Skocz do pozycji: 1.

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

/5

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Skocz do pozycji: 2.

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

/5

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Skocz do pozycji: 3.

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

/5

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Skocz do pozycji: 4.

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

/5

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Skocz do pozycji: 5.

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

/5

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Skocz do pozycji: 6.

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

/5

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Skocz do pozycji: 7.

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

/5

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Skocz do pozycji: 8.

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

/5

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Skocz do pozycji: 9.

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

/5

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Skocz do pozycji: 10.

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

/5

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Skocz do pozycji: 11.

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

/5

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Skocz do pozycji: 12.

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

/5

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Skocz do pozycji: 13.

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

/5

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Skocz do pozycji: 14.

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

/5

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Skocz do pozycji: 15.

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

/5

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Skocz do pozycji: 16.

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

/5

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Skocz do pozycji: 17.

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

/5

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Skocz do pozycji: 18.

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

/5

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Skocz do pozycji: 19.

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

/5

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Skocz do pozycji: 20.

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

/5

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Skocz do pozycji: 21.

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

/5

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Skocz do pozycji: 22.

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

/5

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Skocz do pozycji: 23.

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

/5

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Skocz do pozycji: 24.

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

/5

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Skocz do pozycji: 25.

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

/5

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Skocz do pozycji: 26.

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

/5

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Skocz do pozycji: 27.

Tytuł:

An attempt to assess the modern and the Little Ice Age climatic snowline altitude in the Tatra Mountains

Autorzy:

Zasadni, J.
Kłapyta, P.

Powiązania:

https://bibliotekanauki.pl/articles/294601.pdf

Data publikacji:

2009

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

climatic snowline
temperature-precipitation ELA
Little Ice Age
Tatra Mts.

Opis:

An empirical glacio-climatic relation (Ohmura et al., 1992) and meteorological data (temperature and precipitation) are employed to provide the elevation in the Tatra Mts. climate model, where conditions are suitable for hypothetical glacierisation (temperature-precipitation ELA). During the Little Ice Age (LIA) it is to have been 1.5 centigrade colder than during the warmest decades of the 20th century (Niedźwiedź, 2004); however, some scenarios are used to define precipitation amounts related to the vertical distribution in climate model and temporal variability. The results indicate that during both considered periods - the warmest decades of the 20th century and the coolest period of LIA - the climatic snowline (cSL) was placed in most cases above the highest Tatra Mts. summits and crests. However, its spatial arrangement was unequal. In the vicinity of Kasprowy Wierch, the modern cSL is assessed to be at ca. 2,450-2,650 m a.s.l. and that during LIA at ca. 2,300-2,450 m a.s.l. In the case of Lomnicky Štit (2,634 m) it was at the level of ca. 2,700–2,800 m a.s.l. (modern times) and ca. 2,600–2,700 m a.s.l. (LIA). The discrepancies in the cSL altitude between these two locations can be explained in part by exposition to the prevailing moisture transport and orographically-induced precipitation.

Źródło:

Landform Analysis; 2009, 10; 124-133
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 28.

Tytuł:

The Zadnie Kamienne "ravenous" shear zone (High-Tatric Nappe) - conditions of deformation

Autorzy:

Jurewicz, E.
Słaby, E.

Powiązania:

https://bibliotekanauki.pl/articles/2058790.pdf

Data publikacji:

2004

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Tatra Mts.
Carpathians
shear zone
pressure solution
feldspar growth
geothermometers

Opis:

The Zadnie Kamienne shear zone is a high-angle Riedel type shear zone (R'), exhibiting an antithetic sense of displacement, which may have developed synchronously with the nappe-thrusting of the Giewont Unit (High-Tatric Nappe). The amount of displacement along this zone is very low and does not explain the very intense deformation, which is of the same character as that at the base of the Giewont Unit (mylonitization, stylolitization and vein forming). The explanation of this phenomenon lies in the multiple activity of this zone, the change of the direction of movement and the important role of pressure solution in hydrothermal conditions responsible for dissolution creep, mass loss and stress relaxation. This kind of shear can be referred to as a "ravenous" shear zone. Neo-forming minerals accompanying these processes were applied as a temperature gauge. Simultaneous growth of albite and adularia indicates a temperature of about 350 degrees C. Chlorites accompanying them occur in two thermal episodes, the first of which indicating a similar temperature (292-357 C).

Źródło:

Geological Quarterly; 2004, 48, 4; 371--382
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 29.

Tytuł:

Circulation in present-day karst systems sourcing the vaucluse springs in the Polish Tatra Mts., based on tracer methods and limnimetric observations

Autorzy:

Barczyk, G.

Powiązania:

https://bibliotekanauki.pl/articles/2059632.pdf

Data publikacji:

2003

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

Tatra Mts.
karst
vaucluse springs
karst systems
tracer methods
stationary observations

Opis:

The paper reviews research into karst system recharging the vaucluse springs in the Tatra Mts. Investigations of present-day karst systems are carried out directly with tracer methods, as well as based on interpretations of stationary observations in springs. Direct methods lead to the determination of groundwater migration routes and their rates, with further information from interpretations of results obtained from monitoring the vaucluse springs of the area.

Źródło:

Geological Quarterly; 2003, 47, 1; 97-106
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 30.

Tytuł:

Generowanie numerycznych modeli powierzchni oraz terenu w Tatrach na podstawie chmury punktów z lotniczego skaningu laserowego (ALS)
Generation of digital surface and terrain models of the Tatras Mountains based on airbone laser scanning (ALS) point cloud

Autorzy:

Wężyk, P
Borowiec, N.
Szombara, S.
Wańczyk, R.

