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Tytuł:
Niezwykłość gór. Krajobraz tatrzański w poezji Kazimiery Alberti
The uniqueness of the mountains. Tatra landscape in the poetry of Kazimiera Alberti
L’unicità delle montagne. Il paesaggio dei Tatra nella poesia di Kazimiera Alberti
Autorzy:
Gęsina, Tomasz
Powiązania:
https://bibliotekanauki.pl/articles/784392.pdf
Data publikacji:
2019
Wydawca:
Wydawnictwo Uniwersytetu Śląskiego
Tematy:
Kazimiera Alberti
Tatra landscape
Tatra Mountains in Polish literature
il paesaggio dei Tatra
i monti Tatra nella letteratura polacca
krajobraz tatrzański
Tatry w literaturze polskiej
Opis:
Nell’articolo viene trattato il tema del paesaggio dei monti Tatra nelle opere di debutto di Kazimiera Alberti pubblicate sull’annuario “Wierchy” (1926) e nel volume La rivolta delle valange (Bunt lawin) (1927). L’autore, rifacendosi alle ricerche già esistenti sulla letteratura dei Tatra, ed in particolare soffermandosi su quelle della Giovane Polonia, presenta i motivi più importanti riguardanti i suddetti monti nei lavori della poetessa polacca – il simbolismo della natura, il fascino della cultura montanara, lo svolgersi delle azioni delle opere nel panorama dei Tatra. A tutto ciò si aggiunge una speciale “tatografia”, ovvero una specie di mappa poetica dei Tatra e dei suoi dintorni.
The article deals with the subject of the Tatra landscape in Kazimiera Alberti’s debut poems published in the yearbook „Wierchy” (1926) and in the volume „Avalanche revolt” (Bunt lawin) (1927). The author, referring to the earlier achievements of the Tatra literature, especially the Young Poland period, presents the most important motifs concerning the mountains in the Polish poet’s work – symbolism of nature, fascination with highlander culture, embedding the action of works in Tatra space. All this adds up to a special “tatro(geo)graphy”, which is an underspecified, poetic map of the Tatra Mountains and their surroundings.
Źródło:
Fabrica Litterarum Polono-Italica; 2019, 1; 135-148
2658-185X
Pojawia się w:
Fabrica Litterarum Polono-Italica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The selected factors influencing tourism and recreation development in the Tatra Mountains
Autorzy:
Maziarz, Piotr
Rejman, Krzysztof
Kwiatkowski, Cezary A.
Majcher, Damian
Powiązania:
https://bibliotekanauki.pl/articles/1181360.pdf
Data publikacji:
2017
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Tatra Mountains
recreation
rest
tourism
Opis:
Mountaineering, including the Tatra Mountains tourism, has extremely complex and complicated specifics. In this paper it was made its analysis in the context of the impact of various natural and anthropogenic factors. It was assigned the specific elements of nature to the behavior, actions and plans of tourists, pursuing their passions in the Tatras. The author distinguished both positive and negative environmental influences on tourism. The analysis of the studies allowed foreseeing of the expected changes.
Źródło:
World Scientific News; 2017, 72; 637-656
2392-2192
Pojawia się w:
World Scientific News
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Applying geomathics to determination of landscape altitudinal zones in the mountains
Autorzy:
Guzik, M.
Skawiński, P.
Powiązania:
https://bibliotekanauki.pl/articles/294851.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
landscape altitudinal zones
geomatics
Tatra Mts.
Opis:
The paper presents a method enabling determination of the extent of landscape zones, based on the criterion of area coverage by vegetation. This method made it possible to objectively determine the extent of landscape zones both in the entire Tatra Mts. and in their particular parts. The altitude, at which dominant type of vegetation changes, is considered to mark the boundary of a landscape zone. Boundaries distinguished in this way in the Tatra Mts. are presently situated at: 1,510 m a.s.l. (forest zone), 1,730 m a.s.l. (subalpine zone), and 1,880 m a.s.l. (alpine zone).
Źródło:
Landform Analysis; 2009, 11; 25-32
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geophysical methods in research of permafrost in the Tatra Mountains and northern Scandinavia
Autorzy:
Dobiński, W.
Powiązania:
https://bibliotekanauki.pl/articles/294889.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
permafrost
geophysics
Tatra Mts.
northern Scandinavia
Opis:
A set of geophysical methods were implemented in the research conducted on permafrost of the Tatra Mountains and the Abisko area, Northern Sweden. Results of geophysical surveys show evidence of permafrost in both areas. Comparative studies on the occurrence of permafrost in the Tatras and in the Abisko area indicate that contemporary active as well as fossil permafrost might occur in both locations. Results of the electric resistivity, electromagnetic, shallow refraction seismic, and ground penetrating radar methods reveal similar results and might be successfully used in indirect research on permafrost in the mountainous regions.
Źródło:
Landform Analysis; 2009, 10; 26-32
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmiany cech fizycznych i chemicznych wód źródeł w zlewni Potoku Chochołowskiego (Tatry Zachodnie)
Autorzy:
Wolanin, Anna
Powiązania:
https://bibliotekanauki.pl/articles/634075.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
Tematy:
springs, water chemistry, seasonality, Tatra Mts.
Opis:
Changes in the physical and chemical properties of springwater in the Chochołowski Potok catchment (Western Tatras)The purpose of this paper is to describe the variability of the physical and chemical characteristics of springwater in the Chochołowski Potok catchment. Eleven springs were selected for research purposes. The research was performed from November 2008 to October 2009. Ca 2+ was found as the most common cation, and HCO 3 – was the most common anion in the analysed springwater. The spatial variability of the physical and chemical parameters depends on the geology of an area. Most of the physical and chemical properties of springwater are characterized by seasonal variability. Only a few seasonal differences of the physical and chemical parameters of water are statistically significant (ANOVA). The seasonal changes in springwater chemistry are characterized by high ion concentrations during dry periods in the autumn and winter and low ion concentrations during snowmelt and rainfall-induced floods during the spring and summer. Four factors controlling the physical and chemical properties of springwater were identified.
Źródło:
Prace Geograficzne; 2014, 138
1644-3586
Pojawia się w:
Prace Geograficzne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Changes of thermal conditions in the Polish Tatra Mountains
Autorzy:
Żmudzka, E.
Powiązania:
https://bibliotekanauki.pl/articles/294625.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
thermal conditions
trend
Polish Tatra Mts.
Opis:
The purpose of the report is to determine trends in thermal conditions in the Polish part of the Tatra Mountains. The study makes use of the data from the weather stations in Zakopane and on Kasprowy Wierch Mt. from the years 1951–2006, and mainly from 1966–2006. Various thermal characteristics were considered. The increase of the rate of upward trend in temperature in the Tatras at the turn of the 21st century, as well as the change of the seasonal distribution of the warming in comparison with the preceding long-term periods, have been documented. In 1966–2006, significant trends in the changes of the mean, maximum and minimum temperatures have been observed in the Tatras in summer (respectively, 0.04, 0.05 and 0.03–0.04 centigrade per annum). Certain symptoms of increase of the thermal continentality have also been observed (increase of the annual amplitude of temperature). Besides, important features of changes in thermal conditions at the turn of the 21st century include an increase in the number of hot days, and even appearance of the very hot days at the foothills of the Tatras, increase of the number of frost days and decrease of the number of ice days in the high mountain part of the Tatras, as well as increase of accumulated heat of the growing season and an increase of daily amplitude of temperature across the entire profile of the Tatras.
Źródło:
Landform Analysis; 2009, 10; 140-146
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Outline of Quaternary glaciations in the Tatra Mts. : their development, age and limits
Autorzy:
Lindner, L.
Dzierżek, J.
Marciniak, B.
Nitychoruk, J.
Powiązania:
https://bibliotekanauki.pl/articles/2058873.pdf
Data publikacji:
2003
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Tatra Mts.
Pleistocene
Holocene
glaciers stratigraphy
Opis:
Geomorphological and geological data collected over many years suggest at least eight episodes during which the Tatra Mts. were glaciated during the Quaternary. Evidence of glaciers can be found both in the Slovakian and Polish parts of the mountains as glaciofluvial deposits located at different altitudes, and in some cases also as terminal and lateral moraines. There are no moraines for the three oldest glaciations, Biber, Donau and Günz, maybe as a result of less intense development of glaciers. During the Mindel (Sanian 2) Glaciation the glaciers occuped a larger area in the High Tatra Mts. in comparison to the Western Tatra Mts., whereas during the succeeding younger pre-Riss (Liviecian) Glaciation their development was more restricted. A greater extent of the Tatra Mts. glaciers occurred again during the Riss I (Odranian) Glaciation, while they were less extensive during the Riss II (Wartanian) Glaciation. During the Würm (Vistulian) Glaciation the glaciers were surprisingly large. This might have resulted from many factors, including changes in atmospheric circulation responsible for the distribution of precipitation, as well as changes in the position of the permanent snow limit due to climatic changes and/or neotectonic movements. Glaciers finally retreated from the Tatra Mts. by the end of the pre-optimal part of the Holocene.
