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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:
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:
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:
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:
Paleolithic Man in the Tatra Mountains
Autorzy:
Valde-Nowak, Paweł
Soják, Marián
Powiązania:
https://bibliotekanauki.pl/articles/52089821.pdf
Data publikacji:
2018
Wydawca:
Uniwersytet Jagielloński. Wydawnictwo Uniwersytetu Jagiellońskiego
Tematy:
Palaeolithic
Western Carpathians
Tatra Mountains
Magdalenian
cave-site
Opis:
At the end of 2018, when the Hučivá Cave (Hučivá diera, Rausch Keller) was explored in Tatranská Lomnica, profile deposits in rear areas of the cave were found disturbed by an amateur excavation. One stone artefact was first found in back-dirt clay-layer material at the excavation pit, later joined by four more specimens from the cleaned pit profile. The Typological analysis of the artefacts shows, that their closest parallels are found in inventories of the Magdalenian culture.Hučivá is the only cave in the whole Tatras with documented prehistoric settlement and the only Slovak cave with evidence of the Magdalenian culture. The discovery provides new information concerning subsistence strategies of late Pleistocene hunters in High Tatra Mountain landscapes. In light of this discovery, the possibility of seasonal movements along the northern slopes of this mountains range to the east and then south, through the mountain passes to the upper Spiš region should now be considered.
Źródło:
Acta Archaeologica Carpathica; 2018, LIII; 37-48
0001-5229
2719-4841
Pojawia się w:
Acta Archaeologica Carpathica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Changes of the surface area of Morskie Oko and Wielki Staw in the Tatra Mountains
Autorzy:
Choiński, Adam
Zieliński, Artur
Powiązania:
https://bibliotekanauki.pl/articles/52495720.pdf
Data publikacji:
2023
Wydawca:
Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:
Morskie Oko
Wielki Staw
mass movements
Tatra Mountains
Tatra National Park
Opis:
This dissertation has presented the results of measurements regarding the surface area of Morskie Oko and Wielki Staw lakes performed throughout the period of 140-years with the use of various measurement technologies and analyses of cartographic resources. The research has clearly demonstrated that the obtained results are diverse, which could be influenced by various environmental factors and the time difference of surveys conducted at the ana- lysed objects. Wielki Staw is currently the largest lake in the Polish Tatra Mountains. Its surface area in 2021 covered 33.44 ha. Thus, it appeared to be larger than Morskie Oko, the surface area of which is 1.51 ha. It was also concluded that the difference in the size of these two reservoirs might increase over time since Morskie Oko is situated in an environment that undergoes dynamic transformations and, consequently, has an impact on the evolution of this lake. Moreover, the area surrounding Morskie Oko is one of the most popular tourist locations within the Tatra National Park, which may intensify the anthropogenic impact on the course of, among others, the shoreline.
Źródło:
Quaestiones Geographicae; 2023, 42, 1; 15-24
0137-477X
2081-6383
Pojawia się w:
Quaestiones Geographicae
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:
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:
On the vertical distribution of Ips duplicatus, I. cembrae and some bark- and longhorn beetles (Col.: Curculionidae, Scolytinae; Col.: Cerambycidae) in the Tatra National Park in Poland
Autorzy:
Grodzki, Wojciech
Powiązania:
https://bibliotekanauki.pl/articles/2041646.pdf
Data publikacji:
2020
Wydawca:
Instytut Badawczy Leśnictwa
Tematy:
Ips duplicatus
Ips cembrae
Scolytinae
Cerambycidae
vertical distribution
Tatra Mountains
Opis:
In 2013–2014, a set of 30 pheromone traps baited with synthetic lures attracting I. duplicatus (Duplodor – 15 traps) and I. cembrae (Cembrodor – 15 traps) was installed in 6 altitudinal transects (1000–1400 m a.s.l., every 100 m of elevation) in the eastern, central and western part of the Tatra National Park (TPN) in Poland and operated during the entire growing season. The main aim of the survey was to check if and to what vertical extent these two species of bark beetles, not yet recorded, are presently distributed in TPN. Collected insects, including non-target Scolytinae and Cerambycidae, were determined. Overall 1896 Scolytid bark beetles belonging to 13 species, all occurring in the whole elevation range, were collected. I. duplicatus (28 specimens in total) was collected in the whole elevation profile, similarly as I. cembrae (718 specimens in total). Among Cerambycidae (282 individuals) belonging to 19 species, Rhagium inquisitor and Pidonia lurida, found on all elevations, were the most abundant; 8 species were collected on the highest locality. Pogonocherus decoratus was found for the first time in the Tatra. Results indicate the upward spreading of the studied insects as a possible effect of climate change and the resulting environmental conditions favourable for those organisms.
Źródło:
Folia Forestalia Polonica. Series A . Forestry; 2020, 62, 2; 68-77
0071-6677
Pojawia się w:
Folia Forestalia Polonica. Series A . Forestry
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność właściwości fizycznych pokrywy śnieżnej na Hali Gąsienicowej w kontekście zagrożenia lawinowego
Variability of Physical Properties of Snow Cover at Hala Gąsienicowa in Terms of Avalanche Danger
Autorzy:
Stachura, Gabriel
Powiązania:
https://bibliotekanauki.pl/articles/1818549.pdf
Data publikacji:
2020
Wydawca:
Polskie Towarzystwa Geofizyczne
Tematy:
pokrywa śnieżna
lawiny
Hala Gąsienicowa
Tatry
snow cover
avalanches
Tatra Mountains
Opis:
W artykule dokonano analizy zróżnicowania gęstości oraz twardości warstw pokrywy śnieżnej w profilu w zależności od przebiegu metamorfozy śniegu. Porównano także ich przebieg sezonowy względem ogłaszanego przez Tatrzańskie Ochotnicze Pogotowie Ratunkowe (TOPR) stopnia zagrożenia lawinowego. Celem analizy jest dokładniejsze poznanie oraz weryfikacja już znanych mechanizmów metamorfozy śniegu, w szczególności w odniesieniu do stabilności pokrywy śnieżnej. Gęstość i twardość są właściwościami fizycznymi pokrywy śnieżnej określanymi w ramach szczegółowych badań pokrywy śnieżnej. Badania te wykonywane są raz w tygodniu na Stacji Badań Niwalnych IMGW-PIB na Hali Gąsienicowej. Bazowy zbiór danych do przeprowadzenia analizy stanowiło 141 szczegółowych badań pokrywy śnieżnej wykonanych w latach 2007/2008 – 2016/2017 wraz z dobowymi danymi meteorologicznymi z tego okresu. Porównanie przebiegu sezonowego dokonano na przykładzie trzech sezonów: 2011/2012, 2012/2013 oraz 2016/2017. Zaproponowana przez Kłapową (1980) granica metamorfozy topnieniowej o wartości 400 kg/m3 przypada na pierwszy kwartyl zbioru gęstości dla topniejącego śniegu (gat. 6), co potwierdza prawidłowość jej określenia. Rozstęp gęstości oraz rozstęp twardości dobrze odzwierciedlają zmienność zagrożenia lawinowego przez większą część sezonu. Ze względu na specyfikę parametru twardości, większe zróżnicowanie wykazuje rozstęp gęstości i to ten parametr w sposób bardziej dokładny potrafi oddać zmiany stabilności pokrywy śnieżnej. Niemniej jednak, w sytuacji małej grubości pokrywy śnieżnej oraz w początkowej fazie akumulacji pokrywy śnieżnej jego stosowalność jest bardzo ograniczona - wówczas pomocną informację o stanie pokrywy śnieżnej niesie ze sobą rozstęp twardości, który uwzględnia także cienkie warstwy pokrywy śnieżnej. Rozstęp twardości może być zatem traktowany jako wielkość uzupełniająca dla rozstępu gęstości. Przedstawione w artykule zależności wyznaczone dla Hali Gąsienicowej mogą być pomocne do lokalnej oceny stabilności pokrywy śnieżnej w terenie lawinowym na obszarze całych Tatr oraz w wyższych partiach Karpat.
In this paper the variability of density and hardness of a snow layer has been analysed in relations to metamorphism stage. Furthermore, a comparison between their variability and the level of avalanche danger announced by Tatra Volunteer Rescue Service has been made. The purpose of the analysis is to get to know better about the rules of snow metamorphosis as well as to verify the already known ones, particularly regarding the stability of a snowpack. Snow density and hardness are physical properties of snow layer specified during detailed snowpack investigations. The investigations are conducted weekly at the Nival Research Station of Institute of Meteorology and Water Management at Hala Gąsienicowa (Tatra Mts). The original data base comprises 141 detailed snowpack investigations conducted in winter seasons 2007/2008 – 2016/2017 as well as meteorological data from that time. The comparison of a seasonal variability was exemplified by presenting three seasons – 2011/2012, 2012/2013 and 2016/2017. A limit of wet snow metamorphism assumed by Kłapowa (1980) to be 400 kg/ m3 falls close to the first quartile of density dataset for melting snow (form 6) what in fact confirms her assumption. Density and hardness range reflect well the variability of avalanche danger during most of a season. Due to a specific nature of hardness parameter, it is density range that shows bigger variability and therefore is able to reflect changes in a snowpack stability more accurately. Nevertheless, in case of poor snow depth as well as at the beginning of snow accumulation its application is limited. In such cases hardness range carries a helpful piece of information about the state of a snow cover as it takes into account also thin layers in a snowpack. Hardness range could be therefore considered a complementary parameter to density range. The relations presented in an article, which has been observed for Hala Gąsienicowa, could be useful for a local evaluation of snowpack stability in an avalanche area in Tatra Mts as well as in higher parts of Carpathian Mts.
Źródło:
Przegląd Geofizyczny; 2020, 1-2; 23--39
0033-2135
Pojawia się w:
Przegląd Geofizyczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Possible genetic resemblance among white coated shepherd dogs such as Turkish Akbash Shepherd, Polish Tatra, Kuvasz, Chuvach, and Central Asian Shepherd Dog
Możliwe podobieństwo genetyczne u psów pasterskich o białym umaszczeniu, takich jak turecki owczarek akbash, polski owczarek podhalański, kuvasz, chuvach i owczarek środkowoazjatycki
Autorzy:
Yılmaz, O.
Powiązania:
https://bibliotekanauki.pl/articles/29433614.pdf
Data publikacji:
2022
Wydawca:
Zachodniopomorski Uniwersytet Technologiczny w Szczecinie. Wydawnictwo Uczelniane ZUT w Szczecinie
Tematy:
Canis familiaris
shepherd dogs
genetic relationship
Akbash Sheperd
Tatra Mountains
Kuvasz
Źródło:
Acta Scientiarum Polonorum. Zootechnica; 2022, 21, 1; 11-16
1644-0714
Pojawia się w:
Acta Scientiarum Polonorum. Zootechnica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Possibilities of balancing of anthropogenic changes of relief and water conditions in the Tatra Mountains
Autorzy:
Radziewicz, Tomasz
Mikulska, Małgorzata
Powiązania:
https://bibliotekanauki.pl/articles/2030353.pdf
Data publikacji:
2006-06-01
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
anthropopressure
relief
water conditions
Tatra Mountains
natural system
catchment area
system stability
Opis:
During its entire utilisation history - lasting several hundred years - the area of the Tatra Mountains underwent multidirectional anthropopressure. As the result, all components of their natural environment have been transformed, including relief and water conditions.The analysis of the literature on this topie conducted by the author, as well as his observations performed in the area, confirmed the assumption that transformations caused by human actions developed with varying intensity and admitted various forms depending on the area of action and the magnitude of means applied. The transformation scalę presented here estimates the influence of anthropopressure on the stability of the catchment area systems of larger Tatra streams, partial catchment areas of their confluents and selected slope surfaces. In systems, where the limits of persistence were not exceeded, stability was ensured by natural processes compensating for the conseąuences of anthropopressure. In systems where stability was disturbed, planned preventive measures are necessary.
Źródło:
Miscellanea Geographica. Regional Studies on Development; 2006, 12; 125-130
0867-6046
2084-6118
Pojawia się w:
Miscellanea Geographica. Regional Studies on Development
Dostawca treści:
Biblioteka Nauki
Artykuł
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