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Landforms and Geomorphosite Designation on Mount Gausta (Telemark)

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Landscapes and Landforms of Norway

Part of the book series: World Geomorphological Landscapes ((WGLC))

Abstract

Mount Gausta is the highest point in Telemark. It stands above a vast plateau lying at 1000 m or so in altitude (a fjell), where the large Vestfjorddalen valley is entrenched. There are two parts to it, with a pyramid peaking at 1881 m to the north (Gaustatoppen), and a long plateau at between 1500 and 1600 m (Gaustaråen). The relief is characteristic of north European quartzite mountains because of the large Richter and scree slopes around Gaustatoppen, together with a large blockfield (or felsenmeer) on the Gaustaråen plateau. Thanks to the altitudes and absence of glaciers, it is possible to observe the vertical zonation of periglacial features and glacial relict landforms over nearly 900 m in elevation. The properties of the felsenmeer help determine the altitude of the Weichselian trimline and confirm there was a paleonunatak where Gaustatoppen stands. In addition to presenting the main geomorphological properties of Mount Gausta, the purpose of this chapter is to select geomorphosites, that is say sites of specific interest for visitors, using a deductive method based on defining the major geomorphological components (fjell, Gaustaråen, Gaustatoppen, Vestfjorddalen), and then the types of relief (geomorphotypes) and most significant sites for these reliefs (geomorphosites).

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References

  • Ahlmann HW (1919) Geomorphological studies in Norway. Geogr Ann 1:1–148, 193–252

    Google Scholar 

  • Andersen BG Karlsen M (1986) Glasialkronologi-Isfrontens Tilbaketrekning, Nationalatlas for Norge, Staten Kartverk

    Google Scholar 

  • André MF (1991) Dynamique actuelle et évolution holocène des versants du Spitsberg. Thèse d’Etat, University of Paris I

    Google Scholar 

  • Ballantyne CK (1998) Age and significance of mountain top detritus. Permafrost Periglac Process 9:327–345

    Article  Google Scholar 

  • Benn DI, Evans D (2002) Glaciers and glaciations. Arnold, London

    Google Scholar 

  • Dahl E (1955) Biogeographic and geologic indications of unglaciated areas in Scandinavia during the glacial ages. Bull Geol Soc Am 66:1499–1519

    Article  Google Scholar 

  • Dahl R (1966a) Blockfields, weathering pits and tor-like forms in the Narvik Mountains, Nordland, Norway. Geogr Ann 48A:55–85

    Google Scholar 

  • Dahl R (1966b) Blockfields and other weathering forms in the Narvik Mountains. Geogr Ann 48(A):224–227

    Google Scholar 

  • Dons J (1960a) Telemark supracrustal and associated rocks, in geology of Norway. Norsk Geologisk Undersökelse 208:49–58

    Google Scholar 

  • Dons J (1960b) The stratigraphy of supracrustal rocks, granitization and tectonics in the Précambrian Telemark area. Norsk Geologisk Undersökelse 212:2–27

    Google Scholar 

  • Dons J (1961) Rjukan, Geologisk Kart, Scale 1/100 000. Norges Geologisk Undersölkelse

    Google Scholar 

  • Dons J (1972) The Telemark area, a brief presentation. Sciences de la Terre XVII 1–2:23–29

    Google Scholar 

  • Gjessing J (1966) Some effects of ice erosion on the development of Norwegian valleys and fjords. Nor Geogr Tidsskr 20(8):273–299

    Article  Google Scholar 

  • Gjessing J (1967) Norway’s paleic surface. Nor Geogr Tidsskr 21(2):69–132

    Article  Google Scholar 

  • Gjessing J (1987) Geomorphology of Norway. In Varjo U, Tietze W, Norden (eds) Man and environment. Gebrüder Borntraeger, Berlin-Stuttgart, pp 90–103

    Google Scholar 

  • Godard A (1965) Recherches géomorphologiques en Ecosse du Nord-Ouest. Thèse d’Etat, Lettres, Paris, Publications de la Faculté des Lettres de l’Université de Strasbourg

    Google Scholar 

  • Godard A (1993) Rhythms in the geomorphological evolution and time-space related scale levels in the high latitudes. Zeitschrift für Geomorphologie, Suppl. 93:61–67

    Google Scholar 

  • Högbom B (1914) Über die geologische Bedeutung des Frostes. Bull Geol Inst Univ Uppsala, XII, pp 257–389

    Google Scholar 

  • Ives JD (1958) Mountain-top detritus and the extent of the last glaciation in Northeastern Labrador-Ungava. Can Geogr 12:25–31

