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).
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Ahlmann HW (1919) Geomorphological studies in Norway. Geogr Ann 1:1–148, 193–252
Andersen BG Karlsen M (1986) Glasialkronologi-Isfrontens Tilbaketrekning, Nationalatlas for Norge, Staten Kartverk
André MF (1991) Dynamique actuelle et évolution holocène des versants du Spitsberg. Thèse d’Etat, University of Paris I
Ballantyne CK (1998) Age and significance of mountain top detritus. Permafrost Periglac Process 9:327–345
Benn DI, Evans D (2002) Glaciers and glaciations. Arnold, London
Dahl E (1955) Biogeographic and geologic indications of unglaciated areas in Scandinavia during the glacial ages. Bull Geol Soc Am 66:1499–1519
Dahl R (1966a) Blockfields, weathering pits and tor-like forms in the Narvik Mountains, Nordland, Norway. Geogr Ann 48A:55–85
Dahl R (1966b) Blockfields and other weathering forms in the Narvik Mountains. Geogr Ann 48(A):224–227
Dons J (1960a) Telemark supracrustal and associated rocks, in geology of Norway. Norsk Geologisk Undersökelse 208:49–58
Dons J (1960b) The stratigraphy of supracrustal rocks, granitization and tectonics in the Précambrian Telemark area. Norsk Geologisk Undersökelse 212:2–27
Dons J (1961) Rjukan, Geologisk Kart, Scale 1/100 000. Norges Geologisk Undersölkelse
Dons J (1972) The Telemark area, a brief presentation. Sciences de la Terre XVII 1–2:23–29
Gjessing J (1966) Some effects of ice erosion on the development of Norwegian valleys and fjords. Nor Geogr Tidsskr 20(8):273–299
Gjessing J (1967) Norway’s paleic surface. Nor Geogr Tidsskr 21(2):69–132
Gjessing J (1987) Geomorphology of Norway. In Varjo U, Tietze W, Norden (eds) Man and environment. Gebrüder Borntraeger, Berlin-Stuttgart, pp 90–103
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
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
Högbom B (1914) Über die geologische Bedeutung des Frostes. Bull Geol Inst Univ Uppsala, XII, pp 257–389
Ives JD (1958) Mountain-top detritus and the extent of the last glaciation in Northeastern Labrador-Ungava. Can Geogr 12:25–31
Ives JD (1966) Blockfields, associated weathering forms on mountain tops and the Nunatak hypothesis. Geogr Ann 48A(4):220–223
Jansen IJ (1986) Kvartaergeologi, Jord og Landskap i Telemark gjennom 11000 ar. Institutt for Naturanalyse
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
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
King L (1984) Permafrost in Skandinavien. Heidelberger geographische Arbeiten 76
King L (1986) Zonation and ecology of high mountain permafrost in Scandinavia. Geogr Ann 68A(3):131–139
Klemsdal T, Sjulsen OE (1988) The Norwegian macro-landforms: definitions, distribution and system of evolution. Nor Geogr Tidsskr 42:133–147
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
Linton D (1949) Unglaciated areas in Scandinavia and Great Britain. Irish Geogr 2:25–33
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
Moen A (1987) The regional vegetation of Norway; that of central Norway in particular. Nor Geogr Tiddskiftt 4:179–226
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
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
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
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
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
Oftedahl C (1980) Geology of Norway. Norges Geologiske Undersökelse, Universitetsforlaget 54(356):3–115
Panizza M (2001) Geomorphosites: concepts, methods and examples of geomorphological survey. Chin Sci Bull 46(1):4–6
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
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
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
Reynard E (2009a) Geomorphosites: definition and characteristics. In: Reynard E, Coratza P, Regolini-Bissig G (eds). Friedrich Pfeil, Munich, pp 9–20
Reynard E (2009b) The assessement of geomorphosites, In: Reynard E, Coratza P, Regolini-Bissig G (eds) Friedrich Pfeil, Munich, pp 63–71
Reynard E, Coratza P, Regolini-Bissig G (2009) Geomorphosites. Friedrich Pfeil, Munich
Rudberg S (1962) Geology and morphology of the “fjells”. Biul Peryglac 11:173–186
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
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
Rudberg S (1984) Fennoscandian shield: Finland, Sweden and Norway. In: Embleton C (ed) Geomorphology of Europe. MacMillan Publishers, Londres, pp 55–74
Rudberg S (1988) Gross morphology of Fennoskandia. Six complementary ways of explanation. Geogr Ann 70A(3):135–167
Sellier D (1995) Le felsenmeer du mont Gausta (Telemark, Norvège): Environnement, caractères morphologiques et significations paléogéographiques. Géog Phys Quatern 49(2):185–205
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
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
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
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
Sigmond EMO, Gustavson M, Roberts D (1984) Berggrunnskart over Norge, Nasjonalatlas for Norge
Sollid JL, Torp B (1984) Glasialgeologisk Kart over Norge, 1:1 000 000, Nasjonalatlas for Norge, Geografisk Institutt, Universitet i Oslo
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
Vorren TO (1977) Weichselian ice movements in South Norway and adjacent areas. Boreas 6:247–257
Washburn AL (1979) Geocryology, a survey of periglacial processes and environments. Arnold, Londres
Wille N (1905) Om innvandringen av det arktiske floraelement til Norge. Nyt Magazin for Naturvidenskap 43
Wyckoff D (1934) Geology of the Mt. Gausta region in Telemark, Norway. Nor Geologisk Tidsskrift 13:1–72
Whittow J (2000) Dictionary of physical geography. Penguin Books, 590 pp
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.
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2021 Springer Nature Switzerland AG
About this chapter
Cite this chapter
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
Download citation
DOI: https://doi.org/10.1007/978-3-030-52563-7_11
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-030-52562-0
Online ISBN: 978-3-030-52563-7
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)