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Sassnitz Ferry Port
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 small yet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Promenade
An esplanade or promenade is a long, open, level area, usually next to a river or large body of water, where people may walk. The historical definition of ''esplanade'' was a large, open, level area outside fortress or city walls to provide clear fields of fire for the fortress's guns. In modern usage, the space allows the area to be paved as a pedestrian walk; esplanades are often on sea fronts and allow walking whatever the state of the tide, without having to walk on the beach. History In the 19th century, the razing of city fortifications and the relocation of port facilities made it possible in many cities to create promenade paths on the former fortresses and ramparts. The parts of the former fortifications, such as hills, viewpoints, ditches, waterways and lakes have now been included in these promenades, making them popular excursion destinations as well as the location of cultural institutions. The rapid development of artificial street lighting in the 19th century als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stubnitz
The Stubnitz is a hilly, forested landscape region on the east coast of the Jasmund peninsula on the German Baltic Sea island of Rügen – Germany's largest island. It covers an area of about 2,400 ha and runs from the town of Sassnitz to the municipality of Lohme, Today, it is almost entirely part of the 3,000 ha Jasmund National Park. The name ''Stubnitz'' is probably of Slavic origin; but the literature gives a wide variety of meanings – from ''Stufenland'' ("stepped landscape") to ''Waldung mit Bienenkellern'' ("woods with beehives"). Literature * Johann Jacob Grümbke: ''Streifzüge durch das Rügenland''. (1805), Neuauflage durch F. A. Brockhaus Verlag Leipzig (Hrsg.: Albert Burkhardt), Leipzig, 1988, . * Nationalparkamt Rügen (ed.): ''Die Stubnitz: Der Buchenwald an der Kreideküste'', Lancken-Granitz, 2001 * Verein der Freunde und Förderer des Nationalparks Jasmund e. V. (Hrsg.): ''Die Insel Rügen – Nationalpark Jasmund''. 2nd edition, Sassnitz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rügen Postkarte 048
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] |
Endorheic Depression
An endorheic basin (; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but drainage converges instead into lakes or swamps, permanent or seasonal, that equilibrate through evaporation. They are also called closed or terminal basins, internal drainage systems, or simply basins. Endorheic regions contrast with exorheic regions. Endorheic water bodies include some of the largest lakes in the world, such as the Caspian Sea, the world's largest inland body of water. Basins with subsurface outflows which eventually lead to the ocean are generally not considered endorheic; they are cryptorheic. Endorheic basins constitute local base levels, defining a limit of erosion and deposition processes of nearby areas. Etymology The term was borrowed from French ''endor(rh)éisme'', coined from the combining form ''endo-'' (from grc, ἔνδον ''éndon'' 'wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steppe
In physical geography, a steppe () is an ecoregion characterized by grassland plains without trees apart from those near rivers and lakes. Steppe biomes may include: * the montane grasslands and shrublands biome * the temperate grasslands, savannas and shrublands biome A steppe may be semi-arid or covered with grass or with shrubs or with both, depending on the season and latitude. The term " steppe climate" denotes the climate encountered in regions too dry to support a forest but not dry enough to be a desert. Steppe soils are typically of the chernozem type. Steppes are usually characterized by a semi-arid or continental climate. Extremes can be recorded in the summer of up to and in winter, . Besides this major seasonal difference, fluctuations between day and night are also very great. In both the highlands of Mongolia and northern Nevada, can be reached during the day with sub-freezing readings at night. Mid-latitude steppes feature hot summers and cold wint ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancylus Lake