Powiązania:

https://bibliotekanauki.pl/articles/131204.pdf

Data publikacji:

2008

Wydawca:

Stowarzyszenie Geodetów Polskich

Tematy:

ALS
NMPT
NMT
znormalizowany NMPT
Tatry
DTM
DSM
nDSM
Tatra Mts.

Opis:

Celem pracy było zaprezentowanie metod zastosowanych w półautomatycznym procesie generowania numerycznych modeli bazujących na chmurze punktów zarejestrowanych technologią lotniczego skaningu laserowego (ang. Airborne Laser Scanning; ALS) w trudnych obszarach wysokogórskich Tatr. Teren badań o powierzchni około 60 km2, obejmował masyw Kasprowego Wierchu, Kuźnice oraz fragment miasta Zakopane ze stokami Gubałówki. Dane ALS pozyskano w 2007 roku w 33 pasach (RIEGL LMS-Q560), w zagęszczeniu, co najmniej 20 pkt/m2. Wpasowania połączonych skanów dokonano w oparciu o pomiary tachimetryczne powierzchni planarnych (dachy budynków) i dowiązanie przez dGPS. Błędy położenia punktów w płaszczyźnie poziomej wahały się w przedziale -0.09÷+0.28 m, a błędy wysokościowe w przedziale od -0.12÷0.14 m (HAE). Wykonawca dostarczył dane osobno z 2 skanerów, dla każdego: pierwsze i ostatnie odbicie impulsu. Ze względu na duży rozmiar plików podzielono ja na mniejsze generując 353 obszary robocze o rozmiarze 500·500 m dla każdego skanera i numeru odbicia. Przeprowadzono filtrację chmury punktów oraz ich klasyfikację do zestawów danych: „low points”, „ground", „low vegetation”, „medium vegetation”, „high vegetation” oraz „air points”. W celu wygenerowania NMPT stworzono klasę „ground_inverse" wymagającą kontroli operatora wspomagającego się ortofotomozaiką cyfrową (RGB\CIR; kamera Vexcel). Dla każdego przetwarzanego obszaru roboczego wygenerowano NMT oraz NMPT. Na podstawie zweryfikowanych modeli wygenerowano znormalizowany numeryczny model powierzchni terenu obrazujący wysokości względne obiektów występujących w obszarze opracowania (drzewa, piętro kosodrzewiny, budynki, linie energetyczne, liny wyciągów, etc). Analizy przestrzenne bazujące na wygenerowanych modelach otwierają zupełnie nowe możliwości licznym badaniom naukowym.
The work presented was aimed at constructing a semi-automatic work-flow of Digital Surface Model (DSM) and Digital Terrain Model (DTM) generation based on an ALS point cloud gathered in a very difficult mountain area. The study area located in the Polish part of the Tatras Mountains covered about 60 km2 and included the Kasprowy Wierch, Kuźnice, and downtown Zakopane with the Gubałówka. ALS data, collected in 2007, consisted of 33 scans (minimum density of 20 points/m2). To combine all the scans and match them to the coordinate system, planar surfaces (building roofs) were measured using a tachimeter and a dGPS survey. Position errors of the ALS points in the horizontal plane varied from -0.09m to +0.28m; height errors ranged from -0.12m to 0.14m (HAE). The operator delivered the data separately from 2 Riegl Q- 560 scanners, for every FE and LE. The ALS files, due to their huge size, were divided into smaller ones and generated 353 sheets (500x500 m in size ) for every scanner and number of returns combination. The point cloud was filtered and assigned to the following levels: "low points”, "ground", "low vegetation”, "medium vegetation”, "high vegetation” and "air points”. To generate a DSM, a special class called "ground_inverse" was created; it required an operator control supported by a digital orthophoto (RGB\CIR; Vexcel camera). For every sheet processed, the DTM and DSM were generated. Those verified models served as a basis for developing an nDSM model using the ER Mapper software. The nDSM shows relative heights of objects in the study area (forest stands, dwarf mountain pines, buildings, power lines, ski lifts, etc.). Development of a precise DSM and nDSM as well as analyses of the nDSM open new perspectives for numerous scientific projects.

Źródło:

Archiwum Fotogrametrii, Kartografii i Teledetekcji; 2008, 18b; 651-661
2083-2214
2391-9477

Pojawia się w:

Archiwum Fotogrametrii, Kartografii i Teledetekcji

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 31.

Tytuł:

Role of land relief and structure in the formation of peat bogs in mountain areas, as exemplified by the Polish Carpathians

Autorzy:

Łajczak, A.

Powiązania:

https://bibliotekanauki.pl/articles/294695.pdf

Data publikacji:

2013

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

raised bog
Carpathian Mountains
Beskidy Mountains
Tatra Mts.
Orawsko-Nowotarska Basin

Opis:

It has been often argued that the formation of peat bogs in the mountains is predominantly influenced by a humid climate. Although in many mountains precipitation during the vegetation growth season is greater than evaporation, bogs, especially of the raised type, do not cover all gently sloping areas and often develop only within certain landforms. Local hydrological conditions determined by land relief and structure are the most crucial factor in the development of bogs in such areas. Peat bogs of the Polish Carpathian Mountains demonstrate that bogs, irrespective of altitude, develop mainly in concave landforms or below convex morphological recesses, where outcrops of poorly permeable rocks offer numerous low-capacity but stable outflows of groundwater that continuously humidifies the slopes lying below thus supporting the formation of habitats for hydrophilic plants. This research project covered the parts of the Polish Carpathians having the largest number of bogs, thus allowing local-scale analysis of their location in relation to the lithological, geomorphological and hydrogeological properties of the substratum. It is assumed that an assessment of the influence of substratum on the location and formation of peat bogs is only correct when the coverage of the individual mires in the period preceding their anthropogenic degradation is known. Only then is it possible to establish what types of bedrock and which landforms are most favourable for bog formation.

