Skip to main content
Have a personal or library account? Click to login
Substratum morphology and significance during the Weichselian Odra ice lobe advance in northeast Germany and northwest Poland Cover

Substratum morphology and significance during the Weichselian Odra ice lobe advance in northeast Germany and northwest Poland

Open Access
|Jan 2016

References

  1. Anderson, J.B., Smith Wellner, S., Lowe, A.L., Mosola, A.B. & Shipp, S.S., 2001. Footprint of the Expanded West Antarctic Ice Sheet: Ice Stream History and Behavior.11, 4–9.
  2. Boulton, G.S., Hagdorn, M., Maillot, P.B. & Zatsepin, S., 2009. Drainage beneath ice sheets: groundwater-channel coupling, and the origin of esker system from former ice sheets.28, 621–638.
  3. Clark, I., 2001.. Geostokes Limited, Alloa, 119 pp.
  4. Davis, J.C., 1986.. John Wiley & Sons, New York, 646 pp.
  5. Denton, G.H. & Hughes, T.J., 1981. The Arctic Ice Sheet: An outrageous hypothesis. [In:] G.H. Denton & T.J. Hughes (Eds):. Wiley, New York: 437–467.
  6. Galon, R. & Roszkówna, L., 1961. Extents of the Scandinavian glaciations and of their recession stages on the territory of Poland in the light of analysis of the marginal forms of inland ice.33, 347–364.
  7. Goldsztejn, P. & Skrzypek, G., 2004. Wykorzystanie metod interpolacji do numerycznego kreślenia map powierzchni geologicznych na podstawie nieregularnych danych [Applications of numeric interpolation methods to the geological surface mapping using irregularly spaced data].52, 233–236.
  8. Heine, K., Reuther, A.U., Thieke, H.U., Schulz, R., Schlaak, N. & Kubik, P.W., 2009. Timing of Weichselian ice marginal positions in Brandenburg (northeastern Germany) using cosmogenic in situBe.53, 433–454.
  9. Hermanowski, P., 2007. Morfologia osadów podłoża zlodowacenia Wisły na obszarze polskiej części lobu Odry [Morphology of the Vistulain (Weichselian) glaciation substratum in the area of Polish part of the Odra lobe].55, 133–139.
  10. Hermanowski, P., 2010. Palaeoglaciology of the Weichselian Odra ice lobe, NE Germany and NW Poland.14, 12–24.
  11. Hermanowski, P. & Piotrowski, J.A., 2007. Substratum morphology, ice thickness estimation and the location of tunnel valleys as proxies in the reconstruction of the dynamics of the Odra lobe during the Last Glaciation.(Abstract-Volume) 53, 117.
  12. Hermanowski, P. & Piotrowski, J.A., 2009. Drenaż subglacjalny i jego wpływ na dynamikę lobu Odry zlodowacenia Wisły [Subglacial drainage and its influence on the dynamics of the Weichselian Odla lobe].57, 504–512.
  13. Holmlund, P. & Fastook, J., 1993. Numerical modelling provides evidence of a Baltic Ice Stream during the Younger Dryas.22, 77–86.
  14. Hooke, R.LeB. & Jennings, C.E., 2006. On the formation of the tunnel valleys of the southern Laurentide ice sheet.25, 1364–1372.
  15. Houmark-Nielsen, M., 2003. Signature and timing of the Kattegat Ice Stream: onset of the Last Glacial Maximum sequence at the southwestern margin of the Scandinavian Ice Sheet.32, 227–241.
  16. Houmark-Nielsen, M. & Kjær, K.H., 2003. Southwest Scandinavia, 40–15 kyr BP: palaeogeography and environmental change.18, 769–786.
  17. Houmark-Nielsen, M. & Piotrowski, J.A., 2000., University of Aarhus, Excursion guide, 32 pp.
  18. Jennings, C.E., 2006. Terrestrial ice streams – a view from the lobe.75, 100–124.
  19. Jørgensen, F. & Piotrowski, J.A., 2003. Signature of the Baltic Ice Stream on Funen Island, Denmark during the Weichselian glaciation.32, 242–255.
  20. Kalm, V., 2012. Ice-flow pattern and extent of the last Scandinavian Ice Sheet southeast of the Baltic Sea.44, 51–59.
  21. Karczewski, A., 1968. Wpływ recesji lobu Odry na powstanie i rozwój sieci dolinnej Pojezierza Myśliborskiego i Niziny Szczecińskiej [Influence of the Odra Lobe recession upon the origin and development of the valleys net of Myślibórz Lakeland and Szczecin Lowland].8, 1–106.
