Early Cretaceous rifted passive margin that faced the east- ern parts of the oceanic Alpine Tethys. Following closure of this oceanic basin during the Late Cretaceous and collision of the Inner Western Carpathian orogenic wedge with the Outer Carpathian passive margin at the Cretaceous-Paleocene transition, the Outer Carpathian Basin domain was transformed into a foreland basin that was progressively scooped out by nappes and thrust sheets. In the pre- and syn-orogenic evolution of the Outer Carpathian basins the following prominent periods can be distinguished: (1) Middle Juras- sic-Early Cretaceous syn-rift opening of basins followed by Early Cretaceous post-rift thermal subsidence, (2) latest Creta- ceous-Paleocene syn-collisional inversion, (3) Late Paleocene to Middle Eocene flexural subsidence and (4) Late Eocene-Early Miocene synorogenic closure of the basins. In the Outer Carpathian domain driving forces of tectonic subsidence were syn-rift and thermal post-rift processes, as well as tectonic loads related to the emplacement of nappes and slab-pull. Similar to other orogenic belts, folding of the Outer Carpathians commenced in their internal parts and progressed in time towards the continental foreland. This process was initi- ated at the end of the Paleocene at the Pieniny Klippen Belt/Magura Basin boundary and was completed during early Burdigalian in the northern part of the Krosno Flysch Basin.
    [Show full text]
  • National and Landscape Parks, Nature Reserves
    National and landscape parks, nature reserves MAŁOPOLSKA 14 UNESCO World Heritage List sites 255 attractions on the Wooden Architecture Route Wadowice – town of birth of Pope John Paul II Salt mines in Wieliczka and Bochnia 9 spa resorts 6 national parks 6 geothermal pools Rafting down the Dunajec gorge 2600 km of bicycle trails 3360 km of mountain trails 65 ski stations www.visitmalopolska.pl fb.com/lubiemalopolske The project has been funded by Małopolska Region Rejkiawik IS MAŁOPOLSKA NATIONAL AND LANDSCAPE PARKS, NATURE RESERVES Capital of the region: Kraków MAŁOPOLSKA Major cities: Tarnów, Nowy Sącz, Oświęcim National Parks, Landscape Parks and Nature Reserves Surface area: 15,190 km2 (about 5% of the surface area of Poland) FIN Helsinki Population: 3.4 mil. (about 8% of the population of Poland) N Oslo S Sztokholm Tallin Landscape: EST RUS the tallest peak – Rysy: 2499 m asl Ryga Encounter with Nature LV mountains – Tatras, Beskids, Pieniny, Gorce Dublin DK foothills – Carpathian Foothills IRL Kopenhaga LT Wilno ałopolska is a unique region, especially in GB RUS uplands – Kraków-Częstochowa Upland Mińsk NL terms of its natural diversity. It boasts fanci- lowlands – Vistula valley Londyn BY Amsterdam Berlin ful outliers and hot desert sands, the scenic main rivers – Vistula, Dunajec, Poprad, Raba, Skawa, Biała Bruksela Warszawa D PL ribbon of the Vistula River and the Dunajec water reservoirs – Czorsztyński, Rożnowski, Czchowski, Dobczycki, Klimkówka B Kijów L Praga KRAKÓW MRiver forcing its way between the rocks,
    [Show full text]
  • 1. the Podhale Geothermal System and Heating Project Ð an Overview
    Beata Kepinska: THE PODHALE GEOTHERMAL SYSTEM AND HEATING PROJECT – AN OVERVIEW 1. THE PODHALE GEOTHERMAL SYSTEM AND HEATING PROJECT – AN OVERVIEW Beata Kepinska Polish Academy of Sciences, Mineral and Energy Economy Research Institute Wybickiego 7 Str., 31- 261 Krakow, Poland Abstract • Climatic and tourist value (the centre of winter sport and alpinism, with a number of boarding The Podhale region is regarded as a cradle for houses and hotels, a venue of many winter geothermal energy use for heating purposes in sports competitions); Poland. Since the end of 1980s the research works • A vital, rich folk culture and tradition culti- and activities oriented to geothermal space heating vated by local highlanders; and other uses have been carried out there. There, the first in Poland, Experimental Geothermal Plant • Large resources of geothermal waters charac- terizing by favourable parameters. was put into operation and successively a great regional heating system has been developed. On the other hand, Podhale has been affected by intensive anthropopression, especially extensive More than ten years of the project deve- lopment brought many results of both cognitive and pollution of natural environment caused by burning large quantities of hard coal for heating (heating practical meaning for the proper long-term exploi- season lasts even 8-9 months). Therefore, the pro- tation of the geothermal reservoir and the heating ject of a regional geothermal heating network hav- network operation. The paper introduces main geo- ing been realised since the end of 1980s is of es- logical and reservoir characteristics of the Podhale sential significance to stop further degradation of geothermal system, project’s assumptions, techno- Podhale ecosystem, and to conduct sustainable ma- logical, ecological, economical and some other as- pects and circumstances.
    [Show full text]