Dubrower Berge
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Dubrower Berge
The Dubrower Berge are an ice age range of hills (end moraines) in the German state of Brandenburg. They lie about six kilometres southeast of Fürstenwalde/Spree in the county of Oder-Spree in the triangle between the villages of Langewahl, Alt Golm in the municipality of Rietz-Neuendorf and Neu Golm in the municipality of Bad Saarow. The name is derived from the Slavic language, Slavic ''dub'' which means oak. The Dubrower Berge are easy to reach from Berlin or Frankfurt/Oder on the Bundesautobahn 12, A12 autobahn, just 2 kilometres to the north. A transmission tower has been erected at their highest point, 150 metres above Normalnull, sea level (NN). The extensive stands of woods and variety of landscapes in the Dubrower Berge and surrounding area are used by hikers and cyclists. Near the village of Langewahl in the Dubrower Berge is the Osterquelle spring. See also * Rauen Hills References

Hills of Brandenburg {{Brandenburg-geo-stub ...
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Langewahl
Langewahl is a Municipalities of Germany, municipality in the Oder-Spree district, in Brandenburg, Germany. Nearby are the Dubrower Berge a range of wooded hills popular with hikers and cyclists. Demography File:Bevölkerungsentwicklung Langewahl.pdf, Development of population since 1875 within the current Boundaries (Blue Line: Population; Dotted Line: Comparison to Population development in Brandenburg state; Grey Background: Time of Nazi Germany; Red Background: Time of communist East Germany) References

Localities in Oder-Spree {{Brandenburg-geo-stub ...
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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 ...
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Normalnull
("standard zero") or (short N. N. or NN ) is an outdated official vertical datum used in Germany. Elevations using this reference system were to be marked (“meters above standard zero”). has been replaced by (NHN). History In 1878 reference heights were taken from the Amsterdam Ordnance Datum and transferred to the New Berlin Observatory in order to define the . has been defined as a level going through an imaginary point 37.000 m below . When the New Berlin Observatory was demolished in 1912 the reference point was moved east to the village of Hoppegarten (now part of the town of Müncheberg, Brandenburg, 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 ...).S. German: ''Was ist "Normal-Null"?''. In: ''Physikalische Blätter'' 1958, vol 14, issue 2, p. ...
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Bundesautobahn 12
, also known as Autobahn der Freiheit (English: ''Motorway of Freedom'') is an autobahn in northeastern Germany, connecting Berlin to the Polish Polish may refer to: * Anything from or related to Poland, a country in Europe * Polish language * Poles Poles,, ; singular masculine: ''Polak'', singular feminine: ''Polka'' or Polish people, are a West Slavic nation and ethnic group, w ... border. Exit list , - , colspan="3", ---- , '' References External links 12 A012 Constituent roads of European route E30 {{Germany-road-stub ...
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Slavic Language
The Slavic languages, also known as the Slavonic languages, are Indo-European languages spoken primarily by the Slavs, Slavic peoples and their descendants. They are thought to descend from a proto-language called Proto-Slavic language, Proto-Slavic, spoken during the Early Middle Ages, which in turn is thought to have descended from the earlier Proto-Balto-Slavic language, linking the Slavic languages to the Baltic languages in a Balto-Slavic languages, Balto-Slavic group within the Indo-European family. The Slavic languages are conventionally (that is, also on the basis of extralinguistic features) divided into three subgroups: East Slavic languages, East, South Slavic languages, South, and West Slavic languages, West, which together constitute more than 20 languages. Of these, 10 have at least one million speakers and official status as the national languages of the countries in which they are predominantly spoken: Russian language, Russian, Belarusian language, Belarusian ...
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Bad Saarow
Bad Saarow ( dsb, Zarow; 1950–2002: Bad Saarow-Pieskow) is a municipality in the Oder-Spree district, in Brandenburg, Germany. The place is known for its hot springs and for its mineral-rich mud. Their healing properties have attracted visitors for many years, and in 1923 led to the town's name acquiring the prefix ''Bad'' ("bath", "spa"). Nearby are the Dubrower Berge, a range of wooded hills popular with hikers and cyclists. Demography Sons and daughters of the town * Jörg Schönbohm (1937−2019, born in Neu Golm), former Lieutenant general of the Bundeswehr, 1999−2009 Minister of the Interior of the State of Brandenburg * Cornelia Ernst (born 1956), politician ( The Left) * Marienetta Jirkowsky (1962−1980), death at the Berlin Wall * Axel Schulz (born 1968), boxer * Vivien Kussatz (born 1972), sailor * Isabel Cademartori (born 1988), politician (SPD) * Franziska Mietzner Franziska Mietzner (born 20 December 1988) is a German handballer who plays for B ...
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Rietz-Neuendorf
Rietz-Neuendorf is a municipality in the Oder-Spree district, in Brandenburg, Germany Nearby are the Dubrower Berge a range of wooded hills popular with hikers and cyclists. Climate The city experiences a degraded oceanic climate, common in the border of Germany-Poland (Köppen: ''Cfb''). But due to its location to the east and interior (much more than most German cities), the climate is semicontinental, approaching ''Dfb'', characterized for this using old normals and 0 °C isotherm. The climate is similar with the south coast of Massachusetts (not island) where the strong continental influence is moderated by the sea, but still possessing extremes (hot summers but not above the pleasant threshold and cold winters with several days below zero but without the Arctic outbreaks). The west winds are weakened in their position in Central Europe, but more humid and hotter subtropics can still advance, making the city have four defined seasons of the year. The ecology of t ...
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Oder-Spree
Oder-Spree is a ''Kreis'' (district) in the eastern part of Brandenburg, Germany. Neighboring are (from north clockwise) the district Märkisch-Oderland, the district-free city Frankfurt (Oder), Poland, the districts Spree-Neiße and Dahme-Spreewald, and the ''Bundesland'' Berlin. Geography The district is named after the two major rivers in the district - the Spree river forms a large bend within the district; the Oder river constitutes the eastern border. History The district was created in 1993 by merging the districts Eisenhüttenstadt, Beeskow and Fürstenwalde, and the district-free city Eisenhüttenstadt. Demography File:Bevölkerungsentwicklung Landkreis Oder-Spree.pdf, Development of Population since 1875 within the Current Boundaries (Blue Line: Population; Dotted Line: Comparison to Population Development of Brandenburg state) File:Bevölkerungsprognosen Landkreis Oder-Spree.pdf, Recent Population Development and Projections (Population Development before Census 201 ...
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End 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 ...
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Weichselian Glaciation
The Weichselian glaciation was the last glacial period and its associated glaciation in northern parts of Europe. In the Alpine region it corresponds to the Würm glaciation. It was characterized by a large ice sheet (the Fenno-Scandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age (german: Weichsel-Eiszeit), Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (''Weichsel-Kaltzeit''), Weichselian glacial (''Weichsel-Glazial''), ''Weichselian Stage'' or, rarely, the Weichselian complex (''Weichsel-Komplex''). In Northern Europe it was the youngest of the glacials of the Pleistocene ice age. The preceding warm period in this region was the Eemian interglacial. The last cold period began about 115,000 years ago and ended 11,700 years ago. Its end corresponds with the end o ...
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