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Cape Split, Nova Scotia
Cape Split is a headland located on the Bay of Fundy coast of the Canadian province of Nova Scotia. The Battle off Cape Split happened during the American Revolution. Cape Split is located in Kings County and is a continuation of the North Mountain range, which is made of tholeiitic basalt. The cape separates the main part of the Bay of Fundy from the Minas Basin, a sub-basin to the east. The cape itself is 7 km (4 mi) long and ranges between several kilometres to several dozen metres in width. Both sides of the headland end in high cliffs overlooking treacherous tidal currents in the Minas Channel. Privately owned until recently, the property has now been sold to the Government of Nova Scotia and is being transformed into a provincial park. Its current status is that of a Reserve Park of 427 hectares. A popular hiking trail has existed for decades on Cape Split, taking approximately 2 to 2.5 hours each way to the tip of the headland. Most of the Cape is heavily fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Split01
A cape is a clothing accessory or a sleeveless outer garment which drapes the wearer's back, arms, and chest, and connects at the neck. History Capes were common in medieval Europe, especially when combined with a hood in the chaperon. They have had periodic returns to fashion - for example, in nineteenth-century Europe. Roman Catholic clergy wear a type of cape known as a ferraiolo, which is worn for formal events outside a ritualistic context. The cope is a liturgical vestment in the form of a cape. Capes are often highly decorated with elaborate embroidery. Capes remain in regular use as rainwear in various military units and police forces, in France for example. A gas cape was a voluminous military garment designed to give rain protection to someone wearing the bulky gas masks used in twentieth-century wars. Rich noblemen and elite warriors of the Aztec Empire would wear a tilmàtli; a Mesoamerican cloak/cape used as a symbol of their upper status. Cloth and clothing wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Chronicle Herald
''The Chronicle Herald'' is a broadsheet newspaper published in Halifax, Nova Scotia, Canada owned by SaltWire Network of Halifax. The paper's newsroom staff were locked out of work from January 2016 until August 2017. ''Herald'' management continued to publish using strikebreaker labour, and were accused by the union of refusing to bargain in good faith with the intention of union busting. History Early years Founded in 1874 as ''The Morning Herald'', the paper quickly became one of Halifax's main newspapers. The same company also owned the ''Evening Mail'', which was published in the afternoon. Its main competitors were the ''Chronicle'' in the morning, and the ''Star'' in the afternoon. By 1949 the papers had merged to become ''The Chronicle-Herald'' and ''Mail-Star'' respectively. Graham Dennis era Graham W. Dennis took over as publisher of the newspaper in 1954, at age 26, after the death of his father, senator William Henry Dennis, who in turn had succeeded senator Wil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Kings County, Nova Scotia
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 the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of Nova Scotia
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism Of Nova Scotia
Volcanism, vulcanism or volcanicity is the phenomenon of eruption of molten rock (magma) onto the surface of the Earth or a solid-surface planet or moon, where lava, pyroclastics, and volcanic gases erupt through a break in the surface called a vent. It includes all phenomena resulting from and causing magma within the crust or mantle of the body, to rise through the crust and form volcanic rocks on the surface. Magmas, that reach the surface and solidify, form extrusive landforms. Volcanic processes Magma from the mantle or lower crust rises through the crust towards the surface. If magma reaches the surface, its behavior depends on the viscosity of the molten constituent rock. Viscous (thick) magma produces volcanoes characterised by explosive eruptions, while non-viscous (runny) magma produce volcanoes characterised by effusive eruptions pouring large amounts of lava onto the surface. In some cases, rising magma can cool and solidify without reaching the surface. Instead, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism Of Eastern Canada