Źródło:

Landform Analysis; 2013, 22; 61-73
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 32.

Tytuł:

Accumulation properties of Norway spruce (Picea abies) for different radionuclides

Autorzy:

Tomankiewicz, E.
Mietelski, J.
Gaca, P.
Błażej, S.

Powiązania:

https://bibliotekanauki.pl/articles/148612.pdf

Data publikacji:

2006

Wydawca:

Instytut Chemii i Techniki Jądrowej

Tematy:

137Cs
50Sr
thorium
spruce tree
Tatra Mts.
aggregation coefficients

Opis:

The paper presents results for the 137Cs, 90Sr, 40K activity concentrations and 228Th/232Th, 230Th/232Th activity ratios in several samples needles from two Norway spruce (Picea abies) trees and two soil samples collected in the Tatra Mountains (Poland) area. Activities for artificial 137Cs and 90Sr show moderate values. Statistically different values were found between the mean concentration of 90Sr and 137Cs in current (C) and two years old (C+2) needles of the first tree, whereas for potassium no significant difference was observed. For the second, fallen tree, no significant difference between the mean activity concentration in needles for C+1 and C+2 was found for each radionuclide, but much lower levels of 137Cs contamination were observed. Observed values of the aggregation coefficients for 137Cs and 90Sr are presented.

Źródło:

Nukleonika; 2006, 51,suppl.2; 59-67
0029-5922
1508-5791

Pojawia się w:

Nukleonika

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 33.

Tytuł:

Zarys badań paleobotanicznych czwartorzędu na terenie Tatr, Pienin i Podhala
Overview of palaeobotanical investigations on the Quaternary in the Tatra Mts., Pieniny Mts. and Podhale region

Autorzy:

Hrynowiecka-Czmielewska, A.

Powiązania:

https://bibliotekanauki.pl/articles/2074703.pdf

Data publikacji:

2009

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

badania paleobotaniczne
Tatry
Pieniny
Podhale
palynological investigations
Tatra Mts.
Pieniny Mts.
Podhale Region

Opis:

Palaeobotanical, mainly palynological, investigations, carried out in the Tatra Mts. and Podhale region made it possible to date organic sediments as well as to trace history of migration routes of several plant taxa, mainly trees. The results of pollen analyses allowed for the reconstruction of formation of individual vegetation belts in the Tatra Mts. The development of human settlements was traced on the basis of pollen analyses of the Podhale peat bogs. The decline of the last glaciations (Weichselian) and the Holocene are the best studied periods in this area, as far as palaeobotany is concerned. In the present overview most of earlier studies were taken into consideration.

Źródło:

Przegląd Geologiczny; 2009, 57, 8; 714-718
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

/5

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Skocz do pozycji: 34.

Tytuł:

Tectonic setting of the poszukiwaczy skarbów cave and the GrobyCave (Kraków gorge, western Tatra Mts., Poland)

Autorzy:

Szczygieł, J.
Gaidzik, K.

Powiązania:

https://bibliotekanauki.pl/articles/100852.pdf

Data publikacji:

2012

Wydawca:

Uniwersytet Śląski. Wydział Nauk o Ziemi

Tematy:

jaskinia
tektonika
Tatry
osad
spękanie
cave
tectonics
Tatra Mts.
cover
joint

Opis:

The study area is located in the Tatra Mts., the part of Western Carpathians. In the Poszukiwaczy Skarbów Cave and the Groby Cave a tectonics structures has been documented. The structural analysis were made. In both caves the following joints set have been identified from 4 maximum of statistic analysis: 157/85 (max.I), 143/63 (max.II), 58/63 (max.III), 304/70 (max.IV). Nevertheless joint set participation of individual caves development have been diverse. In the development of the Poszukiwaczy Skarbów Cave, the most important joint set were latitudinal which is conjugate with fractures of III. maximum. This crossing of joints sets contribute to development of the main chamber. Maximum III has been very important in the evolution of passages of the Groby Cave. Conjugated with joint of max. IV determined the conduit direction. Entrance chamber formed in this place because the overthrust disintegrated a rocks there.
Jaskinia Poszukiwaczy Skarbów i Jaskinia Groby zlokalizowane są w Tatrach, w dolnej, zachodniej części Wąwozu Kraków. W jaskiniach wykonano pomiary orientacji struktur tektonicznych. Następnie wykonano analizę strukturalną, która pozwoliła wyznaczyć 4 główne zespoły spękań: 157/85 (max.I), 143/63 (max.II), 58/63 (max.III), 304/70 (max.IV). Udział poszczególnych zespołów spękań w obu jaskiniach był zróżnicowany. W Jaskini Poszukiwacz Skarbów najistotniejszy w rozwoju jaskini jest zespół spękań równoleżnikowych. Jego sprzężenie ze spękaniami III. maksimum uwarunkowało rozwój głównej komory. Spękania maksimum III są również istotne w rozwoju Jaskini Groby. Sprzężone z zespołem spękań max. IV determinowały kierunek korytarzy jaskini. Komora wstępna w Jaskini Groby założona jest na nasunięciu, które przyczyniło się do dezintegracji skał i ułatwiło rozwój sali.

Źródło:

Contemporary Trends in Geoscience; 2012, 1, 1; 93-98
2299-8179

Pojawia się w:

Contemporary Trends in Geoscience

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 35.

Tytuł:

Coarse woody debris in mountain streams and their influence on geomorphology of channels in the Tatra Mts.

Autorzy:

Zielonka, A.
Ciapała, S.
Malina, P.
Piątek, G.

Powiązania:

https://bibliotekanauki.pl/articles/294611.pdf

Data publikacji:

2009

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

dendrochronology
CWD (coarse woody derbis)
stream channel
subalpine forest
Tatra Mts.

