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Gehn (ridge)
The Gehn is a small ridge of hills between Bramsche and Ueffeln in Germany's Central Uplands, that are an extension of the Wiehen Hills (german: Wiehengebirge). The ridge runs from northwest to southeast and is about long and an average of wide. The highest point is the Kettelberg which is high. The Gehn forms a link between the ''Wiehen Hills'' and the Ankum Heights (''Ankumer Höhe''). It is largely forested and is not - like the Ankum Heights- part of a series of ice age terminal moraines from the latest event of the Saalian glaciation, the so-called Drenthe I stage, but is a ridge of Jurassic rock that was pushed up during the folding towards the end of the Cretaceous period. Like the Wiehen Hills and the Ankum Heights, the Gehn belongs to the North Teutoburg Forest-Wiehen Hills Nature Park The TERRA.vita Nature Park (german: Naturpark TERRA.vita) is located in the German states of Lower Saxony and North Rhine-Westphalia and is divided into northern and southern areas. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falk Oberdorf Gehn Physisch
Falk may refer to: * Falk (name), including origin and list of people with this name * Falk, California, a ghost town * Falk Township, Minnesota * Postal abbreviation of Falkirk, an area of Scotland See also *Falx (other) *Faulk (other) Faulk may refer to: People *Andrew Jackson Faulk (1814–1898), 3rd Governor of Dakota Territory * Clarence Faulk (1909–2010), American journalist and broadcaster *John Henry Faulk (1913–1990), American radio show host * Justin Faulk (born 1992 ... * Falck (other) {{disambiguation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bramsche
Bramsche is a town in the district of Osnabrück, Lower Saxony, Germany. It is about north of Osnabrück, at . Population is 30,952 (2018). Subdivisions In 1971/72 12 previously independent municipalities were included into the town. *Achmer *Balkum *Epe and Malgarten *Engter *Evinghausen *Hesepe *Kalkriese – site of the Battle of the Teutoburg Forest *Lappenstuhl *Pente *Schleptrup *Sögeln *Ueffeln Mayors The mayor of Bramsche is Heiner Pahlmann (SPD), re-elected in 2021. He was first elected in May 2014 with 63.0% of the votes. His predecessor Liesel Höltermann (SPD) did not run for mayor any more. Twin towns – sister cities Bramsche is twinned with: * Biskupiec, Poland * Harfleur, France * Ra'anana, Israel * Todmorden, England, United Kingdom Notable people * Peter Urban (born 1948), radio and television moderator *Marieluise Beck (born 1952), politician (Alliance 90/The Greens), Member of Bundestag since 1983 *Filiz Polat (born 1978), politician (Alliance 90/The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Uplands
The Central UplandsDickinson (1964), p.18 ff. (german: die MittelgebirgeN.B. In German die ''Mittelgebirge'' (plural) refers to the Central Uplands; das ''Mittelgebirge'' refers to a low mountain range or upland region (''Mittel'' = "medium" and ''-gebirge'' = "range").) is one of the three major natural regions of Germany. It stretches east to west across the country. To the north lies the North German Plain or Northern Lowland; to the south, the Alps and the Alpine Foreland. Formation The German Central Uplands, like the Scandinavian and British mountain ranges and the Urals, belong to the oldest mountains of Europe, even if their present-day appearance has only developed relatively recently. In the Carboniferous, i.e. about 350 million years ago, Variscan mountain ranges were formed in central Europe by the uplifting caused by tectonic plate collision. Immediately after their formation the erosion of the mountains began under the influence of exogenous processes during the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wiehen Hills
The Wiehen Hills (german: Wiehengebirge, , also locally, just ''Wiehen'') are a hill range in North Rhine-Westphalia and Lower Saxony in Germany. The hills run from west to east like a long finger away from the main upland area of the Lower Saxon Hills, beginning at the Weser River near Minden and terminating in the vicinity of Osnabrück. It is the northernmost of the German Central Upland ranges extending into the Northern Lowlands. Their highest hill is the Heidbrink near Lübbecke with an altitude of . Location The Wiehen Hills lie within the districts of Landkreis Osnabrück, Osnabrück, Kreis Minden-Lübbecke, Minden-Lübbecke and Kreis Herford, Herford. Their northern section runs in an east-west direction roughly from the territory of Bramsche (northwest of Osnabrück) via Ostercappeln, Bad Essen, Preußisch Oldendorf and Rödinghausen, Lübbecke, Hüllhorst and Bad Oeynhausen as far as the towns of Minden and Porta Westfalica on the Porta Westfalica (gorge), Porta We ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ankum Heights