Źródło:
Geological Quarterly; 2003, 47, 3; 269-280
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dramatyczna „sytuacja liryczna”. Juliana Przybosia Z Tatr
A Dramatic “Lyrical Situation”. Z Tatr by Julian Przyboś
Autorzy:
Obremski, Krzysztof
Powiązania:
https://bibliotekanauki.pl/articles/534929.pdf
Data publikacji:
2019
Wydawca:
Wydawnictwo Uniwersytetu Śląskiego
Tematy:
Julian Przyboś
Tatra Mountains
“lyrical situation”
Opis:
The article is an interpretative reading of a poem by Julian Przyboś entitled Z Tatr [From the Tatra Mountains]. What constitutes a starting point here are factual documents reporting the fatal accident which involved the sisters Marzena and Lida Skotnica dying on October 6, 1929 during their attempt to climb the south face of ZamarłaTurnia (in Polish part of the Tatra Mountains). The former of the two sisters was beloved by Przyboś, which to a significant extent explains why the poem in question may be interpreted as a dramatic “lyrical situation”.
Źródło:
Śląskie Studia Polonistyczne; 2019, 14, 2; 267-277
2084-0772
2353-0928
Pojawia się w:
Śląskie Studia Polonistyczne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wypadki wśród turystów podejmujących jesienią pieszą aktywność górską na obszarze Tatr Polskich – analiza za rok 2016
Accidents among autumn hiking tourists in the Polish Tatras: analysis for 2016
Autorzy:
Gawlas, Marta
Powiązania:
https://bibliotekanauki.pl/articles/464922.pdf
Data publikacji:
2018
Wydawca:
Akademia Wychowania Fizycznego we Wrocławiu
Tematy:
Tatrzański Park Narodowy
wypadkowość
Tatrzańskie Ochotnicze Pogotowie Ratunkowe
piesza turystyka górska
the Tatra Mountains
the Tatra National Park
mountain accidents
Tatra Voluntary Rescue Service
mountain hiking
Opis:
Cel badań. Przedstawienie, pod względem przestrzennego rozmieszczenia, wypadków górskich mających miejsce jesienią wśród turystów podejmujących pieszą turystykę górską w Tatrach Polskich. Materiał i metody. Do przeprowadzenia analizy posłużono się danymi pochodzącymi z elektronicznej kroniki Tatrzańskiego Ochotniczego Pogotowia Ratunkowego. Badaniem objęto okres od 23 września do 21 grudnia 2016 r. Wyniki. Największą liczbę wypadków górskich odnotowano na obszarze Tatr Wysokich. Lokalizowały się one w 22 różnych miejscach, ale najczęściej na Szpiglasowej Przełęczy, Zawracie, na Rysach i w okolicach Morskiego Oka. Wnioski. Do głównych elementów środowiska przyrodniczego, które mogły przyczynić się do zajścia wypadku, zakwalifikowano: pokrywę śnieżną, eksponowany teren, mgłę, zachmurzenie, opad śniegu, niską temperaturę i oblodzenia, wysokość, silny wiatr, skalne podłoże i spadające kamienie.
Background. The aim of the paper was to present autumn mountain accidents in the Polish Tatra Mountains among hiking tourist, in terms of their spatial distribution and causes. Material and methods. The analysis involved data from the electronic chronicle of the Tatra Voluntary Rescue Service. The study covered one of the four calendar seasons, autumn, i.e. the period from September 23 to December 21, 2016. Results. The greatest number of mountain accidents happened in the High Tatras. Mountain accidents were located in 22 different places, most often in the Szpiglasowa Pass, Zawrat, Rysy, and the Morskie Oko region. Conclusions. The main elements of the natural environment that could have influenced the occurrence of the mountain accidents included: snow cover, exposed terrain, fog, cloudiness, snowfall, low temperature and icing, altitude, strong wind, rocky ground, and falling stones.
Źródło:
Rozprawy Naukowe Akademii Wychowania Fizycznego we Wrocławiu; 2018, 63; 129-142
0239-4375
Pojawia się w:
Rozprawy Naukowe Akademii Wychowania Fizycznego we Wrocławiu
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Changes in thermal conditions in the high mountain areas and contemporary warming in the Central Europe
Autorzy:
Żmudzka, Elwira
Owsiński, Jan
Powiązania:
https://bibliotekanauki.pl/articles/2034144.pdf
Data publikacji:
2010-06-01
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
contemporary warming
trend
Tatra Mountains
lowland Poland
Opis:
The purpose of the report is to determine trends in thermal conditions in the Polish part of the Tatra Mountains. The results of studies were compared with the results of analogous analyses, carried out for the area of lowland Poland. The study makes use of the data from the weather stations in Zakopane and on Kasprowy Wierch Mt. from the years 19512006, mainly from 1966-2006. The thermal conditions in lowland Poland was determined on the basis of the area-averaged time series (45 stations). Various thermal characteristics were considered. The increase of the rate of upward trend in temperature at the turn of the 21st century, as well as the change of the seasonal distribution of the warming in comparison with the preceding long-term periods, have been documented. Symptoms of increase of the thermal continentality have also been observed.
Źródło:
Miscellanea Geographica. Regional Studies on Development; 2010, 14; 59-70
0867-6046
2084-6118
Pojawia się w:
Miscellanea Geographica. Regional Studies on Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Spatial relationship in interaction between glacier and permafrost in different mountainous environments of high and mid latitudes, based on GPR research
Autorzy:
Dobinski, W.
Grabiec, M.
Gądek, B.
Powiązania:
https://bibliotekanauki.pl/articles/2058744.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Scandinavia
Spitsbergen
Tatra Mts.
glacier - permafrost relationship
Opis:
Ground penetrating radar (GPR) surveys were conducted on both the glaciers and their forefields in the Tatra Mountains, Northern Scandinavia and on Spitsbergen – between the 49 degrees and 77 degrees latitudes. The results show that the glacial and periglacial environments interpenetrate. Permafrost is present in the glacier, and glacial ice may occur in the periglacial environment. What is common for both the environments is the perennial melting point surface, with the temperature close to 0°C. In the glacier it is the boundary of the cold-temperate transition surface and on the forefield – permafrost base.
Źródło:
Geological Quarterly; 2011, 55, 4; 375-388
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Microstructures of shear zones from selected domains of the Western Tatra Mountains
Autorzy:
Kania, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059986.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
structures
kinematics
shear zones
Western Tatra Mountains
Opis:
The paper is focused on the meso- and microstructural characteristics of selected shearing zones in the Western Tatra Mts. The domains of crystalline rocks studied (Długi Upłaz Ridge, Rakoń Mt., Zabraty Ridge and Zabrať Pass, Wołowiec Mt., Trzydniowiański Mt., Czubik Mt. and Jarząbczy Mt.) show evidences of heterogeneous shearing with development of shear zones. Four types of shear zones were distinguished: (1) ductile shear zones in gneisses, (2) brittle-ductile complex shear zones, (3) gneisses with clear later brittle deformation; (4) leucogranites, produced by anatexis with later brittle deformation. The development of these shear zones is characterised by occurrences of various types of fault rocks: cataclasites, S-C cataclasites and mylonites. The different shearing-related rocks and structures are interpreted as an effect of protolith diversity and strain partitioning. Shape-preferred orientation is an important structural feature of all the shearing-related rocks. Kinematic analyses revealed generally a southward sense of shearing documented by structures related to brittle conditions and northwards sense of shearing recognised in ductily sheared crystalline rocks. The time relationships between different shear zone types are discussed, leading to the conclusions that the 1st type of shear zone is pure Variscan, the 2nd type is Variscan with Alpine brittle deformation, and the 3rd and 4th types are mainly Alpine brittle deformations of Variscan syntectonic anatectic leucogranites.
Źródło:
Geological Quarterly; 2015, 59, 4; 679--699
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Kartografia geologiczna Tatr
The geological cartography of the Tatra Mts
Autorzy:
Piotrowska, K.
Wójcik, Z.
Powiązania:
https://bibliotekanauki.pl/articles/2074582.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
mapy geologiczne
Tatry
geological maps
Tatra Mts.
Opis:
The area in question represents northern part of the centralWest Carpathians and the boundary zone of Poland and Slovakia (before 1918 the boundary of Galicia and Upper Hungary). From the end of 18th century the authors of geological maps of this area were mostly Austro-Hungarian geologists, but also specialists from other countries. The first cartographic documents refer to the occurrence of mineral raw materials (Hacquet, 1796). A little later some elements of stratigraphy and tectonics were also considered (Staszic, 1815). Zejszner (1844) was the first to pay attention to biostratigraphy and this problem was continued by his followers. In the "Geological Atlas of Galicia" (1885-1914) the authors took into account tectogenesis, at first following the theory of contraction (Uhlig, 1897, 1899) and, subsequently, the concept of nappes (e.g. Lugeon, 1902, 1903; Uhlig, 1907; Limanowski, 1911; Rabowski & Goetel, 1925; Goetel &. Sokołowski, 1930; Guzik, 1939). Until the beginning of the 21st century, the number of cartographic works (maps and cross-sections) printed separately or as attachments and inserts within texts, reached more than 1000 positions. Particularly the cartography of the 20th century, including the map of the Tatra Mts. 1 : 10 000, represents very valuable basic material for the recently prepared "Detailed Geological Map of the Tatra Mts. 1 : 10 000".
