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Coordinates: 56°01′N 13°13′E / 56.017°N 13.217°E / 56.017; 13.217
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{{Short description|National park in southern Sweden}}
{{Expand French|Parc national de Söderåsen|fa=yes|topic=geo|date=December 2011}}
{{Expand French|Parc national de Söderåsen|fa=yes|topic=geo|date=December 2011}}
{{Clear}}
{{Clear}}
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| coords = {{coord|56|01|N|13|13|E|region:SE_type:landmark|display=inline,title}}
| coords = {{coord|56|01|N|13|13|E|region:SE_type:landmark|display=inline,title}}
| area_km2 = 16.25
| area_km2 = 16.25
| area_ref = <ref name="naturvårdsverket">{{cite web | title=Söderåsen National Park | url=http://www.naturvardsverket.se/en/In-English/Menu/Enjoying-nature/National-parks-and-other-places-worth-visiting/National-Parks-in-Sweden/Soderasen-National-Park/ | publisher=[[Environmental Protection Agency (Sweden)|Naturvårdsverket]] | access-date=2009-02-26 | url-status=dead | archive-url=https://web.archive.org/web/20090404123623/http://www.naturvardsverket.se/en/In-English/Menu/Enjoying-nature/National-parks-and-other-places-worth-visiting/National-Parks-in-Sweden/Soderasen-National-Park/ | archive-date=2009-04-04 | df= }}</ref>
| area_ref = <ref name="naturvårdsverket">{{cite web | title=Söderåsen National Park | url=http://www.naturvardsverket.se/en/In-English/Menu/Enjoying-nature/National-parks-and-other-places-worth-visiting/National-Parks-in-Sweden/Soderasen-National-Park/ | publisher=[[Environmental Protection Agency (Sweden)|Naturvårdsverket]] | access-date=2009-02-26 | url-status=dead | archive-url=https://web.archive.org/web/20090404123623/http://www.naturvardsverket.se/en/In-English/Menu/Enjoying-nature/National-parks-and-other-places-worth-visiting/National-Parks-in-Sweden/Soderasen-National-Park/ | archive-date=2009-04-04 }}</ref>
| established = 2001<ref name="naturvårdsverket" />
| established = 2001<ref name="naturvårdsverket" />
| visitation_num =350,000
| visitation_num =350,000
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}}
}}
{{Swedish National Parks}}
{{Swedish National Parks}}
'''Söderåsen''' is a northwest-southwest elongated [[bedrock]] ridge in [[Scania]] in southern [[Sweden]]. On Söderåsen is Scania's highest point at {{convert|212|m|ft|abbr=on}} above sea level. It is intersected by several [[fissure valley]]s. The ridge extends from [[Röstånga]] in the southeast to the [[Åstorp]] in northwest.
'''Söderåsen''' is a northwest–southwest elongated [[bedrock]] ridge in [[Scania]] in southern [[Sweden]]. On Söderåsen is Scania's highest point at {{convert|212|m|ft|abbr=on}} above sea level. It is intersected by several [[fissure valley]]s. The ridge extends from [[Röstånga]] in the southeast to the [[Åstorp]] in northwest.


Söderåsen National Park is located {{convert|30|km|mi|abbr=on}} east of [[Helsingborg]] in Scania.
Söderåsen National Park is located {{convert|30|km|mi|abbr=on}} east of [[Helsingborg]] in Scania.


==Geography==
==Geography==
In Swedish the word ''ås'' commonly refer to [[esker]]s, a glacial landform, but in the case of Söderåsen it corresponds to a [[tectonic]] landform called [[horst (geology)|horst]].<ref>{{cite news |last=Lundin |first=Jonas |date=November 13, 2013 |title=Söderåsen ingen riktig ås |url=http://landskrona.lokaltidningen.se/soderasen-ingen-riktig-as-/20131113/artikler/711139919 |work=Lokaltidningen Landskrona Svalöv |location= |access-date=October 25, 2017|language=Swedish }}</ref> The last glacial [[ice sheet]], the [[Weichselian glaciation|Weichsel ice]], left the area of Söderåsen 14,000 to 13,500 years [[before present|BP]]. Following this there was a period up to 12,700 years BP of [[periglaciation|cold non-glacial]] conditions with [[permafrost]] and strong winds.<ref>{{cite journal |last1=Berglund |first1=Björn E. |last2=Rapp |first2=Anders|author-link2=Anders Rapp |date=1988 |title=Geomorphology, climate and vegetation in North-West Scania, Sweden, during the Late Weichselian |url= |journal=[[Geographia Polonica]] |volume=55 |issue= |pages=13–35 |doi= |access-date= }}</ref>
In Swedish the word ''ås'' commonly refer to [[esker]]s, a glacial landform, but in the case of Söderåsen it corresponds to a [[tectonic]] landform called [[horst (geology)|horst]]<ref>{{cite news |last=Lundin |first=Jonas |date=November 13, 2013 |title=Söderåsen ingen riktig ås |url=http://landskrona.lokaltidningen.se/soderasen-ingen-riktig-as-/20131113/artikler/711139919 |work=Lokaltidningen Landskrona Svalöv |access-date=October 25, 2017|language=sv }}</ref> in the [[Sorgenfrei-Tornquist Zone]]. The last glacial [[ice sheet]], the [[Weichselian glaciation|Weichsel ice]], left the area of Söderåsen 14,000 to 13,500 years [[before present|BP]]. Following this there was a period up to 12,700 years BP of [[periglaciation|cold non-glacial]] conditions with [[permafrost]] and strong winds.<ref>{{cite journal |last1=Berglund |first1=Björn E. |last2=Rapp |first2=Anders|author-link2=Anders Rapp |date=1988 |title=Geomorphology, climate and vegetation in North-West Scania, Sweden, during the Late Weichselian |journal=[[Geographia Polonica]] |volume=55 |pages=13–35 }}</ref>


=== Kopparhatten ===
=== Kopparhatten ===
On Söderåsen is the viewpoint Kopparhatten at a height of {{convert|200|m|ft|abbr=on}}. It is the highest point in Söderåsens national park. This part of the hill has a particularly dramatic landscape, with up to {{convert|90|m|ft|abbr=on}} deep ravines. Various [[nivation|nivation hollows]] exists in the vicinity of Kopparhatten.<ref name=Floren2013>{{cite thesis |last=Florén |first=Sara |date=2013 |title=Geologisk guide till Söderåsen – 17 geologiskt intressanta platser att besöka |type=BSc |chapter= |publisher=Geologiska institutionen Lunds universitet |docket= |oclc= |url= |access-date=|language=Swedish}}</ref>
On Söderåsen is the viewpoint Kopparhatten at a height of {{convert|200|m|ft|abbr=on}}. It is the highest point in Söderåsens national park. This part of the hill has a particularly dramatic landscape, with up to {{convert|90|m|ft|abbr=on}} deep ravines. Various [[nivation|nivation hollows]] exists in the vicinity of Kopparhatten.<ref name=Floren2013>{{cite thesis |last=Florén |first=Sara |date=2013 |title=Geologisk guide till Söderåsen – 17 geologiskt intressanta platser att besöka |type=BSc |publisher=Geologiska institutionen Lunds universitet |language=sv}}</ref>


===Streams===
===Streams===
The Kvärkabäcken and Skäralid streams that traverses Söderåsen are believed to be [[Antecedent drainage stream|antecedent rivers]] that existed prior to the present-day relief. These rivers may date to [[Neogene]]<ref>{{cite journal|author-last=Japsen|author-first=Peter |author-last2=Green |author-first2=Paul F. |author-last3=Bonow |author-first3=Johan M.|author-last4=Erlström|author-first4=Mikael |date=2016|title=Episodic burial and exhumation of the southern Baltic Shield: Epeirogenic uplifts during and after break-up of Pangaea|journal=[[Gondwana Research]] |volume=35 |issue=|pages=357–377}}</ref> times when the [[South Småland peneplain]] formed. The streams were then likely modified by [[meltwater]] during the [[deglaciation]]s.<ref name=Karna1991>{{cite journal |last1=Lidmar-Bergström |first1=Karna |last2=Elvhage |first2=Christian |last3=Ringberg |first3=Bertil|author-link=Karna Lidmar-Bergström|date=1991 |title=Landforms in Skåne, South Sweden |url= |journal=[[Geografiska Annaler|Geografiska Annaler. Series A, Physical Geography]] |volume=73 |issue=2 |pages=61–91 |doi= |access-date= }}</ref>
The Kvärkabäcken and Skäralid streams that traverses Söderåsen are believed to be [[Antecedent drainage stream|antecedent rivers]] that existed prior to the present-day relief. These rivers may date to [[Neogene]]<ref>{{cite journal|author-last=Japsen|author-first=Peter |author-last2=Green |author-first2=Paul F. |author-last3=Bonow |author-first3=Johan M.|author-last4=Erlström|author-first4=Mikael |date=2016|title=Episodic burial and exhumation of the southern Baltic Shield: Epeirogenic uplifts during and after break-up of Pangaea|journal=[[Gondwana Research]] |volume=35 |pages=357–377}}</ref> times when the [[South Småland peneplain]] formed. The streams were then likely modified by [[meltwater]] during the [[deglaciation]]s.<ref name=Karna1991>{{cite journal |last1=Lidmar-Bergström |first1=Karna |last2=Elvhage |first2=Christian |last3=Ringberg |first3=Bertil|author-link=Karna Lidmar-Bergström|date=1991 |title=Landforms in Skåne, South Sweden |journal=[[Geografiska Annaler: Series A, Physical Geography]] |volume=73 |issue=2 |pages=61–91 }}</ref>


=== Oden Lake ===
=== Oden Lake ===
Oden Lake ({{lang-sv|Odensjön}}) is a lake in Scania, in Sweden and belongs to Söderåsens National park. The lake is circular in shape, with a diameter of {{convert|150|m|ft|abbr=on}} and it is {{convert|19|m|ft|abbr=on}} deep. Oden Lake likely formed from a glacier niche,<ref name=Rapp1982>{{cite journal |last1=Rapp |first1=Anders |last2= |first2=|author-link=Anders Rapp |date=1982 |title=Periglacial nivation cirques and local glaciations in the rock canyons of Söderåsen, Scania, Sweden. A discussion and new interpretation |url= |journal=[[Danish Journal of Geography]] |volume=82 |issue=1 |pages=95–99 |doi=10.1080/00167223.1982.10649159 }}</ref><ref name=Floren2013/> and the name Oden Lake may have been due to the circular shape as compared to the Norse god [[Odin]]'s one eye.<ref>{{cite news |last=Davidson |first=Kristina |date= |title=Okända gåtfulla platser i Skåne |url=http://www.skd.se/2017/06/11/okanda-gatfulla-platser-i-skane/ |work=Skånska Dagbladet |location= |access-date= October 21, 2017|language=Swedish}}</ref> Earlier views have suggested the lake may be an volcanic [[volcanic crater|explosion crater]], a [[nivation|nivation hollow]] or formed by fluvial erosion or as [[plunge pool]] of [[glacifluvial|glacial meltwater]].<ref name=Rapp1982/> 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.<ref name=Rapp1982/>
Oden Lake ({{langx|sv|Odensjön}}) is a lake in Scania, in Sweden and belongs to Söderåsens National park. The lake is circular in shape, with a diameter of {{convert|150|m|ft|abbr=on}} and it is {{convert|19|m|ft|abbr=on}} deep. Oden Lake likely formed from a glacier niche,<ref name=Rapp1982>{{cite journal |last1=Rapp |first1=Anders |author-link=Anders Rapp |date=1982 |title=Periglacial nivation cirques and local glaciations in the rock canyons of Söderåsen, Scania, Sweden. A discussion and new interpretation |journal=[[Danish Journal of Geography]] |volume=82 |issue=1 |pages=95–99 |doi=10.1080/00167223.1982.10649159 }}</ref><ref name=Floren2013/> and the name Oden Lake may have been due to the circular shape as compared to the Norse god [[Odin]]'s one eye.<ref>{{cite news |last=Davidson |first=Kristina |title=Okända gåtfulla platser i Skåne |url=http://www.skd.se/2017/06/11/okanda-gatfulla-platser-i-skane/ |work=Skånska Dagbladet |access-date= October 21, 2017|language=sv}}</ref> Earlier views have suggested the lake may be an volcanic [[volcanic crater|explosion crater]], a [[nivation|nivation hollow]] or formed by fluvial erosion or as [[plunge pool]] of [[glacifluvial|glacial meltwater]].<ref name=Rapp1982/> 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.<ref name=Rapp1982/>


