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Weßlinger See
The Weßlinger See ( 'Lake Weßling') is the smallest lake in the Fünfseenland ( 'five lakes country') in Upper Bavaria. It is completely enclosed by the municipality of Weßling. Overview Lake Weßling is a remnant of a kettle hole created during the Würm glaciation. It has no natural tributary, and due to the use of fertilizers in the catchment area it was close to becoming hypoxic in the 20th century. To counter this problem an oxygen pump was installed in the middle of the lake in the 1970s, which has significantly improved the ecologic balance. Due to its small size and lack of a natural tributary, regionally it is usually one of the warmest lakes in summer and the first lake to freeze over in winter. Especially in summer this means the lake attracts numerous visitors from the Munich Metropolitan Region. Starting in the 19th century, the scenic setting within the Bavarian Alpine Foreland has also attracted several painters and sculptors (e.g. Carl Schuch, Pierre-Auguste R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Starnberg (district)
Starnberg () is a ''Landkreis'' (district) in the southern part of Bavaria, Germany. Neighboring districts are (from the north clockwise) Fürstenfeldbruck, Munich, Bad Tölz-Wolfratshausen, Weilheim-Schongau and Landsberg. Starnberg district and the Hochtaunuskreis regularly compete for the title of Germany's wealthiest district. Geography Main geographic feature of the district are the five lakes – the Starnberger See and Ammersee, as well as the smaller Weßlinger See, Wörthsee and Pilsensee. The lakes were formed by the glaciers of the last ice age. Hence the district is also called '' Fünf-Seen-Land'' (five lake county). History The district was created in 1902, when the ''Bezirksamt München II'' was dissolved, and the new ''Bezirksamt Starnberg'' and ''Bezirksamt Wolfratshausen'' were created. Starting in 1939 they were called ''Landkreis''. In 1972 two municipalities (Bachhausen and Höhenrain) from the district Wolfratshausen were added to the district. In the 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fünfseenland
The Fünfseenland is the name for an area in Upper Bavaria between, and including, the Ammersee and Starnberger See, which contains the remainder of the great glacial lakes of the area (Pilsensee, Wörthsee Wörthsee (Wörth lake) is a lake in the Starnberg district of Bavaria, Germany. It is one of the lakes of the Fünfseenland (Five lakes) region, which contains the remains of a great glacial lake. Location The Wörthsee is located to the east ... and the Weßlinger See). Gallery File:Diessen Ammersee-2.jpg, Ammersee File:2004-07-03 15-58-18 Hechendorf.jpg, Pilsensee File:Starnberger See 1.JPG, Starnberger See File:Steinebach WseeWalchstadt.jpg, Wörthsee File:Weßling Weßlinger See 668.jpg, Weßlinger See File:Aerial image of the Osterseen (view from the south).jpg, Osterseen File:Osterseen Gewitterabend Grosser Ostersee 02.jpg, The big Ostersee File:Maisinger See2.jpg, Maisinger See {{DEFAULTSORT:Funfseenland Lakes of Bavaria ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Bavaria
Upper Bavaria (german: Oberbayern, ; ) is one of the seven administrative districts of Bavaria, Germany. Geography Upper Bavaria is located in the southern portion of Bavaria, and is centered on the city of Munich, both state capital and seat of the district government. Because of this, it is by far the most populous administrative division in Bavaria. It is subdivided into four planning regions (''Planungsverband''): Ingolstadt, Munich, Bayerisches Oberland (Bavarian Highland), and Südostoberbayern (South East Upper Bavaria). The name 'Upper Bavaria' refers to the relative position on the Danube and its tributaries: downstream, Upper Bavaria is followed by Lower Bavaria, then Upper Austria, and subsequently Lower Austria. ''Landkreise'' (districts): * Altötting * Bad Tölz-Wolfratshausen * Berchtesgadener Land * Dachau * Ebersberg * Eichstätt * Erding * Freising * Fürstenfeldbruck * Garmisch-Partenkirchen * Landsberg * Miesbach * Mühldorf * Munich (''München'') ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weßling
