Breitling (channel)
The Breitling is a narrow strait in the Baltic Sea between the island of Poel and the mainland in the northeast of the district of Nordwestmecklenburg. It links the sheltered part of the Bay of Wismar, beginning south of Poeldamm, with the Salzhaff (into which estuaries of the Zaufe and Gollwitz empty). The Breitling is a very shallow body of water, mostly under one metre in depth. Large parts can even become exposed at low water, whereas at high water it can cover the low-lying causeway known as the Poeldamm. In the south the road link runs along a causeway (the Poeldamm) over a low peninsula to Poel over the Breitling. The waterbody is about five kilometres long and no more than one kilometre wide. Flora and fauna The landscape alternates between short stretches of steep shoreline on the mainland side, on the southern shores of the small islands of ''Baumwerder'' and Ahrendsberg and very shallow areas subject to flooding. This is indicated by salt grasslands with alluvial is ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Breitling Zwischen Poel Und Dem Festland
{{dab, geo ...
Breitling may refer to: * Breitling (Warnow), a bay at the mouth of the River Warnow in the Baltic * Breitling (Bay of Wismar), a bay between the mainland and the Baltic Sea island of Poel * Breitling SA, a Swiss watch manufacturer * Breitlingsee, a lake in Brandenburg, Germany * Breitling Jet Team, a civilian aerobatic display team in Europe * Breitling Orbiter ''Breitling Orbiter'' was the name of three different Rozière balloons made by the Bristol based balloon manufacturer Cameron Balloons to circumnavigate the globe, named after the Swiss watchmakers Breitling. The third was successful in March ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Strait
A strait is an oceanic landform connecting two seas or two other large areas of water. The surface water generally flows at the same elevation on both sides and through the strait in either direction. Most commonly, it is a narrow ocean channel that lies between two land masses. Some straits are not navigable, for example because they are either too narrow or too shallow, or because of an unnavigable reef or archipelago. Straits are also known to be loci for sediment accumulation. Usually, sand-size deposits occur on both the two opposite strait exits, forming subaqueous fans or deltas. Terminology The terms ''channel'', ''pass'', or ''passage'' can be synonymous and used interchangeably with ''strait'', although each is sometimes differentiated with varying senses. In Scotland, ''firth'' or ''Kyle'' are also sometimes used as synonyms for strait. Many straits are economically important. Straits can be important shipping routes and wars have been fought for control of them. ... [...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]   |
|
Poel
Poel () or Poel Island (german: Insel Poel), is an island in the Baltic Sea. It forms the natural northern and eastern boundaries of the Bay of Wismar on the German coast. The northern coast of the island is also on the south side of the large gulf known as the Bay of Mecklenburg, which Wismar Bay enters into. Insel Poel thus forms on its northern side the unofficial latitude of the northern boundary of the Wismar Bay. It is close to the cities of Lübeck, Wismar and Schwerin and is part of the Hamburg Metropolitan Region. Administratively it is a municipality in the Nordwestmecklenburg district. It consists of Kirchdorf and Oertzenhof (the main towns) and the smaller villages of Timmendorf, Wangern, Hinterwangern, Weitendorf, Weitendorf-Hof, Brandenhusen, Neuhof, Seedorf, Niendorf, Schwarzer Busch, Kaltenhof, Fährdorf, Malchow, Vorwerk and Gollwitz. It covers an area of and has 2,873 citizens. Satellite pictures show that most of it is used as farmland. With its good air, cl ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Landkreis Nordwestmecklenburg
Nordwestmecklenburg (''Northwestern Mecklenburg'') is a ''Kreis'' (district) in the north-western part of Mecklenburg-Vorpommern, Germany. It is situated on the coast of the Baltic Sea and borders on Schleswig-Holstein to the west. Neighboring districts are (from east clockwise) Rostock, Ludwigslust-Parchim and the district-free city Schwerin, and the district Lauenburg and the district-free city Lübeck in Schleswig-Holstein. The district seat is the town Wismar. Geography The district is roughly situated in a triangle between the towns of Lübeck, Rostock and Schwerin. In the north there is the coast of the Baltic Sea with the small island of Poel. Lakes Two large lakes are partially situated in Nordwestmecklenburg: the eastern half of the Schaalsee () at the western border; and the northern half of the Schweriner See () in the south, as well as two smaller lakes, Bibowee () and Mechower See (). History Nordwestmecklenburg District was established in 1994 by merging the prev ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Bay Of Wismar
The Bay of WismarKohl, Horst; Marcinek, Joachim and Nitz, Bernhard (1986). ''Geography of the German Democratic Republic'', VEB Hermann Haack, Gotha, p. 47. . or more commonly Wismar Bay or ''Wismarbucht'' is a well sheltered multi-sectioned bay in the southwestern Baltic Sea, in Mecklenburg-Vorpommern, Germany, and is considered the south-central part of the much larger arm of the Baltic known as the Mecklenburg Bay (or Mecklenburg Bight, for its long narrow bent shape)—a long fingerlike gulf oriented to the west-southwest (WSW) from the (central) Baltic proper. Wismar bay is considered one of the finest natural harbors on the Baltic, and served as the destination for much seaborne shipping until circa the 1910s when its minimum depths of became too shallow for larger more modern ships. Today, because of the shallow sheltered waters the bay is the subject of much research via underwater archeology There are four lobe like parts of the Bay of Wismar which are themselves bays ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Salzhaff
The Salzhaff is a part of the Bay of Wismar that is almost cut off from the Baltic Sea by the spit of the Wustrow and ''Boiensdorfer Werder'' peninsulas. It is located south of the town of Rerik in Mecklenburg-Vorpommern and southwest of the seaside resort of Kühlungsborn in Central Mecklenburg. It is linked to the Bay of Wismar by the Breitling. The Wustrow Peninsular was used by the military until the withdrawal of the Soviet Army in the early 1990s. The adjacent bay of ''Kroy'' in the western part of the Salzhaff and the sandy island of Kieler Ort just offshore are both conservation areas. The Salzhaff is a popular holiday and recreation region. Its shallow waters are ideally suited to beginners in the sports of sailing and surfing. File:Am Salzhaff 1.JPG, Greylag Geese The greylag goose or graylag goose (''Anser anser'') is a species of large goose in the waterfowl family Anatidae and the type species of the genus ''Anser (bird), Anser''. It has mottled and barred ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Causeway
A causeway is a track, road or railway on the upper point of an embankment across "a low, or wet place, or piece of water". It can be constructed of earth, masonry, wood, or concrete. One of the earliest known wooden causeways is the Sweet Track in the Somerset Levels, England, which dates from the Neolithic age. Timber causeways may also be described as both boardwalks and bridges. Etymology When first used, the word ''causeway'' appeared in a form such as "causey way" making clear its derivation from the earlier form "causey". This word seems to have come from the same source by two different routes. It derives ultimately, from the Latin for heel, ''calx'', and most likely comes from the trampling technique to consolidate earthworks. Originally, the construction of a causeway utilised earth that had been trodden upon to compact and harden it as much as possible, one layer at a time, often by enslaved bodies or flocks of sheep. Today, this work is done by machines. The s ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Ahrendsberg
Ahrendsberg is an uninhabited island, in area, near the island of Poel in the Breitling, a strait off the Bay of Wismar on the Baltic coast of Germany. The island, which is roughly long and up to wide, is dominated by salt meadows with marshy islands and shores that are dissected by creeks. The higher areas are generally very dry and are characterised by stunted vegetation, for example dry, lean grassland with thorn bushes. At the southern tip of the island is a short section of cliff In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on co .... External links www.naturschutz-wismarbucht.de {{authority control Islands of Mecklenburg-Western Pomerania German islands in the Baltic Bay of Wismar Uninhabited islands of Germany ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Alluvial
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined ''alluvion'' (the F ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
|
Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |