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Franconian Alb
The Franconian Jura ( , , or ) is an upland in Franconia, Bavaria, Germany. Located between two rivers, the Danube in the south and the Main in the north, its peaks reach elevations of up to and it has an area of some 7053.8 km2. Emil Meynen, Josef Schmithüsen: '' Handbuch der naturräumlichen Gliederung Deutschlands.'' Bundesanstalt für Landeskunde, Remagen/Bad Godesberg 1953–1962 (9 editions in 8 volumes, updated map 1:1,000,000 scale with major units, 1960). It is part of the Table Jura (). Large portions of the Franconian Jura are part of the Altmühl Valley Nature Park. The scenic meanders and gorges formed by the river Altmühl draw tourists to visit the region. Geologically, the Franconian Jura is the eastern continuation of the Swabian Jura. The mountain chains are separated from each other by the impact crater of the Nördlinger Ries. The northern part of the Franconian Jura is known as Franconian Switzerland Franconian Switzerland (, ) is an upland i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bavaria
Bavaria, officially the Free State of Bavaria, is a States of Germany, state in the southeast of Germany. With an area of , it is the list of German states by area, largest German state by land area, comprising approximately 1/5 of the total land area of Germany, and with over 13.08 million inhabitants, it is the list of German states by population, second most populous German state, behind only North Rhine-Westphalia; however, due to its large land area, its population density is list of German states by population density, below the German average. Major cities include Munich (its capital and List of cities in Bavaria by population, largest city, which is also the list of cities in Germany by population, third largest city in Germany), Nuremberg, and Augsburg. The history of Bavaria includes its earliest settlement by Iron Age Celts, Celtic tribes, followed by the conquests of the Roman Empire in the 1st century BC, when the territory was incorporated into the provinces of Ra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Altmühl
The Altmühl (, ) s.v. is a river in , . It is a left tributary of the river and is approximately long. Course The source of the Altmühl is close to the town of . From here the river runs southeastwards as a narrow brook to enter the (a lake) north of Gunzenhausen. After leavin ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Bavaria
Bavaria, officially the Free State of Bavaria, is a state in the southeast of Germany. With an area of , it is the largest German state by land area, comprising approximately 1/5 of the total land area of Germany, and with over 13.08 million inhabitants, it is the second most populous German state, behind only North Rhine-Westphalia; however, due to its large land area, its population density is below the German average. Major cities include Munich (its capital and largest city, which is also the third largest city in Germany), Nuremberg, and Augsburg. The history of Bavaria includes its earliest settlement by Iron Age Celtic tribes, followed by the conquests of the Roman Empire in the 1st century BC, when the territory was incorporated into the provinces of Raetia and Noricum. It became the Duchy of Bavaria (a stem duchy) in the 6th century AD following the collapse of the Western Roman Empire. It was later incorporated into the Holy Roman Empire, became the independent Ki ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Uplands
The Central UplandsDickinson (1964), p.18 ff. (N.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 Permian period. During ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franconian Jura
The Franconian Jura ( , , or ) is an upland in Franconia, Bavaria, Germany. Located between two rivers, the Danube in the south and the Main in the north, its peaks reach elevations of up to and it has an area of some 7053.8 km2. Emil Meynen, Josef Schmithüsen: '' Handbuch der naturräumlichen Gliederung Deutschlands.'' Bundesanstalt für Landeskunde, Remagen/Bad Godesberg 1953–1962 (9 editions in 8 volumes, updated map 1:1,000,000 scale with major units, 1960). It is part of the Table Jura (). Large portions of the Franconian Jura are part of the Altmühl Valley Nature Park. The scenic meanders and gorges formed by the river Altmühl draw tourists to visit the region. Geologically, the Franconian Jura is the eastern continuation of the Swabian Jura. The mountain chains are separated from each other by the impact crater of the Nördlinger Ries. The northern part of the Franconian Jura is known as Franconian Switzerland Franconian Switzerland (, ) is an upland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kalkberg (Weismain)
The Kalkberg is a high mountain located in the Franconian Alb near Weismain in the Upper Franconian district of Lichtenfels (Bavaria), Germany. It stands at an elevation of above sea level. Geographical location and description The Kalkberg rises approximately above Weismain and the Weismain Valley funnel in the Weismain-Alb, which is a northern foothill of the Franconian Alb. It slopes down to the west towards the foothills of Kleinziegenfeld Valley and to the east into the Krassach Valley, which is the foothills of the Bärental Valley. The Kalkberg is about dominant compared to the next higher mountain, the Teisenberg. The prominence between the Kalkberg and the Teisenberg has an elevation difference of . There is also a secondary peak that has an altitude of above sea level. In the past, pits in the area of the two peaks indicate that lime marl was extracted to produce building lime. A mobile phone mast is located on the mountain's northeast slope. Geology Brown J ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bärental (Upper Franconia)
