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Minas Basin
, image = Lookout On Way to Cape Split - 25006718579.jpg , alt = , caption = Looking east across the Southern Bight of Minas Basin from The Lookoff , image_bathymetry = , alt_bathymetry = , caption_bathymetry = , location = Nova Scotia , group = , coordinates = , type = Inlet , etymology = , part_of = Bay of Fundy , inflow = , rivers = , outflow = , oceans = , catchment = , basin_countries = , agency = , designation = , date-built = , engineer = , date-flooded = , length = , width = , area = , depth = , max-depth = , volume = , residence_time = , salinity = , shore = , elevation = , temperature_high = ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Lookoff, Nova Scotia
The Lookoff is a community in the Canadian province of Nova Scotia Nova Scotia ( ; ; ) is one of the thirteen provinces and territories of Canada. It is one of the three Maritime provinces and one of the four Atlantic provinces. Nova Scotia is Latin for "New Scotland". Most of the population are native Eng ..., located in Kings County. References The Lookoff on Destination Nova Scotia Communities in Kings County, Nova Scotia General Service Areas in Nova Scotia {{KingsNS-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Blomidon
Cape Blomidon ( ) is a headland located on the Bay of Fundy coast of the Canadian province of Nova Scotia. Cape Blomidon is located in Kings County at the northeast edge of the Blomidon Peninsula. Its geology largely comprises sedimentary sandstone, which is unique since it is connected to the North Mountain range and made up of tholeiitic basalt. Cape Blomidon features distinctive reddish-coloured cliffs that reach up to 100 metres in height above the Minas Basin, which stretches out to the east. Cape Split is the geologic continuation of the North Mountain range and juts off the Blomidon Peninsula to the northwest. According to Mi'kmaq legend, Cape Blomidon is the home of Glooscap. The cape and much of the coastal area of the Blomidon Peninsula are protected by Blomidon Provincial Park. Visitor access to this park is located at the southern edge of the peninsula, approximately 3.5 kilometres south of Cape Blomidon. The name "Cape Blomidon" was officially approved on Octo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Levee
A levee (), dike (American English), dyke (Commonwealth English), embankment, floodbank, or stop bank is a structure that is usually earthen and that often runs parallel to the course of a river in its floodplain or along low-lying coastlines. The purpose of a levee is to keep the course of rivers from changing and to protect against flooding of the area adjoining the river or coast. Levees can be naturally occurring ridge structures that form next to the bank of a river, or be an artificially constructed fill or wall that regulates water levels. Ancient civilizations in the Indus Valley, ancient Egypt, Mesopotamia and China all built levees. Today, levees can be found around the world, and failures of levees due to erosion or other causes can be major disasters. Etymology Speakers of American English (notably in the Midwest and Deep South) use the word ''levee'', from the French word (from the feminine past participle of the French verb , 'to raise'). It originat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt Headlands
The Basalt Headlands are a chain of intermittent high-cliffed bluffs and islands that fringe the northern edge of the Minas Basin, Nova Scotia, Canada. Its name comes from the basaltic outcrops that formed about 200 million years ago when this region was volcanically active by continental rifting. See also *Volcanism of Canada
Volcanism, Volcanic activity is a major part of the geology of Canada and is characterized by many types of volcanic landform, including lava flows, volcanic plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, submarine volcano ...
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Basalt
Basalt (; ) is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of Venus, which cover ~80% of the surface, are basaltic; the lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flows that can spread over great areas before cooling and solidifying. Flood basalts are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Farrell River
Farrells River, formerly known as Parrsboro River, is a small river that flows south into an aboiteau on Parrsboro Harbour on the Minas Basin near the town of Parrsboro, Nova Scotia. Miꞌkmaq The Mi'kmaq (also ''Mi'gmaq'', ''Lnu'', ''Miꞌkmaw'' or ''Miꞌgmaw''; ; ) are a First Nations people of the Northeastern Woodlands, indigenous to the areas of Canada's Atlantic Provinces and the Gaspé Peninsula of Quebec as well as the nort ... summer encampments bordered the river near the current Glooscap restaurant on a flat which is now blueberry fields with bee hives. A story is told of a small plane flown by novice Air Force pilots that was forced to land in heavy fog in Parrsboro Bay. The local people, hearing the engines in trouble in the sky, lit fires along the Farrell River to indicate a landing strip on the ice at the mouth of the river. The young pilot landed the plane, but bounced, and it cleared the bridge, barely tipping telegraph wires and landing on the other sid ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canard River