Opis:

Dead wood plays important function in the riverine environment. Dead trees lying in stream channels modify the speed of the current and the shape of the channel, thus have a great influence on channel morphology. Coarse woody debris (CWD) exert influence on variation in channel width and gradient as well as promote lateral channel migration and sediment storage. In this paper we study the characteristics of dead wood delivered to two mountain streams, the Waksmundzki Stream and Pyszniański Stream in the Tatra Mts. The inflow of dead trees to the stream channels was determined with the use of dendrochronological methods. In both channels, a similar number of CWD was found – ca. 60 units per 100 m. In the Waskmundzki Stream more logs were aggregated in form of dams than in the Pyszniański Stream. The distribution of diameters, decay classes, and length classes was similar for both streams. Bank erosion is the most common cause of inflow of dead wood to the stream channel. Cross-dating of the moment of death of trees lying in the stream may indicate that inflow of dead wood to the channels is a continuous process. Fragmented remains of dead trees create geomorphological formations like dams and steps, which highly modify the channels.

Źródło:

Landform Analysis; 2009, 10; 134-139
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 36.

Tytuł:

How to find a gold on the touristic path - a gold-mining in the Tatra Mts.
Jak znaleźć złoto na ścieżce turystycznej - kilka słów o górnictwie złota w Tatrach

Autorzy:

Gawęda, A.

Powiązania:

https://bibliotekanauki.pl/articles/344504.pdf

Data publikacji:

2010

Wydawca:

Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Stowarzyszenie Naukowe im. Stanisława Staszica

Tematy:

Tatry
granitoidy
złoto
antymonit
mylonit
Tatra Mts.
granitoids
gold
antimony
mylonite

Opis:

Gold mineralization is known in the Tatra Mts from the 15th century. The historical mining places could be indentified along the present-day touristic paths, which were used in the past as miner's roads. Both gold occurrence and genetically connected antimony mineralization are located in the flat-lying mylonitic zones, dipping 5-10 degree to NW, cutting the Tatra granite. Mylonites are mineralized by quartz and albite. The famous gold-mining galleries are known from Krywań Mt., where gold and antimonite could be found inside quartz veins straight on the touristic path until now. The important sources of gold were also the secondary fluvioglacial deposits. Gold from the Tatra Mts, regardless its origin - both primary and secondary - is of good quality, with Ag content in the range of 1.2-14.8 wt.%. Locally the veinlets of electrum are also observed. Gold in the Tatra Mts. is associated with antimonite. Its crystals are usually coated with secondary antimony oxides and hydroxides. The historical gold-mining places could be of special importance for geotouristic purposes, as they bring the information about both histories of human mining activity in the mountains and about the geological processes, forming the ores, which released the people's strongest emotions for a few thousand years.
Mineralizacja złotem znana jest w Tatrach od XV wieku. Ślady eksploatacji i zorganizowanej działalności górniczej można zaobserwować przy współczesnych ścieżkach turystycznych. Wiele z nich ma niemal identyczny przebieg do starych dróg górniczych. Mineralizacja zlotem oraz związana z nią genetycznie mineralizacja związkami antymonu ulokowane są w obrębie stref mylonitycznych, tnących granit tatrzański. Strefy te są silnie zmineralizowane kwarcem i albitem i zapadają płasko (5-10 stopni) na NW. Najsłynniejsze sztolnie poszukiwaczy złota znajdują się na Krywaniu. Złoto i antymonit tworzą wpryśnięcia w żyłach kwarcowych. Okruchy złotonośnego kwarcu znaleźć można nawet dziś na ścieżce turystycznej. Istotnym ekonomicznie źródłem złota były w przeszłości wtórne osady fluwioglacjalne u stóp Krywania. Złoto tatrzańskie - zarówno to ze źródeł pierwotnych, jak i wtórnych - miało dobrą jakość, a zawartość w nim srebra (Ag) mieściła się w granicach 1,2-14,8 % wag. Pod mikroskopem można lokalnie stwierdzić obecność żyłek i odmieszań elektrum. Kryształy antymonitu, związanego genetycznie ze złotem, są zwykłe pokryte wtórnymi tlenkami i wodorotlenkami antymonu. Miejsca historycznej eksploatacji górniczej w Tatrach pełnią niezwykłe ważną rolę geoturystyczną: są równocześnie źródłem informacji na temat aktywności ludzkiej w terenie górskim, jak również zawierają ważne dla geologów wskazówki na temat procesów geologicznych, prowadzących do powstania złóż, które wywoływały najsilniejsze ludzkie emocje przez wiele tysięcy lat.

Źródło:

Geoturystyka; 2010, 2; 59-64
1731-0830

Pojawia się w:

Geoturystyka

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 37.

Tytuł:

Carbonate-clastic sediments of the Dudziniec Formation in the Kościeliska Valley (High-Tatric series, Tatra Mountains, Poland) : role of syndepositional tectonic activity in facies development during the Early and Middle Jurassic

Autorzy:

Jezierska, A.
Łuczyński, P.
Staśkiewicz, A.

Powiązania:

https://bibliotekanauki.pl/articles/2060544.pdf

Data publikacji:

2016

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

carbonates
clastics
synsedimentary tectonics
Dudziniec Formation
Lower and Middle Jurassic
Tatra Mts.

