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Region Skåne

1999 establishments in SwedenRegioner of SwedenSkåne County
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Region Skåne logo

Region Skåne is the regional council of Skåne County in Scania, Sweden. Region Skåne was formed on 1 January 1999 by the amalgamation of the county councils of Malmöhus County and Kristianstad County and some of the tasks handled by Malmö Municipality. The regional assembly is the highest political body in the region and its members are elected by the population of Skåne Country, as opposed to the County Administrative Board (länsstyrelsen) which represents the interests of the state within the county, under the chairmanship of the county governor. The region's main responsibility is for the public healthcare system, public transport and development within the region, which includes co-ordination of development of commerce, communication, culture and collaboration with other regions both in and outside of Sweden. By devolution the newly formed region assumed some powers from the Skåne County Administrative Board, the state authority in Skåne County. Before Region Skåne was formed in 1999 on a trial basis, the regional development was the responsibility of a Regional Association, comprising the 33 municipalities together with the then current health services principals, namely the Kristianstad and Malmöhus county councils and the Health Services authority in the City of Malmö. Similar provisions had also been extended to the Region Västra Götaland and the Region Gotland during a trial period.

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Region Skåne
Höörs kommun

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Geographical coordinates (GPS)

Latitude Longitude
N 56 ° E 13.45 °
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Address

Åkeshus


Höörs kommun
Sweden
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Central Skåne Volcanic Province

The Central Skåne Volcanic Province was a site of volcanic activity in the Scania region of Sweden during the Mesozoic Era of the Earth's geological history. The volcanism began with a first and main phase in late Sinemurian to Toarcian times around 191 to 178 Ma. Then volcanism continued sporadically for another 80 million years. More than one hundred volcanic necks of basaltic composition exist in Scania evidencing this volcanism. In central Scania, volcanism was in the form of a volcanic field of cinder cones that had Strombolian eruption styles. These cones produced tuffite deposits made largely of lapilli with rare volcanic bombs. Pyroclastic materials were subsequently palagonitized or largely altered to clay minerals. While eruptions occurred on land the sea was likely very close to the area. Besides purely pyroclastic sediments, lahar deposits have also been identified around the remnants of the volcanoes.Beneath a lahar deposit at Korsaröd (Djupadal Formation), Early Jurassic plant fossils including wood, pollen and spores have been exceptionally well preserved. The degree of preservation is such that cell-scale features like organelles and chromosomes have been identified in the fossils. At this location plants grew in a substrate with extensive hydrothermal alteration.The volcanism is possibly the result of decompression melting of the lithospheric mantle beneath. The volcanism is linked to a rift flank fault along the Sorgenfrei–Tornquist Zone, which is a failed rift associated with extension in the North Sea and the opening of the North Atlantic. The background to the volcanism is the break-up of Pangea, and thus it is analogous to the much more voluminous Karoo-Ferrar flood basalts of Southern Africa.

Ringsjön
Ringsjön

Ringsjön is a lake situated in the middle of Skåne County, Sweden. At 41 square kilometres (10,100 acres), it is the second largest lake in the county. The western and eastern parts of the lake, called Västra Ringsjön and Östra Ringsjön respectively, are separated by a headland. Västra Ringsjön has a depth of 6 metres (20 ft) at its deepest known point, while Östra Ringsjön has a depth of 17 metres (56 ft).Ringsjön provides drinking water for the inhabitants of Skåne if the water tunnel connected to the lake Bolmen would cease to work. This happened in 2009, when the tunnel was almost completely blocked after a collapse.Fish species found in Ringsjön are European perch, carp bream, moderlieschen, northern pike, zander, common carp, burbot, common roach, rainbow trout, crucian carp, common rudd, common whitefish, tench, eel, and brown trout. Ringsjön has had an overpopulation of carp bream and common roach for a long time, leading to an increased algal bloom, and in 2005 work began on removing 80% of these species from the lake.Many cranes make stopovers in Ringsjön on their migration to the northern parts of Sweden. They usually arrive to the lake at the end of March, but have been seen as early as 2 March.In the winter, Ringsjön is a popular place for ice yachting because of its smooth ice, and the lake gets visitors from all over Europe. The European Championships in ice yachting were held on Ringsjön in 2006. A biking competition, titled Ringsjön Runt (English: Around Ringsjön), is held annually by the lake. It attracts an average of 4000–5000 cyclists, and has been held for over forty years. The course consists of four laps around Ringsjön; one lap is 3.5 Scandinavian miles (35 km) long.Bosjökloster Castle is located on the shore of Ringsjön in Höör Municipality.