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Gellen
The Gellen or Gellen Peninsula (german: Halbinsel Gellen) is a spit at the southern end of the island of Hiddensee off the north German Baltic coast. Its southern part is protected as an important bird reserve and is part of protection zone I of the Western Pomerania Lagoon Area National Park. It is therefore not accessible to the public. It consists of post-ice age sand depositions and is growing annually by a few metres to the south. The dredging of the shipping channel between the island of Bock and the Gellen prevents a graded shoreline from being formed, which would otherwise be typical of the eastern Baltic Sea area with its numerous spits. Topography The peninsula is a maximum of 500 metres wide and ca. 5 kilometres long, but only a few metres high. Its individual berms may be clearly seen. Topographically it may be divided into two areas: * Altgellen ( Neuendorf to Klimphores Bay) * Neugellen (Klimphores Bay to the southern tip), formed from about 12th century. The south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hiddensee
Hiddensee () is a car-free island in the Baltic Sea, located west of Germany's largest island, Rügen, on the German coast. The island has about 1,000 inhabitants. It was a holiday destination for East German tourists during German Democratic Republic (GDR) times, and continues to attract tourists today. It is the location of the University of Greifswald's ornithological station. Gerhart Hauptmann and Walter Felsenstein are buried there. Name The name ''Hedinsey'' surfaces as early as the ''Prose Edda'' and the ''Gesta Danorum'' written by Saxo Grammaticus and means "Island of Hedin". The legendary Norwegian king, Hedin, was supposed to have fought here for a woman or even just for gold. Under Danish rule the name ''Hedins-Oe'' ("Hedin's Island") was common. Even in 1880 the island was shown in German maps as ''Hiddensjö'' and, in 1929, in German holiday guides as ''Hiddensöe''. Its full Germanization to ''Hiddensee'' is thus relatively recent. Geography Hiddensee is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hiddensee Historische Karte
Hiddensee () is a car-free island in the Baltic Sea, located west of Germany's largest island, Rügen, on the German coast. The island has about 1,000 inhabitants. It was a holiday destination for East German tourists during German Democratic Republic (GDR) times, and continues to attract tourists today. It is the location of the University of Greifswald's ornithological station. Gerhart Hauptmann and Walter Felsenstein are buried there. Name The name ''Hedinsey'' surfaces as early as the ''Prose Edda'' and the ''Gesta Danorum'' written by Saxo Grammaticus and means "Island of Hedin". The legendary Norwegian king, Hedin, was supposed to have fought here for a woman or even just for gold. Under Danish rule the name ''Hedins-Oe'' ("Hedin's Island") was common. Even in 1880 the island was shown in German maps as ''Hiddensjö'' and, in 1929, in German holiday guides as ''Hiddensöe''. Its full Germanization to ''Hiddensee'' is thus relatively recent. Geography Hiddensee is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gellen
The Gellen or Gellen Peninsula (german: Halbinsel Gellen) is a spit at the southern end of the island of Hiddensee off the north German Baltic coast. Its southern part is protected as an important bird reserve and is part of protection zone I of the Western Pomerania Lagoon Area National Park. It is therefore not accessible to the public. It consists of post-ice age sand depositions and is growing annually by a few metres to the south. The dredging of the shipping channel between the island of Bock and the Gellen prevents a graded shoreline from being formed, which would otherwise be typical of the eastern Baltic Sea area with its numerous spits. Topography The peninsula is a maximum of 500 metres wide and ca. 5 kilometres long, but only a few metres high. Its individual berms may be clearly seen. Topographically it may be divided into two areas: * Altgellen ( Neuendorf to Klimphores Bay) * Neugellen (Klimphores Bay to the southern tip), formed from about 12th century. The south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gellenstrom
The Gellenstrom is a shipping channel in the Baltic Sea and forms the northwestern access to the ports of Stralsund and Strelasund. It is located in the Baltic Sea west of the peninsula of Gellen which gives it its name and which forms part of the island of Hiddensee. In addition, it is the main route from the Darss-Zingst Bodden Chain to the Baltic. The Gellenstrom has a guaranteed depth of 3.70 metres and is controlled by the Gellen light which marks its northern approach. The maximum speed limit is 10 kn. To the south is the port of Barhöft, which is also accessible from the Gellenstrom via the Barhöft Creek (''Barhöft -Rinne''). To the west is the island of Bock Bock is a strong beer in Germany, usually a dark lager. Several substyles exist, including: *Doppelbock (''Double Bock''), a stronger and maltier version *Eisbock (''Ice Bock''), a much stronger version made by partially freezing the beer an ..., which was formed from sand dredged from the channe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dornbusch (Hiddensee)
The Dornbusch is a region of low rolling hills in the northern part of the German Baltic Sea island of Hiddensee. It consists mainly of ice age depositions, that were left behind after the glacier thawed. It is one of three island cores of the Hiddensee responsible for the emergence of the lowland. The Dornbusch measures about 2.45 kilometres from north to south and about 2.85 kilometres from east to west. Its highest point, at 72 metres above sea level, is the ''Schluckswiekberg'', on which the Dornbusch Lighthouse, the symbol of Hiddensee, stands. With much of its cliffed coast still active it represents an important landscape in the West Pomeranian Lagoon Area National Park and is part of protection zone II. Numerous footpaths run through its varied countryside. History The formation of the uplands goes back to the last glaciation phase in northern Germany, the Weichselian. The Dornbusch was created about 12,500 years ago by a small finger of the ice front that left its ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bock (island)