Opis:

Sediments of the Dudziniec Formation (Lower Jurassic – Aalenian) outcropping in the Kościeliska Valley (autochthonous unit of the High-Tatric series) are represented by a range of mixed carbonate-clastic deposits. Seven lithofacies have been distinguished based on lithology, sedimentary structures, colour and composition of intra- and extraclasts, with sandstones and crinoidal limestones as end members of a continuous spectrum of facies. The study area represents a shallower part of the sedimentary basin located in the vicinity of source areas, as compared to the Chochołowska Valley region located in the west. Facies characteristics and distribution were controlled mainly by synsedimentary tectonic activity, with sandy varieties representing periods of faulting with enhanced influx of extraclasts, and with crinoidal limestones corresponding to intervals of relative tectonic stability. Such influence of synsedimentary tectonics on the deposition in the Early Jurassic strongly resembles the Middle Jurassic development in the High-Tatric area. Neptunian dykes cutting the Dudziniec Formation, and most probably filled by Lower Jurassic sediments, are yet another indication of tectonic instability of the area in the Early Jurassic.

Źródło:

Geological Quarterly; 2016, 60, 4; 869--880
1641-7291

Pojawia się w:

Geological Quarterly

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 38.

Tytuł:

Evolution of the Bystrej Valley caves (Tatra Mts, Poland) based on corrosive forms, clastic deposits and U-series speleothem dating

Autorzy:

Kicińska, D.
Hercman, H.
Najdek, K.

Powiązania:

https://bibliotekanauki.pl/articles/191650.pdf

Data publikacji:

2017

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

cave evolution
scallops
heavy minerals
U-series speleothem dating
palaeohydrology
Tatra Mts.

Opis:

The origin and age of cave deposits, as well as palaeogeographical changes in the Bystrej catchment during the last ca. 250 ka, were reconstructed in Magurska, Kasprowa Niżnia, Goryczkowa, Kalacka and Bystrej caves (the Bystrej Valley). The reconstruction is based on the study of corrosive forms, heavy mineral analyses and U-series dating of speleothems. Two generations of palaeoflows were distinguished by observations of scallops and heavy mineral analyses. In the older stage, now abandoned caves drained massifs surrounding the Bystrej Valley and part of an adjacent valley. The direction of palaeoflow changed as a result of the water capture after Kasprowa Niżnia Cave came into being. In the later stages, the evolution of cave systems was controlled by glaciation-deglaciation cycles. Probably at this time, some caves located in the lowest parts of the massifs also started to be formed. U-series speleothem dating allows the determination of five phases of speleothem deposition: ca. 220–150 ka, ca. 135–105 ka, ca. 95–70 ka, ca. 40–23 ka and during the Holocene.

Źródło:

Annales Societatis Geologorum Poloniae; 2017, 87, 1; 101-119
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 39.

Tytuł:

Zastosowanie metod dendrochronologicznych w badaniach lawin śnieżnych
The dendrochronological methods of snow avalanche investigation

Autorzy:

Kaczka, R. J.
Janecka, K
Lempa, M.
Rączkowska, Z.

Powiązania:

https://bibliotekanauki.pl/articles/294466.pdf

Data publikacji:

2015

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

lawiny śnieżne
dendrochronologia
rekonstrukcja
GIS
Tatry
snow avalanche
dendrochronology
reconstruction
Tatra Mts.

Opis:

Lawiny śnieżne pomimo swojej siły pozostawiają niejednorodny zapis w środowisku. Z tego powodu rekonstrukcja momentu wystąpienia i wielkości lawiny jest zadaniem trudnym. Jednym z pośrednich dowodów ich aktywności są miejsca, gdzie lawiny docierają do lasu pozostawiając swój ślad w skali makro (obniżanie górnej granicy lasu) i mikro (uszkodzenia pojedynczych drzew). Odpowiednio zaadaptowane metody dendrochronologiczne pozwalają datować zdarzenia lawinowe. W wyniku połączenia analiz dendrochronologicznych z innymi metodami badawczymi uzyskujemy wielowymiarowy obraz aktywności lawin w przeszłości. Zastosowanie podstawowych technik dendrochronologicznych do datowania zdarzeń lawinowych zostało omówione na przykładzie wyników badań w Białym Żlebie w Tatrach Wysokich. Opracowana dla tego miejsca rekonstrukcja aktywności lawin obejmuje ponad 100 lat i wskazuje na pięć dużych zdarzeń lawinowych w okresie od 1912 do 2009 roku. Włączenie do analiz technik GIS umożliwiło rozszerzenie rekonstrukcji o elementy przestrzenne, informujące o zasięgu przeszłych zdarzeń.
Despite their strength, snow avalanches leave a very diverse record in the environment. For this reason, the reconstruction of the occurrence, time and magnitude of avalanches is a really demanding task. It can only be performed in places where avalanches reach forests, leaving their marks in the macroscale (lowering the upper timberline) and microscale (damaging individual trees). Appropriately adapted dendrochronological methods allow dating the avalanche events. Combining the dendrochronological analyses with other techniques enables to obtain a multi-dimensional image of avalanche events. The application of the basic dendrogeomorphological techniques is discussed on the example of the results of the research from the Biały Żleb chute located in the High Tatras. The obtained reconstruction of avalanche activity covers more than 100 years and points to five major avalanche events in the period from 1912 to 2009. The employment of GIS techniques allowed to extend the reconstruction by a spatial element indicating the range of the past events.

Źródło:

Landform Analysis; 2015, 28; 15-27
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 40.

Tytuł:

The spatial patterns of the Tatra high - mountain landscape structure

Autorzy:

Boltižiar, M.

Powiązania:

https://bibliotekanauki.pl/articles/294897.pdf

Data publikacji:

2009

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

high-mountain landscape structure
geomorphic forms and processes
spatial patterns
Tatra Mts.

