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Kernmünsterland
The Kernmünsterland is a major landscape unit in western Germany. It covers an area of about 2700 km² and lies at the heart of the Westphalian Basin and the historic region of Münsterland in the north of Westphalia. It is bounded to the west, north and east by the sandy countryside of the Westmünsterland and Ostmünsterland, whilst in the south it is bordered by the loess landscapes of the Hellweg Börde and Emscherland. Geologically it rises clearly over the surrounding area on a bed of thinly covered Upper Cretaceous strata.E. Meynen and J. Schmithüsen: ''Handbuch der naturräumlichen Gliederung Deutschlands'' - Bundesanstalt für Landeskunde, 6th edition Remagen 1959 (total of 9 editions in 8 books 1953-1962, updated 1960 1:1,000,000 map with major units) The Kernmünsterland is roughly bounded by the valley of the River Lippe to the south and that of the Ems to the northeast, the Lippe valley being considered part of Kernmünsterland, whilst the Ems valley is counted as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beckum Hills
The Beckum Hills (german: Beckumer Berge), named after the town of Beckum, are a range of low hills, up to , in the region of Münsterland in the German state of North Rhine-Westphalia (Germany). Along with the Baumberge and its foothills and the Haltern Hills they are among the few prominent elevations in the otherwise gently rolling Münsterland (which lies at in the centre), the River Werse passes the ridge at 100 m to the east and the Lippe passing it at a height of 60 m near Hamm- Uentrop at some distance away from their highest point. In terms of natural regions the Beckum Hills belong to the Kernmünsterland, being located in the southeast of that region. Location The Beckum Hills lie in the southeastern part of Münsterland, mainly on the territory of the municipalities of Beckum (west), Wadersloh (southeast), Oelde (northeast) and Ennigerloh (northwest) - all in Warendorf district. Their extreme southwest lies in the municipality of Lippetal ( Soest ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baumberge
The Baumberge are the highest hills in the natural regions of Münsterland and Kernmünsterland with a maximum height of . They are located between Münster (Westfalen), Münster and Coesfeld, which is itself close to the southwest edge of the Baumberge. The hilly terrain has several geological, hydrography, hydrographic and architectural features. Natural regions The Baumberge and their immediate foothills are subdivided into natural regions as follows:Geographische Landesaufnahme: The natural region units on ''Sheet 83/84 - Osnabrück/Bentheim'' (Sofie Meisel 1961; centre of sheet), ''Sheet 95/96 - Kleve/Wesel'' (Wilhelm von Kürten 1977; east) and ''Sheet 97 - Münster'' (Sofie Meisel 1960; west) - Bundesanstalt für Landeskunde, Bad Godesberg â†maps/ref> * ''(to 54 Westphalian Basin)'' ** ''(to 541 Kernmünsterland)'' *** ''(to 541.0 Burgsteinfurt Land)'' **** 541.00 Osterwick Hills (''Osterwicker Hügelland'') - 128 m; gently rolling, NW foothills, separated from the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haltern Hills
The Haltern Hills (german: Halterner Berge)E. Meynen and J. Schmithüsen: ''Handbuch der naturräumlichen Gliederung Deutschlands'' - Bundesanstalt für Landeskunde, 6th edition Remagen 1959 (total of 9 deliveries of 8 books 1953-1962, updated 1:1,000,000 map of major units, 1960) comprise the three ridges of Hohe Mark (mit Rekener Kuppen), Hohe Mark (146 m), Borkenberge (133 m) and Haard (154 m) located respectively northwest, east and south of the German town of Haltern am See in Westphalia. They are the only submontane subunit in the major natural region of Westmünsterland, and are found in the southeast of the region. Immediately to the east is the southwestern part of the Kernmünsterland, also part of the Westphalian Lowland. They are separated by the valleys of the rivers Lippe (river), Lippe (northern boundary of the Haard with the other two ridges) and a line from the Halterner Mühlenbach via the Halterner Stausee and Stever river to its confluence (eastern boundary of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Westphalian Basin
The Westphalian Lowland, also known as the Westphalian Basin is a flat landscape that mainly lies within the German region of Westphalia, although small areas also fall within North Rhine (in the extreme southwest) and in Lower Saxony (on the northern periphery). Together with the neighbouring Lower Rhine Plain to the west, it represents the second most southerly region of the North German Plain, after the Cologne Bight. It is variously known in German as the ''Westfälische Bucht'' (Westphalian Bay), the ''Münsterländer'' or ''Westfälische Tieflands-'' or ''Flachlandsbucht'' (Münsterland or Westphalian Lowland or Plain). The Westphalian Lowland consists of the individual regions of Münsterland, the Emscherland in the (western) south, and regions even further south that flank the Sauerland around the Hellweg. The Westphalian Lowland is classified as a major unit group within the natural regions of Germany and is number ''54'' in the ''Handbook of the Natural Regional Divis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coesfeld
Coesfeld (; Westphalian: ''Koosfeld'') is the capital of the district of Coesfeld in the German state of North Rhine-Westphalia. History Coesfeld received its city rights in 1197, but was first recorded earlier than that in the biography of St. Ludger, patron and first bishop of the diocese of Munster who was born north of Coesfeld in Billerbeck. The day before he died, Ludger spent the night in Coesfeld and heard mass in the morning in the church he founded. He was on his way from his abbey in Essen to Münster. The road he followed passed Coesfeld and Billerbeck, and after preaching in the St. Lambert's church, 26 March 809, he travelled on to Billerbeck, where he died in the evening. The Coesfeld St. Jacobikirche dates from the same period as the city charter. For centuries, Coesfeld was an important stopping place for pilgrims traveling one of the more popular Germanic Jakobi routes ( Way of St. James) leading from Warendorf over Münster (via Billerbeck) to Coesfeld, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lünen
