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Söderåsen is a northwest–southwest elongated bedrock ridge in Scania in southern Sweden. On Söderåsen is Scania's highest point at 212 m (696 ft) above sea level. It is intersected by several fissure valleys. The ridge extends from Röstånga in the southeast to the Åstorp in northwest.
In Swedish the word ås commonly refer to eskers, a glacial landform, but in the case of Söderåsen it corresponds to a tectonic landform called horst[2] in the Sorgenfrei-Tornquist Zone. The last glacial ice sheet, the Weichsel ice, left the area of Söderåsen 14,000 to 13,500 years BP. Following this there was a period up to 12,700 years BP of cold non-glacial conditions with permafrost and strong winds.[3]
Kopparhatten
On Söderåsen is the viewpoint Kopparhatten at a height of 200 m (660 ft). It is the highest point in Söderåsens national park. This part of the hill has a particularly dramatic landscape, with up to 90 m (300 ft) deep ravines. Various nivation hollows exists in the vicinity of Kopparhatten.[4]
Streams
The Kvärkabäcken and Skäralid streams that traverses Söderåsen are believed to be antecedent rivers that existed prior to the present-day relief. These rivers may date to Neogene[5] times when the South Småland peneplain formed. The streams were then likely modified by meltwater during the deglaciations.[6]
Oden Lake
Oden Lake (Swedish: Odensjön) is a lake in Scania, in Sweden and belongs to Söderåsens National park. The lake is circular in shape, with a diameter of 150 m (490 ft) and it is 19 m (62 ft) deep. Oden Lake likely formed from a glacier niche,[7][4] and the name Oden Lake may have been due to the circular shape as compared to the Norse god Odin's one eye.[8] Earlier views have suggested the lake may be an volcanic explosion crater, a nivation hollow or formed by fluvial erosion or as plunge pool of glacial meltwater.[7] These various theories that had accumulated up to the 1980s were proposed by Alfred Gabriel Nathorst, Lennart von Post, Mats Åkesson and Anders Rapp among others.[7]
Flora, fauna, and funga
The landscape offers views of leafy deciduous forests and powerful screes with high rocks, flowing watercourses and wide vistas.
The forest, is made up of different types of wood as for example beech, oak and ash. The ground of the forest is covered with a notable amount of plant species. The area is rich with mushrooms, insects, water creatures, mosses, birds and bats.
Because of the rugged landscape, many characteristics of primeval forest have been preserved, such as an abundance of dead trees. This makes the insect life rich, with many rare beetles. The flora is also extremely rich, with species such as hollowwort, enchanter's nightshade and tall meadow-rue.
Panoramic view from Kopparhatten
Söderåsen National Park
The Söderåsen National Park (Swedish: Söderåsens nationalpark) is a designated area of about 16 km2 (6.2 sq mi). It was established in 2001 in the municipalities of Klippan and Svalöv and ranges from the Skäralid ravine in the north to the Nackarpsdalen in the south. It was already a protected area, and when it became a national park, the protection of the land increased.
Some of the noted features in the national park are the Oden Lake in Nackarpsdalen and the viewpoints Kopparhatten, Hjortsprånget and Lierna along the Skäralidsdalen.
References
^ ab. Naturvårdsverket. Archived from the original on 2009-04-04. Retrieved 2009-02-26.
^Lundin, Jonas (November 13, 2013). "Söderåsen ingen riktig ås". Lokaltidningen Landskrona Svalöv (in Swedish). Retrieved October 25, 2017.
^Berglund, Björn E.; Rapp, Anders (1988). "Geomorphology, climate and vegetation in North-West Scania, Sweden, during the Late Weichselian". Geographia Polonica. 55: 13–35.
^ abFlorén, Sara (2013). Geologisk guide till Söderåsen – 17 geologiskt intressanta platser att besöka (BSc) (in Swedish). Geologiska institutionen Lunds universitet.
^Japsen, Peter; Green, Paul F.; Bonow, Johan M.; Erlström, Mikael (2016). "Episodic burial and exhumation of the southern Baltic Shield: Epeirogenic uplifts during and after break-up of Pangaea". Gondwana Research. 35: 357–377.
^ abcRapp, Anders (1982). "Periglacial nivation cirques and local glaciations in the rock canyons of Söderåsen, Scania, Sweden. A discussion and new interpretation". Danish Journal of Geography. 82 (1): 95–99. doi:10.1080/00167223.1982.10649159.
^Davidson, Kristina. "Okända gåtfulla platser i Skåne". Skånska Dagbladet (in Swedish). Retrieved October 21, 2017.
External links
Wikimedia Commons has media related to Söderåsen National Park.
