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Belle River, Saint Pierre And Miquelon
The Belle River is the largest river in the French overseas collectivity of Saint Pierre and Miquelon. The river flows through the archipelago's largest island of Miquelon-Langlade, which is formed by a thin strip of land called a tombolo A tombolo is a sandy or shingle isthmus. A tombolo, from the Italian ', meaning 'pillow' or 'cushion', and sometimes translated incorrectly as ''ayre'' (an ayre is a shingle beach of any kind), is a deposition landform by which an island become ... that connects the two northern and southern "islands" of Miquelon and Langlade, respectively. The river is fed by several streams and ponds on Langlade, and flows northwest for the majority of its length. The river's course turns northeast shortly before emptying into the sea on the eastern side of the island in the community of Anse du Gouverneur. References Rivers of Saint Pierre and Miquelon {{SaintPierreMiquelon-geo-stub ...
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Saint Pierre And Miquelon
Saint Pierre and Miquelon (), officially the Territorial Collectivity of Saint-Pierre and Miquelon (french: link=no, Collectivité territoriale de Saint-Pierre et Miquelon ), is a self-governing territorial overseas collectivity of France in the northwestern Atlantic Ocean near the Canadian province of Newfoundland and Labrador.Saint Pierre and Miquelon
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Saint Pierre and Miquelon is a remaining vestige of the once-vast territory of ...
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Overseas Collectivity
The French overseas collectivities (''collectivité d'outre-mer'' or ''COM'') are first-order administrative divisions of France, like the French regions, but have a semi-autonomous status. The COMs include some former French overseas colonies and other French overseas entities with a particular status, all of which became COMs by constitutional reform on 28 March 2003. The COMs differ from overseas regions and overseas departments, which have the same status as metropolitan France but are located outside Europe. As integral parts of France, overseas collectivities are represented in the National Assembly, Senate and Economic and Social Council. Though some are outside the European Union, all can vote to elect members of the European Parliament (MEPs). (All of France became one multi-member EU constituency in 2019.) The Pacific COMs use the CFP franc, a currency pegged to the euro, whereas the Atlantic COMs use the euro itself. As of 31 March 2011, there were five COMs: * ...
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Miquelon-Langlade
Miquelon-Langlade is the larger but less populated of the two communes (municipalities) making up the French overseas collectivity of Saint Pierre and Miquelon, located to the south of Newfoundland in the Gulf of St. Lawrence. It consists of three geological islands: Miquelon, Langlade and Le Cap, connected with tombolos. The communal seat is the settlement of Miquelon, on the northern tip, where the entire island's permanent population of 580 (as of 2019) is located. Miquelon Airport provides flights to Montreal and to nearby Saint-Pierre. Geography Located in the Gulf of St. Lawrence, west of Newfoundland's Burin Peninsula, Miquelon-Langlade covers a total land area of . It comprises three islands connected by tombolos: Le Cap in the north, Miquelon (''Grand Miquelon'') in the center, and Langlade (''Petite Miquelon'') in the south. On the south of the Miquelon Island is a large lagoon known as the Grand Barachois which is host to a large population of seals and other wild ...
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Tombolo
A tombolo is a sandy or shingle isthmus. A tombolo, from the Italian ', meaning 'pillow' or 'cushion', and sometimes translated incorrectly as ''ayre'' (an ayre is a shingle beach of any kind), is a deposition landform by which an island becomes attached to the mainland by a narrow piece of land such as a spit or bar. Once attached, the island is then known as a tied island. Several islands tied together by bars which rise above the water level are called a tombolo cluster. Two or more tombolos may form an enclosure (called a lagoon) that can eventually fill with sediment. Formation The shoreline moves toward the island (or detached breakwater) due to accretion of sand in the lee of the island, where wave energy and longshore drift are reduced and therefore deposition of sand occurs. Wave diffraction and refraction True tombolos are formed by wave refraction and diffraction. As waves near an island, they are slowed by the shallow water surrounding it. These waves th ...
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