Geography Of Halifax, Nova Scotia
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Geography Of Halifax, Nova Scotia
The Halifax Regional Municipality (HRM) in Nova Scotia, Canada has a widely varied geography. Physical geography Halifax Regional Municipality has an area of approximately , and is approximately in length between its eastern and westernmost extremities. HRM's shoreline "as the crow flies" is approximately in length, while its northern boundary is usually between 50 and 60 km inland. The coast, which is mostly rock with small isolated sand beaches in sheltered bays, is heavily indented by numerous inlets the largest of which are St. Margarets Bay, Halifax Harbour, Cole Harbour, Musquodoboit Harbour, Jeddore Harbour, Ship Harbour and Sheet Harbour. Given this fact, it takes approximately 3 hours to drive along the shore from Hubbards, located in the southwestern end of HRM, to Ecum Secum, away at the northeastern end. The Chebucto Peninsula, created by the indentations of St. Margarets Bay and Halifax Harbour (including the Bedford Basin), is a defining feature for the sh ...
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Halifax Regional Municipality, Nova Scotia
Halifax is the capital and largest municipality of the Canadian province of Nova Scotia, and the largest municipality in Atlantic Canada. As of the 2021 Census, the municipal population was 439,819, with 348,634 people in its urban area. The regional municipality consists of four former municipalities that were amalgamated in 1996: Halifax, Dartmouth, Bedford, and Halifax County. Halifax is a major economic centre in Atlantic Canada, with a large concentration of government services and private sector companies. Major employers and economic generators include the Department of National Defence, Dalhousie University, Nova Scotia Health Authority, Saint Mary's University, the Halifax Shipyard, various levels of government, and the Port of Halifax. Agriculture, fishing, mining, forestry, and natural gas extraction are major resource industries found in the rural areas of the municipality. History Halifax is located within '' Miꞌkmaꞌki'' the traditional ancestral lands o ...
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Nova Scotia Highway 102
Highway 102 is a north-south highway in the Canadian province of Nova Scotia that runs from Halifax to Onslow, immediately north of the town of Truro. It is the busiest highway in Atlantic Canada. In 2000, the section of Highway 102 between Fall River and Truro was redesignated as Veterans Memorial Highway. Between Fall River and Halifax it is known as Bicentennial Drive or the Bicentennial Highway. History The highway parallels the route of its predecessor, Trunk 2, and was developed in stages from 1958 to the 1970s. Initially, some sections were controlled access two-lane, as well as four-lane. The route has also changed somewhat, particularly during the mid-1970s when the last part to be constructed resulted in the bypass of Shubenacadie and Stewiacke. The initial speed limit on the highway was 100 km/h (60 mph) until 1997, when it was raised to 110 km/h (70 mph) for the section between the interchange with Highway 118 (approximately km 26) and exit ...
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Halifax, Nova Scotia
Halifax is the capital and largest municipality of the Canadian province of Nova Scotia, and the largest municipality in Atlantic Canada. As of the 2021 Census, the municipal population was 439,819, with 348,634 people in its urban area. The regional municipality consists of four former municipalities that were amalgamated in 1996: Halifax, Dartmouth, Bedford, and Halifax County. Halifax is a major economic centre in Atlantic Canada, with a large concentration of government services and private sector companies. Major employers and economic generators include the Department of National Defence, Dalhousie University, Nova Scotia Health Authority, Saint Mary's University, the Halifax Shipyard, various levels of government, and the Port of Halifax. Agriculture, fishing, mining, forestry, and natural gas extraction are major resource industries found in the rural areas of the municipality. History Halifax is located within ''Miꞌkmaꞌki'' the traditional ancestral lands ...
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Coniferous
Conifers are a group of cone-bearing seed plants, a subset of gymnosperms. Scientifically, they make up the division Pinophyta (), also known as Coniferophyta () or Coniferae. The division contains a single extant class, Pinopsida. All extant conifers are perennial woody plants with secondary growth. The great majority are trees, though a few are shrubs. Examples include cedars, Douglas-firs, cypresses, firs, junipers, kauri, larches, pines, hemlocks, redwoods, spruces, and yews.Campbell, Reece, "Phylum Coniferophyta". Biology. 7th. 2005. Print. P. 595 As of 1998, the division Pinophyta was estimated to contain eight families, 68 genera, and 629 living species. Although the total number of species is relatively small, conifers are ecologically important. They are the dominant plants over large areas of land, most notably the taiga of the Northern Hemisphere, but also in similar cool climates in mountains further south. Boreal conifers have many wintertime adaptations. The ...
