Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
The Schmidt hammer method was successfully used in determining early stages of weathering of glacially-abraded Jurassic limestone surfaces within the post-LIA forefield of the Biferten glacier (Switzerland).It was shown that the formerly glaciated landforms are differentiated in terms of mean and maximum R-values and when comparing between standard deviation of R-values from polished and non-polished surfaces.It is concluded that the most important factors in R-value differentiation within the young marginal zones are duration of weathering and rock structure.However, the first factor can only be detected on non-polished surfaces.
Czasopismo
Rocznik
Tom
Strony
11--15
Opis fizyczny
Bibliogr. 21 poz., rys.
Twórcy
autor
- Department of Geomorphology, Faculty of Geography and Regional Studies,University of Warsaw, Krakowskie Przedmieście 30, 00-927 Warsaw, Poland, mfdbski@uw.edu.p
Bibliografia
- Aa A.R. & Sjastad J.A., 2000. Schmidt hammer age evaluation of the moraine sequence in front of Boyabreen, western Norway. Norsk Geologisk Tidskrift 80: 27–32.
- Chlebicki A., 2007. Nielichenizujące grzyby epi- i endolityczne (litobionty). Wiadomości Botaniczne 51(1/2): 5–13.
- Day M.J. & Goudie A.S., 1977. Field assessment of rock hardness using the Schmidt test hammer. British Geomorphological Research Group Technical Bulletin 18: 19–29.
- Etienne S., 2002. The role of biological weathering in periglacial areas: a study of weathering rinds in south Iceland. Geomorphology 47: 75–86.
- Evans D.J.A., Archer S. & Wilson D.J.H., 1999. A comparison of the lichenometric and Schmidt hammer dating techniques based on data from the proglacial areas of some Icelandic glaciers. Quaternary Science Reviews 18: 13–41.
- German R., Hantke R. & Mader M., 1979. Der subrezente Drumlin im Zungenbecken des Biferten-Gletschers (Kanton Glarus, Schweiz). Jahreschefte der Gesellschaft für Naturkunde in Württemberg 134: 96–103.
- Goudie A.S., 2006. The Schmidt Hammer in geomorphological research. Progress in Physical Geography 30(6): 703–718.
- Kotarba A., Król K. & Rutkowski J., 2002. Zastosowanie młotka Schmidta do badania granitów tatrzańskich. In: VI Zjazd Geomorfologów Polskich„Środowiska górskie – ewolucja rzeźby” – streszczenia referatów i posterów (papers and posters’ summaries), Jelenia Góra: 79–80.
- Matthews J.A.&Owen G., 2008. Endolithic lichens, rapid biological weathering and Schmidt hammer R-values on recently exposed rock surfaces: Storbreen glacier forefield, Jotunheimen, Norway. Geografiska Annaler 90A(4): 287–297.
- McCarroll D., 1989. Potential and Limitations of the Schmidt Hammer for Relative-Age Dating: Field Tests on Neoglacial Moraines, Jutunheimen, Southern Norway. Arctic and Alpine Research 21(3): 268–275.
- McCarroll D., 1991. The Schmidt hammer, weathering and rock surface roughness. Earth Surface Processes and Landforms 16: 477–480.
- McCarroll D., 1993. The vertical extent of ice sheets in Nordfjord, western Norway: measuring degree of rock surface weathering. Boreas 22: 255–265.
- Owen G., Matthews J.A. & Albert P.G., 2007. Rates of Holocene chemical weathering, “Little Ice Age” glacial erosion and implications for Schmidt-hammer dating at a glacier-foreland boundary, Fabergstolsbreen, southern Norway. The Holocene 17(6): 829–834.
- Placek A., 2006. Młotek Schmidta w badaniach geomorfologicznych – ewaluacja i przykłady zastosowania metody. Czasopismo Geograficzne 77(3): 182–205.
- Placek A.& Migoń P., 2005.Zastosowanie młotka Schmidta w badaniach geomorfologicznych – potencjał, ograniczenia i wstępne wyniki badań w Sudetach. In: A.Kotarba, K.Krzemień & J. Święchowicz (eds.) Współczesna ewolucja rzeźby Polski, 19–22 września 2005, Kraków: 367–371.
- Runkiewicz L.& Brunarski L., 1977. Instrukcja stosowania młodków Schmidta do nieniszczącej kontroli jakości betonu w konstrukcji, nr 210. Instytut Techniki Budowlanej, Warszawa: 44 pp.
- Selby M.J., 1980. A rock mass strength classification for geomorphic purposes: with tests from Antarctica and New Zealand. Zeitschrift für Geomorphologie. N.F. 24(1): 31–51.
- Shakesby A.A., Matthews J.A. & Owen G., 2006. The Schmidt hammer as a relative-age dating tool and its potentioal for calibrated-age dating in Holocoene glaciated environments. Quaternary Science Reviews 25: 2846–2867.
- Van der Meer J.J.M., 1983. A recent drumlin with fluted surface in the Swiss Alps.In: E.B.Evenson, C.Schlüchter & J.Rabassa (eds.) Tills and Related Deposits: Genesis, Petrology, Application, Stratigraphy. A.A. Balkema, Rotterdam: 105–110.
- Winkler S., 2000. The “Little Ice Age” maximum in the Southern Alps, New Zealand: preliminary results at Mueller Glacier. The Holocene 10(5): 643–647.
- Winkler S., 2005. The Schmidt hammer as a relative-age dating technique: potential and limitations of its application on Holocene moraines in Mt Cook National Park, Southern Alps, New Zealand. New Zealand Journal of Geology & Geophysics 48: 105–116.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ5-0052-0087