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You can help expand this article with text translated from the corresponding article in French December 2011 Click show for important translation instructions View a machine translated version of the French article Machine translation like DeepL or Google Translate is a useful starting point for translations but translators must revise errors as necessary and confirm that the translation is accurate rather than simply copy pasting machine translated text into the English Wikipedia Do not translate text that appears unreliable or low quality If possible verify the text with references provided in the foreign language article You must provide copyright attribution in the edit summary accompanying your translation by providing an interlanguage link to the source of your translation A model attribution edit summary is Content in this edit is translated from the existing French Wikipedia article at fr Parc national de Soderasen see its history for attribution You should also add the template Translated fr Parc national de Soderasen to the talk page For more guidance see Wikipedia Translation Soderasen is a northwest southwest elongated bedrock ridge in Scania in southern Sweden On Soderasen is Scania s highest point at 212 m 696 ft above sea level It is intersected by several fissure valleys The ridge extends from Rostanga in the southeast to the Astorp in northwest Soderasen National ParkSoderasens nationalparkIUCN category II national park View from KopparhattenLocationSkane County SwedenNearest cityKlippanCoordinates56 01 N 13 13 E 56 017 N 13 217 E 56 017 13 217Area16 25 km2 6 27 sq mi 1 Established2001 1 Visitors350 000Governing bodyNaturvardsverketAbiskoAsnenBjornlandetBla JungfrunDalby SoderskogDjuroFulufjalletFarnebofjardenGarphyttanGotska SandonHamraHaparanda ArchipelagoKoster havetMuddusNorra KvillPadjelantaPieljekaiseSarekSkuleskogenStenshuvudStora SjofalletStore MosseSanfjalletSoderasenTivedenTresticklanTyrestaTofsingdalenVadvetjakkaAngsoclass notpageimage National parks of Sweden clickable map Soderasen National Park is located 30 km 19 mi east of Helsingborg in Scania Contents 1 Geography 1 1 Kopparhatten 1 2 Streams 1 3 Oden Lake 2 Flora fauna and funga 3 Soderasen National Park 4 References 5 External linksGeography EditIn Swedish the word as commonly refer to eskers a glacial landform but in the case of Soderasen it corresponds to a tectonic landform called horst 2 in the Sorgenfrei Tornquist Zone The last glacial ice sheet the Weichsel ice left the area of Soderasen 14 000 to 13 500 years BP Following this there was a period up to 12 700 years BP of cold non glacial conditions with permafrost and strong winds 3 Kopparhatten Edit On Soderasen is the viewpoint Kopparhatten at a height of 200 m 660 ft It is the highest point in Soderasens national park This part of the hill has a particularly dramatic landscape with up to 90 m 300 ft deep ravines Various nivation hollows exists in the vicinity of Kopparhatten 4 Streams Edit The Kvarkabacken and Skaralid streams that traverses Soderasen are believed to be antecedent rivers that existed prior to the present day relief These rivers may date to Neogene 5 times when the South Smaland peneplain formed The streams were then likely modified by meltwater during the deglaciations 6 Oden Lake Edit Oden Lake Swedish Odensjon is a lake in Scania in Sweden and belongs to Soderasens National park The lake is circular in shape with a diameter of 150 m 490 ft and it is 19 m 62 ft deep Oden Lake likely formed from a glacier niche 7 4 and the name Oden Lake may have been due to the circular shape as compared to the Norse god Odin s one eye 8 Earlier views have suggested the lake may be an volcanic explosion crater a nivation hollow or formed by fluvial erosion or as plunge pool of glacial meltwater 7 These various theories that had accumulated up to the 1980s were proposed by Alfred Gabriel Nathorst Lennart von Post Mats Akesson and Anders Rapp among others 7 Flora fauna and funga EditThe landscape offers views of leafy deciduous forests and powerful screes with high rocks flowing watercourses and wide vistas The forest is made up of different types of wood as for example beech oak and ash The ground of the forest is covered with a notable amount of plant species The area is rich with mushrooms insects water creatures mosses birds and bats Because of the rugged landscape many characteristics of primeval forest have been preserved such as an abundance of dead trees This makes the insect life rich with many rare beetles The flora is also extremely rich with species such as hollowwort enchanter s nightshade and tall meadow rue Panoramic view from KopparhattenSoderasen National Park EditThe Soderasen National Park Swedish Soderasens nationalpark is a designated area of about 16 km2 6 2 sq mi It was established in 2001 in the municipalities of Klippan and Svalov and ranges from the Skaralid ravine in the north to the Nackarpsdalen in the south It was already a protected area and when it became a national park the protection of the land increased Some of the noted features in the national park are the Oden Lake in Nackarpsdalen and the viewpoints Kopparhatten Hjortspranget and Lierna along the Skaralidsdalen References Edit a b Soderasen National Park Naturvardsverket Archived from the original on 2009 04 04 Retrieved 2009 02 26 Lundin Jonas November 13 2013 Soderasen ingen riktig as Lokaltidningen Landskrona Svalov in Swedish Retrieved October 25 2017 Berglund Bjorn E Rapp Anders 1988 Geomorphology climate and vegetation in North West Scania Sweden during the Late Weichselian Geographia Polonica 55 13 35 a b Floren Sara 2013 Geologisk guide till Soderasen 17 geologiskt intressanta platser att besoka BSc in Swedish Geologiska institutionen Lunds universitet Japsen Peter Green Paul F Bonow Johan M Erlstrom Mikael 2016 Episodic burial and exhumation of the southern Baltic Shield Epeirogenic uplifts during and after break up of Pangaea Gondwana Research 35 357 377 Lidmar Bergstrom Karna Elvhage Christian Ringberg Bertil 1991 Landforms in Skane South Sweden Geografiska Annaler Series A Physical Geography 73 2 61 91 a b c Rapp Anders 1982 Periglacial nivation cirques and local glaciations in the rock canyons of Soderasen Scania Sweden A discussion and new interpretation Danish Journal of Geography 82 1 95 99 doi 10 1080 00167223 1982 10649159 Davidson Kristina Okanda gatfulla platser i Skane Skanska Dagbladet in Swedish Retrieved October 21 2017 External links Edit Wikimedia Commons has media related to Soderasen National Park Sweden s National Parks Soderasen National Park from the Swedish Environmental Protection Agency Retrieved from https en wikipedia org w index php title Soderasen amp oldid 1165792135, wikipedia, wiki, book, books, library,
