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Wyszukujesz frazę "Wozniak, P." wg kryterium: Autor


Wyświetlanie 1-5 z 5
Tytuł:
Kamieniołom Sadowa Góra w Jaworznie : przyszłość pod znakiem GEOsfery!
Sadowa Góra quarry in Jaworzno : future under the sign of GEOsphere!
Autorzy:
Woźniak, P.
Krzeczyńska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075100.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Sadowa Góra quarry in Jaworzno
geotourism
Eco-Geological Education Centre GEOsphere project
kamieniołom Sadowa Góra w Jaworznie
geoturystyka
Geologiczne Centrum Edukacyjne
projekt GEOsfera
Opis:
Due to initiative of both theGeological administration at Jaworzno's City hall as well as Polish Geological Institute-NRI Upper Silesian Branch, a project on the Sadowa Góra Eco-Geological Educational Centre facility has been realized. The project has been supported financially by the EU and its European Regional Development Fund under the Regional Operational Programme for the Silesian University and done in 2007–2013. The implementation of the programme was divided into two parts. The primary one concentrated on the comprehensive technical and educational exploitation of the old Sadowa Góra quarry. The secondary one consisted of plans to build an educational and museum-like facility. The educational centre is planned as a focal point of Jaworzno and its residents. The GEOsphere completion (phase I) ought to be achieved by May 2014.
Źródło:
Przegląd Geologiczny; 2014, 62, 10/1; 510--513
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Oblicza geologii - przykładowe projekty ścieżek geoturystycznych
Faces of geology - examples of project of geotouristic trails
Autorzy:
Krzeczyńska, M.
Woźniak, P.
Powiązania:
https://bibliotekanauki.pl/articles/2074864.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
szlaki turystyczne
geoturystyka
różnorodność geologiczna
touristic paths
geotourism
geological diversity
Opis:
In order to enhance its touristic and environmental offer with new geology facilities, Polish Geological Institute – National Research Institute has started to design new geotouristic paths in Poland. These paths will have a positive economic boost on the areas and at the same time utilize certain components of abiotic environment. They will also expose the true value of geology facilities in particular parts and geological diversity of the entire country. Several projects of fresh paths in different areas of Poland have been developed. Due to the support of local authorities, four of them have become existent recently. The rest of them are still being implemented or are looking for a financial aid. Two of those paths were designed for the online usage and they function as virtual strolls. They are available at this website: http://geoportal.pgi.gov.pl/portal/page/portal/muzeum.
Źródło:
Przegląd Geologiczny; 2011, 59, 4; 340-351
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Głazy narzutowe Trójmiejskiego Parku Krajobrazowego : potencjał badawczy i geoturystyczny
Erratic boulders of the Trójmiejski Landscape Park : potential for research and geotourism
Autorzy:
Woźniak, P. P.
Tylmann, K.
Kobiela, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075272.pdf
Data publikacji:
2015
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
głazy narzutowe
petrografia
nuklid
geoturystyka
antropopresja
Trójmiejski Park Krajobrazowy
erratic boulders
petrography
terrestrial cosmogenic nuclides dating
geotourism
anthropopression
Trójmiejski Landscape Park
Opis:
The paper presents the results of erratic boulders studies in the area of Trójmiejski Landscape Park (TLP) located west of the Gulf of Gdañsk. The research objects were boulders protected as natural monuments (66 erratics) and all boulders with long axis ³ 50 cm within two testing areas (1100 erratics). Results show that erratics of the TLP often occur in clusters and their spatial density is even near 300 items/km2 in some areas. The authors selected 44 boulders which may be interesting research objects and/or have high values for geotourism. Nine erratics reveal features potentially suitable for the terrestrial cosmogenic nuclides (TCN) dating. Moreover, high number of boulders in the TLP area gives the possibility for investigations of the directions of glacial paleo-transport based on indicator erratics and analysis of glacial striae. Distinctive zones of significant clusters of boulders characterised by high attractiveness and diversified values were also indicated.
Źródło:
Przegląd Geologiczny; 2015, 63, 4; 256--262
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geopark Góra Św. Anny – "król-tułacz" wrócił na stolicę!
The St. Annes Mountain Geopark - "The King Wanderer" is back on his throne!
Autorzy:
Woźniak, P.
Sikora, R.
Lasoń, K.
Markowiak, M.
Haisig, J.
Szulc, J.
Hagdorn, H.
Powiązania:
https://bibliotekanauki.pl/articles/2074853.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Góra Św. Anny
geopark
geoturystyka
edukacja geologiczna
St. Anne's Mountain
geoturism
geologic education
Opis:
Due to numerous geological phenomena on a virtually small territory, the St. Anne's Mountain and its areas has an excellent chance to become one of the most significant geotouristic regions in Poland. The designed geopark, apart from its main goal which is to promote the earth education, will also affect the tourism and economy growth within the region. The area will enable us to look into the future of our planet through the prism of processes, which created its environment in the past. Discovering the earth mysteries, acquainting oneself with the contents of drafted plates, and close contact to geology will encourage people, especially the younger generation, to explore the adjacent surroundings and the whole world. The St. Anne's Mountain was given national status by the Ministry of the Environment on the basis of the review, made by the Polish Geological Institute - National Research Institute Upper Silesian Branch in Sosnowiec, entitled: The St. Anne's Mountain Geopark - the documentation and suggestions on its protection. Research along with observation results on the field and laboratory works between 2008 and 2010 were included in the above mentioned review.
Źródło:
Przegląd Geologiczny; 2011, 59, 4; 291-310
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A new stratigraphic position of some Early Pleistocene deposits in central Poland
Autorzy:
Bujak, Ł.
Woronko, B.
Winter, H.
Marcinkowski, B.
Werner, T.
Stachowicz-Rybka, R.
Żarski, M.
Woźniak, P. P.
Rosowiecka, O.
Powiązania:
https://bibliotekanauki.pl/articles/2060173.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Late Miocene
Early Pliocene
Early Pleistocene
pollen analysis
palaeomagnetism
mineralogy
Central Poland
Opis:
A new borehole in Rożce (SW Mazovian Lowland) drilled in 2012, combined with a wide variety of research methods (palaeomagnetism, palynological analysis, studies of plant macroremains and textural features of deposits) shed new light on the age and stratigraphic position of the Early Pleistocene deposits, formerly assigned as the Lower Pleistocene. The study focuses on the deposits from 50.7-104.0 m depth, between glacial till of the Nidanian Glaciation (ca. 0.9 Ma) and the Poznań Clays (ca. 5.322 Ma). The deposits situated directly underneath the till (50.7-60.2 m) are related to the Nidanian Glaciation and show a reversed polarity and correlate with the end of the Matuyama Epoch. The deposits from 60.2-104.0 m depth were accumulated during the Early Pliocene, i.e. approximately 5.332-4.6 million years ago. They appear to correlate with the middle part of the Gilbert Palaeomagnetic Epoch and thus they are considerably older than previously thought. The cored section indicates a stratigraphic gap of about 3.5 Ma from the Lower Pliocene to the first advance of the Scandinavian ice sheets into Poland, which are thought to have occurred in the early Middle Pleistocene. The analysed deposits accumulated under variable climatic conditions showing two periods with significant aridity alternated with two periods of increased humidity. Deposits of the arid periods contain no pollen, butaeolian sand quartz grains are found. During periods of more humid climate the area was covered by various types of mixed forest.
Źródło:
Geological Quarterly; 2016, 60, 1; 238--251
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-5 z 5

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