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Glacial Erratics On And Around Rügen
This is a list of erratics on and around Rügen – the largest island off the Baltic coast of Germany. An erratic is usually defined (in Germany) as an individual block of rock lying on the surface of the land which has a volume of at least one cubic metre and which was transported by a glacier to its present site during the ice age. Before the establishment of ice age theories, many stories and legends were woven around the giant "erratic blocks" of rock. On Rügen, there are a lot of interesting large erratics due to the particular location of the island during the ice ages and due to continuous coastal erosion. In the New Stone Age people built megalithic tombs out of erratics. On Rügen many of these have survived. Until the 19th century large erratics were used as quarries, in order to produce construction material for monuments (e. g. in 1854 the Prussia Columns near Neukamp and Groß Stresow or for the Ernst Moritz Arndt Tower on the Rugard, for coastal and harbour d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Natural Monument
A natural monument is a natural or natural/cultural feature of outstanding or unique value because of its inherent rarity, representative of aesthetic qualities or cultural significance. Under World Commission on Protected Areas guidelines, natural monuments are level III, described as: :"Areas are set aside to protect a specific natural monument, which can be a landform, sea mount, submarine cavern, geological feature such as a cave or even a living feature such as an ancient grove. They are generally quite small protected areas and often have high visitor value." This is a lower level of protection than level II (national parks) and level I (wilderness areas). The European Environment Agency's guidelines for selection of a natural monument are: * The area should contain one or more features of outstanding significance. Appropriate natural features include waterfalls, caves, craters, fossil beds, sand dunes and marine features, along with unique or representative fauna and flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Göhren (Rügen) , a village in Most District
;See also
* , a Kriegsmarine coastal tanker
{{geodis ...
Göhren may refer to the following places: ;Germany * Göhren (Tramm), a village in the municipality Tramm in the district Ludwigslust-Parchim, Mecklenburg-Vorpommern * Göhren, Rügen, a municipality in the district Vorpommern-Rügen, Mecklenburg-Vorpommern * Göhren, Thuringia, a municipality in the district Altenburger Land, Thuringia ;Czech Republic * KlÃny KlÃny (german: Göhren) is a municipality and village in Most District in the Ústà nad Labem Region of the Czech Republic. It has about 200 inhabitants. KlÃny lies approximately north-west of Most (city), Most, west of Ústà nad Labem, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buskam
The Buskam, also Buhskam or Buskamen is a large glacial erratic boulder, 325 metres off the coast of Göhren, Rügen, northern Germany.Ingrid Schmidt: ''Hünengrab und Opferstein'', Hinstorff, Rostock 2001, p.42, Erratics (german: Findlinge) have been scattered all over northern Germany by the glaciers of the Ice Age, but are usually much smaller. The Buskam has a volume of about 600 m3, a circumference of about 40 metres, and weights about 1,600 tons. A third of it (206 m3) lies above the water surface. Cavities in the rock indicate that the Buskam was used as a ritual place in prehistory, when such caved rocks were commonly used for ritual sacrifice. An iron crucifix was attached to it after the conversion of Pomerania. According to local legends, the Buskam is the site where witches dance during Walpurgis Night, mermaids are also supposed to dance often on the rock. See also *Glacial erratics on and around Rügen *Early history of Pomerania After the glac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geotope
A geotope is the geological component of the abiotic matrix present in an ecotope. Example geotopes might be an exposed outcrop of rocks, an erratic boulder, a grotto or ravine, a cave, an old stone wall marking a property boundary, and so forth. It is a loanword from German ''( Geotop)'' in the study of ecology and might be the model for many other similar words coined by analogy. As the prototype, it has enjoyed wider currency than many of the other words modelled on it, including physiotope Physiotope is the total abiotic matrix of habitat present within any certain ecotope. The physiotope is the landform, the rocks and the soils, the climate and the hydrology, and the geologic processes which marshalled all these resources together in ..., with which it is used synonymously. But the geotope is properly the rocks and not the whole lay of the land (which would be the physiotope). For usage in the context of geoheritage, like e.g. in Friedrich Wiedenbein's contributions (see ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bornholm
Bornholm () is a Danish island in the Baltic Sea, to the east of the rest of Denmark, south of Sweden, northeast of Germany and north of Poland. Strategically located, Bornholm has been fought over for centuries. It has usually been ruled by Denmark, but also by Sweden and by Lübeck. The ruin of Hammershus, at the northwestern tip of the island, is the largest medieval fortress in northern Europe, testament to the importance of its location. Bornholm and Ertholmene comprise the last remaining Danish territory in Skåneland east of Øresund, having been surrendered to Sweden in 1658, but regained by Denmark in 1660 after a local revolt. The island is known as ("sunshine island") because of its weather and ("rock island") because of its geology, which consists of granite, except along the southern coast. The heat from the summer is stored in the rock formations and the weather is quite warm until October. As a result of the climate, a local variety of the common fig, known ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Stream
A glacier stream is a channelized area that is formed by a glacier in which liquid water accumulates and flows. Glacial streams are also commonly referred to as "glacier stream" or/and "glacial meltwater stream". The movement of the water is influenced and directed by gravity and the melting of ice. The melting of ice forms different types of glacial streams such as supraglacial, englacial, subglacial and proglacial streams. Water enters supraglacial streams that sit at the top of the glacier via filtering through snow in the accumulation zone and forming slush pools at the FIRN zone. The water accumulates on top of the glacier in supraglacial lakes and into supraglacial stream channels. The meltwater then flows through various different streams either entering inside the glacier into englacial channels or under the glacier into subglacial channels. Finally, the water leaves the glacier through proglacial streams or lakes. Proglacial streams do not only act as the terminus point ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 depos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Cliff
Seacliff or Sea Cliff or Sea Cliffe may refer to: ;Places ''Australia'' *Seacliff, South Australia, suburb of Adelaide *Seacliff Park, South Australia, a suburb of Adelaide *Sea Cliff Bridge, in Illawarra, New South Wales ''New Zealand'' *Seacliff, New Zealand, settlement in Otago, New Zealand **Seacliff Lunatic Asylum, a former mental hospital near the settlement ''United Kingdom'' *Seacliff, a beach, estate and harbour near North Berwick, Scotland. *Sea Cliffe, Ballure Road, Ramsey, Isle of Man, one of Isle of Man's Registered Buildings ''United States'' *Seacliff, California, a census-designated place near Aptos, California *Seacliff State Beach, a California State Beach in Aptos, California *Sea Cliff, California, a community in Ventura County *Sea Cliff, San Francisco, California, a neighborhood in San Francisco County *Sea Cliff, New York ;Ship *DSV Sea Cliff, U.S. Navy research deep submergence vehicle {{disambig, geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Medial Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Provenà ... [...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 end o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Divide
An ice divide is the boundary on an ice sheet, ice cap or glacier separating opposing flow directions of ice, analogous to a water divide. Ice divides are important for geochronological investigations that use ice cores, since such coring is typically made at highest point of an ice sheet dome to avoid disturbances arising from horizontal ice movement. Ice divides are used for looking at how the atmosphere varied over time. Coring at dome peaks increases precision of reconstructions as it is the place where horizontal motion is at its least. The Raymond Effect operates at ice divides, creating anticlines in the radar-detected isochrones, allowing greater capture of older ice when coring. Analysis of ice cores relies on the downward motion of ice, trapping changes of atmospheric gases through time into its layers. Scientist locate ice divides and take ice cores from them, which are typically long cylindrical poles of ice, and analyse them to find chemical elements that the snow an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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