Ancylus Lake is a name given by geologists to a large freshwater lake that existed in northern Europe approximately from 9500 to 8000 years B.C being in effect one of various predecessors to the modern Baltic Sea. Origin, evolution and demise The Ancylus Lake replaced the Yoldia Sea after the latter had been severed from its saline intake across a seaway along the Central Swedish lowland, roughly between Gothenburg and Stockholm. The cutoff was the result of isostatic rise being faster than the concurrent post-glacial sea level rise. In the words of Svante Björck the Ancylus Lake "is perhaps the most enigmatic (and discussed) of the many Baltic stages". The lake's outlet and elevation relative to sea-level was for long time surrounded by controversy. It is now known that the lake was above sea level, included Lake Vänern, and drained westward through three outlets at Göta Älv, Uddevalla and Otteid. As result of the continued isostatic uplift of Sweden, the outlets in cent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baltic Sea
The Baltic Sea is an arm of the Atlantic Ocean that is enclosed by Denmark, Estonia, Finland, Germany, Latvia, Lithuania, Poland, Russia, Sweden and the North and Central European Plain. The sea stretches from 53°N to 66°N latitude and from 10°E to 30°E longitude. A marginal sea of the Atlantic, with limited water exchange between the two water bodies, the Baltic Sea drains through the Danish Straits into the Kattegat by way of the Øresund, Great Belt and Little Belt. It includes the Gulf of Bothnia, the Bay of Bothnia, the Gulf of Finland, the Gulf of Riga and the Bay of Gdańsk. The " Baltic Proper" is bordered on its northern edge, at latitude 60°N, by Åland and the Gulf of Bothnia, on its northeastern edge by the Gulf of Finland, on its eastern edge by the Gulf of Riga, and in the west by the Swedish part of the southern Scandinavian Peninsula. The Baltic Sea is connected by artificial waterways to the White Sea via the White Sea–Baltic Canal and to the German ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old And Young Moraine
Old and Young Drift are geographic names given to the morainic landscapes that were formed in Central Europe; the Old Drift during the older ice ages and the Young Drift during the latest glaciations – the Weichselian in North Germany and the Würm in the Alps. Their landforms are quite different. Areas of Old Drift have been heavily flattened and transformed as a result of geomorphic processes such as denudation and erosion, whilst areas of Young Drift have largely retained their original shape. Whilst the majority of Old Drift moraines were formed during the Saale glaciation about 130,000 to 140,000 years ago, the Young Drift moraines in Central Europe are only about 15,000 to 20,000 years old. The terms Old and Young Drift are used for all elements of the glacial series even though the meltwater deposits and landforms are not strictly moraines. Old Drift The Old Drift landscapes were tundras or cold deserts during the last ice age. Periglacial processes resulted in sig ... [...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] |
Stubbenkammer
The Jasmund National Park (German: ''Nationalpark Jasmund'') is a nature reserve on the Jasmund peninsula, in the northeast of Rügen island in Mecklenburg-Vorpommern, Germany. It is famous for containing the largest chalk cliffs in Germany, the '' Königsstuhl'' (German = "king's chair"). These cliffs are up to above the Baltic Sea. The beech forests behind the cliffs are also part of the national park. Consisting of only , this is the smallest national park in Germany. The park was founded in 1990 by the last government of East Germany (GDR) prior to the German reunification. On June 25, 2011, the beech forest in the park was added to the UNESCO World Heritage List as an extension of the Primeval Beech Forests of Europe site because of its undisturbed nature and its testimony to the ecological history of Europe since the last Ice Age. Chalk cliffs The cliffs of Jasmund National Park belong to the Rügen Chalk unit. The chalk cliffs face constant erosion. With every sto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Steinbach (Sassnitz)
Steinbach is a small stream on the island of Rügen, Mecklenburg-Vorpommern, Germany. Its source is in the Jasmund National Park, and it flows into the Baltic Sea in the town of Sassnitz. See also *List of rivers of Mecklenburg-Vorpommern A list of rivers of Mecklenburg-Vorpommern, Germany: A * Aubach * Augraben, tributary of the Nebel * Augraben, tributary of the Tollense B * Barthe *Beke * Bietnitz * Boize * Brebowbach * Bresenitz * Brüeler Bach D *Datze * Delvenau * Dollbek ... Rivers of Mecklenburg-Western Pomerania Rivers of Germany {{Mecklenburg-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Promenade")
