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Ormanäs och Stanstorp

Populated places in Höör MunicipalityPopulated places in Skåne CountySkåne County geography stubs

Ormanäs och Stanstorp is a locality situated in Höör Municipality, Skåne County, Sweden with 438 inhabitants in 2010.

Excerpt from the Wikipedia article Ormanäs och Stanstorp (License: CC BY-SA 3.0, Authors).

Ormanäs och Stanstorp
Höörs kommun

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Latitude Longitude
N 55.9 ° E 13.5 °
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243 93 Höörs kommun
Sweden
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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.

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.