The Bärental is a small, 3.7 km long left-side valley of the Weismain Valley funnel within the Weismain-Alb region. It is situated entirely within the town of Weismain in the Lichtenfels district of Bavaria. This valley is located in the northernmost region of the Franconian Alb and is traversed by the Krassach River. Within the valley, there are 16 inhabitants, including the village of Krassach, 66 people (as of 1 January 2012). The three inhabited settlements are Herbstmühle, Krassacher Mühle, and Krassach. The valley holds appeal for hikers and is situated entirely within the nature park of Franconian Switzerland Veldensteiner Forest. Geography and description The Bärental originates from the Franconian Alb, located approximately two kilometers northeast of Seubersdorf, at an elevation of around 465 meters above sea level. Initially, the valley follows a westerly course before curving northward just prior to reaching Wunkendorf. This bend in the valley is marke ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Franconian Switzerland
Franconian Switzerland (, ) is an upland in Upper Franconia, Bavaria, Germany and a popular tourist retreat. Located between the River Pegnitz in the east and the south, the River Regnitz in the west and the River Main in the north, its relief, which reaches 600 metres in height, forms the northern part of the Franconian Jura (''Frankenjura''). Like several other mountainous landscapes in the German-speaking lands, e.g. Holstein Switzerland, Märkische Schweiz, or Pommersche Schweiz, Franconian Switzerland was given its name by Romantic artists and poets in the 19th century who compared the landscape to Switzerland. Franconian Switzerland is famous for its high density of traditional breweries. Name The region was once called ''Muggendorfer Gebürg'' ('' Muggendorf hills''). The first tourists arrived during the age of Romanticism. Two law students of Erlangen University, Ludwig Tieck and Wilhelm Heinrich Wackenroder have been credited as "discoverers" of the region. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nördlinger Ries
The Nördlinger Ries is an impact crater and large circular depression in western Bavaria and eastern Baden-Württemberg. It is located north of the Danube in the district of Donau-Ries. The city of Nördlingen is located within the depression, about south-west of its centre. Etymology "Ries" is derived from Raetia, since the tribe of Raetians lived in the area in pre- Roman times. Description The depression is a meteorite impact crater formed 14.808 ± 0.038 million years ago in the Miocene. The crater is most commonly referred to simply as the ''Ries crater'' or ''the Ries''. The original crater rim had an estimated diameter of . The present floor of the depression is about below the eroded remains of the rim. It was originally assumed that the Ries was of volcanic, glacial or tectonic origin. Oliver Sachs introduced, in this context, the term "pioneer era" (up to 1870) and marked the beginning of early modern research on the Ries (from 1870), meaning the perio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Impact Crater
An impact crater is a depression (geology), depression in the surface of a solid astronomical body formed by the hypervelocity impact event, impact of a smaller object. In contrast to volcanic craters, which result from explosion or internal collapse, impact craters typically have raised rims and floors that are lower in elevation than the surrounding terrain. Impact craters are typically circular, though they can be elliptical in shape or even irregular due to events such as landslides. Impact craters range in size from microscopic craters seen on lunar rocks returned by the Apollo Program to simple bowl-shaped depressions and vast, complex, multi-ringed impact basins. Meteor Crater is a well-known example of a small impact crater on Earth. Impact craters are the dominant geographic features on many solid Solar System objects including the Moon, Mercury (planet), Mercury, Callisto (moon), Callisto, Ganymede (moon), Ganymede, and most small moons and asteroids. On other planet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swabian Jura
The Swabian Jura ( , more rarely ), sometimes also named Swabian Alps in English, is a mountain range in Baden-Württemberg, Germany, extending from southwest to northeast and in width. It is named after the region of Swabia. It is part of the Table Jura (). The Swabian Jura occupies the region bounded by the Danube in the southeast and the upper Neckar in the northwest. In the southwest it rises to the higher mountains of the Black Forest. The highest mountain in the region is the Lemberg (Swabian Alb), Lemberg (). The area's profile resembles a high plateau, which slowly falls away to the southeast. The northwestern edge is a steep escarpment (called the Albtrauf or Albanstieg, rising up , covered with forests), while the top is flat or gently rolling. In economic and cultural terms, the Swabian Jura includes regions just around the mountain range. It is a popular recreation area. The whole ''Schwäbische Alb'' area is a UNESCO Global Geoparks, UNESCO global geopark coveri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
