The Varanger Peninsula (Norway) and the Problem of the Fossilisation of Periglacial Phenomena in Europe

References

• Åhman, R., 1977: Palsar i Nordnorge. Meddelande från Lunds Universitet, Geografiska Institutionen, Avhandlingar LXXVIII, 165 pp.
   Google Scholar
• Bout, P. and Gotard, A., 1973: Aspects du modelé periglaciaire en Scandinavie du Nord. Biul. Peryglacjalny, 22: 51–79.
   Google Scholar
• Dahl, R., 1966: Block fields, weathering pits and torlike forms in the Narvik Mountains, Nordland, Norway. Geogr. Ann. 48: 55–85.
   Google Scholar
• Dytik, J., 1956: Coup d'oeil sur la Pologne periglaciaire. Biul. Peryglacjalny 4: 195–238.
   Google Scholar
• Friedman I.D., Johansson C. E., Oskarsson N., Svensson H., Thorarinsson S. and Williams, Ir. R. S., 1971: Observations on Icelandic polygon surfaces and palsa areas. Photo interpretation and field studies. Geogr. Ann. 53 A: 115–145.
   Google Scholar
• Grigoriev, A. A., 1925: Die Typen des Tundramikrorelief von Polareurasien, ihre geographische Verbreitung und Genesis. Geogr. Zeitschr., 31.
   Google Scholar
• Jahn, A., 1963: Origin and development of patterned ground in Spitsbergen. Permafrost Intern. Confer. 1963, Lafayette, Ind., Proc. Nat. Acad. Sci. Nat. Research Council, Pub. 1287, pp. 140–145.
   Google Scholar
• Jahn, A. 1975: Problems of the periglacial zone. Polish Scientific Publishers, Warszawa, 223 pp.
   Google Scholar
• Jahn, A. 1976a: Geomorphological modelling and nature protection in Arctic and Subarctic environments. Geoforum, 7: 121–137.
   Google Scholar
• Jahn, A. 1976b: Pagórki mrozowe typu palsa /Palsa-type frost mounds/, Studia Societ. Scie. Torunensis, Torun-Polonia, III, Sec. C., Nr. 4–6: 123–139.
   Google Scholar
• Johnsson, G., 1963: Periglacial phenomena in Southern Sweden. Geogr. Ann. 44: 378–404.
   Google Scholar
• Kaiser, K., 1960: Klimazeugen des periglazialen Dauerfrostbodens in Mittelund Westeuropa. Eiszeitalter und Gegenwart, 11: 121–141.
   Google Scholar
• Liestøl. O., 1960: Glaciers of the present day. In Holtedal, O. Geology of Norway. Nor. Geol. Unders. 208. 540 pp.
   Google Scholar
• Marthinussen, M., 1960: Coast- and Qord area of Finnmark with remarks on some other districts, pp. 416–432, in Holtedahl. O., Geology of Norway. Nor. Geol. Unders. Nr. 208.
   Google Scholar
• Marthinussen, M. 1974: Contributions to the Quarternary geology of North-easternmost Norway and the closely adjoining foreign territories. Nor. Geol. Unders., Nr. 315, p. 157.
   Google Scholar
• Poser, H., 1947: Dauerfrostboden und Temperaturverhältnisse während der Würm-Eiszeit im nicht vereisten Mittel- und Westeuropa. Naturwissenschaften 34: 10–18.
   Web of Science ®Google Scholar
• Rapp, A. and Annersten, L., 1969: Permafrost and tundra polygons in Northern Sweden. In The periglacial environment, Past and Present, ed. by T.L. Péwé. Arctic Institute of North America.
   Google Scholar
• Rudberg, S., 1977: Periglacial zonation in Scandinavia. Symposium: Formen, Formengesellschaften und Untergrenzen in den heutigen periglazialen Höhenstufen der Hochgebirge Europas und Afrikas zwischen Arktis und Aquator. Abhand. d. Akad. d. Wissensch, in Göttingen, Math-Physik.K1. Dritte Folge, Nr. 31, pp. 92–104.
   Google Scholar
• Salvigsen, O., 1977: An observation of palsa-like forms in Nordaustlandet Svalbard. Nor. Polarinst. Årb. 1976: 364–367.
   Google Scholar
• Schunke, E., 1977: Periglazialformen und -Formengesellschaften in der europäischatlantischen Arktis und Subarktis. Symposium: Formen, Formengesellschaften und Untergrenzen in den heutigen periglazialen Höhenstufen der Hochgebirge Europas und Afrikas zwischen Arktis und Aquator. Abhand. d. Akad. d. Wissensch, in Göttingen, Math.-Physik. Kl., Dritte Folge. Nr. 31, pp. 39–62.
   Google Scholar
• Sollid, J. L., Andersen, S., Hamre, N., Kjetdsen, O., Salvigsen, O., Sturød, S., Tveitå, T. and Wilhelmsen, A., 1973: Deglaciation of Finmark, North Norway. Nor. Geogr. Tidsskr. 27(4): 233–325.
   Google Scholar
• Sollid, J. L., and Sorbel, L., 1975: Younger Dryas ice-marginal deposits in Tröndelag, Central Norway. Nor. Geogr. Tidsskr. 29: 1–9.
   Google Scholar
• Strömquist, L., 1973: Geomorfologiska studier av blockhav och blockfält i Norra Skandinavien. Uppsala Universitet, Naturgeografiska Institutionen, Rapport 22, 161 pp.
   Google Scholar
• Svensson, H., 1962: Ice-wedges in fossil tundra polygons on the Varanger Peninsula. Svensk Geogr. Årsb.: 185–187.
   Google Scholar
• Svensson, H. 1963: Tundra polygons. Photographic interpretation and field studies in North-Norwegian polygon areas. Nor. Geol. Unders. Nr. 223: 298–327.
   Google Scholar
• Svensson, H. 1970: Frozen-ground morphology of northeastemmost Norway. Ecology of the subarctic regions. Proceed, of the Helsinki Symposium, pp. 161–168.
   Google Scholar
• Svensson, H. 1977: Observations on polygonal Assuring in non-perma-frost areas of the Norden Countries. Symposium: Formen, Formengesellschaften und Untergrenzen in den heutigen periglazialen Höhenstufen der Hochgebirge Europas und Afrikas zwischen Arktis und Aquator. Abhand. d. Akad. d. Wissensch, in Göttingen, Math.-Physik. Kl., Dritte Folge Nr. 31: 63–76.
   Google Scholar
• Svensson, H., Källander, H., Maack, A., and Ohrngren, S., 1967: Polygonal ground and solifluction features. Photographic interpretation and field studies in Northernmost Scandinavia. Lund Studies in Geography, S.A., No. 40, 67 pp.
   Google Scholar
• Troll, C., 1944: Strukturböden, Solifluktion und Frostklimate der Erde. Geol. Rundsch. 34: 545–694.
   Google Scholar
• Washburn, A. L., 1973: Periglacial processes and environments. Edward Arnold. Publ., 320 pp.
   Google Scholar
• Velitchko, A.A., 1973: The natural process in Pleistocene /in RussI Pubi. Office “Nauka”, Moscow, 256 pp.
   Google Scholar
• Velitchko, A.A., 1963: Frost cracking in a middlealtitude climate. Biul. Peryglacjalny, 12: 175–189.
   Google Scholar
• Worsley, P., 1974: Absolute dating of the Sub-Boreal climatic detezrioration—fossil pine evidence from Strimasund Västerbotten County, Sweden. Geol. Föreningens i Stockholm, Förhandlingar, 96: 399–403.
   Google Scholar