Źródło:
Przegląd Geologiczny; 2008, 56, 12; 1069-1078
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Piaskowiec kwarcytowy w dolnej części formacji z Kopieńca między Doliną Bystrej i Doliną Olczyską w Tatrach
Quartzitic sandstone in the lower part of the Kopieniec Formation between the Bystra Valley and the Olczyska Valley in the Tatra Mountains (Poland)
Autorzy:
Iwanow, A.
Zabielski, R.
Połońska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2074849.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Lower Jurassic
Kopieniec Formation
Fatricum
Tatra Mts.
Opis:
Quartzitic sandstone was distinguished at the lower part of the Kopieniec Formation from the Lower Subtatric Nappe (Kriżna Nappe; Fatricum) between the Bystra Valley and the Olczyska Valley, in the Tatra Mts. In previous editions of the detail geological maps of the Tatra Mts, this sandstone was not marked in this area. The quartzitic sandstone crops out at Wysokie hill, east of Kuźnice and can be easily recognized in the field. The sandstone is located above the series of the dark-grey organodetrital limestones and the black calcareous sandstones of the Fatra Formation (Rhaetian) and below the typical brownish- gray claystone of the Kopieniec Formation (Hettangian). Maximum thickness of quartzitic sandstone is about 15 m.
Źródło:
Przegląd Geologiczny; 2011, 59; 235-244
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wypadkowość i akcje ratownicze w Tatrach polskich w latach 2006-2011
Casualty statistics and rescue operations carried out in Polish Tatra Mountains in the years 2006-2011
Autorzy:
Kaganek, Krzysztof
Skwarczyński, Kuba
Powiązania:
https://bibliotekanauki.pl/articles/526927.pdf
Data publikacji:
2013
Wydawca:
Collegium Civitas
Tematy:
security
accidents
rescue operations
Polish Tatra Mountains
Opis:
This article raises important issues regarding security aspects in the mountains. In this assessment, we have analysed casualty statistics and rescue operations carried out in Polish Tatra Mountains in the years 2006-2011. The main aim of this study was to analyse casualty statistics and rescue operations done in Polish Tatra Mountains in the chosen years for our survey and above all stressing the rapid growth of changes occurring in relation to casualty statistics in the region in question. In our assessment, we have applied the analysis of the documents made available to us by the courtesy of Polish Tatra Mountains Voluntary Rescue Team. The parametres resulting largely from these statistics, focussed the main attention on assessment of the overall sum of casualty figures in each separate year, as well as death accidents, serious and slight injuries and rescue operations carried out so far.
Źródło:
Securitologia; 2013, 2(18); 7-18
1898-4509
Pojawia się w:
Securitologia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Determination of the activity level of gamma radionuclides -artificial 137Cs and for comparison -natural 40K and the selected heavy metals in the Tatra Mountains ecosystem.
Autorzy:
Kubica, Barbara Maria
Stobiński, Marcin
Powiązania:
https://bibliotekanauki.pl/articles/763973.pdf
Data publikacji:
2016
Wydawca:
Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
Tematy:
137Cs,40K,Tatra Mts, monitoring
Opis:
This paper presents the results of determination of artificial 137 Cs and natural 40K  activity concentrations and same heavy metals in soil samples from Tatra Mts. Results  show some differences in the vertical distribution and of examined radionuclides and metals. The change of  activity of 137Cs in the  soil samples depends mostly on the soil volume density and on the concentration of organic material. The state of "zero" 137Cs activity was developed in the form of maps.
Źródło:
Annales Universitatis Mariae Curie-Skłodowska, sectio AA – Chemia; 2016, 71, 1
2083-358X
Pojawia się w:
Annales Universitatis Mariae Curie-Skłodowska, sectio AA – Chemia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Turystyczna eksploracja gór wyrażona przez architekturę
Mountain tourist exploration expressed by architecture
Autorzy:
Kronowski, D.
Powiązania:
https://bibliotekanauki.pl/articles/369474.pdf
Data publikacji:
2010
Wydawca:
Zachodniopomorski Uniwersytet Technologiczny w Szczecinie. Wydawnictwo Uczelniane ZUT w Szczecinie
Tematy:
architektura tatrzańska
alpejska
Tatry
Alpy
projekty
schronisko
schron
szałas
architecture tatra
alpine
Tatra Mts.
Alps
projects
shelter
hut
Opis:
Na przełomie XIX i XX wieku pierwsze szlaki i obiekty turystyczne wytyczano dzięki inwestorom prywatnym, a w późniejszym okresie dzięki towarzystwom krajoznawczym oraz organizacjom, takim jak Polskie Towarzystwo Tatrzańskie oraz Polskie Towarzystwo Turystyczno Krajoznawcze. Architektura górska w Tatrach Polskich ewoluowała od form adaptowanych z szałasów do obiektów o większej kubaturze, ściśle nawiązujących do regionalizmu dyktowanego przez ówczesne władze. Możliwość tworzenia nowego dała pole do popisu rzeszom architektów zafascynowanych kulturą i podbojem inteligenckim Tatr, a także przenoszeniem z Alp wzorców sportowych.
At the turn of the century the first trails and tourist facilities created by private investors, and thereafter through the Homeland Study societies and organizations such as PTT and PTTK. Mountain architecture in the Polish Tatra has evolved from a form adapted, from shelters to objects larger volume, characterized by strict reference to regionalism im-posed by the authorities. The possibility of creating a new, gave scope for architects fas-cinated with the myriad of cultural intelligentsia.
Źródło:
Przestrzeń i Forma; 2010, 13; 135-154
1895-3247
2391-7725
Pojawia się w:
Przestrzeń i Forma
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Groundwater ages and altitudes of recharge areas in the Polish Tatra Mts. as determined from 3H, d18O and d2H data
Autorzy:
Zuber, A.
Małecki, J.
Duliński, M.
Powiązania:
https://bibliotekanauki.pl/articles/2060203.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Tatra Mts.
groundwater
environmental isotopes
tritium ages
Opis:
Large and medium karstic springs in the Polish Tatra Mts. occasion ally sampled during low flows exhibited little scatter of stable isotope composition and distinct differences between particular sampling sites. For extreme stable isotope values of four springs, the recharge altitudes were estimated by making use of topographic and geological maps. The altitude effect found in that way served for determining the recharge altitudes of other sampled sites. The altitude-effect gradients found in that way are -0.21‰/100 m and-1.45‰/100 m for delta exp.18 O and delta exp. 2 H, respectively. In general, large karstic springs (exsurgents) have the highest recharge altitudes whereas medium spring and deep wells are characterized by much lower altitudes. Tritium data interpreted with the aid of lumped parameter models yielded mean ages of ca. 3 years for low flows in large karstic springs, ca. 10 years for medium springs, and 50 to 100 years for deep wells, all with very wide age distributions. For four deep wells, the regional hydraulic conductivity estimated from tritium ages (0.8 ´ 10-6 m/s) is about 20 times lower than the geometric mean found from pumping tests (17 ´ -10–6 m/s) suggesting the existence of obstacles to regional flow.
Źródło:
Geological Quarterly; 2008, 52, 1; 71-71
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Koncepcja rozwoju transportu szynowego w powiecie tatrzańskim
Concept of rail transport development in the Tatra Region
Autorzy:
Czaska, M.
Mazurkiewicz, R.
Powiązania:
https://bibliotekanauki.pl/articles/249409.pdf
Data publikacji:
2017
Wydawca:
Stowarzyszenie Inżynierów i Techników Komunikacji Rzeczpospolitej Polskiej
Tematy:
kolej wąskotorowa
kolej turystyczna
koleje tatrzańskie
powiat tatrzański
Zakopane
narrow gauge railways
tourist rail
Tatra railways
Tatra county
Opis:
Tatry są najliczniej odwiedzanymi górami w Polsce. Położony u stóp tych gór powiat tatrzański boryka się z poważnymi problemami komunikacyjnymi. Biorąc pod uwagę podróże stałych mieszkańców powiatu oraz osób przyjezdnych, szacuje się, że ich łączna liczba w skali roku przekracza 4 miliony. W artykule opisano stan transportu zbiorowego w powiecie w ujęciu historycznym i współczesnym, bazującego przede wszystkim na niskopojemnych i mało wygodnych busach. Podano propozycję stworzenia systemu turystycznej kolei dowozowej, łączącej centralne części Zakopanego i Bukowiny Tatrzańskiej z większością punktów wyjściowych na szlaki turystyczne w Tatrach. Przedstawiono główne założenia techniczne dla takiej kolei. Koncepcję poparto kilkoma przykładami funkcjonujących rozwiązań zagranicznych.