    Article  Google Scholar 

  • Ives JD (1966) Blockfields, associated weathering forms on mountain tops and the Nunatak hypothesis. Geogr Ann 48A(4):220–223

    Google Scholar 

  • Jansen IJ (1986) Kvartaergeologi, Jord og Landskap i Telemark gjennom 11000 ar. Institutt for Naturanalyse

    Google Scholar 

  • Kerguillec R (2015) Seasonal distribution and variability of atmospheric freeze/thaw cycles in Norway over the last six decades (1950–2013). Boreas 44(3):526–542

    Article  Google Scholar 

  • Kerguillec R, Sellier D (2015) Selection of geomorphosites in the Rondane National Park (central Norway): landform and popularization. Géomorphol Relief Process Environment 21(2):131–144

    Article  Google Scholar 

  • King L (1984) Permafrost in Skandinavien. Heidelberger geographische Arbeiten 76

    Google Scholar 

  • King L (1986) Zonation and ecology of high mountain permafrost in Scandinavia. Geogr Ann 68A(3):131–139

    Google Scholar 

  • Klemsdal T, Sjulsen OE (1988) The Norwegian macro-landforms: definitions, distribution and system of evolution. Nor Geogr Tidsskr 42:133–147

    Article  Google Scholar 

  • Laverdière C, Bernard C, Dionne JC (1968) Les types de broutures glaciaires; 1, Classification et nomenclature franco-anglaise. Revue géographique de Montréal XXII 1:21–33

    Google Scholar 

  • Linton D (1949) Unglaciated areas in Scandinavia and Great Britain. Irish Geogr 2:25–33

    Google Scholar 

  • Lundqvist J (1987) Late weichselian glaciation and deglaciation in Scandinavia. In Sibrova V, Bowen DQ, Richmond GM (eds) Quaternary glaciation in Northern Hemisphere. Pergamon, Oxford, pp 269–292

    Google Scholar 

  • Moen A (1987) The regional vegetation of Norway; that of central Norway in particular. Nor Geogr Tiddskiftt 4:179–226

    Article  Google Scholar 

  • Moine B, Ploquin A (1971) Caractères géochimiques des séries de roches supracrustales du Telemark, Précambrien épizonal de la Norvège du Sud. Comptes-rendus de la Société géologique de France 3:139–141

    Google Scholar 

  • Nesje A (1989) The geographical and altitudinal distribution of blockfields in southern Norway and its significance to the Pleistocene Ice sheet. Zeitschrift für Geomorphologie, Suppl. 72:41–53

    Google Scholar 

  • Nesje A, Dahl SO (1990) Autochthonous blockfields in southern Norway: implications for the geometry, thickness, and isostatic loading of the Late Weichselian Scandinavian ice sheet. J Quat Sci 5(3):225–234

    Article  Google Scholar 

  • Nesje A, Dahl SO, Anda E, Rye N (1988) Block fields in southern Norway: significance for the Late Weichseilian ice sheet. Nor Geol Tidsskr 68:149–169

    Google Scholar 

  • Nordseth K (1987) Climate, hydrology and biogeography of Norway. In: Varjo U, Tietze W, Norden (eds) Man and environment. Gebrüder Borntraeger, Berlin-Stuttgart, pp 159–169

    Google Scholar 

  • Oftedahl C (1980) Geology of Norway. Norges Geologiske Undersökelse, Universitetsforlaget 54(356):3–115

    Google Scholar 

  • Panizza M (2001) Geomorphosites: concepts, methods and examples of geomorphological survey. Chin Sci Bull 46(1):4–6

    Article  Google Scholar 

  • Peulvast JP (1978) Le bourrelet scandinave et les Calédonides: un essai de reconstitution des modelés de la morphogenèse en Norvège. Géographie physique et Quaternaire XXXII 4:295–320

    Google Scholar 

  • Peulvast JP (1985) Relief, érosion différentielle et morphogenèse dans un bourrelet montagneux de haute latitude: Lofoten-Vesteralen et Sogn-Jotun (Norvège). Thèse d’Etat, Université de Paris I

    Google Scholar 

  • Peulvast JP (1987) Surfaces d’aplanissement étagées dans les Scandes: principes et implications de l’étude des paléosurfaces dans une montagne de haute latitude. Revue de Géomorphologie Dynamique XXXVI 3:83

    Google Scholar 

  • Reynard E (2009a) Geomorphosites: definition and characteristics. In: Reynard E, Coratza P, Regolini-Bissig G (eds). Friedrich Pfeil, Munich, pp 9–20

    Google Scholar 

  • Reynard E (2009b) The assessement of geomorphosites, In: Reynard E, Coratza P, Regolini-Bissig G (eds) Friedrich Pfeil, Munich, pp 63–71