The Ankum Heights (german: Ankumer Höhe), also called the Fürstenau Hills (''Fürstenauer Berge''), are a ridge of hills up to 140 m high in the western part of the state of Lower Saxony on the North German Plain. Geography The densely forested Ankum Heights, which are about long and only a few kilometres wide, lies roughly north-northwest of the city of Osnabrück on the boundary of the districts of Emsland and Osnabrück between Herzlake to the northwest and Bramsche to the southeast, Fürstenau in the southwest and Bersenbrück in the northeast. The southeastern foothills of the ridge, which form the northwestern part of the North Teutoburg Forest-Wiehen Hills Nature Park reach almost as far as the Alfsee lake. East of the Ankum Heights are the Damme Hills, to the southeast are the west-northwestern outliers of the Wiehen Hills, to the south is Tecklenburg Land and the northwestern outliers of the Teutoburg Forest, to the west the Lingen Heights and the Emslan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Terminal Moraine
A terminal moraine, also called end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by the front edge of the ice, is driven no further and instead is deposited in an unsorted pile of sediment. Because the glacier acts very much like a conveyor belt, the longer it stays in one place, the greater the amount of material that will be deposited. The moraine is left as the marking point of the terminal extent of the ice. Formation As a glacier moves along its path, the surrounding area is continuously eroding. Loose rock and pieces of bedrock are constantly being picked up and transported with the glacier. Fine sediment and particles are also incorporated into the glacial ice. The accumulation of these rocks and sediment together form what is called glacial till when deposited. Push moraines are formed when a glacier retreats from a previou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saalian Glaciation
The Saale glaciation or Saale Glaciation, sometimes referred to as the Saalian glaciation, Saale cold period (german: Saale-Kaltzeit), Saale complex (''Saale-Komplex'') or Saale glacial stage (''Saale-Glazial'', colloquially also the ''Saale-Eiszeit'' or ''Saale-Zeit''), covers the middle of the three large glaciations in Northern Europe and the northern parts of Eastern, Central and Western Europe by the Scandinavian Inland Ice Sheet between the older Elster glaciation and the younger Weichselian glaciation, also called the Last Glacial Period. Age and definitions It succeeded the Holstein interglacial and was followed by the Eemian interglacial. The Saale complex is currently estimated, depending on the source, as existing from around 300,000 to 130,000 years ago or 347,000 to 128,000 years ago (duration: around 219,000 years), roughly contemporaneous with the glaciation of the Riss Glacial in the Alpine region. The actual "ice age" includes only part of the Saale glaciation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Teutoburg Forest-Wiehen Hills Nature Park
The TERRA.vita Nature Park (german: Naturpark TERRA.vita) is located in the German states of Lower Saxony and North Rhine-Westphalia and is divided into northern and southern areas. The park is also known as the ''Osnabrück Land Nature Park'' and sometimes by its old name of ''North Teutoburg Forest-Wiehen Hills Nature Park''. The woodlands of the Nature Park comprise about 70% of its total area.Sehere/ref> The Nature Park Northern area The northern part of the nature park begins in the Emsland near Herzlake and extends from there over the southern fringes of the Oldenburger Münsterland and Osnabrück Land in a southeast direction over the Ankum Heights to Bramsche. From there it widens out north of Osnabrück over the Wiehen Hills eastwards and then over the gorge of Porta Westfalica, continuing further to the east as far as the Bückeburg, which lies east of the Weser and north of the Wesergebirge; the park area thus extends into the northwestern part of the Wesergeb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ridges Of Lower Saxony
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 hill A hill is a landform that extends above the surrounding terrain. It often has a distinct Summit (topography), summit. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally con ...s 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 drainage, Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