Opis:

The paper focuses on the identification and classification of spatial patterns in the relation to landforms and geomorphic processes considering the middle-scale and micro-scale of the high-mountain landscape. These determine not only the shape of patches or the character of boundaries, but also the character of fragmentation, the heterogeneity of patches, the gradient and the tendency of patches development. Georelief, especially its spatial morphodynamic attributes, represents relevant phenomena of the landscape which facilitate to understand the scale and hierarchy of the landscape structure. The algorithm of this study is based on the spatial identification of landforms, processes and patterns considering large-scale aerial photographs, a field reconnaissance and the partial classification. The main aim of this paper is to create the classification system of spatial patterns as the physiognomic spatial attributes of the landscape structure mosaic in the high-mountain areas. The genesis of spatial structure patterns and their formation enables us to understand better the origin of the high-mountain landscape structure, its function and contents in this environment. Such a classification can be regarded as a basis for the quantitative statistic analyses of the landscape structure and for the detailed research of spatial patterns.

Źródło:

Landform Analysis; 2009, 10; 11-17
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 41.

Tytuł:

Preliminary results of fractal analysis of the poligonal survey from cave: case study of Małołączniak area (Tatra Mts.)

Autorzy:

Szczygieł, J.
Mendecki, M. J.

Powiązania:

https://bibliotekanauki.pl/articles/1395716.pdf

Data publikacji:

2013

Wydawca:

Uniwersytet Śląski. Wydział Nauk o Ziemi

Tematy:

badanie
jaskinia
Tatry
fractal dimension
cave survey
box counting technique
Tatra Mts.

Opis:

Traverses (polygons) from two caves have been tested: Wielka Śnieżna Cave System (2858 vectors) and Śnieżna Studnia cave (742). The box counting technique was applied to evaluate the fractal analysis of spatial orientation of traverses. The polygonal survey of Wielka Śnieżna Cave, Śnieżna Studnia and both caves merged together have a fractal geometry. It may be concluded that these caves are close to the full recognition of passages forming by a hydrological system and they could have close relation with geological structures. The usual explanation of fractal dimension D higher than 1 indicates that caves with such dimension fill more space than those with ideal dimension of 1.00 (for example a straight line), and the geological constraints limit the dimension to be lower than 2 (Verbovsek 2007). It may suggest that systems can be developped into more complicated passages in future. The fact that both caves merged together also have showed fractal geometry indicates that they are belonging to the same hydrological system. It was noticed that D-value of merged caves is slightly larger than individual cave. It can be explained by “occupying” more space in rock mass.

Źródło:

Contemporary Trends in Geoscience; 2013, 2, 1; 95-100
2299-8179

Pojawia się w:

Contemporary Trends in Geoscience

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 42.

Tytuł:

Z dziejów budowy kościoła w Poroninie. Architektura Franciszka Mączyńskiego pod Tatrami
From the history of building the church in Poronin

Autorzy:

Bentkowska-Mitana, A.

Powiązania:

https://bibliotekanauki.pl/articles/369300.pdf

Data publikacji:

2011

Wydawca:

Zachodniopomorski Uniwersytet Technologiczny w Szczecinie. Wydawnictwo Uczelniane ZUT w Szczecinie

Tematy:

kościół
Poronin
Mączyński
architektura sakralna
Tatry
church
Maczynski
sacred architecture
Tatra Mts.

Opis:

Kościół parafialny w Poroninie pod wezwaniem św. Marii Magdaleny jest wyjątkową wizytówką nie tylko Podhala, ale także Małopolski. Został on zaprojektowany przez Franciszka Mączyńskiego, jednego z najwybitniejszych architektów krakowskich działających na przełomie XIX i XX wieku. Budowlę zaczęto wznosić w 1917 roku niedługo po pożarze, który strawił drewniany kościół. Oryginalny, zachowany projekt kościoła Franciszka Mączyńskiego, znacznie rożni się od jego teraźniejszego kształtu. Największą zmianą w projekcie Franciszka Mączyńskiego wydaje się być wieża. Architektura kościoła w Poroninie pokazuje wielki talent projektanta, który potrafił łączyć różne style wręcz idealnie. Co więcej, budowla harmonijnie wpisuje się w otaczająca ją przestrzeń.
Tha parish church in Poronin dedicated to the Saint Mary Magdalene is an exceptional architectural landmark not only in Podhale but also in the Malopolska province. It was designed by Fr. Maczynski, one of the best architects in Cracow at the turn of the 20th centuries. They started to put up the church in 1917, not long after the previous wooden church had burnt down. Its original project has a lot of differences that can be seen in the draft which survived and was published in 'The history fo the church in Poronin" written by T. Bafia and B. Nocon, but the most important change seems to be the tower. Comparing this church to other parish churches in Podhale an obvious difference can be seen. It shows great talent of its designer who compiled different style s perfectly. What is more, it harmouniously incorporates to the neighbouring area.

Źródło:

Przestrzeń i Forma; 2011, 15; 377-390
1895-3247
2391-7725

Pojawia się w:

Przestrzeń i Forma

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 43.

Tytuł:

Morphotype variation of orthophragminids as a palaeoecological indicator: A case study of Bartonian limestones, Pod Capkami Quarry, Tatra Mts, Poland

Autorzy:

Machaniec, E.
Jach, R.
Gradziński, M.

Powiązania:

https://bibliotekanauki.pl/articles/191441.pdf

Data publikacji:

2011

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

Larger benthic foraminifera
orthophragminids
morphotype
transgression
palaeoenvironment
Eocene
Tatra Mts.
Western Carpathians

Opis:

Nummulites-Discocyclina bioclastic packstone and Discocyclina rudstone occur in the transgressive sequence of the Middle–Upper Eocene deposits in the Tatra Mts. The succession of the studied facies is a direct response to a rapid environmental change, related to progressive deepening. Facies transition from Nummulites- Discocyclina bioclastic packstone of proximal mid-ramp to Discocylina rudstone of distal mid- and outer-ramp is an exemplary record of a deposition during deepening conditions. Increasing of diversity of the genus Discocyclina, decreasing of diversity of other foraminifera up the section and vertical variation of orthophragminid mor- photypes from the ovate- through saddle- to the disc-shaped tests are related to deepening and shadowing of the depositional environment.

