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Wyświetlanie 1-15 z 205
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
Wyświetlanie 1-15 z 205

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