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Języki publikacji
Abstrakty
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.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
95--100
Opis fizyczny
Bibliogr. 14 poz., rys., tab.
Twórcy
autor
- Department of Fundamental Geology, Faculty of Earth Science, University of Silesia, Bedzińska Str. 60, 41-200 Sosnowiec
autor
- Department of Applied Geology, Faculty of Earth Science, University of Silesia, Bedzińska Str. 60, 41-200 Sosnowiec
Bibliografia
- 1. Bac-Moszaszwili M., Burchart J., Głazek J., Iwanow A., Jaroszewski W., Kotanski Z., Lefeld J., Mastella L., Ozimkowski W., Roniewicz P., Skupiński A., Westwaliwicz-Mogilska E., (1979). Geological Map of Polish Tatra Mts. 1:30 000, Wyd. Geol., Warszawa.
- 2. Curl, R. l. (1986). Fractal dimensions and Geometries of Caves. Mathematical geology, 18(8), 765-783.
- 3. Falconer K. (2003). Fractal Geometry. Mathemat ical Foundations and Applications. Wiley, Chichester
- 4. Fuja D., Filar F., Albrzykowski G. (2002) survey data of the Śnieżna Studnia Cave, unpublished.
- 5. Grodzicki J ,Kardaś R (1989). Tectonics of the Czerwone Wierchy (Massif Tatra Mts.) in the light on observations in caves. Annales Societatis Geologorum Poloniae, 59, 275-293 (In Polish).
- 6. Kardaś R. (2002). survey data of the Wielka Śnieżna Cave , unpublished.
- 7. Kortas L. (2003). Analiza wybranych parametrów dynamiki nieliniowej dla sejsmiczności naturalnej i indukowanej. PhD Thesis, AGH-Uniwersity, Krakow (In Polish).
- 8. Kusumayudha, S. B., Zen, M. T., Notosiswoyo, S., & Guatama, R. S. (2000). Fractal analysis of the Oyo River , cave systems , and topography of the Gunungsewu karst area and Food Research Organization (NARO), Japan who permitted usage of NARO software for box-counting technique, central Java , Indonesia. Hydrogeology Journal, 8, 271-278.
- 9. Małecka D. (1993). Hydrogeologia krasu tatrzańskiego, In: Jaskinie Tatrzańskiego Parku Narodowego, Jaskinie wschodniego zbocza Doliny Kościeliskiej, J. Grodzicki (eds.), Wyd. TPN i PTPNoZ, 3, 11-33 (in Polish).
- 10. Piotrowska K, Cymerman Z, Rączkowski W, (2009). Detailed geological map of the Tatra Mts. in scale 1:10000 – sheet Czerwone. National Geological Institut-Polish ReserchInstitut. Warszawa.
- 11. Sasaki H. (1994). Fraktal Analysis System for Windows. Website (access 15th of August 2013) http://cse.naro.affrc.go.jp/sasaki/fractal/fractal-e.html
- 12. Szczygieł J. (2013). The role of fold-andthrust structure in the large shafts and chambers development: case study of the Polish Tatra Mts. In: Proceedings of 16th International Congress of Speleology
- 13. Filippi M., Bosak P. (red.), 3: 137-143. Teper L. (1998). Wpływ nieciągłości podłoża karbonu na sejsmotektonikę połnocnej części Gornośląskiego Zagłębia Węglowego, Wyd. Uniw. Śląskiego, Katowice (In Polish).
- 14. Verbovsek, T. (2007). Fractal analysis of the distribution of cave length in Slovenia. Acta Carsologica, 36(3), 369-377.
Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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