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Skåne County

1997 establishments in SwedenCounties of SwedenScaniaSkåne CountyStates and territories established in 1997
Sweden Scania location map
Sweden Scania location map

Skåne County (Swedish: Skåne län [ˈskôːnɛ ˈlɛːn]), sometimes referred to as Scania County in English, is the most southern county, or län, of Sweden, basically corresponding to the traditional province Scania. It borders the counties of Halland, Kronoberg and Blekinge and connects to Capital Region, Denmark by the Öresund Bridge. The seat of residence for the Skåne Governor is the city of Malmö. The headquarters of Skåne Regional Council are located in both Kristianstad and Malmö.The present county was created in 1997 when Kristianstad County and Malmöhus County were merged; it covers around 3% of Sweden's total area, while its population of 1.3 million comprises 13% of Sweden's total population. Prince Oscar is Duke of Skåne.

Excerpt from the Wikipedia article Skåne County (License: CC BY-SA 3.0, Authors, Images).

Skåne County
Höörs kommun

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Wikipedia: Skåne CountyContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 55.995309 ° E 13.441772 °
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Address

Månstorp


243 92 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.