Lünen is a town in North Rhine-Westphalia, Germany. It is located north of Dortmund, on both banks of the River Lippe. It is the largest town of the Unna district and part of the Ruhr Area. In 2009 a biogas plant was built to provide electric power to the city. Lünen is the first city in the world to receive electricity via public utility companies that is generated on the base of animal waste. The plant produces up to 6.6 MW, supplying 26,000 homes with heat and electricity. Culture and main sights Structure *Saint George's Church *Saint Mary's Church *Chateau of Schwansbell *Colani-UFO *Freiherr-vom-Stein School *Town hall of Lünen *Geschwister-Scholl School *Industrial Monument "Moor Crane" Museum *Museum of the town Lünen *Mining Museum in Lünen South *Mining residential Museum in Lünen Brambauer Theatre *Heinz-Hilpert theater Politics The current mayor of Lünen is independent politician Jürgen Kleine-Frauns since 2015; he was originally elected as a member of Tog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Werne
Werne an der Lippe (; Westphalian: ''Wäen'') is a town in the Federal state of North Rhine-Westphalia in the Unna district in Germany. It is located on the southern edge of the Münsterland region near the Ruhrgebiet. The population of Werne is about 32,000. History Middle Ages and early modern period The first Bishop of Münster, Liudger established Werne as a parish by erecting a chapel in the southern parts of the Dreingau (''"in pago dreginni"''). He acted on orders of Charlemagne who, having finally brought the region under the fold of Francia following the conclusion of the Saxon Wars, was eager to press on with Christianization. The Latin text of the oldest preserved document (''"in villa quae dicitur werina"''), which dates from 834 and is being kept at the Leiden University Library, indicates that by this time a village had already formed around the chapel. Traders and peasants continued to accrete throughout the next three centuries. At some point between the y ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Selm
Selm is a town in the district of Unna, in North Rhine-Westphalia, Germany. It is situated approximately 20 kilometers north of Dortmund and 25 kilometers west of Hamm. Geography The town belongs to the southern part of the Münsterland. It is surrounded by (beginning in the west) Olfen, Lüdinghausen, Nordkirchen (all in the district of Coesfeld), Werne, Lünen (both in the district of Unna), Waltrop, and Datteln (both belonging to the district of Recklinghausen). History The first traces of living people in the area date from the younger half of the Stone Age. In 858 it was mentioned as ''Seliheim'' in the Dreingau. In the early Middle Ages Selm was ruled by the count of Cappenberg, then by the bishop of Münster. In the beginning of the 19th century it was transferred to Prussia, to which it remained, as part of the province of Westphalia, until 1946. In 1906 the coal mine ''Zeche Hermann'' was established, transferring coal from 1,200 m under underground. The coal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kreis Unna
The Unna () district is a Kreis (district) in central North Rhine-Westphalia, Germany. Neighboring authorities are the district of Coesfeld, the city of Hamm, the districts of Soest and Märkischer Kreis, the cities of Hagen and Dortmund, and the district of Recklinghausen. History The area of the present district of Unna was formerly part of the County of the Mark, which later belonged to Prussia. In 1753 local government of the area was reformed, creating the first district of Hamm. During the French occupation of the Napoleonic period it was included in the Ruhr département, but once returned to the rule of Prussia, the district of Hamm was recreated, although with several changes. In 1901 the town of Hamm itself became a separate urban authority, but the district retained the name of, and its administration continued to be located in Hamm until 1929. In that year the administration was moved to Unna, when the district name also changed to Unna to reflect the new administrat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kreis Recklinghausen
Recklinghausen () is a ''Kreis'' (district) in the centre of North Rhine-Westphalia, Germany. It is surrounded by the neighbouring districts of Borken, Coesfeld, Unna, Gelsenkirchen, Bottrop, and Wesel. The district administration is located in the city of the same name. Apart from the Region Hannover, Kreis Recklinghausen is the largest non-city district in Germany by population. History During medieval times, the area surrounding present-day Recklinghausen was known as ''Vest'' Recklinghausen, a territory which belonged to the Electorate of Cologne. From 1446 to 1576, this area was leased to the lordship of Gemen (now a part of the city Borken) and Schaumburg-Lippe. In 1811, the territory was added to the Grand Duchy of Berg, and in 1815 it became part of the Prussian Province of Westphalia. The district was created in 1816. After several changes it obtained its present borders with the last reorganizations of 1975–76. It is also one of the oldest districts located in Germ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ostbevern
Ostbevern is a municipality in the district of Warendorf, in North Rhine-Westphalia, Germany. Geography Ostbevern is situated on the river Bever, approx. 18 km north-east of Münster and 18 km north-west of Warendorf. Neighbouring municipalities Ostbevern borders Ladbergen, Lienen, Glandorf (in Lower Saxony), Warendorf, Telgte and Greven. Division of the town The municipality Ostbevern consists of the village Ostbevern, the district Brock and the surrounding farming land. History In 1088 Bevern was first mentioned in an official document under the name ''Beverne''. Presumably in the 12th century the parish Bevern was split into Ostbevern and Westbevern (which is now part of Telgte). During the Napoleonic Wars the municipality first fell to Prussia, then to Berg. Since 1810 it then belonged to the French Empire, until Ostbevern was assigned to prussia again at the Congress of Vienna. Since World War II Ostbevern lies in North Rhine-Westphalia. Politics Communal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