Weßling is a municipality in the district of Starnberg in Bavaria, Germany. History Weßling was first mentioned in the 13th century, when it was passed to Seefeld Castle. In 1810 it was recorded to consist of 37 farms and in 1877 to have a population of 230. Since, starting from the 19th century, it was visited by several painters and sculptors (e.g. Carl Schuch, Pierre-Auguste Renoir, Wilhelm Trübner), the town is regarded by some as an artists' colony. In 1903, when Weßling had a population of 350, the construction of a railway from Munich to Herrsching led to a moderately increased influx of population around Lake Weßling. The town of Oberpfaffenhofen, which is now part of Weßling, gained some importance as an industrial and research location in 1936, when an airport was built there by the aircraft manufacturer Dornier. In 1972 and 1976 the municipalities of Hochstadt and Oberpfaffenhofen respectively were incorporated into Weßling. Geography Weßling is located ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kettle Hole
A kettle (also known as a kettle lake, kettle hole, or pothole) is a depression/hole in an outwash plain formed by retreating glaciers or draining floodwaters. The kettles are formed as a result of blocks of dead ice left behind by retreating glaciers, which become surrounded by sediment deposited by meltwater streams as there is increased friction. The ice becomes buried in the sediment and when the ice melts, a depression is left called a kettle hole, creating a dimpled appearance on the outwash plain. Lakes often fill these kettles; these are called kettle hole lakes. Another source is the sudden drainage of an ice-dammed lake. When the block melts, the hole it leaves behind is a kettle. As the ice melts, ramparts can form around the edge of the kettle hole. The lakes that fill these holes are seldom more than deep and eventually fill with sediment. In acid conditions, a kettle bog may form but in alkaline conditions, it will be kettle peatland. Overview Kettles are fluviog ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Würm Glaciation
The Würm glaciation or Würm stage (german: Würm-Kaltzeit or ''Würm-Glazial'', colloquially often also ''Würmeiszeit'' or ''Würmzeit''; cf. ice age), usually referred to in the literature as the Würm (often spelled "Wurm"), was the last glacial period in the Alpine region. It is the youngest of the major glaciations of the region that extended beyond the Alps themselves. Like most of the other ice ages of the Pleistocene epoch, it is named after a river, in this case the Würm in Bavaria, a tributary of the Amper. The Würm ice age can be dated to about 115,000 to 11,700 years ago, but sources differ about the dates, depending on whether the long transition phases between the glacials and interglacials (warmer periods) are allocated to one or other of those periods. The average annual temperatures during the Würm ice age in the Alpine Foreland were below −3 °C (today +7 °C). That has been determined from changes in the vegetation (pollen analysis), as well a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hypoxia (environmental)
Hypoxia refers to low oxygen conditions. Normally, 20.9% of the gas in the atmosphere is oxygen. The partial pressure of oxygen in the atmosphere is 20.9% of the total barometric pressure. In water, oxygen levels are much lower, approximately 7 ppm or 0.0007% in good quality water, and fluctuate locally depending on the presence of photosynthetic organisms and relative distance to the surface (if there is more oxygen in the air, it will diffuse across the partial pressure gradient). Atmospheric hypoxia Atmospheric hypoxia occurs naturally at high altitudes. Total atmospheric pressure decreases as altitude increases, causing a lower partial pressure of oxygen, which is defined as hypobaric hypoxia. Oxygen remains at 20.9% of the total gas mixture, differing from hypoxic hypoxia, where the percentage of oxygen in the air (or blood) is decreased. This is common in the sealed burrows of some subterranean animals, such as blesmols. Atmospheric hypoxia is also the basis of altitude tra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Munich Metropolitan Region
