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Schwanenstein 2
The Schwanenstein is a glacial erratic on the island of Rügen in Germany. It lies about 100 metres east of the harbour at Lohme on the northern shore of the Jasmund peninsula about 20 metres off the beach in the Baltic Sea. It weighs 162 tonnes and has a volume of 60 m³. It is thus the fifth largest erratic of about 20 other large glacial boulders that are part of Rügen's legally protected geotopes. It is stylistically portrayed in Lohme's coat of arms. Origin and features The Schwanenstein is made of so-called granite, hammer granite and was very probably transported here from the island of Bornholm during the Weichselian glaciation, last ice age. Its reddish appearance is due to the presence of a high proportion of potassium feldspar. On its west side a marked crevice runs through the stone that, over the course of time, has been enlarged by the crystallisation pressure of frozen ice and may well result in the shearing off of a large slab of rock in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schwanenstein 1
The Schwanenstein is a glacial erratic on the island of Rügen in Germany. It lies about 100 metres east of the harbour at Lohme on the northern shore of the Jasmund peninsula about 20 metres off the beach in the Baltic Sea. It weighs 162 tonnes and has a volume of 60 m³. It is thus the fifth largest erratic of about 20 other large glacial boulders that are part of Rügen's legally protected geotopes. It is stylistically portrayed in Lohme's coat of arms. Origin and features The Schwanenstein is made of so-called hammer granite and was very probably transported here from the island of Bornholm during the last ice age. Its reddish appearance is due to the presence of a high proportion of potassium feldspar. On its west side a marked crevice runs through the stone that, over the course of time, has been enlarged by the crystallisation pressure of frozen ice and may well result in the shearing off of a large slab of rock in the near future. Legends and sto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Potassium Feldspar
Potassium feldspar refers to a number of minerals in the feldspar group, and containing potassium: *Orthoclase Orthoclase, or orthoclase feldspar ( endmember formula K Al Si3 O8), is an important tectosilicate mineral which forms igneous rock. The name is from the Ancient Greek for "straight fracture," because its two cleavage planes are at right angl ... ( endmember formula K Al Si3 O8), an important tectosilicate mineral that forms igneous rock * Microcline, chemically the same as orthoclase, but with a different crystalline structure * Sanidine, the high-temperature form of potassium feldspar * Adularia, a more ordered low-temperature variety of orthoclase or partially disordered microcline * Amazonite (sometimes called "Amazon stone"), a green variety of microcline {{SIA Feldspar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Rügen
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erratics On And Around Rügen (''Tapinoma erraticum''), a species of ant
{{disambiguation ...
Erratic may refer to: * Erratic, a project of music artist Jan Robbe * Glacial erratic, a piece of rock that differs from the size and type of rock native to the area in which it rests * Erratic ant The erratic ant (''Tapinoma erraticum'') is a species of dolichoderine ant first described in 1789 by Latreille. This species ranges throughout Central Europe from the mountains of south Italy to north Germany. It is present in coastal areas o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Series
The glacial series refers to a particular sequence of landforms in Central Europe that were formed during the Pleistocene glaciation beneath the ice sheets, along their margins and on their forelands during each glacial advance.''Die glaziale Serie und glaziale Sonderformen in Schleswig-Holstein'' . Forum Erdkunde, Uni Lünibürg. Accessed on 6 January 2008. Definition The term "glacial series" (german: Glaziale Serie) was used as early as 1882 by initially for the northern |
Glacial Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is dep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prora