The Tatra mountains are the most visited mountains in Poland. The Tatra County located at the foot of these mountains, faces serious communication problems. Taking into account travels of permanent residents of the county and visitors, it is estimated that their total annual number exceeds 4 million. The state of collective transport in the county in historical and contemporary terms, operators using primarily low-cost and less comfortable buses have been described in the article. A proposal to create a tourist system for the railroad connecting the central parts of Zakopane and Bukowina Tatrzańska with most of the starting points for hiking trails in the Tatras has been made. The main technical assumptions for such a railway have been presented. The concept has been supported by several examples of functioning foreign solutions.
Źródło:
Zeszyty Naukowo-Techniczne Stowarzyszenia Inżynierów i Techników Komunikacji w Krakowie. Seria: Materiały Konferencyjne; 2017, 2(113); 35-44
1231-9171
Pojawia się w:
Zeszyty Naukowo-Techniczne Stowarzyszenia Inżynierów i Techników Komunikacji w Krakowie. Seria: Materiały Konferencyjne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Jurassic unconformities in the High-Tatric succession, Tatra Mountains, Poland
Autorzy:
Jezierska, A.
Łuczyński, P.
Powiązania:
https://bibliotekanauki.pl/articles/2060619.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
unconformities
Triassic
Jurassic
High-Tatric series
Tatra Mts.
Opis:
During the Triassic/Jurassic boundary interval and in the Jurassic, the Triassic carbonate platforms occupying the northern shelf of the Western Tethys were subjected to disintegration. Record of these processes in the Alpine-Carpathian area is incomplete and contains a number of stratigraphic gaps. In the High-Tatric succession of the Tatra Mountains (Central Western Carpathians) stratigraphic gaps expressed by unconformity surfaces occur between the Triassic and the Middle Jurassic. In particular areas, the Triassic is directly overlain by the Dudziniec Formation (Sinemurian-Bajocian), the Smolegowa Formation (Bajocian), the Krupianka Formation (Bathonian) or the Raptawicka Turnia Formation (Callovian-Hauterivian). The occurrence of Bajocian and Bathonian deposits is limited to isolated lenticular bodies or to infillings of neptunian dykes penetrating the Triassic. Spatial relations between particular Jurassic lithosomes and the occurrence of stratigraphic gaps between particular units allow discerning four main unconformities. In the stratigraphical order these are: base of the Dudziniec Format ion (erosional unconformity), base of the Smolegowa Formation (penacordance or parat conformity), base of the Krupianka Format ion (erosional unconformity) and base of the Raptawicka Turnia Formation (drowning unconformity). Following episodes of erosion modified the previously developed unconformity surfaces, which resulted in complex modern architecture of the Triassic/Jurassic contact, as well as between particular Jurassic formations.
Źródło:
Geological Quarterly; 2016, 60, 2; 273--290
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Contemporary Climate Changes in the High Mountain Part of the Tatras
Autorzy:
Żmudzka, Elwira
Powiązania:
https://bibliotekanauki.pl/articles/2035472.pdf
Data publikacji:
2011-06-01
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
air temperature
precipitation
snow cover
trend
Tatra Mountains
Opis:
The purpose of this study was to determine the contemporary changes of precipitation and nival conditions in the high-mountain area of Tatras. Main features of thermal climate changes are the background of this investigation. The study makes use of the daily data from the weather station on Kasprowy Wierch Mt. from the years 1966-2006. Various climate characteristics were considered. The increase of the air temperature is not accompanied by significant changes in precipitation conditions. The signs of the more continentality climate features are also visible. The warming and a slight decrease in precipitation and the evolution of circulation conditions significantly influence the length of the period with the snow cover and not significantly its depth.
Źródło:
Miscellanea Geographica. Regional Studies on Development; 2011, 15; 93-102
0867-6046
2084-6118
Pojawia się w:
Miscellanea Geographica. Regional Studies on Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Little Ice Age in the High Tatra mountains
Autorzy:
Kotarba, Adam
Powiązania:
https://bibliotekanauki.pl/articles/2027035.pdf
Data publikacji:
2006
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
geomorphic events
climate change
landform evolution
Tatra Mountains
Opis:
Cli mate de te rio ra tion of the Lit tle Ice Age was mani fested in the most spec tacu lar way in the gla ci ated high moun -tains, but it should also be ana lysed in term of a cli matic con cept. Spa tial varia tion in LIA cli mate is il lus trated also in non- glaciated ar eas of the North ern Hemi sphere in a broader con tex. Ex treme cli matic events were forc ing fac tors for moun tain slope de for ma tion by geo mor phic pro cesses in the High Ta tra Moun tains. The old chroni cles, li che no met ric dat ing of land forms and la cus trine sedi ments are used to de ter mine the be gin ning of “Lit tle Ice Age – type events” (about AD 1400) and its end (about AD 1920). Dur ing this time span the set of cli matic con di tions re spon si ble for trig - ger ing high- energy geo mor phic pro cesses was rec og nised. The cata strophic hy dro me te oro logi cal events were con centrated in cer tain pe ri ods. Clus ter ing of weather anoma lies and natu ral dis as ters re sult ing from them are dis cussed in the pa per.
Źródło:
Studia Quaternaria; 2006, 23; 47-53
1641-5558
2300-0384
Pojawia się w:
Studia Quaternaria
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Long-term trends and factors influencing rainwater chemistry in the Tatra Mountains, Poland
Autorzy:
Małecki, Jerzy J.
Matyjasik, Marek
Krogulec, Ewa
Porowska, Dorota
Powiązania:
https://bibliotekanauki.pl/articles/2055855.pdf
Data publikacji:
2022
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Tematy:
temporal trends
rainwater chemistry
atmospheric pollution
Tatra Mountains
Opis:
The results of rainwater chemistry monitoring in the Tatra Mountains, Poland, during the periods 1993–1994 and 2002–2019 were used to determine long-term trends and the factors influencing rainwater chemistry in the last two decades. In the early 1990’s, the study area was characterized by prominent acid rains with a pH of 4.4 that affected surface water, meadows, and forest ecosystems. A rising pH temporal trend has been observed during the following years, indicating improving air quality. This trend has also been observed in measured ionic concentrations and reduced wet deposition loads of sulfur- and nitrogen-containing acid-forming compounds. The neutralization capacity of rainwater in Kasprowy Wierch increased over the last twenty years and has mostly been dominated by NH4 + . The ammonium availability index has been steadily increasing between years 2002 and 2019 but remains less than 1. This statistically significant relationship also indicates that a portion of neutralization occurs in the lower part of the atmosphere due to ammonium-related neutralization processes. The acidic potential (AP) and the ratio AP/NP (acidic potential/neutralization potential) have been declining during the same time. The stated trends in rainwater chemistry reflect the transformation to more environmentally sustainable economies in the region. Similar changes have been observed in neighboring countries in the region, including Slovakia, the Czech Republic, and Lithuania.
Źródło:
Geology, Geophysics and Environment; 2022, 48, 1; 19--38
2299-8004
2353-0790
Pojawia się w:
Geology, Geophysics and Environment
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Upper Jurassic bacteria from the Raptawicka Turnia Limestone Formation in the Mały Giewont area (Western Tatra Mountains, Poland)
Autorzy:
Pszczółkowski, A.
Powiązania:
https://bibliotekanauki.pl/articles/2060080.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
fossil bacteria
micro-oncoids
Kimmeridgian-Tithonian
Tatra Mountains
Opis:
Fossil filamentous and non-filamentous bacteria are reported from the Upper Jurassic limestones of the Raptawicka Turnia Limestone Formation in the Mały Giewont sections of the Western Tatra Mountains (Poland). The filamentous bacteria are subdivided into five groups: thin uniseriate, large multi-cell, large spiral, tapering and branched forms. The thin uniseriate filaments are the main microbial component of the peloids and micro-oncoids from the studied formation, mainly in the Upper Kimmeridgian-Tithonian limestones. The presence of the heterocyte-like terminal cells suggests their interpretation as cyanobacteria similar to the modern order Nostocales and perhaps to the family Nostocaceae. The large multi-cell and tapering filaments are uncommon in the studied limestones. The branched filaments found in the Tithonian limestones, although thinner, probably also may be compared with some modern representatives of the order Nostocales. Non-filamentous fossil bacteria found in the studied limestones consist of rod-shaped bacilli, monotrichous bacilli and spirilla; they belong mainly to the phylum Proteobacteria. Some microborings observed in the microfossils occurring in the micro-oncoids remind the ichnotaxon Scolecia filosa Radtke known to be of wide palaeobathymetric range. The thinnest microborings resemble another group of ichnofossils named “Pygmy form”, probably also of bacterial origin. The Upper Kimmeridgian-Tithonian micro-oncoids were formed mainly by filamentous bacteria (Cyanobacteria) that overgrew successively their nuclei with a few to several laminae. Frequent occurrence of pelagic microfossils as nuclei of micro-oncoids does not match a transport of these coated grains from much shallower sedimentary environments. The fossil filamentous bacteria filling up the peloids and micro-oncoids could be adapted to conditions that existed in the sublittoral zone below the wave base.
Źródło:
Geological Quarterly; 2018, 62, 4; 840--857
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Facies development and sedimentary environments of the Carpathian Keuper deposits from the Tatra Mountains, Poland and Slovakia
Autorzy:
Rychliński, T.
