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Linderödsåsen
The Linderödsåsen is a ridge, geologically a '' horst,'' in the province of Skåne in southernmost Sweden. It lies at the edge of the Baltic shield, in the Tornquist Zone, and continues with the Hallandsås in north western direction towards the Kattegat.Swedish University of Agricultural SciencesBedrocks in Sweden/ref> It stretches through Skåne from northwest to southeast. On the map it is situated in the middle of the province. It continues south-east down to the shore, mostly consisting of rocks, and ends with the notable steep Stenshuvud steep at . In its central parts, around Höör Municipality, the ridge has a height of 100–120 meters. The average width is 15-30 kilometers. Its highest point is at 196 meters. Administratively, it used to mark the border between Malmöhus County and Kristianstad County (united in 1999 as Skåne County Skåne County ( sv, Skåne län, link=no ), sometimes referred to as Scania County in English, is the most southern count ...
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Tornquist Zone
The Trans-European Suture Zone (TESZ), also known as the Tornquist Zone, is the crustal boundary between the Precambrian East European Craton and the Phanerozoic orogens of South-Western Europe. The zone runs from the North Sea to the Black Sea. The north-western part of the zone was created by the collision of Avalonia and Baltica/East European Craton in the Late Ordovician. The south-eastern part of the zone, now largely concealed by deep sedimentary basins, developed through Variscan and Alpine orogenic events. Various branches of the TESZ go under different names: * The Teisseyre-Tornquist Zone (TTZ) in Ukraine and Poland. * The Sorgenfrei-Tornquist Zone (STZ) through Scania (Sweden), Kattegat, and North Jutland (Denmark). * The Trans-European Fault (TEF), Thor-Tornquist Suture or Thor Suture through southern Denmark. The latter two branches (STZ and TEF) span a triangular area of numerous faults, called the Tornquist Fan. History of Discovery In 1893 the Polish geologi ...
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Scania
Scania, also known by its native name of Skåne (, ), is the southernmost of the historical provinces of Sweden, provinces (''landskap'') of Sweden. Located in the south tip of the geographical region of Götaland, the province is roughly conterminous with Skåne County, created in 1997. Like the other former provinces of Sweden, Scania still features in colloquial speech and in cultural references, and can therefore not be regarded as an archaic concept. Within Scania there are 33 municipalities of Sweden, municipalities that are autonomous within the Skåne Regional Council. Scania's largest urban areas of Sweden, city, Malmö, is the third-largest city in Sweden, as well as the fifth-largest in Scandinavia. To the north, Scania borders the former provinces of Halland and Småland, to the northeast Blekinge, to the east and south the Baltic Sea, and to the west Öresund. Since 2000, a road and railway bridge, the Öresund Bridge, bridges the Öresund, Sound and connects Scania ...
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Hallandsås
Hallandsås is a horst on the border between the Swedish counties Skåne and Halland. It is part of a geological formation that includes an island in the sea outside the village of Torekov near Båstad called ''Hallands Väderö''. The geological formation continues with the Linderödsåsen in Skåne. It was formed during the Late Cretaceous period 80 million years ago. It reaches its highest point at ''Högalteknall'' near the village of ''Hasslöv'' at 224 metres. In modern times it is most noted for the project which serves to create a tunnel through it to speed up railway communications, the Hallandsås Tunnel and the two skiing centres which were opened during the 1980s. In older times it was most noted for being a dangerous route for the postal services which often were robbed by people in the area. The "Snapphane A ''snapphane'' was a member of a 17th-century pro-Danish guerrilla organization, auxiliaries or paramilitary troops that fought against the Swedes in the Sec ...
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Land Of Skåne
Land, also known as dry land, ground, or earth, is the solid terrestrial surface of the planet Earth that is not submerged by the ocean or other bodies of water. It makes up 29% of Earth's surface and includes the continents and various islands. Earth's land surface is almost entirely covered by regolith, a layer of rock, soil, and minerals that forms the outer part of the crust. Land plays important roles in Earth's climate system and is involved in the carbon cycle, nitrogen cycle, and water cycle. One-third of land is covered in trees, 15% is used for crops, and 10% is covered in permanent snow and glaciers. Land terrain varies greatly and consists of mountains, deserts, plains, plateaus, glaciers, and other landforms. In physical geology, the land is divided into two major categories: mountain ranges and relatively flat interiors called cratons. Both are formed over millions of years through plate tectonics. A major part of Earth's water cycle, streams shape the landscape ...
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Ridge
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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Horst (geology)
In physical geography and geology, a horst is a raised fault block bounded by Fault (geology), normal faults. Horsts are typically found together with Graben, grabens. While a horst lifted or remains stationary, the grabens on either side Subsidence, subside. This is often caused by Extensional tectonics, extensional forces pulling apart the crust. Horsts may represent features such as plateaus, mountains, or ridges on either side of a valley. Horsts can range in size from small fault-blocks, up to large regions of stable continent that have not been not folded or warped by tectonic forces. The word ''Horst'' in German language, German means "mass" or "heap," and was first used in the geological sense in 1883 by Eduard Suess in ''The Face of the Earth.''Originally published in 1883 in German as "Das Antlitz der Erde", translated and published in English in 1904 Geomorphology Horsts may have either symmetrical or asymmetrical cross-sections. If the normal faults to either side ...
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Sweden
Sweden, formally the Kingdom of Sweden,The United Nations Group of Experts on Geographical Names states that the country's formal name is the Kingdom of SwedenUNGEGN World Geographical Names, Sweden./ref> is a Nordic country located on the Scandinavian Peninsula in Northern Europe. It borders Norway to the west and north, Finland to the east, and is connected to Denmark in the southwest by a bridgetunnel across the Öresund. At , Sweden is the largest Nordic country, the third-largest country in the European Union, and the fifth-largest country in Europe. The capital and largest city is Stockholm. Sweden has a total population of 10.5 million, and a low population density of , with around 87% of Swedes residing in urban areas in the central and southern half of the country. Sweden has a nature dominated by forests and a large amount of lakes, including some of the largest in Europe. Many long rivers run from the Scandes range through the landscape, primarily ...
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Baltic Shield
The Baltic Shield (or Fennoscandian Shield) is a segment of the Earth's crust belonging to the East European Craton, representing a large part of Fennoscandia, northwestern Russia and the northern Baltic Sea. It is composed mostly of Archean and Proterozoic gneisses and greenstone which have undergone numerous deformations through tectonic activity. It contains the oldest rocks of the European continent with a thickness of 250–300 km. The Baltic Shield is divided into five ''provinces'': the Svecofennian and Sveconorwegian (or Southwestern gneiss) provinces in Fennoscandia, and the Karelian, Belomorian and Kola provinces in Russia. The latter three are divided further into several ''blocks'' and ''complexes'' and contain the oldest of the rocks, at 2500-3100 Ma (million years) old. The youngest rocks belong to the Sveconorwegian province, at 900-1700 Ma old. Thought to be formerly part of an ancient continent, the Baltic Shield grew in size through collisions with n ...
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Kattegat
The Kattegat (; sv, Kattegatt ) is a sea area bounded by the Jutlandic peninsula in the west, the Danish Straits islands of Denmark and the Baltic Sea to the south and the provinces of Bohuslän, Västergötland, Halland and Skåne in Sweden in the east. The Baltic Sea drains into the Kattegat through the Danish Straits. The sea area is a continuation of the Skagerrak and may be seen as a bay of the North Sea, but in traditional Scandinavian usage, this is not the case. The Kattegat is a rather shallow sea and can be very difficult and dangerous to navigate because of the many sandy and stony reefs and tricky currents, which often shift. In modern times, artificial seabed channels have been dug, many reefs have been dredged by either sand pumping or stone fishing, and a well-developed light signaling network has been installed, to safeguard the very heavy international traffic of this small sea. There are several large cities and major ports in the Kattegat, including, in d ...
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Stenshuvud
Stenshuvud is a hill in the southeastern corner of Sweden, in the province of Scania, close to Kivik in Simrishamn Municipality. Since 1986, it is one of the National parks of Sweden. The park covers an area of about . The hill is high and faces the Baltic Sea. Since the surrounding landscape is relatively flat, it can be seen from a great distance and has traditionally been used as a landmark for seafarers. Many visitors trek up the hill to enjoy the view which is very good in clear weather. Most of the area is covered with broadleaf forest, especially European hornbeam. The park also contains heaths, meadows and swamps. Because of the mild climate and varied habitats, many different animal and plant species can be encountered in the park. The park contains unusual Swedish wildlife such as the hazel dormouse, Eurasian golden oriole, European tree frog and agile frog. There are about 600 vascular plant species, including several types of orchids and the very rare barren strawb ...
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Höör Municipality
Höör Municipality (''Höörs kommun'') is a municipality in the central part of Skåne County in southern Sweden. Its seat is located in the town of Höör. The present municipality was formed in 1969 through the merger of "old" Höör with the municipalities of Norra Frosta, Snogeröd and Tjörnarp parish from the dissolved Sösdala Municipality. Geography Höör Municipality credits itself by being different from the rest of Scania: Apart from agricultural areas, Höör Municipality also has several forests and the lake Ringsjön. Ringsjön is the second largest lake in Skåne County and covers some 40 km², about three times the size of the town of Höör. The two main attractions of the municipality that draw visitors are the zoological garden Skånes Djurpark, and the ''Bosjökloster Castle'' established in the 12th century. The castle is situated in a scenic location in a cape in the lake Ringsjön; the zoological garden is situated just north of the town of ...
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Malmöhus County
Malmöhus County ( sv, Malmöhus län) was a county of Sweden 1719–1996. On 1 January 1997 it was merged with Kristianstad County to form Skåne County. It had been named after Malmöhus, a castle in Malmö, which was also where the governor originally lived. History Malmöhus County was part of Skåne province which was controlled by Denmark until 1658. In 1657, Denmark declared war on Sweden, while Sweden was at war with Russia, Poland, and Austria. Swedish forces were sent immediately from Poland to Denmark. Denmark was defeated which required the transfer of Skåne, Halland, Blekinge and Bohuslän provinces to Sweden under the Treaty of Roskilde. Denmark attempted to regain the lost provinces until 1710, but was unsuccessful. Geography Malmöhus County was part of Scania province situated on a peninsula that projects into the Baltic Sea on the northeast of the Öresund straits. The geography differs in many aspects from the rest of Sweden. The coastal regions typically hav ...
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