The Colossus of Prora, commonly known as simply "Prora", is a building complex in the municipality of Binz on the island of Rügen, Germany. It was built by Nazi Germany between 1936 and 1939 as part of the Strength Through Joy (Kraft durch Freude or KdF) project. It consisted of eight identical buildings and was in length parallel to the beach, with the surviving structures stretching . Although the buildings were planned as a holiday resort, construction was not completed and they were not used for this purpose. After World War II, the complex found various military uses, first by the Soviet Army, then by the East German Volksarmee, and then by the German Bundeswehr. Today it houses a large youth hostel, a hotel and vacation apartments. The complex has a formal heritage listing as a particularly striking example of Nazi architecture. Location Prora lies on an extensive bay between the Sassnitz and Binz regions, known as the Prorer Wiek, on the narrow heath (the ''Prora' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volkspolizei
The ''Deutsche Volkspolizei'' (DVP, German for "German People's Police"), commonly known as the ''Volkspolizei'' or VoPo, was the national police force of the German Democratic Republic (East Germany) from 1945 to 1990. The Volkspolizei was a highly-centralized agency responsible for most civilian law enforcement in East Germany, maintaining 257,500 personnel at its peak. History The ''Volkspolizei'' was effectively founded in June 1945 when the Soviet Military Administration in Germany (SVAG) established central police forces in the regions of Nazi Germany it occupied following after World War II.Thomas Lindenberger, ‘The German People's Police (1945 - 1990)’, in Hans Ehlert and Rüdiger Wenzke (ed.) ‘In the service of the party - Handbook of Armed Organs of the GDR’ (Berlin, 1998) pp. 98-100 The SVAG approved the arming of community-level police forces on 31 October 1945, but nevertheless remained a non-militarised force, and by 1946 the ''Volkspolizei'' comprised ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sassnitz
Sassnitz (, before 1993 in german: Saßnitz) is a town on the Jasmund peninsula, Rügen Island, in the state of Mecklenburg-Vorpommern, Germany. The population as of 2012 was 9,498. Sassnitz is a well-known seaside resort and port town, and is a gateway to the nearby Jasmund National Park with its unique chalk cliffs. The decommissioned British submarine HMS ''Otus'' was purchased by a German entrepreneur and towed to Sassnitz to be a floating museum. The Sassnitz area is most popular for its famous chalk rocks (''Kreidefelsen''), which inspired artists like Caspar David Friedrich. Geography File:Sassnitz (2011-05-21).JPG, Sassnitz aerial view (2011), the famous chalk cliffs of the Jasmund National Park to the right. More aerial photos' File:Sassnitz Mukran (2011-05-21) 7.JPG, Sassnitz Mukran, the ferry port of Sassnitz File:Sassnitz Kreidefelsen 2011.jpg, Chalk rocks in the front, spa town of Sassnitz in the back File:Herthasee und Herthaburg auf Rügen.jpg, The sma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swan
Swans are birds of the family Anatidae within the genus ''Cygnus''. The swans' closest relatives include the geese and ducks. Swans are grouped with the closely related geese in the subfamily Anserinae where they form the tribe Cygnini. Sometimes, they are considered a distinct subfamily, Cygninae. There are six living and many extinct species of swan; in addition, there is a species known as the coscoroba swan which is no longer considered one of the true swans. Swans usually mate for life, although "divorce" sometimes occurs, particularly following nesting failure, and if a mate dies, the remaining swan will take up with another. The number of eggs in each clutch ranges from three to eight. Etymology and terminology The English word ''swan'', akin to the German , Dutch and Swedish , is derived from Indo-European root ' ('to sound, to sing'). Young swans are known as '' cygnets'' or as '' swanlings''; the former derives via Old French or (diminutive suffix et 'little') from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 en ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schwanenstein 3
The Schwanenstein is a glacial erratic on the island of Rügen in Germany. It lies about 100 metres east of the harbour at Lohme on the northern shore of the Jasmund peninsula about 20 metres off the beach in the Baltic Sea. It weighs 162 tonnes and has a volume of 60 m³. It is thus the fifth largest erratic of about 20 other large glacial boulders that are part of Rügen's legally protected geotopes. It is stylistically portrayed in Lohme's coat of arms. Origin and features The Schwanenstein is made of so-called hammer granite and was very probably transported here from the island of Bornholm during the last ice age. Its reddish appearance is due to the presence of a high proportion of potassium feldspar. On its west side a marked crevice runs through the stone that, over the course of time, has been enlarged by the crystallisation pressure of frozen ice and may well result in the shearing off of a large slab of rock in the near future. Legends and sto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