== Flora and fauna ==
== Flora, fauna, and funga ==
The landscape offers views of leafy [[deciduous]] forests and powerful [[scree]]s with high rocks, flowing watercourses and wide vistas.
The landscape offers views of leafy [[deciduous]] forests and powerful [[scree]]s with high rocks, flowing watercourses and wide vistas.


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== Söderåsen National Park ==
== Söderåsen National Park ==
The Söderåsen National Park ({{lang-sv|Söderåsens nationalpark}}) is a designated area of about {{convert|16|km2|mi2|abbr=on}}. It was established in 2001 in the municipalities of [[Klippan Municipality|Klippan]] and [[Svalöv Municipality|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.
The Söderåsen National Park ({{langx|sv|Söderåsens nationalpark}}) is a designated area of about {{convert|16|km2|mi2|abbr=on}}. It was established in 2001 in the municipalities of [[Klippan Municipality|Klippan]] and [[Svalöv Municipality|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.
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.
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{{National parks of Sweden}}
{{National parks of Sweden}}

{{authority control}}


{{DEFAULTSORT:Soderasen}}
{{DEFAULTSORT:Soderasen}}
[[Category:National parks of Sweden]]
[[Category:National parks of Sweden]]
[[Category:Geography of Skåne County]]
[[Category:Geography of Skåne County]]
[[Category:Geography of the Øresund Region]]
[[Category:Protected areas established in 2001]]
[[Category:Protected areas established in 2001]]
[[Category:2001 establishments in Sweden]]
[[Category:2001 establishments in Sweden]]

Latest revision as of 20:21, 29 October 2024

Söderåsen National Park
Söderåsens nationalpark
View from Kopparhatten
Map
LocationSkåne County, Sweden
Nearest cityKlippan
Coordinates56°01′N 13°13′E / 56.017°N 13.217°E / 56.017; 13.217
Area16.25 km2 (6.27 sq mi)[1]
Established2001[1]
Visitors350,000
Governing bodyNaturvårdsverket
class=notpageimage|
National parks of Sweden (clickable map)

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.

Söderåsen National Park is located 30 km (19 mi) east of Helsingborg in Scania.

Geography

[edit]

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

[edit]

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

[edit]

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

[edit]

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

[edit]

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

[edit]

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

[edit]
  1. ^ a b "Söderåsen National Park". Naturvårdsverket. Archived from the original on 2009-04-04. Retrieved 2009-02-26.
  2. ^ Lundin, Jonas (November 13, 2013). "Söderåsen ingen riktig ås". Lokaltidningen Landskrona Svalöv (in Swedish). Retrieved October 25, 2017.
  3. ^ Berglund, Björn E.; Rapp, Anders (1988). "Geomorphology, climate and vegetation in North-West Scania, Sweden, during the Late Weichselian". Geographia Polonica. 55: 13–35.
  4. ^ a b Florén, Sara (2013). Geologisk guide till Söderåsen – 17 geologiskt intressanta platser att besöka (BSc) (in Swedish). Geologiska institutionen Lunds universitet.
  5. ^ 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.
  6. ^ Lidmar-Bergström, Karna; Elvhage, Christian; Ringberg, Bertil (1991). "Landforms in Skåne, South Sweden". Geografiska Annaler: Series A, Physical Geography. 73 (2): 61–91.
  7. ^ a b c Rapp, 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.
  8. ^ Davidson, Kristina. "Okända gåtfulla platser i Skåne". Skånska Dagbladet (in Swedish). Retrieved October 21, 2017.
[edit]
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