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Acadian Forest
The Acadians (french: Acadiens , ) are an ethnic group descended from the French who settled in the New France colony of Acadia during the 17th and 18th centuries. Most Acadians live in the region of Acadia, as it is the region where the descendants of a few Acadians who escaped the Expulsion of the Acadians (aka The Great Upheaval / ''Le Grand Dérangement'') re-settled. Most Acadians in Canada continue to live in majority French-speaking communities, notably those in New Brunswick where Acadians and Francophones are granted autonomy in areas such as education and health. Acadia was one of the 5 regions of New France. Acadia was located in what is now Eastern Canada's Maritime provinces, as well as parts of Quebec and present-day Maine to the Kennebec River. It was ethnically, geographically and administratively different from the other French colonies and the French colony of Canada (modern-day Quebec). As a result, the Acadians developed a distinct history and culture. T ...
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Musquodoboit River
The Musquodoboit River is a Canadian river located in central Nova Scotia in the northeastern part of Halifax Regional Municipality. The river is approximately in length with roughly being traversable by paddle. It has a watershed area of The name "Musquodoboit" is Mi'kmaq, roughly translated to "beautiful water". It rises in the extreme northeastern part of the county near the boundary with Pictou and Guysborough counties. Rising in the Cobequid Mountains, the river runs in a southwesterly direction along the Halifax-Colchester county line through the fertile Musquodoboit Valley; Glenmore Mountain is on the north and a series of low hills are on the south. Near the halfway point, the river changes course at a right angle, running toward the southeast where it empties into a bay on the Atlantic Ocean called Musquodoboit Harbour. other communities along its length include Middle Musquodoboit, Moose River, Elderbank, Meaghers Grant and Upper Musquodoboit. Dollar Lake flows in ...
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Drumlin
A drumlin, from the Irish word ''droimnín'' ("littlest ridge"), first recorded in 1833, in the classical sense is an elongated hill in the shape of an inverted spoon or half-buried egg formed by glacial ice acting on underlying unconsolidated till or ground moraine. Assemblages of drumlins are referred to as fields or swarms; they can create a landscape which is often described as having a 'basket of eggs topography'. The low ground between two drumlins is known as a dungeon; dungeons have colder microclimates in winter from settling cold air. Morphology Drumlins occur in various shapes and sizes, including symmetrical (about the long axis), spindle, parabolic forms, and transverse asymmetrical forms. Generally, they are elongated, oval-shaped hills, with a long axis parallel to the orientation of ice flow and with an up-ice (stoss) face that is generally steeper than the down-ice (lee) face. Drumlins are typically 250 to 1,000 meters long and between 120 and 300 meters wide ...
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Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ...
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Bedrock
In geology, bedrock is solid Rock (geology), rock that lies under loose material (regolith) within the crust (geology), crust of Earth or another terrestrial planet. Definition Bedrock is the solid rock that underlies looser surface material. An exposed portion of bedrock is often called an outcrop. The various kinds of broken and weathered rock material, such as soil and subsoil, that may overlie the bedrock are known as regolith. Engineering geology The surface of the bedrock beneath the soil cover (regolith) is also known as ''rockhead'' in engineering geology, and its identification by digging, drilling or geophysics, geophysical methods is an important task in most civil engineering projects. Superficial deposition (geology), deposits can be very thick, such that the bedrock lies hundreds of meters below the surface. Weathering of bedrock Exposed bedrock experiences weathering, which may be physical or chemical, and which alters the structure of the rock to leave ...
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Glaciation
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period ...
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Greenwood NS
Green wood is unseasoned wood. Greenwood or Green wood may also refer to: People * Greenwood (surname) Settlements Australia * Greenwood, Queensland, a locality in the Toowoomba Region * Greenwood, Western Australia, a suburb of Perth Canada * