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Marine terraces in Kaffioyra and Hermansenoya (Oscar II Land, NW Spitsbergen)

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EN
The main relief elements which document the sea level changes on the Kaffioyra Plain and the Isle of Hermansenoya, including the sea transgressions, are both abrasive (marine terraces) and accumulative (raised beaches). Such landforms have been relatively well preserved in the area of Kaffioyra. However, the issues relating to the number of such forms and their age remain questionable. They refer to the number of glacial episodes, the extension of the glaciers during these periods as well as the limit of the sea transgressions during and after the deglaciation of the NW Spitsbergen during the Weichselian and Holocene periods. The first detailed geomorphological research which was conducted in Kaffioyra and its vicinity and included geomorphological mapping, was carried out by Niewiarowski and Sinkiewicz during the Toruń Polar Expeditions to Spitsbergen in 1978 and 1985 (Niewiarowski et al. 1993). The authors listed the exact number and extension of the old marine terraces as well as the Late Weichselian marine limit. According to these studies, the Kaffioyra's marine terraces are of two generations. The Isle of Hermansenoya, located four km off the Kaffioyra's shores, has one generation of former marine terraces. The maximum Late Weichselian marine limit in Kaffioyra reached 46–48 m a.s.l., while in Hermansenoya it reached about 33 m a.s.l. On both the Kaffioyra Plain and the Isle of Hermansenoya there is evidence of the Holocene sea level changes.
Czasopismo
Rocznik
Tom
Strony
25--33
Opis fizyczny
Bibliogr. 37 poz., rys.
Twórcy
autor
  • University of Nicolaus Copernicus in Toruń, Institute of Geography, Department of Geomorphology and Quaternary Palaeogeography, Gagarina 9, PL-87-100 Toruń, Polan, tomjaw@umk.pl
Bibliografia
  • Andersson T., 2000. Raised beach deposits and new 14C ages from Pricepynten, Prins Karls Forland, western Svalbard. Polar Research, 19 (2): 271–273.
  • Andersson T., Forman S.L., Ingolfsson O. & Manley W.F., 1999. Late Quaternary environmental history of central Prins Karls Forland, Svalbard. Boreas, 28: 292–307.
  • Andersson T., Forman S.L., Ingolfsson O. & Manley W.F., 2000. Stratigraphic and morphologic constraints on the Weichselian glacial history of northern Prins Karls Forland, western Svalbard. Geografiska Annaler 82 A (4): 455–470.
  • Bergsten H., Andersson T. & Ingolfsson O., 1998. Foraminiferal stratigraphy of raised marine deposits,representing isotope stage 5, Prins Karls Forland, western Svalbard. Polar Research, 17: 81–91.
  • Boulton G.S., 1979. Glacial history of the Spitsbergen archipelago and the problem of a Barents Shelf ice sheet. Boreas, 8: 31–57.
  • Forman S.L., 1989. Late Weichselian glaciation and deglaciation of Forlandsundet area, western Spitsbergen, Svalbard. Boreas, 18: 51–60.
  • Forman S.L., 1990. Post-glacial relative sea-level history of northwestern Spitsbergen, Svalbard. Geological Society of America Bulletin, 102: 1580–1590.
  • Forman S.L.&Ingolfsson O., 2000. Late Weichselian glacial history and postglacial emergence of Phippsoya, Sjuoyane, northern Svalbard: a comparison of modelled and empirical estimates of a glacial-rebound hinge line. Boreas, 29: 16–25.
  • Forman S.L. & Miller G.H., 1984. Time dependent soil morphologies and pedogenic processes on raised marine beaches, Broggerhalvoya, Spitsbergen, Svalbard Archipelago. Arctic and Alpine Research, 16: 381–394.
  • Forman S.L., Lubinski D.J. Ingolfsson O., Zeeberg J.J., Snyder J.A., Siegert M.J. & Matishov G.G., 2004. A review of postglacial emergence on Svalbard, Franz Josef Land and Novaya Zemlya, northern Eurasia. Quaternary Science Reviews, 23: 1391–1434.
  • Forman S.L., Mann D. & Miller G.H., 1987. Late Weichselian and Holocene relative sea-level history of Broggerhalvoya, Spitsbergen. Quaternary Research, 27: 41–50.
  • Goslar T. & Pazdur M., 1985. Contamination studies of mollucs shell samples. Radiocarbon, 27: 33–42.
  • Hequette A. & Ruiz M.H., 1989. Les variations postglaciaires de la ligne de rivage au Spitsberg nord-occidental, Svalbard, Zeitschrift für Geomorphologie, 33: 323–337.
  • Klimaszewski M., 1960. Geomorphological studies of the western part of Spitsbergen between Kongsfjorden and Eidembukta, Zeszyty Naukowe Uniwersytetu Jagiellońskiego, 32: 91–168.
  • Krol M., Grześ M., Sobota I., Ćmielewski M. & Jaworski T., 2010. Submarine evidence of the Late Weichselian and Little Ice Age (LIA) glaciers limits in the St. Jonsfjorden Region (Svalbard). Bulletin of Geography, in press.
  • Landvik J.Y., Mangerud J. & Salvigsen O., 1987: The Late Weichselian and Holocene shoreline displacement on the west-central coast of Svalbard. Polar Research, 5: 29–44.
  • Landvik J.Y., Bondevik S., Elverhoi A., Fjeldskaar W., Mangerud J., Salvigsen O., Siegert M.J., Svendsen J.I. & Vorren T.O., 1998. The last glacial maximum of the Barents Sea and Svalbard area: ice sheet extent and configuration. Quaternary Science Reviews, 17: 43–7.
  • Landvik J.Y., Ingolfsson O., Mienert J., Lehman S.J., Solheim A., Elverhoi A. & Ottesen D., 2005. Rethinking Late Weichselian ice-sheet dynamics in coastal NW Svalbard. Boreas, 34: 7–24.
  • Lankauf K.R., 1982. Waldemar Glacier, Oscar II Land. Topographic map 1:5000, Acta Universitatis Nicolai Copernici, Geografia 16 [Suppl.].
  • Lankauf K.R., 2002. Recesja lodowców rejonu Kaffioyry (Ziemia Oskara II – Spitsbergen) w XX wieku. Prace Geograficzne IG i PZ PAN 183, Warszawa: 224 pp.
  • Lehman, S. J.&Forman, S. L. 1992. Late Weichselian glacier retreat in Kongsfjorden, west Spitsbergen, Svalbard. Quaternary Research, 37: 139–154.
  • Miller G.H., Sejrup H.P., Lehman S.J. & Forman S.L., 1989. Glacial history and marine environmental change during the last interglacial-glacial cycle, western Spitsbergen, Svalbard: Boreas, 18: 273–296.
  • Mangerud J., Bolstad M., Elgersma A., Helliksen D., Lycke J.Y., Lonne J., Salvigsen O., Sandahl T. & Sejrup H.P., 1987. The Late Weichselian glacial maximum in western Svalbard. Polar Research, 5: 275–278.
  • Mangerud J., Dokken T., Hebbeln D., Heggen B., Ingolfsson O., Landvik J.V., Mejdahl V., Svendsen J.I. & Vorren T.O., 1998. Fluctuations of the Svalbard-Barents Sea ice sheet during the last 150 000 years. Quaternary Science Reviews, 17: 11–42.
  • Moign A., 1974. Geomorphologie du strandflat au Svalbard: problemes (age, origine, processus), methodes de travail. Inter-Nord, 13–14: 67–72.
  • Niewiarowski W., 1982. Morphology of the forefield of the Aavatsmark Glacier (Oscar II Land, north-west Spitsbergen) and phases of its formation. Acta Universitatis Nicolai Copernici, Geografia, 16: 15–43.
  • Niewiarowski W. & Myzyk B., 1983. Kaffioyra coast (Oscar II Land, NW Spitsbergen), its morphogenetic factors and processes, Acta Universitatis Nicolai Copernici, Geografia, 18: 17–43.
  • Niewiarowski W. & Sinkiewicz M., 1993. Geomorphological map of Kaffioyra and its surroundings. [Annex to the article by W. Niewiarowski, M.F. Pazdur, M. Sinkiewicz, 1993]: Polish Polar Research 14 (3).
  • Niewiarowski W. & Sinkiewicz M., 1988. Frost mounds in Kaffioyra and Hermansenoya, NW Spitsbergen, and their origin. In: Senneset, K. (eds.) Permafrost Fifth Intern. Conference, Proc., 1. Tapir Publishers, Trondheim: 824–829.
  • Niewiarowski W., Pazdur M.F. & Sinkiewicz M., 1993. Glacial and marine episodes in Kaffioyra, northwestern Spitsbergen, during the Vistulian and the Holocene. Polish Polar Research 14 (3): 243–258.
  • Olszewski A., 1977. Geomorphological investigations of the marginal zone of Elise Glacier. Acta Universitatis Nicolai Copernici, Geografia 13: 67–74.
  • Plichta W., 1993. Gleby Kaffiöyry, Spitsbergen. Szkic monograficzny, Wydawnictwo Naukowe UMK, Toruń.
  • Salvigsen O., 1984. Two observations of pumice levels from the west coast of Spitsbergen. Polar Research, 2: 115–116.
  • Siegert M.J. & Dowdeswell J.A., 2004. Numerical reconstructions of the Eurasian Ice Sheet and climate during the Late Weichselian. Quaternary Science Reviews, 23: 1273–1283.
  • Sinkiewicz M., 1982. Transformations of moraine forms under slope processes exemplified by some morains of Kaffioyra (NW Spitsbergen). Acta Universitatis Nicolai Copernici, Geografia 16: 123–149.
  • Zapolski R., 1977a. Geodetic and topographic accomplishments of the “Toruń Polar Expedition, Spitsbergen – 1975”. Acta Universitatis Nicolai Copernici, Geografia 13: 21–37.
  • Zapolski R., 1977b. Marginal zone of Elise Glaciers, Oscar II Land, West Spitsbergen. Topographic map 1:5000, Acta Universitatis Nicolai Copernici, Geografia 13 [Suppl.].
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ5-0052-0057
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