Źródło:

Annales Societatis Geologorum Poloniae; 2011, 81, No 2; 199-205
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 44.

Tytuł:

Evidence of bacteriogenic iron and manganese oxyhydroxides in Albian-Cenomanian marine sediments of the Carpathian realm (Poland)

Autorzy:

Bąk, M.
Bąk, K.
Górny, Z.
Stożek, B.

Powiązania:

https://bibliotekanauki.pl/articles/191443.pdf

Data publikacji:

2015

Wydawca:

Polskie Towarzystwo Geologiczne

Tematy:

iron
manganese
iron-related bacteria
Albian–Cenomanian
Silesian Nappe
Tatra Mts.
Carpathians

Opis:

The Albian and Cenomanian marine sediments of the Silesian and Tatric basins in the Carpathian realm of the Western Tethys contain ferric and ferromanganese oxyhydroxides, visible macroscopically as brown stainings. They coat calcareous bioclasts and mineral clasts, fill pore spaces, or locally form continuous, parallel microlayers, tens of micrometers thick. Light-microscope (LM) and scanning-electron-microscope (SEM) obser- vations show that the coatings contain elongated capsules, approximately 3–5 µm across and enriched in iron and manganese, which may be remnants of the original sheaths of iron-related bacteria (IRB). Moreover, the ferric and ferromanganese staining observed under LM is similar to bacterial structures, resembling the sheaths, filaments and rods formed by present-day bacteria of the Sphaerotilus–Leptothrix group. All of the possible bacteria-like structures are well preserved owing to processes of early diagenetic cementation. If the observed structures are fossil IRB, these organisms could have played an important role in iron and manganese accumulation on the sea floor during Albian–Cenomanian time. The most plausible source of metals for bacterial concentration in the Silesian Basin might have been submarine low-temperature hydrothermal vents, as previously was hypothesized for Cenomanian–Turonian deposits on the basis of geochemical indices.

Źródło:

Annales Societatis Geologorum Poloniae; 2015, 85, 2; 371-385
0208-9068

Pojawia się w:

Annales Societatis Geologorum Poloniae

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 45.

Tytuł:

Changes in the spruce forests of the Polish Tatra Mts. during the last 80 years

Autorzy:

Kozłowska, A.

Powiązania:

https://bibliotekanauki.pl/articles/294585.pdf

Data publikacji:

2009

Wydawca:

Stowarzyszenie Geomorfologów Polskich

Tematy:

spruce forests
Polish Tatra Mts.
floristic changes during 80 years
vegetation typology

Opis:

On the basis of the historical (dating from the 1920s) and contemporary phytosociological relevés, taken in the spruce forests of the Polish Tatra Mts., the changes were determined that took place in these forests. This area had been for centuries under the influence of human economic activities, mainly pasturing and wood extraction, and then protected in the Tatra National Park. These changes differ according to the altitudinal vegetation belts. In the coniferous forests of the upper montane belt, the changes due to wind breaks or tree stand ageing did not lead to transition to other forest associations. A tendency can yet be noticed of losing a part of the species combinations characteristic for the associations or higher syntaxonomic units, which might be linked with the stopping of grazing in the forests and development of the undergrowth of tall herb character. The association of the fir-and-spruce forests in the lower montane belt displayed much bigger changes. There was an increase of the role of species of the deciduous forests, while the role of the coniferous forest species was limited in the studied patches, which clearly indicates the evolution of the forests towards the beech woods, typical for the lower montane belt. This means a progressing limitation of the spruce forests in the limestone Tatras to the advantage of return of the beech woodsdominated there in older time.

Źródło:

Landform Analysis; 2009, 10; 64-69
1429-799X

Pojawia się w:

Landform Analysis

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 46.

Tytuł:

Radionuclides 137Cs and 40K in the soils of the Tatra National Park (TPN, Poland)

Autorzy:

Kubica, B.
Skiba, S.
Drewnik, M.
Stobiński, M.
Kubica, M.
Gołaś, J.
Misiak, R.

Powiązania:

https://bibliotekanauki.pl/articles/148560.pdf

Data publikacji:

2010

Wydawca:

Instytut Chemii i Techniki Jądrowej

Tematy:

137Cs
40K
Tatra Mts.
gamma spectrometry
maps of the radioisotopes

Opis:

The paper presents the results of radioactivity determination of artificial 137Cs and natural 40K in soil samples taken from the Tatra Mountains in Poland (Tatra National Park – TPN). Soil samples were collected as the cores of 10 cm in diameter and 10 cm in depth. These cores were divided into 3 slices. It has been found that the content of 137Cs was the highest at the sites of the altitude over 1300 m a.s.l. The values of 137Cs concentration in the soils examined varied – from 55.8 Bqźkg–1 (dry mass) (417.8 Bqźm–2) for the Tomanowa Pass (1685 m a.s.l.) to 5111 Bqźkg–1 (dry mass) (8400 Bqźm–2) for the Krzyzne Pass (2112 m a.s.l.). In most cases, the values were lower than the average radiocaesium concentration established for Poland.

Źródło:

Nukleonika; 2010, 55, 3; 377-386
0029-5922
1508-5791

Pojawia się w:

Nukleonika

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 47.

Tytuł:

Kolej zębata Śtrba - Śtrbske Pleso

Autorzy:

Graff, M.