Powiązania:
https://bibliotekanauki.pl/articles/191399.pdf
Data publikacji:
2008
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Carpathian Keuper
Triassic
Fatricum
sedimentary environments
Tatra Mts.
Opis:
The lower-middle Upper Triassic succession of the Fatricum domain from the Tatra Mts is commonly called the Carpathian Keuper. During Late Triassic, the Fatricum Basin was a proximal part of the central Inner Carpathian Basin. In early Carnian times, carbonate sedimentation stopped. Emersion of the Middle Triassic carbonate platform resulted in development of palaeokarst and pedogenic fabrics and deposition of conglomerates. Typical Carpathian Keuper sediments – variegated shales with intercalations of sandstones and dolomites represent mixed continental/shallow marine environments. Variegated mudstones with pedogenic carbonate concretions and intercalations of thin sandstone beds originated in mudflat environment under the semi-arid climate condition. Thick-bedded, cross-stratified sandstones with common plant debris represent fluvial deposits. They were deposited during the periods of climate pluvialisation. According to ?13C and ?18O data, thick, continuous dolomitic sediments containing local cherts represent marine sediments of perilittoral environments, which were commonly emerged as evidenced by common palaeokarst and palaeosols featuring these complexes. Cyclicity in the lower part of the Carpathian Keuper resulted from climatic changes, whereas dolomite-clastic cycles from the upper part of the succession were generated probably by sea level fluctuations. Moreover, deposition of the Keuper succession was controlled by synsedimentary tectonic which resulted in big facies variability.
Źródło:
Annales Societatis Geologorum Poloniae; 2008, 78, No 1; 1-18
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Methodology and potential of image analysis and unconventional use of GIS tools in determining grain size distribution and fractal dimension : a case study of fault rocks in the Western Tatra Mts. (Western Carpathians, Poland)
Autorzy:
Kania, Maciej
Powiązania:
https://bibliotekanauki.pl/articles/2058666.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
petrotectonics
image analysis
GIS
mylonites
cataclasites
Tatra Mts.
Opis:
A methodology of textural analyses based on image analysis is proposed and tested based on study of fault rock samples from the Tatra Mts., Poland. The procedure encompasses: (1) SEM-BSE imagery of thin sections; (2) image classification using the maximum likelihood method, performed with GIS software; (3) statistical analysis and fractal dimension (self-similarity) analysis. The results of this method are comparable to those obtained with methods involving specialized software. The proposed analytical procedure particularly improves qualitative observations with quantitative data on grain shape and size distribution. The potential of the method is shown, as an auxiliary tool in determining the nature of deformation processes: the role of high-temperature dynamic recrystallization processes is recorded using grain shape indicators, whilst the switch from ductile to brittle conditions is reflected by the grain size distribution pattern.
Źródło:
Geological Quarterly; 2019, 63, 2; 345--358
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Megacrysts of kyanite from Baranec Mt., Western Tatra Mountains, Slovakia
Autorzy:
Pyka, Paulina
Szopa, Krzysztof
Gawęda, Aleksandra
Powiązania:
https://bibliotekanauki.pl/articles/127621.pdf
Data publikacji:
2013
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
kyanite
metamorphic envelope
Western Tatra Mts.
Western Carphatians
Opis:
Large crystals of kyanite (<15 cm in size) occur in quartz segregations in Paleozoic gneissses on Baranec Mt., Western Tatra Mountains, northern Slovakia. Blue kyanite crystals coexist with quartz and plagioclase. The kyanite contains inclusions of apatite, monazite. gamet, rutile and biotite and overgrowths of retrograde sillimanite. muscovite and biotite. The kyanite crystals are the largest found up to now in the Tatra crystalline massif or in the other Western Carpathians crystalline cores. Kyanite. with the co-existing mineral assemblage, is indicative of a HP stage duiing Hercynian metamorphism of the Western Tatra Mountains.
Źródło:
Mineralogia; 2013, 44, 1/2; 31-37
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wpływ turystyki na zmianę warunków przyrodniczych rejonu Kalatówek w Tatrach polskich
Impact of tourism on changes of environment in the Kalatówki area, Polish Tatra Mountains
Autorzy:
Dusza, A.
Powiązania:
https://bibliotekanauki.pl/articles/2074486.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
turystyka
ochrona środowiska
zanieczyszczenia gleby
metale ciężkie
Tatrzański Park Narodowy
tourism
environment
soil
heavy metal
Tatra Mts.
Tatra Mts. National Park
Opis:
Kalatówki is located in the midlle of the Tatra National Park. It has been a popular place for tourist trips since over 100 years. Different types of tourist activity influence environment in many ways, both direct and indirect. Tourism and skiing are most important activities in the Kalatówki area. Tourism causes changes in soils’ physical parameters (bulk density, particle density, soil moisture, porosity, porosity indicator and TOC) on tourist routes and resting-places. Higher heavy metals contents (chromium, copper, iron, lead, zinc) in soils around cable railway mechanisms are connected with skiing infrastructure influence. Minimizing the negative tourism influence on environment of Kalatówki region is possible only thanks to changes in touristic infrastructure and tourists’ attitudes.
Źródło:
Przegląd Geologiczny; 2006, 54, 8; 694-699
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Aptian foraminiferal stratigraphy and Nannoconus assemblages from the Kopka section (Western Tatra Mountains, Poland)
Autorzy:
Pszczółkowski, A.
Powiązania:
https://bibliotekanauki.pl/articles/191202.pdf
Data publikacji:
2015
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Aptian
planktonic foraminifers
Nannoconus
Kopka section
Western Tatra Mountains
Opis:
In the Kopka section (Dolina Kościeliska valley, Western Tatra Mountains), the upper part of the Kościeliska Marl Formation consists of biomicrites with marly interbeds. These deposits, 76 m thick, are assigned to the Praehedbergella excelsa and Leupoldina cabri zones, of Aptian age. The taxa identified belong mainly to the genera Praehedbergella Gorbachik and Moullade, 1973, Globigerinelloides Cushman and Ten Dam, 1948 (emended by Longoria 1974 and Verga and Premoli Silva, 2003a) and Gorbachikella Banner and Desai, 1988. Nineteen Nannoconus taxa were identified during an SEM study of 34 samples. The occurrence of N. vocontiensis in the higher part of the section allows the nannoconid assemblages in the upper part of the section to be distinguished from those in the lower part. Four Nannoconus assemblages were recognized in these limestones: (1) Nannoconus bucheri-N. steinmannii, (2) N. truitti frequens, (3) N. vocontiensis and (4) N. aff. regularis. The wide-canal Nannoconus specimens are more frequent than the narrow-canal ones in the limestones of earliest Aptian age (Praehedbergella excelsa Zone), but the wide-canal forms predominate consistently in the upper part of the section, still within the L. cabri Zone.
Źródło:
Annales Societatis Geologorum Poloniae; 2015, 85, 1; 123-138
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Tectonic control of cave developmen t: a case study of the Bystra Valley in the Tatra Mts., Poland
Autorzy:
Szczygieł, J.
Gaidzik, K.
Kicińska, D.
Powiązania:
https://bibliotekanauki.pl/articles/191732.pdf
Data publikacji:
2015
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Cave morphology
speleogenesis
tectonics
neotectonics
Tatra Mts.
Western Carpathians
Opis:
Tectonic research and morphological observations were carried out in six caves (Kalacka, Goryczkowa, Kasprowa Niżna, Kasprowa Średnia, Kasprowa Wyżnia and Magurska) in the Bystra Valley, in the Tatra Mountains. There are three cave levels, with the youngest active and the other two inactive, reflecting development partly under epiphreatic and partly under phreatic conditions. These studies demonstrate strong control of the cave pattern by tectonic features, including faults and related fractures that originated or were rejuvenated during uplift, lasting from the Late Miocene. In a few local cases, the cave passages are guided by the combined influence of bedding, joints and fractures in the hinge zone of a chevron anticline. That these cave passages are guided by tectonic structures, irrespective of lithological differences, indicates that these proto-conduits were formed by “tectonic inception”. Differences in the cave pattern between the phreatic and epiphreatic zones at a given cave level may be a result of massif relaxation. Below the bottom of the valley, the effect of stress on the rock mass is related to the regional stress field and only individual faults extend below the bottom of the valley. Thus in the phreatic zone, the flow is focused and a single conduit becomes enlarged. The local extension is more intense in the epiphreatic zone above the valley floor and more fractures have been sufficiently extended to allow water to flow. The water migrates along a network of fissures and a maze could be forming. Neotectonic displacements (of up to 15 cm), which are more recent than the passages, were also identified in the caves. Neotectonic activity is no longer believed to have as great an impact on cave morphology as previously was thought. Those faults with displacements of several metres, described as younger than the cave by other authors, should be reclassified as older faults, the surfaces of which have been exposed by speleogenesis. The possible presence of neotectonic faults with greater displacements is not excluded, but they would have had a much greater morphological impact than the observed features suggest.
Źródło:
Annales Societatis Geologorum Poloniae; 2015, 85, 2; 387-404
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Problems in geoecological approach to high-mountain environment (based on studies of relief : vegetation relationships)
Autorzy:
Kozłowska, A.
Rączkowska, Z.
Powiązania:
https://bibliotekanauki.pl/articles/294595.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
high-mountain landscape
relief
vegetation
geoecological aproach
Tatra Mts.
Opis:
The paper discusses the issues associated with the geoecological rendition of high mountains, taking as a basis the authors’ studies of interrelations between relief and vegetation. The fundamental prerequisites for these studies are presented, with emphasis on the fact that the relation between the two elements is indirect and takes place via the intermediary of the habitat. With respect to the scales, both spatial and temporal, applied in the study of landscape, it is established that the majority of relations between vegetation and relief is analysed on the micro-scale, and much less frequently on the meso-scale. Application of areal methods in respective studies provides the possibility of determining the measure of relation between the elements considered. The linear methods (like, e.g., the catena method) allow for grasping the gradient differentiation of the spatial patterns on high mountain slopes. It was established that the main source of problems with landscape representation of high mountains is the mosaic character of the landscape structure. Due to this, even though the interrelations between the elements of the environment – including relief and vegetation – are distinctly visible, they have not been made precise enough with the mathematically defined dependencies, which make development of models of structure and functioning of high mountain slopes more difficult.
Źródło:
Landform Analysis; 2009, 10; 70-76
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mountain hiking in Tatra National Park
Autorzy:
Mokras-Grabowska, Justyna
Powiązania:
https://bibliotekanauki.pl/articles/627926.pdf
Data publikacji:
2016
Wydawca:
Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego
Tematy:
specialised tourism
active tourism
mountain hiking
Tatra National Park
Opis:
Tatra National Park is the most frequently visited national park in Poland. During the peak season (summer), it attracts both ‘fully aware’ tourists, properly prepared for mountain hiking, and ‘casual’ hikers, motivated mainly by the shallow desire to ‘tick off’ the most popular places in the highest Polish mountains. The article describes the specific character of mountain hikers in Tatra National Park during the summer season, with particular attention paid to the motivations and skills involved in active tourism.
Źródło:
Turyzm; 2016, 26, 1; 71-78
0867-5856
2080-6922
Pojawia się w:
Turyzm
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Lower Jurassic spiculite series from the Križna Unit in the Western Tatra Mts, WesternCarpathians, Poland
Dolnojurajskie spikulity jednostki kriżniańskiej w Tatrach Zachodnich, Karpaty Zachodnie, Polska
Autorzy:
Jach, R.
Powiązania:
https://bibliotekanauki.pl/articles/191369.pdf
Data publikacji:
2002
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
spiculites
crinoidal limestones
siliceous sponges
Lower Jurassic
Tatra Mts.
Opis:
Lower Jurassic spiculite series was studied in the Polish part of the Križna Unit in the Western Tatra Mts. This series consists of interbedded spiculites and crinoidal limestones. The spiculites are built almost entirely of siliceous sponge spicules belonging to Hexactinellida and Demospongiae classes. The prolific growth of siliceous sponge community was caused by favourable topographic and bathymetric conditions and by increased content of dissolved silica in the seawater. The spicules were not transported. Crinoidal limestones intercalating with spiculites are composed predominantly of crinoidal ossicles redeposited from shallower parts of the basin by gravity currents generated by storm events. The deposits of the studied series reveal a shallowing upward trend, marked by upward gradual replacement of hexactinellids by demosponges and by thickening and coarsening of the crinoidal limestone layers.
Źródło:
Annales Societatis Geologorum Poloniae; 2002, 72, No 2; 131-144
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geometric analysis of steep-dipping dislocations within the granitoid core in the Polish part of the Tatra Mts
Analiza geometryczna stromych dyslokacji w trzonie granitowym polskiej części Tatr Wysokich
Autorzy:
Jurewicz, E.
Powiązania:
https://bibliotekanauki.pl/articles/191417.pdf
Data publikacji:
2002
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
Tatra Mts.
faults
slickenside
stress axes
Middle Miocene extension
Opis:
The paper is focused on steep dipping dislocations within the granitoid core of the Polish part of the Tatra Mts. Two groups of dislocations were distinguished: single faults with flat and smooth planes, and mylonitic and cataclastic zones. With the help of TectonicsFP software, the reconstruction of the stress pattern, responsible for the formation of single faults, is presented basing on slip structures on their planes. The structures can be linked with the Middle Miocene (Sarmatian) 106-120° extension; in effect a set of normal oblique-slip, ~35/60N faults was formed with a horizontal sinistral component. The geometry of the system of mylonitic and cataclastic zones should be analysed after reversing them to positions prior to the post-Palaeogene rotational upheaval of the Tatra Mts. The orientation of some dislocation zones, described in literature, is revised.
Źródło:
Annales Societatis Geologorum Poloniae; 2002, 72, No 1; 89-98
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Origin of calcite-cemented Holocene slope breccias from the Długa Valley (the Western Tatra Mountains
Autorzy:
Gradziński, M.
Jach, R.
Stworzewicz, E.
Powiązania:
https://bibliotekanauki.pl/articles/191437.pdf
Data publikacji:
2001
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
slope breccias
calcite cements
radiocarbon dating
Holocene
Tatra Mts.
Opis:
New locality of slope breccias was found in the Western Tatra Mts. It occures in the Długa Valley on a steep slope of ravine beneath the belt of Jurassic radiolarite cliffs. The brecccia consists of angular clasts of radiolarite bound with calcite cements. Void spaces between the clasts contain shells of Holocene snails. The cements are built of columnar crystals composed of acicular subcrystals and of skeletal crystals. The crystals grew rapidly from supersaturated solution due to CO2 degassing. Cementation occurred in vadose conditions in the Atlantcic Phase soon after the scree formation.
Źródło:
Annales Societatis Geologorum Poloniae; 2001, 71, No 2; 105-113
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Influence of site conditions on the windstorm impast : a case study of the High Tatras foothills in 2004
Autorzy:
Minár, J.
Falan, V.
Bánovský, M.
Damankošová, Z.
Kouch, M.
Powiązania:
https://bibliotekanauki.pl/articles/294593.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
windstorm
sites
geoecological research
statistical methods
Tatra National Park
Opis:
The calamity situation in the forests of the Tatra National Park, caused by a windstorm on the 19th of November 2004, had widespread damaging effects. The wind calamity caused slashes and wind throws as well. The aim of our paper is to describe influence of the site conditions (parameters of vegetation, soil and georelief) on the windstorm impact at chosen representative localities in the High Tatras foothills. The results obtained by methods of large-scaled geo-ecological field research, remote sensing, geographical information system environment and statistical analyses are presented in this paper. Geotops of saddles, elevations of moraine and colluvial slopes with planted spruce growths and spruce-bilberry forests have been damaged most. Small damage was recorded on geotops of erosion slopes with spruce-bilberry and fir forests, depressions and slopes of moraines covered with mixed pioneer forests. The most important were herein the characteristics of the rock skeleton (mainly size and weathering), soil texture, georelief orientation or wind exposition. The important role of the altitude probably expresses a regional positional factor (distance from the uphill line).
Źródło:
Landform Analysis; 2009, 10; 95-101
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Konstelacja Witkacy. Z Zofią Radwańską z Muzeum Tatrzańskiego rozmawia Paweł Drabarczyk vel Grabarczyk
Autorzy:
Drabarczyk vel Grabarczyk, Paweł
Powiązania:
https://bibliotekanauki.pl/articles/2011168.pdf
Data publikacji:
2021-12-13
Wydawca:
Uniwersytet Kardynała Stefana Wyszyńskiego w Warszawie
Tematy:
Zofia Radwańska
Stanisław Witkacy
Muzeum Tatrzńskie
The Tatra Museum
Opis:
Wywiad z Zofią Radwańską z Muzeum Tatrzańskiego
Źródło:
Artifex Novus; 2021, 5; 210-217
2544-5014
Pojawia się w:
Artifex Novus
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Tadeusz i Stefan Zwolińscy: przyczynek do biografii speleologicznej
Autorzy:
Lewkowicz, Łukasz
Powiązania:
https://bibliotekanauki.pl/articles/2034867.pdf
Data publikacji:
2021-12-31
Wydawca:
Wydawnictwo Adam Marszałek
Tematy:
Tadeusz Zwoliński
Stefan Zwoliński
speleohistory
Tatra Mountains
speleohistoria
Tatry
Opis:
The research aim of the article was to present the broadly understood speleological activity of the brothers Tadeusz and Stefan Zwoliński. The text presents biographies of both described characters, then the individual stages of their speleological activity are analyzed in detail, and in the end the legacy of the Zwoliński brothers is characterized. The speleological activity of the Zwoliński brothers lasted several dozen years in total: it began during the Austro-Hungarian period, was continued with many successes in the interwar period and ended after the Second World War in the Polish People’s Republic. At the threshold of their activity, only 44 caves in the Polish Tatras were known. The activity of the Zwoliński brothers finally brought the knowledge of nearly 120 new cave facilities. Their various publications also provided a model for the development of cave documentation and influenced the tourist and scientific activities carried out there. The article is a contribution to further research on the history of Polish speleology.
Celem badawczym artykułu było ukazanie szeroko rozumianej działalności speleologicznej braci Tadeusza i Stefana Zwolińskich. W tekście przedstawione zostały biogramy obu opisywanych postaci, następnie szczegółowo poddano analizie poszczególne etapy ich aktywności speleologicznej, w zakończeniu zaś scharakteryzowano dziedzictwo, jakie zostawili po sobie Zwolińscy. Aktywność speleologiczna braci Zwolińskich trwała łącznie kilkadziesiąt lat: rozpoczęła się jeszcze w okresie istnienia Austro-Węgier, kontynuowana była z wieloma sukcesami w dwudziestoleciu międzywojennym i zakończyła się po II wojnie światowej w Polskiej Rzeczpospolitej Ludowej. U progu ich aktywności znanych było zaledwie 44 jaskiń w Tatrach Polskich. Działalność Zwolińskich przyniosła ostatecznie poznanie blisko 120 nowych obiektów. Ich różnego rodzaju publikacje dostarczyły również wzoru do opracowywania dokumentacji jaskiń i wpłynęły na prowadzoną w nich działalność turystyczną i naukową. Artykuł stanowi przyczynek do dalszych badań dotyczących historii polskiej speleologii.
Źródło:
Polish Biographical Studies; 2021, 9; 219-251
2353-9291
Pojawia się w:
Polish Biographical Studies
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Skamieniałości śladowe wczesnego i środkowego triasu domeny Fatricum w Tatrach i ich znaczenie paleośrodowiskowe
Early and Middle Triassic trace fossils of the Fatricum domain in the Tatra Mountains and their palaeoenvironmental significance
Autorzy:
Rychliński, T.
Uchman, A.
Powiązania:
https://bibliotekanauki.pl/articles/2074730.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
ichnofauna
paleośrodowisko
trias
Fatricum
Tatry
palaeoenvironment
Triassic
Tatra Mts.
Opis:
Trace fossils of the Olenekian clastic deposits (Fatricum domain) in the Tatra Mts. include Rhizocorallium isp., Palaeophycus striatus, cf. Palaeophycus isp. and cf. Chondrites isp., while Planolites isp., Thalassinoides isp., Rhizocorallium isp. and Balanoglossites isp. occur in the Anisian carbonates. The Anisian trace fossil assemblage is less diverse and abundant than in the coeval carbonates of the Tatricum domain. Both, the Olenekian and Anisian trace fossils represent the impoverished Cruziana ichnofacies influenced by the increased salinity. Bioturbational structures are much less abundant than in the Anisian of the Tatricum. They are partly obliterated by diagenetic processes.
Źródło:
Przegląd Geologiczny; 2010, 58, 11; 1079-1086
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Impact of the COVID-19 Pandemic on Tourism in the Tatra County (Poland)
Autorzy:
Druet, Paweł
Powiązania:
https://bibliotekanauki.pl/articles/2196345.pdf
Data publikacji:
2023-03-31
Wydawca:
Uniwersytet Gdański. Instytut Geografii
Tematy:
SARS-CoV-2
COVID-19
pandemic
tourism
Tatra County
Opis:
The COVID-19 pandemic and the numerous restrictions implemented because of it have had a huge impact on the tourism sector around the world. The aim of this study is to identify and assess their effects on tourism in the Tatra County, the area in which there are some of the most popular tourist places in Poland – the Tatra National Park and the town of Zakopane. The study showed that the COVID-19 pandemic caused a significant decrease in the tourist traffic in this area in 2020, and as a result, a smaller number of incidents requiring the intervention of the Tatra Volunteer Search and Rescue, less demand for accommodation or fewer foreign tourists. In addition, entrepreneurs directly or indirectly involved in the tourism industry recorded lower revenues or losses. Smaller revenues were also recorded in the mentioned town of Zakopane.
Źródło:
Journal of Geography, Politics and Society; 2023, 13, 1; 55-65
2084-0497
2451-2249
Pojawia się w:
Journal of Geography, Politics and Society
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Petrogenesis of kyanite-quartz segregations in mica schists of the Western Tatra Mountains (Slovakia)
Autorzy:
Pyka, Paulina
Gawęda, Aleksandra
Szopa, Krzysztof
Muller, Axel
Sikorska, Magdalena
Powiązania:
https://bibliotekanauki.pl/articles/127586.pdf
Data publikacji:
2014
Wydawca:
Polskie Towarzystwo Mineralogiczne
Tematy:
kyanite-quartz segregation
aluminium mobilization
mass-balance
Tatra Mountains
Opis:
In the Tatra Mountains (Slovakia) metamorphic complex, kyanite-quartz segregations with biotite-rich selvage occur in mylonitized mica schists. In this paper, the problem of fluid flow and aluminium mobility during the uplift of the crystalline massif, and the position of the segregations in the history of Western Tatra metamorphic complex, is adressed. The reaction Alm + Rt Ilm + Ky + Qtz is considered to be the result of a pressure drop from above to below 9 kbar. Ti-in-biotite geothermometry shows the temperature range to be 579- 639ºC that is related to heating and decompression associated with granite intrusion. Major-element mass-balance calculations show that Al remained stable in the selvage + segregation system whereas other elements (e.g. Cr, HFSE) were mobilized. The kyanite-quartz segregations formed from local fluids generated during dehydration of the metapelitic rocks during uplift. The main mechanism was likely diffusion-driven mass-transfer into extensionrelated cracks.
Źródło:
Mineralogia; 2014, 45, 3/4; 99-120
1899-8291
1899-8526
Pojawia się w:
Mineralogia
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Do pheromone trapping always reflect Ips typographus (L.) population level? A study from the Tatra National Park in Poland
Autorzy:
Grodzki, Wojciech
Powiązania:
https://bibliotekanauki.pl/articles/2041268.pdf
Data publikacji:
2021
Wydawca:
Instytut Badawczy Leśnictwa
Tematy:
pheromone monitoring
bark beetles
protected areas
Picea abies
mountains
Tatra
Opis:
Pheromone traps are used for monitoring I. typographus populations in Norway spruce stands of the Tatra National Park (TPN) in Poland. The presented study is based on the set of pheromone traps of precisely known location (23) located in the whole area of the TPN and operated continuously in 2010–2019. The data on the captures of beetles were compared with two kinds of data concerning the mortality: the area covered by standing dead trees (airborne photographs) in the no-intervention zone, and the volume of trees infested by bark beetles processed in the active protection zone. No relationship was found between the mean numbers of beetles captured yearly in all pheromone traps in the whole TPN area and the volume of infested trees removed from the stands in the active protection zone. The captures in the two selected study areas were correlated with the area of spots with dead trees in the 500 m circle around the traps, however, this correlation is not statistically significant. There is no relation of captures to the volume of processed infested trees. The captures decreased in the growing seasons after the wind damage, and increased markedly after the drought started in 2015. The results of pheromone trapping are affected by several factors, as wind damage and defence potential of trees resulting from their physiological status. Pheromone traps represent valuable source of information about the bark beetle I. typographus population dynamics, although the collected data do not enable direct definition of its population level, especially in the protected areas with different and unstable (changed in 2017) approach to the protection of stands. As most of the information on beetles is captured in the first half of the growing season, the data collected till the end of July are sufficient for monitoring purposes; thus, the trapping should be reduced to the period May–July.
Źródło:
Folia Forestalia Polonica. Series A . Forestry; 2021, 63, 1; 36-47
0071-6677
Pojawia się w:
Folia Forestalia Polonica. Series A . Forestry
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Charakterystyka morfologiczna i geochemiczna kryształów cyrkonu z migmatytu ze Smreczyńskiego Wierchu (Tatry Zachodnie)
Morphological and geochemical characteristics of zircon crystals from Smreczyński Wierch migmatite (Western Tatra Mts.)
Autorzy:
Burda, J.
Powiązania:
https://bibliotekanauki.pl/articles/2074380.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
kryształ cyrkonu
katodoluminescencja
migmatytyzacja
zircon morphology
cathodoluminescence
migmatites
Tatra Mts.
Opis:
In the Polish part of the metamorphic envelope of the granitoid Rohače pluton, migmatites are the predominant component. Migmatisation took place in the amphibolite facies conditions (T = 690–780C ; P =7.5–11 kbar). To observe the response of zircon crystals to the melt formation, zircon from the anatectic group of migmatites was investigated (both from leucosome and mesosome of stromatitic migmatite). Different generations of zircon present in leuco- and mesosome reflect different geological processes acting during the rock formation. Zircon from leucosome represent mainly the euhedral varieties, with two typological maxima: S1-2 (I generation) and S21-22 (II generation). Zircon from mesosome represents the anhedral varieties with one maximum at S1 (I gen-eration). In CL images the first generation (S1-2) comprises an inherited core surrounded by younger metamorphic and magmatic rims. The microchemical analyses showed that the inherited cores have higher Zr/Hf ratios than the overgrowing rims. The second genera-tion (S21-22) revealed only oscillatory zonation. The zones with strong luminescence are characterized by a decrease of Hf and U con-tent. Zircon showing polyphase internal structure might represent a component of mesosome which survived the dissolution in granitic melt, while zircon with oscillatory zonation might have crystallized from anatectic melt.
Źródło:
Przegląd Geologiczny; 2005, 53, 2; 127--133
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Uwagi o rozwoju jaskiń w strukturze płaszczowinowej Czerwonych Wierchów w Tatrach
Remarks on caves development in the Czerwone Wierchy Nappe in the Tatra Mts.
Autorzy:
Bac-Moszaszwili, M.
Nowicki, T.
Powiązania:
https://bibliotekanauki.pl/articles/2074415.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Tatry
budowa geologiczna
jaskinie
Karst development
geological structures
Tatra Mts.
Opis:
The Czerwone Wierchy Nappe is the main part of the Czerwone Wierchy Massif. Several big cave systems are developed in this structural unit, e.g., Wielka Śnieżna Cave System, Kozia, Ptasia, Mała w Mułowej and a lot of smaller caves. Cross-section I presents two main parts of Czerwone Wierchy Nappe-Organy and Idziary units which are separated by the Organy Dislocation. Similar structure is characteristic for whole Czerwone Wierchy Nappe (Kotański, 1963). The abundance of caves near Organy fault is a result of intensive tectonic processes in this area what is visible at the western slope of the Miętusia Valley. Further to the east , so far scientists (Kotański, 1961; Grodzicki & Kardaś, 1989) suggested that whole the Wielka Śnieżna Cave System is developed within the dziary Unit. Our geological cross-sections of the upper part of Miętusia Valley, (based on Grochocka-Rećko, 1963) show that only upper, vertical parts ofWielka Śnieżna and Śnieżna Studnia caves are developed in the dziary Unit, similarly as the upper, vertical part of the Mała Cave. Lower parts of cave systems are related to the Organy Dislocation and the Organy Unit. It seems that geological structure of the Czerwone Wierchy Massif is a dominant factor controlling the cave passages development. As a results of geological structure, the main path of water flow, at the level ca. 1000 m a.s.l., from lower parts of Wielka Śnieżna Cave in Miętusia Valley towards Lodowe Źródło in Kościeliska Valley developed solely along Middle Triassic layers in a latitudinal fold turn of the Organy Unit (Mała Łąka Fold, Kotański, 1961).
Źródło:
Przegląd Geologiczny; 2006, 54, 1; 56-60
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Glacial and periglacial relief on the southern slopes of the Western Tatra Mts. (Slovakia) - the results of the first detailed geomorphological mapping of the Žiarska, Jamnicka, Račkova and Bystra Valleys
Autorzy:
Kłapyta, P.
Powiązania:
https://bibliotekanauki.pl/articles/294354.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
deglaciation
moraine systems
relict rock glaciers
morphostratigraphy
Western Tatra Mts.
Opis:
The article presents the results of the first detailed geomorphological mapping of the Žiarska, Jamnicka, Raekova, and Bystra Valleys, situated on the southern slope of the Western Tatra Mountains. The field work was supplemented by digital topographic as well as statistical analysis of rock glaciers distribution. The author focused on the distribution and morphological features of moraines and rock glaciers. Variability of both sets of deposits strongly reflects topographic influences on debris and snow accumulation. The main factor controlling the geometry of landforms was solar irradiance modified by the influence of the local cirque topography. Two generations of the rock glaciers indicate distinct phases of periglacial conditions during the Late Glacial period.
Źródło:
Landform Analysis; 2009, 10; 50-57
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Concept of landscape horizontal belts in the Polish Tatra Mountains
Autorzy:
Niedźwiecki, J.
Powiązania:
https://bibliotekanauki.pl/articles/294603.pdf
Data publikacji:
2009
Wydawca:
Stowarzyszenie Geomorfologów Polskich
Tematy:
Tatra Mts.
landscape belts
high mountains
mountain landscap
slope system
Opis:
The history of changes of geoecological belts in the mountains exerts influence on the structure and functioning of the landscape. In many mountain regions, a convergence of two basic altitudinal lines occurs: the contemporary upper timberline and the cold Pleistocene snow line. The Tatra Mts. are an example of such a situation. These lines constitute the border between the high-mountain landscape and the landscape of mid- and low mountains (according to the Polish classification). However, this convergence also marks out the horizontal border across the profile of the valley, which separates the part with completely established high mountain landform complex (with postglacial cirques)from the remaining part of the valley. The montane belt can be also divided into two parts characterized by different landscape structure, due to existence of the influence of catenal processes from the subsystem of high-mountain belt. On these bases, the author introduces the concept of landscape horizontal belts in the mountain landscape of the Polish Tatra Mts., dividing the latter into three functional belts: the typical high-mountain landscape, the transitional landscape, and the typical landscape of mid- and low mountains.
Źródło:
Landform Analysis; 2009, 10; 102-107
1429-799X
Pojawia się w:
Landform Analysis
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
TURYSTYKA TATRZAŃSKA I ETOS TURYSTY W DOBIE NOWOCZESNOŚCI
CONTEMPORARY TATRA TOURISM AND ITS ETHOS
Autorzy:
Datko, Joanna
Powiązania:
https://bibliotekanauki.pl/articles/693964.pdf
Data publikacji:
2012
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
contemporary Tatra tourism
ethos
commercialisation
współczesna turystyka tatrzańska
etos
komercjalizacja
Opis:
The paper touches upon some origins of contemporary Tatra tourism and its ethos in the ever-changing modern world. It provides a theoretical outline of the concept of ‘ethos’ regarding touristic exploration of the Tatra Mountains and the characteristics of the elements that have determined tourism in the last twenty years (based on qualitative research). The main features of tourism in the Tatra that are now being observed are popularisation, commercialisation, decline of some traditional ways of thinking about mountaineering and practicing it as well as changes within the ethos and its peculiar community (or rather disappearance of them both). In this context very important are also some environmental issues, such as devastation of the natural ecosystem and expansion of urban practices deeper and deeper into the Tatra National Park. Last but not least one other issue touched upon in the paper is the ‘touristic’ knowledge and skills that are now very rare among the tourist who visit the Tatra, which also leads to the decline of the ethos.
Artykuł porusza zagadnienie specyfiki turystyki tatrzańskiej i etosu turysty w realiach postępujących zmian cywilizacyjnych i kulturowych. Zawiera szkic teoretyczny dekonstruujący pojęcie „etos” w odniesieniu do eksploracji turystycznej przestrzeni Tatr oraz opartą na badaniach jakościowych charakterystykę elementów współcześnie ją konstytuujących, a także ich przemian w ciągu ostatnich dwóch dekad. Jedną z głównych cech turystyki uprawianej na terenie Tatr jest jej umasowienie, swoista komercjalizacja, postępujący zanik pewnych tatrzańskich tradycji oraz przekształcenia (a raczej odchodzenie) owego tworzącego się latami etosu i wynikającej zeń wspólnotowości. W tym kontekście pojawiają się również głosy dotyczące coraz szybszej dewastacji tatrzańskiego środowiska przyrodniczego i wdzierania się praktyk miejskich na obszary górskie (ekspansja Zakopanego) oraz niechęci olbrzymiej rzeszy turystów tatrzańskich do nabywania wiedzy i umiejętności determinujących istnienie etosu.
Źródło:
Ruch Prawniczy, Ekonomiczny i Socjologiczny; 2012, 74, 2; 265-278
0035-9629
2543-9170
Pojawia się w:
Ruch Prawniczy, Ekonomiczny i Socjologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Middle Triassic evolution of the Tatricum sedimentary basin : an attempt of sequence stratigraphy to the Wierchowa Unit in the Polish Tatra Mountains
Autorzy:
Jaglarz, P.
Szulc, J.
Powiązania:
https://bibliotekanauki.pl/articles/191483.pdf
Data publikacji:
2003
Wydawca:
Polskie Towarzystwo Geologiczne
Tematy:
basin analysis
paleoenvironments
sequence stratigraphy
late Scythian-Ladinian
Tatra Mts.
Opis:
The paper focuses on paleoenvironmental reconstruction and sequence stratigraphy of the Tatricum Basin for the late Scythian-Ladinian interval. The reconstruction is based on observations carried out in the Kominiarski Wierch section, situated in the Polish part of the Tatra Mts. Sedimentological and geochemical studies indicate that during middle Triassic time the Tatricum Basin was situated upon an isolated and restricted carbonate platform dominated by shallow water carbonate and evaporitic sedimentation. The basin was a tectonically stable area controlled by eustatic fluctuations. Incipient tectonic movements first occurred in late Ladinian time only. The studied sedimentary succession is composed of several stacked, shallowing-upward cycles that are interpreted as 3rd order depositional sequences. The constructed sedimentary sequence framework corresponds well with the sequence stratigraphic scheme of the Northern Alpine Triassic and enables a better chronostratigraphic resolution of the Triassic in the Tatra Mts.
Źródło:
Annales Societatis Geologorum Poloniae; 2003, 73, No 3; 169-182
0208-9068
Pojawia się w:
Annales Societatis Geologorum Poloniae
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-50 z 205

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