Forggensee
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Forggensee
The Forggensee, also called the Roßhaupten Reservoir, is a reservoir located north of Füssen in the county of Ostallgäu in Bavaria, Germany and one of many lakes in the region around Hohenschwangau and Neuschwanstein castles. With a surface area of 15.2 km², it is the fifth-largest lake in Bavaria and the largest reservoir in Germany by area. The River Lech flows through it. The Forggensee is known primarily as a tourist destination for aquatic sports and recreation. Besides Füssen, other settlements on the lake include Halblech, Rieden am Forggensee and Roßhaupten. The lake takes its name from the former hamlet of Forggen which has been submerged by the reservoir. Origin Following the climax of the last ice age, the Lech-Wertach foreland glacier, which covered the entire Ostallgäu, gradually melted back from its maximum extent at Kaufbeuren. In the course of its retreat, as in the entire Pre-Alpine area, new morainic ridges were formed from the masses of debr ...
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Forggensee Luftbild
The Forggensee, also called the Roßhaupten Reservoir, is a reservoir located north of Füssen in the county of Ostallgäu in Bavaria, Germany and one of many lakes in the region around Hohenschwangau and Neuschwanstein castles. With a surface area of 15.2 km², it is the fifth-largest lake in Bavaria and the largest reservoir in Germany by area. The Lech (river), River Lech flows through it. The Forggensee is known primarily as a tourist destination for aquatic sports and recreation. Besides Füssen, other settlements on the lake include Halblech, Rieden am Forggensee and Roßhaupten. The lake takes its name from the former hamlet of Forggen which has been submerged by the reservoir. Origin Following the climax of the Würm Ice Age, last ice age, the Lech-Wertach foreland glacier, which covered the entire Ostallgäu, gradually melted back from its maximum extent at Kaufbeuren. In the course of its retreat, as in the entire Pre-Alps, Pre-Alpine area, new morainic ridges ...
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Füssen
Füssen is a town in Bavaria, Germany, in the district of Ostallgäu, situated one kilometre from the Austrian border. The town is known for violin manufacturing and as the closest transportation hub for the Neuschwanstein and Hohenschwangau castles. As of , the town has a population of . History Füssen was settled in Roman times, on the Via Claudia Augusta, a road that leads southwards to northern Italy and northwards to Augusta Vindelicum (today's Augsburg), the former regional capital of the Roman province Raetia. The original name of Füssen was "Foetes", or "Foetibus" (inflected), which derives from Latin "Fauces", meaning "gorge", probably referring to the Lech gorge. In Late Antiquity Füssen was the home of a part of the Legio III Italica, which was stationed there to guard the important trade route over the Alps. Füssen later became the site of the "Hohes Schloss" (High Castle), the former summer residence of the prince-bishops of Augsburg. Below the Hohes Schloss is ...
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River Lech
The Lech (, ''Licca'') is a river in Austria and Germany. It is a right tributary of the Danube in length with a drainage basin of . Its average discharge at the mouth is . Its source is located in the Austrian state of Vorarlberg, where the river rises from lake Formarinsee in the Alps at an altitude of . It flows in a north-north-easterly direction and crosses the German border, forming the Lechfall, a waterfall; afterwards the river enters a narrow gorge (the Lechschlucht). Leaving the Alps, it enters the plains of the Allgäu at Füssen at an elevation of in the German state of Bavaria, where it used to be the location of the boundary with Swabia. The river runs through the city of Füssen and through the Forggensee, a man-made lake which is drained in winter. Here, it forms rapids and a waterfall. The river flows further northwards through a region called the Lechrain, and passes the cities of Schongau, Landsberg, Augsburg (where it receives the Wertach) and Rain bef ...
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Lech (river)
The Lech (, ''Licca'') is a river in Austria and Germany. It is a right tributary of the Danube in length with a drainage basin of . Its average discharge at the mouth is . Its source is located in the Austrian state of Vorarlberg, where the river rises from lake Formarinsee in the Alps at an altitude of . It flows in a north-north-easterly direction and crosses the German border, forming the Lechfall, a waterfall; afterwards the river enters a narrow gorge (the Lechschlucht). Leaving the Alps, it enters the plains of the Allgäu at Füssen at an elevation of in the German state of Bavaria, where it used to be the location of the boundary with Swabia. The river runs through the city of Füssen and through the Forggensee, a man-made lake which is drained in winter. Here, it forms rapids and a waterfall. The river flows further northwards through a region called the Lechrain, and passes the cities of Schongau, Landsberg, Augsburg (where it receives the Wertach) and Rain be ...