Powiązania:

https://bibliotekanauki.pl/articles/251935.pdf

Data publikacji:

2014

Wydawca:

Instytut Naukowo-Wydawniczy TTS

Tematy:

kolej zębata
Słowacja
Tatry
Strbske Pleso
Strba
rack railway
Slovakia
Tatra Mts.

Opis:

Znajdująca się w słowackich Tatrach kolej zębata Śtrba -Śtrbske Pleso łączy dwie stacje: pierwszą, położoną przy linii magistralnej Bratysława - Żylina - Koszyce, i drugą przy Jeziorze Szczyrbskim, będącą jednocześnie stacją końcową TEŹ (sł. Tatranske Elektricke Źeleznicej). Na trasie kolei zębatej Śtrba -Śtrbske Pleso znajduje się jedna stacja pośrednia - Tatransky Lieskovec.

Źródło:

TTS Technika Transportu Szynowego; 2014, 3; 25-28
1232-3829
2543-5728

Pojawia się w:

TTS Technika Transportu Szynowego

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 48.

Tytuł:

Budowa geologiczna masywu Ciemniaka na podstawie danych z Jaskini Małej w Mułowej (Tatry Zachodnie)
Geological structure of the Ciemniak Massif on the basis of data from the Mała Cave in Mułowa (Western TatraMts.)

Autorzy:

Szczygieł, J.
Borowska, U.
Jaglarz, P.

Powiązania:

https://bibliotekanauki.pl/articles/2075153.pdf

Data publikacji:

2014

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

cave
tectonics
High-Tatric Unit
Tatra Mts.
jaskinia
tektonika
Wysokie Wierchy
Tatry

Opis:

The Mała Cave in Mułowa has been explored to a depth of 555 m at the beginning of the 21th century. It makes a good opportunity to review the knowledge on the geological structure of the Ciemniak Massif. The geological research was performed in two main conduits of the cave. The Mała Cave in Mułowa developed in Lower and Middle Triassic carbonates belonging to the dziary Unit (CzerwoneWierchy Nappe – part of the High-Tatric Allochthon), as well as in marly shales of the Zabijak Formation and limestones of the Wysoka Turnia Limestone Formation belonging to the High-Tatric Autochthon. The cave is the second outcrop of the lower limb of the main syncline of the dziary Unit. It follows that the dziary Unit in the Ciemniak area is represented by a recumbent, open syncline with completely preserved both limbs. This syncline is open northtoward . The fold axes are subhorizontal and the axis surface is inclined ~37o N. From a depth of 300 m (below the entrance), the cave was formed at the contact of Cretaceous rocks belonging to the autochthonous cover and Triassic rocks of the dziary Unit.

Źródło:

Przegląd Geologiczny; 2014, 62, 7; 349--355
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 49.

Tytuł:

Nowe znalezisko śladów dinozaurów w górnym triasie Tatr
A new find of dinosaur footprints in the Upper Triassic of the Tatra Mountains, southern Poland

Autorzy:

Niedźwiedzki, G.

Powiązania:

https://bibliotekanauki.pl/articles/2074394.pdf

Data publikacji:

2005

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

górny trias
ślad dinozaura
Tatry
Upper Triassic
Rhaetian
dinosaur footprints
Tatra Mts.

Opis:

New material of dinosaur footprints has been found in the Late Triassic fluvial-lacustrine deposits of the Tatra Mountains, Poland. Footprints discovered in a well-known Rhaetian strata of the Tomanová Formation represent pedal ichnites of Kayentapus sp. and Anomoepus sp. These are the second reported record of dinosaur footprints in the Tatra Mountains.

Źródło:

Przegląd Geologiczny; 2005, 53, 5; 410--413
0033-2151

Pojawia się w:

Przegląd Geologiczny

Dostawca treści:

Biblioteka Nauki

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Skocz do pozycji: 50.

Tytuł:

Agresywność wód powierzchniowych i podziemnych zlewni Białego Potoku (Tatry Zachodnie)
Aggressiveness of surface and ground water of the Biały Stream Basin (West Tatra Mts.)

Autorzy:

Szostakiewicz-Hołownia, M.

Powiązania:

https://bibliotekanauki.pl/articles/2062825.pdf

Data publikacji:

2009

Wydawca:

Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy

Tematy:

agresywność wód
model geochemiczny
Tatry Zachodnie
water aggressiveness
geochemical model
West Tatra Mts.

Opis:

Agresywność wód to ich właściwość powodująca niszczenie skał. W konsekwencji jest ona jednym z czynników modelujących powierzchnię Ziemi. Ponadto warunkując rozpuszczanie ośrodka skalnego istotnie wpływa na właściwości fizykochemiczne i skład jonowy wód powierzchniowych i podziemnych. W artykule przedstawiono wyniki oceny agresywności wód opadowych powierzchniowych i podziemnych zlewni potoku Białego. Badany obszar jest zbudowany głównie ze skał węglanowych (dolomitów i wapieni). Do oceny agresywności badanych wód wykorzystano twardość ogólną, indeks Langeliera oraz wskaźnik nasycenia wód względem węglanu wapnia obliczony programem PHREEQC.
Aggressiveness is the property of water, which causes destruction of rocks. The aggressiveness is also one of the major factors controlling the Earth surface and chemical composition of water. The paper presents the results of estimation of aggressiveness of precipitation, surface and ground waters. The study area (Biały Stream Basin) is composed mainly of carbonates. The amount of aggressiveness was estimated using the hardness of water, Langelier Saturation Index and SI values calculated by PHREEQC.

Źródło:

Biuletyn Państwowego Instytutu Geologicznego; 2009, 436, z. 9/2; 515-521
0867-6143

Pojawia się w:

Biuletyn Państwowego Instytutu Geologicznego

Dostawca treści:

Biblioteka Nauki

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