The island of Bock lies in the Baltic Sea southwest of the island of Hiddensee and east of the peninsula of Zingst. It belongs to the municipality of Groß Mohrdorf in the northeast German state of Mecklenburg-Vorpommern. The island of Bock was artificially created by the dumping of sand from the channel to Stralsund (the Gellenstrom) and lies within the core zone of the West Pomeranian Lagoon Area National Park. It is a nature reserve and is uninhabited. Its name is derived from the word ''aufgebockt'' ("propped up"). The name arose because many ships ran aground on the former sandbank and thus became "propped up" in a sense. In the west the island is only separated from the Kleine Werder island group by narrow, shallow watercourses. Just off the island to the north is one of the few ''windwatts'' on the German Baltic Sea coast. In favourable wind conditions and the resulting low water levels the mudflat Mudflats or mud flats, also known as tidal flats or, in Ireland, slob o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Storm Surge
A storm surge, storm flood, tidal surge, or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low-pressure weather systems, such as cyclones. It is measured as the rise in water level above the normal tidal level, and does not include waves. The main meteorological factor contributing to a storm surge is high-speed wind pushing water towards the coast over a long fetch. Other factors affecting storm surge severity include the shallowness and orientation of the water body in the storm path, the timing of tides, and the atmospheric pressure drop due to the storm. There is a suggestion that climate change may be increasing the hazard of storm surges. Some theorize that as extreme weather becomes more intense and sea level rises due to climate change, storm surge is expected to cause more risk to coastal populations. Communities and governments can adapt by building hard infrastructure, like surge barriers, soft infrastructure, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peninsulas Of Mecklenburg-Western Pomerania
A peninsula (; ) is a landform that extends from a mainland and is surrounded by water on most, but not all of its borders. A peninsula is also sometimes defined as a piece of land bordered by water on three of its sides. Peninsulas exist on all continents. The size of a peninsula can range from tiny to very large. The largest peninsula in the world is the Arabian Peninsula. Peninsulas form due to a variety of causes. Etymology Peninsula derives , which is translated as 'peninsula'. itself was derived , or together, 'almost an island'. The word entered English in the 16th century. Definitions A peninsula is usually defined as a piece of land surrounded on most, but not all sides, but is sometimes instead defined as a piece of land bordered by water on three of its sides. A peninsula may be bordered by more than one body of water, and the body of water does not have to be an ocean or a sea. A piece of land on a very tight river bend or one between two rivers is sometimes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Abrasion Coast
A cliffed coast, also called an abrasion coast, is a form of coast where the action of marine waves has formed steep cliffs that may or may not be precipitous. It contrasts with a flat or alluvial coast. Formation In coastal areas in which the land surface dips at a relatively steep angle below the water table, the continuous action of marine waves on the coastline, known as abrasion, may create a steep declivity known as a cliff, the slope angle of which depends on a variety of factors including the jointing, bedding and hardness of the materials making up the cliff as well as the erosional processes themselves.Herbert Louis and Klaus Fischer: ''Allgemeine Geomorphologie'', de Gruyter, 4th ed., Berlin 1979, pp. 532-537 The slope is constantly being eroded. The waves attacking the cliff-foot form a wave-cut notch by constant abrasion action producing an overhang. This overhang grows in size as the cliff is undercut, until it collapses under its own weight. The loose ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ammophila (Poaceae)
''Ammophila'' (synonymous with ''Psamma'' P. Beauv.) is a genus of flowering plants consisting of two or three very similar species of Poaceae, grasses. The common names for these grasses include marram grass, bent grass, and beachgrass. These grasses are found almost exclusively on the first line of coastal sand dunes. Their extensive systems of creeping underground stems or rhizomes allow them to thrive under conditions of shifting sands and high winds, and to help stabilize and prevent coastal erosion. ''Ammophila'' species are native to the coasts of the Atlantic Ocean, North Atlantic Ocean where they are usually the dominant species on sand dunes. Their native range includes few inland regions, with the Great Lakes of North America being the main exception. The genus name ''Ammophila'' originates from the Greek words ἄμμος (''ámmos''), meaning "sand", and φίλος (''philos''), meaning "friend". The ''Ammophila'' grasses are widely known as examples of xerophytes, p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dune
A dune is a landform composed of wind- or water-driven sand. It typically takes the form of a mound, ridge, or hill. An area with dunes is called a dune system or a dune complex. A large dune complex is called a dune field, while broad, flat regions covered with wind-swept sand or dunes with little or no vegetation are called ''ergs'' or ''sand seas''. Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have a shorter ''slip face'' in the lee side. The valley or trough between dunes is called a ''dune slack''. Dunes are most common in desert environments, where the lack of moisture hinders the growth of vegetation that would otherwise interfere with the development of dunes. However, sand deposits are not restricted to deserts, and dunes are also found along sea shores, along streams in semiarid climates, in areas of glacial outwash, and in other areas where poorly cemented sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beach Nourishment
Beach nourishment (also referred to as beach renourishment, beach replenishment, or sand replenishment) describes a process by which sediment, usually sand, lost through longshore drift or erosion is replaced from other sources. A wider beach can reduce storm damage to coastal structures by dissipating energy across the surf zone, protecting upland structures and infrastructure from storm surges, tsunamis and unusually high tides. Beach nourishment is typically part of a larger integrated coastal zone management aimed at coastal defense. Nourishment is typically a repetitive process since it does not remove the physical forces that cause erosion but simply mitigates their effects. The first nourishment project in the United States was at Coney Island, New York in 1922 and 1923. It is now a common shore protection measure used by public and private entities. History The first nourishment project in the U.S. was constructed at Coney Island, New York in 1922–1923. Before ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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