    Google Scholar 

  • Reynard E, Coratza P, Regolini-Bissig G (2009) Geomorphosites. Friedrich Pfeil, Munich

    Google Scholar 

  • Rudberg S (1962) Geology and morphology of the “fjells”. Biul Peryglac 11:173–186

    Google Scholar 

  • Rudberg S (1973) Glacial erosion forms of medium size—a discussion based on four Swedish case studies. Zeitschrift für Geomorphologie, Suppl. Band 17:33–48

    Google Scholar 

  • Rudberg S (1977) Periglacial zonation in Scandinavia. In: Poser H (ed) Formen, Formengesellschaften und Untergrenzen in den heuteigen periglazialen Höhenstufen der Hochgebirge Europas und Afrikas zwischen Arktis und Äquator. Bericht über ein Symposium, Akad. Wiss. Göttingen Abh., Math-Phys., Kl. Folge E 31, 92–104

    Google Scholar 

  • Rudberg S (1984) Fennoscandian shield: Finland, Sweden and Norway. In: Embleton C (ed) Geomorphology of Europe. MacMillan Publishers, Londres, pp 55–74

    Google Scholar 

  • Rudberg S (1988) Gross morphology of Fennoskandia. Six complementary ways of explanation. Geogr Ann 70A(3):135–167

    Google Scholar 

  • Sellier D (1995) Le felsenmeer du mont Gausta (Telemark, Norvège): Environnement, caractères morphologiques et significations paléogéographiques. Géog Phys Quatern 49(2):185–205

    Google Scholar 

  • Sellier D (2002) Géomorphologie des versants quartzitiques en milieux froids : l’exemple des montagnes de l’Europe du Nord-Ouest. Thèse de doctorat d’Etat, Université de Paris I Panthéon-Sorbonne

    Google Scholar 

  • Sellier D (2007) Le rôle des relais de processus glaciaires et périglaciaires dans la genèse des felsenmeers. Du continent au bassin versant: théories et pratiques en géographie physique (Hommage au Professeur Alain Godard). Presses Universitaires Blaise Pascal, Collection Nature et Société, Clermont-Ferrand, pp 355–374

    Google Scholar 

  • Sellier D (2010) L’analyse intégrée du relief et la sélection déductive des géomorphosites: application au relief de la Charente-Maritime (France). Géomorphol Reliefs Process Environ 2:199–214

    Article  Google Scholar 

  • Sellier D (2013) Le relief de la Loire-Atlantique: patrimoine géomorphologique et géomorphosites. In: Morice JR, Saupin G, Vivier N (eds) Les nouveaux patrimoines des Pays de la Loire, Presses universitaires de Rennes, pp 236–255

    Google Scholar 

  • Sigmond EMO, Gustavson M, Roberts D (1984) Berggrunnskart over Norge, Nasjonalatlas for Norge

    Google Scholar 

  • Sollid JL, Torp B (1984) Glasialgeologisk Kart over Norge, 1:1 000 000, Nasjonalatlas for Norge, Geografisk Institutt, Universitet i Oslo

    Google Scholar 

  • Verschure RH, Maijer C, Andriessen PAM (1990) Isotopic age determination in South Norway: II. The problem of errorchron ages from Telemark rhyolites. Nor Geologisk Undersökelse 418:47–60

    Google Scholar 

  • Vorren TO (1977) Weichselian ice movements in South Norway and adjacent areas. Boreas 6:247–257

    Article  Google Scholar 

  • Washburn AL (1979) Geocryology, a survey of periglacial processes and environments. Arnold, Londres

    Google Scholar 

  • Wille N (1905) Om innvandringen av det arktiske floraelement til Norge. Nyt Magazin for Naturvidenskap 43

    Google Scholar 

  • Wyckoff D (1934) Geology of the Mt. Gausta region in Telemark, Norway. Nor Geologisk Tidsskrift 13:1–72

    Google Scholar 

  • Whittow J (2000) Dictionary of physical geography. Penguin Books, 590 pp

    Google Scholar 

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Acknowledgements

The authors would like to thank Simon Charrier, cartographer, who redrew the maps, and the Institute of Geography of Nantes University and the Laboratory Géolittomer-Nantes (CNRS) for founding the translation of the manuscript.

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Correspondence to Dominique Sellier .

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Sellier, D., Kerguillec, R. (2021). Landforms and Geomorphosite Designation on Mount Gausta (Telemark). In: Beylich, A.A. (eds) Landscapes and Landforms of Norway. World Geomorphological Landscapes. Springer, Cham. https://doi.org/10.1007/978-3-030-52563-7_11

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