The Canard River is a river in Kings County, Nova Scotia, Canada which drains into the Minas Basin of the Bay of Fundy between the communities of Canard and Starr's Point. It is known for its fertile river banks and extensive dyke land agriculture. Geography The river has its source in a number of small brooks which flow from the sandy pine woods of what is now the Camp Aldershot military base, near Steam Mill Village. The Canard River has a short length of 15 km but its lower reaches are wide and deep due to the enormous tides of the Minas Basin. The river was once tidal for most of its length but a series of dykes first built in the 1600s held back the tide which is now stopped near the river's mouth by the Wellington Dyke. The upper reaches of the river are often referred to by the dykes which once spanned the river - Upper Dyke and Middle Dyke. History The Canard river was known to the Mi'kmaq people as Apocheechumochwakade meaning "home of the black duck". The Mi' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salmon River (Nova Scotia)
The Salmon River is a Canadian river in central Nova Scotia's Colchester County. Rising in the Cobequid Hills in the central-northeastern part of the county, the river descends through a broad glacial valley at the head of Cobequid Bay, the eastern extremity of the Bay of Fundy. The river discharges into the bay at a point between Lower Truro and Lower Onslow, the historic head of navigation. A tidal bore is observed daily on the lower part of the river to the head of the tide at Truro. The river is known for ice jams during the spring freshet. Poor planning has led to urban sprawl in Truro and the neighbouring areas of the county impacting the river's floodplain A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Goudi .... During the 1869 Saxby Gale, the entire floodplain and signifi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gaspereau River
The Gaspereau River is a river in Kings County, Nova Scotia, Canada. It has a length of approximately 24 km from its source at Gaspereau Lake on the South Mountain south of Kentville to its mouth at Hortonville on the Minas Basin. The lower portion of the river is tidal for 6.5 km until Melanson and there are extensive tidal marshes in the lower reaches. The upper 16 km runs swiftly over gravel beds, boulders and bedrock, except for several dammed sections which form narrow and deep channels. Damming for Hydroelectric generation has resulted in twelve major lakes being connected to the river creating a watershed of 1,375 square kilometres. A major tributary is the Black River which joins the Gaspeareau at White Rock. The Black River once flowed further north into the Cornwallis River but connected to the Gaspereau through a natural erosion process known as river capture. Fishery Although the Gaspereau is a short river, the riverbed habitat and connecting lakes f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cornwallis River
The Cornwallis River is in Kings County, Nova Scotia, Canada. It has a meander length of approximately through eastern Kings County, from its source on the North Mountain at Grafton to its mouth near Wolfville on the Minas Basin. The lower portion of the river beginning at Kentville is tidal and there are extensive tidal marshes in the lower reaches. In its upper watershed at Berwick, the river draws on the Caribou Bog while a longer branch continues to the official source, a stream on the North Mountain at Grafton. History The original peoples of the area, the Mi'kmaq, knew it as ''The Narrow River'', or Chijekwtook There are also references to the Mi'kmaq calling the river Jijuktu'kwejk (pronounced, "''Gee-gee-wok-tuk''"). The river was named Riviere St. Antoine by Samuel de Champlain after his arrival in the New World in the early 17th Century. Later it was called the Riviere des Habitants by the Acadians, who built a series of settlements around its mouth including th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shubenacadie River
The Shubenacadie River is a river in Nova Scotia, Canada. It has a meander length of approximately 72 km from its source at Shubenacadie Grand Lake to its mouth at the historic seaport village of Maitland on Cobequid Bay, site of the building of the '' William D. Lawrence'', the largest wooden ship ever built in Canada. In 2009, the ''I Backpack Canada'' blog named the Shubenacadie one of the top five whitewater rivers in Canada. The lower 30 km of the river (from the point where the Stewiacke River meets to the mouth) is tidal and the river experiences a tidal bore twice daily, with some bores reaching up to 3 m in height at certain points along the river. Local tourism operators offer adventure seekers a chance to ride with the bore on high-horse power Zodiac Hurricanes. Tidal Bore Rafting was invented at the Tidal Bore Rafting Resort by H. Knoll. It is also a popular surfing spot for experienced Sea Kayakers. The river flows through part of northern Halifax Cou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avon River (Nova Scotia)
__NOTOC__ The Avon River is a small river in central Nova Scotia, Canada. A northerly flowing river, the Avon River's flow rises at an elevation of 145 metres (475 ft.) at Card and Bag Lakes on the South Mountain (Nova Scotia), South Mountain, a distance of approximately 29 kilometres (18 miles) southwest of the town of Windsor, Nova Scotia, Windsor. Its meander length is . At Windsor Forks the main tributary, the West Branch Avon River, adds its flow, along with that of the Southwest Branch Avon, to the Avon. The West Branch Avon River rises at an elevation of 175 metres (574 ft.) at Black River Lake. Both the flows of the Avon and the West Branch have been impeded by hydropower developments in the early twentieth century. Near the rural community of Martock, Nova Scotia, Martock, the river enters a broad glacial river valley forming a ria where it becomes tide, tidal, creating an estuary for its remaining route to the Minas Basin at Kempt Shore, several kilometres dow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