The Munich Metropolitan Region is one of eleven metropolitan regions in Germany, consisting of the agglomeration areas of Munich, Augsburg, Ingolstadt, Landshut, Rosenheim and Landsberg am Lech. It is Germany's fifth most populous metropolitan region after the Rhine-Ruhr Metropolitan-Region, the Frankfurt Rhine-Main-Region, the Berlin-Brandenburg Metropolitan-Region and the Stuttgart Metropolitan-Region. Metropolitan Region *State: Bavaria *Districts: Lower Bavaria, Upper Bavaria, Swabia *Area: 27,700 km2 (40% of the state of Bavaria) *Population: 5,991,144 *GDP: 210 billion euro (53% of the Bavarian GDP) In comparison to the other ten German Metropolitan Regions, the Munich Metropolitan Region had: *the highest population growth (about 5% from 1997 to 2004) *the largest increase in employment (over 5% from 1997 to 2004) *the highest gross value added per employed person (2003) *the highest tax revenue per inhabitant (2003) Larger Urban Zone The Munich Larger Urban Z ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bavarian Alpine Foreland
The Alpine Foreland, less commonly called the Bavarian Foreland,Dickinson, Robert E (1964). ''Germany: A regional and economic geography'' (2nd ed.). London: Methuen, pp. 585-586. . Bavarian Plateau or Bavarian Alpine Foreland (german: Bayerisches Alpenvorland), refers to a triangular region of plateau and rolling foothills in Southern Germany, stretching from Lake Constance in the west to beyond Linz on the Danube in the east, with the Bavarian Alps forming its south boundary and the Danube its northern extent. Geography The Alpine Foreland has been shaped under the influence of the ice ages and has a rich variety of landforms. A molasse basin of extensive Tertiary and Quaternary sediments —silt and clay, sand and sedimentary rocks from Alpine erosion— overlay the Alpine nappes. Features such as the morainic hills, gravel sandar and lakes have left a record of various glaciation stages in this region. The Alpine Foreland is crossed by the rivers Iller, Wertach, Lech, I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carl Schuch
Carl Eduard Schuch (30 September 1846 – 13 September 1903) was an Austrian painter, born in Vienna, who spent most of his lifetime outside Austria, in Germany, Italy and France. He painted primarily still lifes and landscapes. From 1865 to 1867, he studied landscape painting under the academician Ludwig Halauska. Among his early works are studies of heads which he said he wished to paint "like still-lifes, tone by tone, without emotion". During the period 1882–94 he was based in Paris, where he was greatly impressed by the work of Claude Monet—whom he described as "the Rembrandt of ''plein-air'' painting"—although he was attracted most of all to Rembrandt and the artists of the Barbizon school.Forster-Hahn and Riopelle 2001, p. 164 In 1884 and 1885 he spent the summer months in the Netherlands, studying the Dutch old masters as well as the contemporary painters of the Hague School, and filling notebooks with detailed descriptions of the colors he observed in paintings t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pierre-Auguste Renoir
Pierre-Auguste Renoir (; 25 February 1841 – 3 December 1919) was a French artist who was a leading painter in the development of the Impressionist style. As a celebrator of beauty and especially feminine sensuality, it has been said that "Renoir is the final representative of a tradition which runs directly from Rubens to Watteau." He was the father of actor Pierre Renoir (1885–1952), filmmaker Jean Renoir (1894–1979) and ceramic artist Claude Renoir (1901–1969). He was the grandfather of the filmmaker Claude Renoir (1913–1993), son of Pierre. Life Youth Pierre-Auguste Renoir was born in Limoges, Haute-Vienne, France, in 1841. His father, Léonard Renoir, was a tailor of modest means, so, in 1844, Renoir's family moved to Paris in search of more favorable prospects. The location of their home, in rue d’Argenteuil in central Paris, placed Renoir in proximity to the Louvre. Although the young Renoir had a natural proclivity for drawing, he exhibited a greater t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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