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The Quaternary transformation of older inherited mountain landscapes

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Quaternary transformation of the inherited mountain relief was controlled by three factors: cyclic climatic changes, resistance of the substratum and neotectonic uplift. Cyclic climatic fluctuations in the majority of European mountains were reflected in the alternation of interglacial and cold stages, the former characterized by a dominance of forest and chemical weathering, the latter by permafrost, solifluction, wind activity and, at higher elevations, by glacier advances. The transitinal phases played an important role as periods of reestablishment of water circulation and transfer of regolith and sediment, formed during the previous cold or interglacial stage. The rates of degradation of inherited planation surfaces and slopes depend on bedrock resistance. In the case of less resistant flysch deposits, degradation during a single (last) cold stage reached 10 metres. Therefore, the higher planation levels may have been either better preserved on more resistant bedrock or even emphasized by cryoplanation processes. The lowest piedmont developed on less resistant beds was lowered to 50 m. In the young mountains, the Quaternary uplift may have played an additional role. In the case of uplift reaching or exceeding several hundred metres, the former fluvial forms were shifted to the cryonival or even nival (glacial) vertical zone where they became entirely transformed.
Rocznik
Tom
Strony
53--60
Opis fizyczny
Bibliogr. 34 poz., rys., wykr.
Twórcy
autor
  • Polish Academy of Sciences, Institute of Geography and Spatial Organization, Department of Geoenvironmental Research; 31-018 Krakow, sw. Jana 22
Bibliografia
  • Baumgart-Kotarba M., Dec J., Kotarba A., Ślusarczyk R., 2008. Glacial trough and sediment infill of the Biała Woda valley (the High Tatra Mountains) using geophysical and geomorphological methods. Studia Geomorphologica Carpatho-Balcanica 42, 75–108.
  • Clapperton C. M., Sudgen D. E., 1977. The Late Devensian glaciations of North-East Scotland. [in:] Studies in the Scotish Lateglacial Environment. Pergamon Press, Oxford, 15–32.
  • Czudek T., Demek J., 1973. Die Reliefentwicklung während der Dauerfrostbodendegradation. Rozprawy CSAV, Praha, 83, 2, 67 pp.
  • Dziewański J., Starkel L., 1967. Slope covers on the middle terrace at Zabrodzie upon the San. Studia Geomorphologica Carpatho-Balcanica 1, 21–35.
  • Gansser A., 1964. Geology of the Himalayas. Interscience Publishers, London, 350 pp.
  • Gębica P., 2004. Przebieg akumulacji w górnym vistulianie w Kotlinie Sandomierskiej. Prace Geograficzne IGiPZ PAN 193, 229 pp.
  • Hradecky J., Panek T., Smolkova V., Šilhan K., 2011. Weichselian alluvial fan at the foot of the Moravskoslezske Beskidy. Excursion Guide-Book, Carpatho-Balcan-Dinaric Conference on Geomorphology, Ostravice, 11.
  • Klimaszewski M., 1971. The effects of solifluction processes in the development of mountain slopes in the Beskidy (Flysch Carpathians). Folia Quaternaria 38, 1–8.
  • Kostienko N. P., 1962. The most characteristic neotectonic features of Hissar-Alay Pamir and Tadzhic Depression (in Russian). [in:] Materialy Sovieshchanja, Tadzhik University, Duszanbe, 113–136.
  • Kowalkowski A., Starkel L., 1984. Altitudinal belts of geomorphic processes in the Southern Khangai Mts. (Mongolia). Studia Geomorphologica Carpatho-Balcanica 18, 95–115.
  • Linton D. L., 1955. The problem of tors. Geographical Journal 121, 470–487.
  • Margielewski W., 2006. Records of the Late Glacial — Holocene palaeoenvironmental changes in landslide forms and deposits of the Beskid Makowski and Beskid Wyspowy Mts. area (Polish Outer Carpathians). Folia Quaternaria 76, 149 pp.
  • Mazur E., 1963. Żilinska Kotlina a prilahle pohoria (geomorphologia a kvarter). Slovenska Akademia Vied, Bratislawa, 186 pp.
  • Migoń P., 2011. Geomorphic diversity of the Sudetes — effects of structure and global changes super-imposed. Geographia Polonica 84, Spec. Issue, part. 2., 93–105.
  • Minar J., Bielik M., Kovac M., Plašienka D., Barka I., Stankoviansky M., Zeyen H., 2011. New morphostructural subdivision of the Western Carpathians: An approach intergrating geodynamics into targeted morphometric analysis. Tectonophysics 502, 158–174.
  • Minar J., Bizubova M., Gallay M., 2004. General aspects of denudation chronology of the West Carpathians. Studia Geomorphologica Carpatho-Balcanica 38, 5–22.
  • Pellegrini G. B., Surian N., Albanese D., 2006. Landslide activity in response to alpine deglaciation: the case of the Belluno Prealps (Italy). Geogr. Fisica Dinamica Quaternaria 29, 185–196.
  • Pękala K., Repelewska-Pękalowa J., 1993. Solifluction and retreat slope processes in the mountains of Central Asia (Mongolia). Paläoklimaforschung 11, Akad. der Wissenschaften, Mainz, 87–101.
  • Sobolewska M., Starkel L., Środoń A., 1964. Młodoplejstoceńskie osady z florą kopalną w Wadowicach. Folia Quaternaria 16, 1-60.
  • Starkel L., 1960. Periglacial covers in the Beskid Wyspowy (Carpathians). Biuletyn Peryglacjalny 8, 155–169.
  • Starkel L., 1965. Rozwój rzeźby polskiej części Karpat Wschodnich. Prace Instytutu Geografii PAN 50, 157 pp.
  • Starkel L., 1968. Remarques sur l’etagement’ des processes morphogenetiques dans les Carpates au cours de la derniere glaciations. Biuletyn Peryglacjalny 17, 205–220.
  • Starkel L., 1969. L’evolution des versants des Carpates a flysch an Quaternarie. Biuletyn Peryglacjalny 18, 349–379.
  • Starkel L., 1980. Altitudinal zones in mountains with continental climate. Prace Geograficzne IG PAN 136, 91–96.
  • Starkel L., 1985. Controversial opinions on the role of tectonic movements and climatic changes in the Quaternary evolution of the Polish Carpathians. Studia Geomorphologica Carpatho-Balcanica 19, 45–60.
  • Starkel L., 1987 a. Long term and short-term rhythmicity in terrestrial landforms and deposits. [in:] Climate: History Periodicity and Predictability. M. R. Rampino et al. (ed.), van Nostrand Reinhold, New York, 323–332.
  • Starkel L., 1987 b. The role of the inherited forms in the present-day relief of the Polish Carpathians. [in:] International Geomorphology 1986. Part. 2, V. Gardiner (ed.), J. Wiley, 1030–1045.
  • Starkel L., 1995. Evolution of the Carpathian valleys and the Forecarpathian Basins in the Vistulian and Holocene. Studia Geomorphologica Carpatho-Balcanica 29, 5–40.
  • Starkel L., Gębica P., Superson J., 2007. Last Glacial-Interglacial cycle in the evolution of river valleys in southern and central Poland. Quaternary Science Reviews 26, 2924–2936.
  • Valdiya K. S., 1998. Dynamic Himalaya. Educational Monographs, University Press, India, 178 pp.
  • Zheng B., Jiao K., 1991. Quaternary glaciations and periglaciations in the Qinghai — Xizhang (Tibetan) Plateau. [in:] Excursion Guidebook XI, INQUA XIII International Congress, Beijing, 54 pp.
  • Zuchiewicz W. 1984. The late Neogene-Quaternary tectonic mobility of the Polish West Carpathians. A case study of the Dunajec drainage basin. Annales Societatis Geologorum Poloniae 54, 133–189.
  • Zuchiewicz W., 2010. Neotektonika Karpat Polskich i zapadliska przedkarpackiego. Wydawnictwo AGH, Kraków, 234 pp.
  • Zuchiewicz W., 2011. Planation surfaces in the Polish Carpathians: myth or reality. Geographia Polonica 84, Spec. Issue, part. 2, 155–178.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-10e784ff-451c-4cfe-abb2-8e4780304ec3
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