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Flint Fields
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] |
Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and start fires. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill'' Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along streams and be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nature Reserve (Germany)
A ''Naturschutzgebiet'' (abbreviated NSG) is a category of protected area (nature reserve) within Germany's Federal Nature Conservation Act (the ''Bundesnaturschutzgesetz'' or ''BNatSchG''). Although often translated as 'Nature Reserve' in English, the Federal Agency for Nature Conservation (BfN) refers to them as 'Nature Conservation Areas'. It meets the criteria of an IUCN Category IV Habitat and Species Management Area.https://www.bfn.de/fileadmin/MDB/documents/themen/gebietsschutz/IUCN_Kat_Schutzgeb_Richtl_web.pdf Document of the Federal Agency for Nature Conservation of Germany Points of law The use of the term ''Naturschutzgebiet'' or terms that could be confused with it for anything other than the legally protected areas is forbidden under this law. Signage Because legal restrictions are placed on activity within German nature reserves they have to be signed on the ground. Only by this means can e.g. walkers know that they are entering a nature reserve and may not e. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jasmund
Jasmund is a peninsula of the island of Rügen in Mecklenburg-Vorpommern, Germany. It is connected to the Wittow peninsula and to the Muttland main section of Rügen by the narrow land bridges Schaabe and Schmale Heide, respectively. Sassnitz, Sagard and the Mukran 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 ... international ferry terminal are on Jasmund. Jasmund is also famous for the Rügen Chalk cliffs within the Jasmund National Park, a nature reserve in the northeast of Rügen island. References Peninsulas of Mecklenburg-Western Pomerania Geography of Rügen {{VorpommernRügen-geo-stub ... [...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. 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, li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stone Fields In The Schmale Heath And Extension
The Stone Fields in the Schmale Heath and Extension (german: Steinfelder in der Schmalen Heide und Erweiterung) is a nature reserve (Naturschutzgebiet), 199 hectares in area, on the German island of Rügen in Mecklenburg-Western Pomerania. It includes large flint fields (german: Feuersteinfelder), a representative section of the Schmale Heath and a separate extension with near-natural coastal dunes. The reserve was created on 27 April 1935. Two extensions of the nature reserve area came into force in the years 1959 and 1990. The areas are located seven kilometres north of Binz between the Kleiner Jasmunder Bodden and the Baltic Sea. The reserve is assessed as in good condition. The high numbers of visiting tourists in the flint fields causes disturbances, though, to the fauna. The nature reserve is accessible via a footpath from Neu Mukran. In 2009 the nature reserve areas were taken over by the German Federal Environment Foundation (''Deutsche Bundesstiftung Umw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schmale Heide
The Schmale Heide (literally "Narrow Heath") is a 9.5-kilometre-long and roughly 2-kilometre-wide bar between the Baltic seaside resort of Binz and the village of Neu Mukran near Sassnitz on the German island of Rügen. It lies in the municipality of Binz and is bounded to the northwest by the lagoon of the Kleiner Jasmunder Bodden and to the east by the bay of Prorer Wiek. Formation The shape of the heavily segmented coastline of Rügen was the result of interplay between variations in the mean sea level and rebound processes following the last ice age, the Weichselian glaciation. It is believed that the region of the present-day West Pomeranian Baltic Sea coast after the last ice age glacial advance (the North Rügen-East Usedom Step) has remained ice-free and largely part of the mainland for about 13,000 years. The level of the world's oceans was once lower than today due to the ice age. About 9,000 years ago, a meltwater lake, the Ancylus Lake, was formed, whose surfac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Binz
Binz is the largest seaside resort on the German island of Rügen. It is situated between the bay of Prorer Wiek and the ''Schmachter See'' (a lake) in the southeast of the island. To the north of Binz stretches the Schmale Heide (the "narrow heath"), a tongue of land which joins the Muttland region of Rügen to the Jasmund peninsula. The land to the south and east of Binz is hilly, reaching a height of over 100 metres above sea level. Binz is known for its well-kept historical resort architecture and natural scenery, close to the Jasmund National Park and its chalk cliffs. Geography Location Binz lies on the eastern coast of the island of Rügen between the bay of Prorer Wiek and the lake of Schmachter See. North of Binz is the Schmale Heide, a neck of land that links the Muttland – Rügen's central region – with the peninsula of Jasmund. East and south of the municipality, the land is rolling, in the southeast, in the Granitz, the land climbs to just over . The r ... [...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 sm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rügen
Rügen (; la, Rugia, ) is Germany's largest island. It is located off the Pomeranian coast in the Baltic Sea and belongs to the state of Mecklenburg-Western Pomerania. The "gateway" to Rügen island is the Hanseatic city of Stralsund, where it is linked to the mainland by road and railway via the Rügen Bridge and Causeway, two routes crossing the two-kilometre-wide Strelasund, a sound of the Baltic Sea. Rügen has a maximum length of (from north to south), a maximum width of in the south and an area of . The coast is characterized by numerous sandy beaches, lagoons () and open bays (), as well as projecting peninsulas and headlands. In June 2011, UNESCO awarded the status of a World Heritage Site to the Jasmund National Park, famous for its vast stands of beeches and chalk cliffs like King's Chair, the main landmark of Rügen island. The island of Rügen is part of the district of Vorpommern-Rügen, with its county seat in Stralsund. The towns on Rügen are: Berg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Ear ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
