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Fährinsel
Fährinsel is a small Baltic Sea island off the eastern shore of the island of Hiddensee and which belongs to the Insel Hiddensee municipality. It is separated from Hiddensee by the narrow ''Bäk'', only 120 metres wide in places. It forms the western part of the border between the Schaproder Bodden and the Vitter Bodden. The island is 1.23 km long and up to 580 metres wide. It has an area of ca. 37 ha. Ferry services between Rügen and Hiddensee used to run via Fährinsel. It was closed in 1952 when the port at Schaprode was upgraded to handle mailboat services. Fährinsel is a nature reserve and out-of-bounds to visitors. It is a roosting place for thousands of birds and the grazing area for a herd of Gotland sheep. Geography Fährinsel consists of a fan of several berms, up to 2 metres high, and spits, as well as silted-up areas of the lagoon, the Schaproder Bodden. About 12,500 years ago, during the last cold phase of the ice age, glacial ice masses piled u ... [...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] |
Insel 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] |
Schaproder Bodden
The Schaproder Bodden is a ''bodden'' on the Baltic Sea coast between the island of Hiddensee in the west and the islands of Rügen and Ummanz in the east. To the north the Schaproder Bodden is linked to the Vitter Bodden by the so-called ''Trog'' between the Fährinsel and the ''Stolper Haken'' of Rügen island. To the south the ''bodden'' transitions into the Kubitzer Bodden. A boundary would be the line between the southern tips of the Hiddensee (Geller Haken) and Ummanz or the link from the Geller Haken - Insel Heuwiese. The Schaproder Bodden is 4.5 metres deep at three places, otherwise it is very shallow (mostly under 1.5 metres deep). Another source claims water depts. of 6 m.''Bootsangeln auf den Rügener Boddengewässern'' retrieved 15 August 2018. The ''bodden'' was named after < ... [...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] |
Flat Coast
At a flat coast or flat shoreline, the land descends gradually into the sea. Flat coasts can be formed either as a result of the sea advancing into gently-sloping terrain or through the abrasion of loose rock. They may be basically divided into two parallel strips: the shoreface and the beach. Flat coasts consist of loose material such as sand and gravel. Wind transports finer grains of sand inland over the dunes. The sea washes pebbles and sand away from the coast and dumps it at other locations. Flat coast littoral series The typical sequence of landforms created by the sea is described as a "littoral series". Sandbars, runnels and creeks The littoral series of a flat coast starts in the permanently flooded shallow water region, or shoreface, with a sand or gravel reef (also called a bar). The longshore bar is an elongated ridge of sand found parallel to the shore in the surf zone on many flat coasts. It consists mainly of sand or gravel, depending on the material avail ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Erosion
Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves, currents, tides, wind-driven water, waterborne ice, or other impacts of storms. The landward retreat of the shoreline can be measured and described over a temporal scale of tides, seasons, and other short-term cyclic processes. Coastal erosion may be caused by hydraulic action, abrasion, impact and corrosion by wind and water, and other forces, natural or unnatural. On non-rocky coasts, coastal erosion results in rock formations in areas where the coastline contains rock layers or fracture zones with varying resistance to erosion. Softer areas become eroded much faster than harder ones, which typically result in landforms such as tunnels, bridges, columns, and pillars. Over time the coast generally evens out. The softer areas fill up with sediment eroded from hard areas, and rock formations are eroded away. Also erosion commonly ... [...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 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] |
Juniper
Junipers are coniferous trees and shrubs in the genus ''Juniperus'' () of the cypress family Cupressaceae. Depending on the taxonomy, between 50 and 67 species of junipers are widely distributed throughout the Northern Hemisphere, from the Arctic, south to tropical Africa, throughout parts of West Asia, western, Central Asia, central and South Asia, southern Asia, east to eastern Tibet in the Old World, and in the mountains of Central America. The highest-known juniper forest occurs at an altitude of in southeastern Tibet and the northern Himalayas, creating one of the highest tree lines on earth. Description Junipers vary in size and shape from tall trees, tall, to columnar or low-spreading shrubs with long, trailing branches. They are evergreen with needle-like and/or scale-like leaves. They can be either monoecious or dioecious. The female Conifer cone, seed cones are very distinctive, with fleshy, fruit-like coalescing scales which fuse together to form Juniper berry, a&n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flint Field
Flint fields (german: Feuersteinfelder) 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 Aachen-Lousberg, Kleinkems, Schernfeld, Osterberg bei Pfünz, , Abensberg- [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calluna
''Calluna vulgaris'', common heather, ling, or simply heather, is the sole species in the genus ''Calluna'' in the flowering plant family Ericaceae. It is a low-growing evergreen shrub growing to tall, or rarely to and taller, and is found widely in Europe and Asia Minor on acidic soils in open sunny situations and in moderate shade. It is the dominant plant in most heathland and moorland in Europe, and in some bog vegetation and acidic pine and oak woodland. It is tolerant of grazing and regenerates following occasional burning, and is often managed in nature reserves and grouse moors by sheep or cattle grazing, and also by light burning. ''Calluna'' was separated from the closely related genus ''Erica'' by Richard Anthony Salisbury, who devised the generic name ''Calluna'' probably from the Ancient Greek (), "beautify, sweep clean", in reference to its traditional use in besoms. The specific epithet ''vulgaris'' is Latin for 'common'. ''Calluna'' is differentiated from ''Er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salt Meadow
A salt marsh or saltmarsh, also known as a coastal salt marsh or a tidal marsh, is a coastal ecosystem in the upper coastal intertidal zone between land and open saltwater or brackish water that is regularly flooded by the tides. It is dominated by dense stands of salt-tolerant plants such as herbs, grasses, or low shrubs. These plants are terrestrial in origin and are essential to the stability of the salt marsh in trapping and binding sediments. Salt marshes play a large role in the aquatic food web and the delivery of nutrients to coastal waters. They also support terrestrial animals and provide coastal protection. Salt marshes have historically been endangered by poorly implemented coastal management practices, with land reclaimed for human uses or polluted by upstream agriculture or other industrial coastal uses. Additionally, sea level rise caused by climate change is endangering other marshes, through erosion and submersion of otherwise tidal marshes. However, recent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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