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Sydney River
The Sydney River is a short river located in Cape Breton County, Nova Scotia, Cape Breton County, Nova Scotia, Canada. Historically, it was also referred to as the Spanish River from the 18th century Early modern France, French name for its estuary, Spanish Bay (Nova Scotia), Baie d’Espagnols. It separates the communities of Coxheath, Nova Scotia, Coxheath and Westmount, Nova Scotia, Westmount, on the north bank of the river, from Howie Centre, Sydney River, Nova Scotia, Sydney River, and Sydney, Nova Scotia, Sydney on the south and east banks. Sydney River rises in Blacketts Lake and runs to its mouth, between the Westmount shore near Amelia Point and Battery Point on the Sydney shore, at the South Arm of Sydney Harbour, draining a drainage basin, watershed of 140 km south of the crest of the Coxheath Hills. The river is an estuary for the last below the "Sydney Steel Corporation, Sysco Dam" in the community of Sydney River, Nova Scotia, Sydney River. The dam was const ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sydney, Nova Scotia
Sydney is a former city and urban community on the east coast of Cape Breton Island in Nova Scotia, Canada within the Cape Breton Regional Municipality. Sydney was founded in 1785 by the British, was incorporated as a city in 1904, and dissolved on 1 August 1995, when it was amalgamated into the regional municipality. Sydney served as the Cape Breton Island's colonial capital, until 1820, when the colony merged with Nova Scotia and the capital moved to Halifax. A rapid population expansion occurred just after the turn of the 20th century, when Sydney became home to one of North America's main steel mills. During both the First and Second World Wars, it was a major staging area for England-bound convoys. The post-war period witnessed a major decline in the number of people employed at the Dominion Steel and Coal Corporation steel mill, and the Nova Scotia and Canadian governments had to nationalize it in 1967 to save the region's biggest employer, forming the new crown corpora ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of The Cape Breton Regional Municipality
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Rivers Of Nova Scotia
Nova Scotia's rivers all flow into the Atlantic Ocean through four unique watersheds: the Gulf of Maine, the Northumberland Strait, the Gulf of Saint Lawrence and into the Atlantic Ocean itself. Gulf of Maine The Gulf of Maine system includes the Bay of Fundy, which includes the Cumberland and Minas Basins. In Nova Scotia, the system occupies the shores from Fort Lawrence to Cape St. Mary (44°05′N). Bay of Fundy The Bay of Fundy coastline in Nova Scotia begins at Fort Lawrence and circles Cape Chignecto eastward to Truro. It then follows west along the Annapolis Valley as far as Brier Island on the Digby Neck. Within the Bay of Fundy are two basins: Chignecto Bay which begins at Fort Lawrence and ends at Cape Chignecto, and the Minas Basin that encompasses everything east of Ramshead Point (near Diligent River) and Cape Split. *Apple River (Note: westernmost river on the north coast of the Bay of Fundy) *Fox River *Ramshead River *Diligent River (Note: easternmost river o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yellow Lampmussel
''Lampsilis cariosa'', the yellow lampmussel, is a species of freshwater mussel, an aquatic bivalve mollusk in the family Unionidae, the river mussels. Its natural habitat is rivers. Distribution and conservation status This species is found in Canada and the United States. It lives in New Brunswick and in Nova Scotia in Canada, where the Committee on the Status of Endangered Wildlife in Canada (COSEWIC) has listed it as a species of special concern. The Canadian Species at Risk Act listed it in the List of Wildlife Species at Risk The List of Wildlife Species at Risk currently has more than 800 entries for Canadian wild life species considered vulnerable; including 363 classified as endangered species, —190 threatened species, —235 special concern, and 22 extirpated ( ... as being a species of special concern in Canada.COSEWIC. 2005Canadian Species at Risk Committee on the Status of Endangered Wildlife in Canada. 64 pp., page 27. References cariosa Bivalve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bras D'Or Lake
Bras d'Or Lake (Mi'kmaq language, Mi'kmawi'simk: Pitupaq) is an irregular estuary in the centre of Cape Breton Island in Nova Scotia, Canada. It has a connection to the open sea, and is tidal. It also has inflows of fresh water from rivers, making the brackish water a very productive natural habitat. It was designated the Bras d'Or Lake Biosphere Reserve by UNESCO in 2011. Toponym Pronounced ( or ), maps before 1872 name it ''Le Lac de Labrador'' (or more simply ''Labrador''). ''Labrador'' was the name given by the Portuguese to much of eastern Canada. It meant ''farmer'', and is cognate with ''laborer''. An error of folk etymology, the name is spelt to resemble the French language ''Arm of'' ''Gold'', a homonym. It is also called locally ''The Bras d'Or Lakes''. In Mi'kmaq language, Mi'kmawi'simk, the lake's name, ''Pitupaq'', refers to the brackish waters, meaning "the long salt water." Geography The lake has a surface area of 1099 square kilometers. Three Arm (geogr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Bay (Nova Scotia)
East Bay is a bay of the Bras d'Or Lake on Cape Breton Island in the Canadian province of Nova Scotia. It lies entirely within Cape Breton County. Description East Bay is one of three long narrow arms that extend to the east of the main body of the Bras d'Or Lake, the others being St. Andrews Channel and Great Bras d'Or Channel. As East Bay is part of the Bras d'Or Lake system and the lake is essentially a fiordal system connected to the North Atlantic via two restricted channels at the Great Bras d'Or Channel north of Boularderie Island and the Little Bras d'Or Channel to south of Boularderie Island, the waters of East Bay are brackish, partially fresh/ salt water. East Bay opens to the south-west directly onto the Bras d'Or Lake and lies between the Boisdale Hills to the north and the East Bay Hills to the south. The bay measures wide at its mouth, between Benacadie Point to the north, and Middle Cape to the south and runs easterly to its terminus at Portage. East ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mi'kmaq People
The Mi'kmaq (also ''Mi'gmaq'', ''Lnu'', ''Miꞌkmaw'' or ''Miꞌgmaw''; ; ) are a First Nations in Canada, First Nations people of the Indigenous peoples of the Northeastern Woodlands, Northeastern Woodlands, indigenous to the areas of Canada's Atlantic Canada, Atlantic Provinces and the Gaspé Peninsula of Quebec as well as the northeastern region of Maine. The traditional national territory of the Mi'kmaq is named Miꞌkmaꞌki (or Miꞌgmaꞌgi). There are 170,000 Mi'kmaq people in the region, (including 18,044 members in the recently formed Qalipu First Nation in Newfoundland.) Nearly 11,000 members speak Miꞌkmaq language, Miꞌkmaq, an Eastern Algonquian languages, Eastern Algonquian language. Once written in Miꞌkmaq hieroglyphic writing, Miꞌkmaw hieroglyphic writing, it is now written using most letters of the Latin alphabet. The Mi'kmaq, Maliseet, and Passamaquoddy, Pasamaquoddy nations signed a series of treaties known as the Covenant Chain of Peace and Friendship ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Portage
Portage or portaging (Canada: ; ) is the practice of carrying water craft or cargo over land, either around an obstacle in a river, or between two bodies of water. A path where items are regularly carried between bodies of water is also called a ''portage.'' The term comes from French, where means "to carry," as in "portable". In Canada, the term "carrying-place" was sometimes used. Early French explorers in New France and French Louisiana encountered many rapids and cascades. The Native Americans carried their canoes over land to avoid river obstacles. Over time, important portages were sometimes provided with canals with locks, and even portage railways. Primitive portaging generally involves carrying the vessel and its contents across the portage in multiple trips. Small canoes can be portaged by carrying them inverted over one's shoulders and the center strut may be designed in the style of a yoke to facilitate this. Historically, voyageurs often employed tump lines on t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eskers
An esker, eskar, eschar, or os, sometimes called an ''asar'', ''osar'', or ''serpent kame'', is a long, winding ridge of stratified sand and gravel, examples of which occur in glaciated and formerly glaciated regions of Europe and North America. Eskers are frequently several kilometres long and, because of their uniform shape, look like railway embankments. Etymology The term ''esker'' is derived from the Irish word ''eiscir'' (Old Irish: ''escir''), which means "ridge or elevation, especially one separating two plains or depressed surfaces". The Irish word was and is used particularly to describe long sinuous ridges, which are now known to be deposits of fluvio-glacial material. The best-known example of such an ''eiscir'' is the '' Eiscir Riada'', which runs nearly the whole width of Ireland from Dublin to Galway, a distance of , and is still closely followed by the main Dublin-Galway road The synonym ''os'' comes from the Swedish word ''ås'', "ridge". Geology Most esker ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kame
A kame, or ''knob'', is a glacial landform, an irregularly shaped hill or mound composed of sand, gravel and till that accumulates in a depression on a retreating glacier, and is then deposited on the land surface with further melting of the glacier. Kames are often associated with kettles, and this is referred to as ''kame and kettle'' or ''knob and kettle'' topography. The word ''kame'' is a variant of ''comb'' (''kame'', or ''kaim'' is the Old Scottish word for ''comb''), which has the meaning "crest" among others. The geological term was introduced by Thomas Jamieson in 1874. According to White, "kames were formed by meltwater which deposited more or less washed material at irregular places in and along melting ice. At places the material is very well washed and stratified; at others it is more poorly washed, with inclusions of till masses that fell from ice but were covered before they were completely washed. Kame gravels thus tend to be variable and range from fine to c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Valley
U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic. Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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