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Neuschwanstein
Neuschwanstein Castle (german: Schloss Neuschwanstein, , Southern Bavarian: ''Schloss Neischwanstoa'') is a 19th-century historicist palace on a rugged hill above the village of Hohenschwangau near Füssen in southwest Bavaria, Germany. The palace was commissioned by King Ludwig II of Bavaria as a retreat and in honour of Richard Wagner. Ludwig chose to pay for the palace out of his personal fortune and by means of extensive borrowing, rather than Bavarian public funds. Construction began in 1869, but was never fully completed. The castle was intended as a private residence for the King, until he died in 1886. It was open to the public shortly after his death. Since then more than 61 million people have visited Neuschwanstein Castle. More than 1.3 million people visit annually, with as many as 6,000 per day in the summer. Location The municipality of Schwangau lies at an elevation of at the southwest border of the German state of Bavaria. Its surroundings are character ...
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Rieden Am Forggensee
Rieden am Forggensee is a municipality in the district of Ostallgäu in Bavaria in Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe .... References Ostallgäu {{Ostallgäu-geo-stub ...
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Ostallgäu
Ostallgäu is a ''Landkreis'' (district) in Swabia, Bavaria, Germany. It is bounded by (from the west and clockwise) the districts of Oberallgäu, Unterallgäu, Augsburg, Landsberg, Weilheim-Schongau and Garmisch-Partenkirchen, and by the Austrian state of Tyrol. The town of Kaufbeuren is enclosed by but does not belong to the district. History Before 1803 the region was split into several tiny states, most of them clerical states. When these states were dissolved in 1803, the Ostallgäu region became part of Bavaria. The kings of Bavaria soon developed a special relationship with the region and built their famous castles of Hohenschwangau and Neuschwanstein there. The district was established in 1972 by merging the former districts of Kaufbeuren, Marktoberdorf and Füssen. Geography "Ostallgäu" literally means "Eastern Allgäu". The term Allgäu is applied to the part of the Alps located in Swabia and their northern foothills. The district extends from the crest of the Alps ...
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Bannwaldsee
Bannwaldsee is a lake near Schwangau, Bavaria, Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe .... At an elevation of 785.9 m, its surface area is 2.28 km². See also * List of lakes in Bavaria External links * Lakes of Bavaria Ostallgäu {{Ostallgäu-geo-stub ...
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Lower Marine Molasse
The Molasse basin (or North Alpine foreland basin) is a foreland basin north of the Alps which formed during the Oligocene and Miocene epochs. The basin formed as a result of the flexure of the European plate under the weight of the orogenic wedge of the Alps that was forming to the south. In geology, the name "molasse basin" is sometimes also used in a general sense for a synorogenic (formed contemporaneously with the orogen) foreland basin of the type north of the Alps. The basin is the type locality of molasse, a sedimentary sequence of conglomerates and sandstones, material that was removed from the developing mountain chain by erosion and denudation, that is typical for foreland basins. Geographic location The Molasse basin stretches over 1000 kilometers along the long axis of the Alps, in France, Switzerland, Germany and Austria. The west end is at Lake Geneva, where the basin's outcrop is just 20 km wide. Further to the northeast the basin becomes wider. It forms t ...
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Lech Glacier
Lech may refer to: People * Lech (name), a name of Polish origin * Lech, the legendary founder of Poland * Lech (Bohemian prince) Products and organizations * Lech (beer), Polish beer produced by Kompania Piwowarska, in Poznań * Lech Poznań, football club in Poznań * Lech Poznań II, the reserve team of Lech Poznań * Lech Rypin, football club in Rypin * Lech (airship), the first Polish zeppelin * Lech (motorcycle), defunct Polish motorcycle manufacturer Places * Lech (river) in Austria and Germany * Lech am Arlberg, a village and noble ski resort in Vorarlberg, Austria * Lechia, an ancient name of Poland Other uses * "Lech", a song by Slipknot from '' .5: The Gray Chapter'' * Lecherous behavior or person * Lech Coaster, a roller coaster in Poland See also * Leszek * Slavic names * Lechia (other) Lechia is the historical and/or alternative name of Poland. Current use Other uses of the name Lechia are; In sports: * Men's football; ** Lechia Gdańsk, Po ...
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Meltwaters
Meltwater is water released by the melting of snow or ice, including glacial ice, tabular icebergs and ice shelves over oceans. Meltwater is often found in the ablation zone of glaciers, where the rate of snow cover is reducing. Meltwater can be produced during volcanic eruptions, in a similar way in which the more dangerous lahars form. When meltwater pools on the surface rather than flowing, it forms melt ponds. As the weather gets colder meltwater will often re-freeze. Meltwater can collect or melt under the ice's surface. These pools of water, known as subglacial lakes can form due to geothermal heat and friction. Water source Meltwater provides drinking water for a large proportion of the world's population, as well as providing water for irrigation and hydroelectric plants. This meltwater can originate from seasonal snowfall, or from the melting of more permanent glaciers. Climate change threatens the precipitation of snow and the shrinking volume of glaciers. Some ...
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Flysch
Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to th ...
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