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Schaabe Rügen
The Schaabe is a bar (landform), bar, almost twelve kilometres long, on the German Baltic Sea island of Rügen. It joins the peninsulas of Jasmund and Wittow. Washed up and shaped by the sea, it forms a sickle-shaped shoreline on the bay of Tromper Wiek and separates the lagoons of the Großer Jasmunder Bodden and ''Breeger Bodden'' from the Baltic Sea, Baltic. The fine, washed up sand forms a giant natural bathing bay, that is bordered by the villages of Glowe and Juliusruh (a village in the municipality of Breege). Unlike the second largest bar on the island of Rügen, the Schmale Heide between Jasmund and the Granitz, which is dominated by the construction of the former Nazi "Strength Through Joy" resort of Prora and decades of military use and its associated infrastructure, the Schaabe between Glowe and Juliusruh is undeveloped apart from a managed forest, the only through road and its accompanying cycle path. Formation The Schaabe began to form about 4,500 years ago, wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schaabe North
The Schaabe is a bar, almost twelve kilometres long, on the German Baltic Sea island of Rügen. It joins the peninsulas of Jasmund and Wittow. Washed up and shaped by the sea, it forms a sickle-shaped shoreline on the bay of Tromper Wiek and separates the lagoons of the Großer Jasmunder Bodden and ''Breeger Bodden'' from the Baltic. The fine, washed up sand forms a giant natural bathing bay, that is bordered by the villages of Glowe and Juliusruh (a village in the municipality of Breege). Unlike the second largest bar on the island of Rügen, the Schmale Heide between Jasmund and the Granitz, which is dominated by the construction of the former Nazi "Strength Through Joy" resort of Prora and decades of military use and its associated infrastructure, the Schaabe between Glowe and Juliusruh is undeveloped apart from a managed forest, the only through road and its accompanying cycle path. Formation The Schaabe began to form about 4,500 years ago, when Rügen was still an is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flint Field
Flint fields () are large natural deposits of flint. They are found in numerous Jurassic and Cretaceous beds across the whole of Europe.''Breege'' at www.ruegenurlaub.de. Retrieved 19 Jun 2019 Such deposits may be found in -Lousberg, Kleinkems, , Osterberg bei Pfünz, , |
Sediment
Sediment is a solid material that is transported to a new location where it is deposited. It occurs naturally and, through the processes of weathering and erosion, is broken down and subsequently sediment transport, transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension (chemistry), suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water (fluvial, fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and stream channel, river channel deposits are examples of fluvial transport and deposition (geology), deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slavonia
Slavonia (; ) is, with Dalmatia, Croatia proper, and Istria County, Istria, one of the four Regions of Croatia, historical regions of Croatia. Located in the Pannonian Plain and taking up the east of the country, it roughly corresponds with five Counties of Croatia, Croatian counties: Brod-Posavina County, Brod-Posavina, Osijek-Baranja County, Osijek-Baranja, Požega-Slavonia County, Požega-Slavonia, Virovitica-Podravina County, Virovitica-Podravina, and Vukovar-Syrmia County, Vukovar-Syrmia, although the territory of the counties includes Baranya (region), Baranya, and the definition of the western extent of Slavonia as a region varies. The counties cover or 22.2% of Croatia, inhabited by 806,192—18.8% of Croatia's population. The largest city in the region is Osijek, followed by Slavonski Brod and Vinkovci. Slavonia is located in the Pannonian Basin, largely bordered by the Danube, Drava, and Sava rivers. In the west, the region consists of the Sava and Drava valleys and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ralswiek
Ralswiek is a municipality in the Vorpommern-Rügen district, in Mecklenburg-Vorpommern, Germany Germany, officially the Federal Republic of Germany, is a country in Central Europe. It lies between the Baltic Sea and the North Sea to the north and the Alps to the south. Its sixteen States of Germany, constituent states have a total popu .... References External links Official website of Ralswiek Viking Age populated places Towns and villages on Rügen {{VorpommernRügen-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kleiner Jasmunder Bodden
The Kleiner Jasmunder Bodden belongs to the North Rügen Bodden and is a water body on the southern edge of the Baltic Sea in the German state of Mecklenburg-Vorpommern. Description It is a '' bodden'', a type of lagoon that occurs in northern Europe especially on the coast of Pomerania. It is around seven kilometres long and five kilometres across at its widest point, but in places it is considerably narrower. It has an area of 28.4 square kilometres.Kleiner Jasmunder Bodden at ruegen-mv.de. Retrieved 30 Sep 21. Geography The lagoon is bounded to the north by the Jasmund peninsula, to the east by the[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Storm Flood
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. As extreme weather becomes more intense and the sea level rises due to climate change, storm surges are expected to cause more risk to coastal populations. Communities and governments can adapt by building hard infrastructure, like surge barriers, soft infrastructure, like coastal dunes or mangroves, improving coastal construction practices and building social strategie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffed 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 coast, 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 (geology), 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 und ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Management
Coastal management is defence against flooding and erosion, and techniques that stop erosion to claim lands. Protection against rising sea levels in the 21st century is crucial, as sea level rise accelerates due to climate change. Changes in sea level damage beaches and coastal systems are expected to rise at an increasing rate, causing coastal sediments to be disturbed by tidal energy. Coastal zones occupy less than 15% of the Earth's land area, while they host more than 40% of the world population. Nearly 1.2 billion people live within of a coastline and of sea level, with an average density three times higher than the global average for population. With three-quarters of the world population expected to reside in the coastal zone by 2025, human activities originating from this small land area will impose heavy pressure on coasts. Coastal zones contain rich resources to produce goods and services and are home to most commercial and industrial activities. History Coastal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