  22. Karczewski, A., 2001. Parseta lobe – Pomeranian Phase (Central Pomerania). [In:] J.A Piotrowski & W. Wysota (Eds):, INQUA Commission on Glaciation, 88–90.
  23. Keilhack, K., 1898. Die Stillstandslagen des letzten Inlandeises und die hydrgraphische Entwicklung des pommerschen Küstengebietes.19, 90–152.
  24. Lasberg, K. & Kalm, V., 2013. Chronology of the Late Weichselian glaciation in the western part of the East European Plain.42, 995–1007.
  25. Marks, L., 2002. Last Glacial Maximum in Poland.21, 103–110.
  26. Marks, L., 2005. Pleistocene glacial limits in the territory of Poland.53, 988–993.
  27. Mojski, J.E., 2005.[]. Polish Geological Institute, Warszawa, 404 pp.
  28. Piotrowski, J.A., 1994. Tunnel-valley formation in northwest Germany – geology, mechanisms of formation and subglacial bed condition for the Bornhöved tunnel valley.89, 107–141.
  29. Piotrowski, J.A., 1997a. Subglacial groundwater flow during the last glaciation in northwestern Germany.111, 217–224.
  30. Piotrowski, J.A., 1997b. Subglacial hydrology in north-western Germany during the last glaciation: groundwater flow, tunnel valleys and hydrogeological cycles.16, 169–185.
  31. Piotrowski, J.A., Bartels, F., Salski, A. & Schmidt G., 1996. Geostatistical Regionalization of Glacial Aquitard Thickness In Northwestern Germany, Based on Fuzzy Kriging., 28: 437–452.
  32. Piotrowski, J.A., Hermanowski, P. & Piechota, A.M., 2009. Meltwater discharge through the subglacial bed and its land-forming consequences from numerical experiments in the Polish lowland during the last glaciation.34, 481–492.
  33. Punkari, M., 1997. Glacial and glaciofluvial deposits in the interlobate areas of the Scandinavian Ice Sheet.16, 741–753.
  34. Przybylski, B., 2008. Geomorphic traces of a Weichselian ice stream in the Wielkopolska Lowland, western Poland.37, 286–296.
  35. Rinterknecht, V., Braucher, R., Böse, M., Bourlès, D. & Mercier, J.-L., 2012. Late Quaternary ice sheet extents in northeastern Germany inferred from surface exposure dating.44, 89–95.
  36. Smith, A.M. & Murray, T., 2009. Bedform topography and basal conditions beneath a fast-flowing West Antarctic ice stream.28, 584–596.
  37. Stokes, C.R., Clark, C.D., Lian, O.B. & Tulaczyk, S., 2007. Ice stream sticky spots: A review of their identification and influence beneath contemporary and palaeo-ice streams.81, 217–249.
  38. Szewczyk, J., Nowicki, Z. & Gientka, D., 2007. Występowanie głębokiej zmarzliny w okresie zlodowacenia Wisły na obszarze Niżu Polskiego – implikacje paleohydrogeologiczne oraz geotermiczne [Evaluation of the deep Vistulian permafrost on Polish Lowlands – geothermal and paleohydrogeological implications).13, 203–211.
  39. Tulaczyk, S., Kamb, B. & Engelhardt, H.F., 2000. Basal mechanics of ice stream B, West Antarctica. I. Till mechanics.105, 463–482.
  40. Walder, J.S., 1982. Stability of sheet flow of water beneath temperate glaciers and implications for glacier surging.28, 273–293.
  41. Woldstedt, P., 1931. Über Randlagen der letzten Vereisung in Ostdeutchland und Polen und über die Herausbildung des Netze-Warthe Urstromtales.52, 59–67.
  42. Wysota, W., 2007. Successive subglacial depositional processes as interpreted from basal tills in the Lower Vistula valley (N Poland).193, 21–31.
DOI: https://doi.org/10.1515/logos-2015-0016 | Journal eISSN: 2080-6574 | Journal ISSN: 1426-8981
Language: English
Page range: 241 - 248
Submitted on: Nov 14, 2014
Accepted on: Mar 18, 2015
Published on: Jan 22, 2016
Published by: Adam Mickiewicz University
In partnership with: Paradigm Publishing Services

© 2016 Piotr Hermanowski, published by Adam Mickiewicz University
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.