The volcanology of Eastern Canada includes the hundreds of volcanic areas and extensive lava formations in Eastern Canada. The region's different volcano and lava types originate from different tectonic settings and types of volcanic eruptions, ranging from passive lava eruptions to violent explosive eruptions. Eastern Canada has very large volumes of magmatic rock called large igneous provinces. They are represented by deep-level plumbing systems consisting of giant dike swarms, sill provinces and layered intrusions. The most capable large igneous provinces in Eastern Canada are Archean (3,800-2,500 million years ago) age greenstone belts containing a rare volcanic rock called komatiite. Greenstone belts Abitibi greenstone belt The 2,677 million year old Abitibi greenstone belt in Ontario and Quebec is one of the largest Archean greenstone belts on Earth and one of the youngest parts of the Superior craton which sequentially forms part of the Canadian Shield. Komatii ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism Of Canada
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 volcanoes, calderas, diatremes, and maars, along with less common volcanic forms such as tuyas and subglacial mounds. Though Canada's volcanic history dates back to the Precambrian eon, at least 3.11 billion years ago, when its part of the North American continent began to form, volcanism continues to occur in Western and Northern Canada in modern times, where it forms part of an encircling chain of volcanoes and frequent earthquakes around the Pacific Ocean called the Pacific Ring of Fire. Because volcanoes in Western and Northern Canada are in relatively remote and sparsely populated areas and their activity is less frequent than with other volcanoes around the Pacific Ocean, Canada is commonly thought to occupy a gap in the Ring of Fire between the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Split, Nova Scotia
Cape Split is a headland located on the Bay of Fundy coast of the Canadian province of Nova Scotia. The Battle off Cape Split happened during the American Revolution. Cape Split is located in Kings County and is a continuation of the North Mountain range, which is made of tholeiitic basalt. The cape separates the main part of the Bay of Fundy from the Minas Basin, a sub-basin to the east. The cape itself is 7 km (4 mi) long and ranges between several kilometres to several dozen metres in width. Both sides of the headland end in high cliffs overlooking treacherous tidal currents in the Minas Channel. Privately owned until recently, the property has now been sold to the Government of Nova Scotia and is being transformed into a provincial park. Its current status is that of a Reserve Park of 427 hectares. A popular hiking trail has existed for decades on Cape Split, taking approximately 2 to 2.5 hours each way to the tip of the headland. Most of the Cape is heavily fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Government Of Nova Scotia
The Government of Nova Scotia (french: Gouvernement de la Nouvelle-Écosse, gd, Riaghaltas Alba Nuadh) refers to the provincial government of the Provinces and territories of Canada, Canadian province of Nova Scotia. Nova Scotia is one of Canada's four Atlantic Provinces, and the second-smallest province by area. The Capital city, capital of the province, Halifax, is Nova Scotia's largest city and its political capital. Halifax is where the Province House, Canada's oldest legislative building, is located. The Government of Nova Scotia consists of three branches: legislative, executive and judicial. Its powers and structure are set out in the Constitution Act, 1867. In modern Canadian use, the term "government" refers broadly to the cabinet of the day (formally the Executive Council of Nova Scotia), elected from the Nova Scotia House of Assembly and the non-political staff within each provincial department or agency – that is, the civil service. The Provinces and territories of C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bay Of Fundy
The Bay of Fundy (french: Baie de Fundy) is a bay between the Canadian provinces of New Brunswick and Nova Scotia, with a small portion touching the U.S. state of Maine. It is an arm of the Gulf of Maine. Its extremely high tidal range is the highest in the world. The name is likely a corruption of the French word , meaning 'split'. Hydrology Tides The tidal range in the Bay of Fundy is about ; the average tidal range worldwide is only . Some tides are higher than others, depending on the position of the moon, the sun, and atmospheric conditions. Tides are semidiurnal, meaning they have two highs and two lows each day, with about six hours and 13 minutes between each high and low tide. Because of tidal resonance in the funnel-shaped bay, the tides that flow through the channel are very powerful. In one 12-hour tidal cycle, about 100 billion tons (110 billion short tons) of water flows in and out of the bay, which is twice as much as the combined total flow of all the rive ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Minas Basin
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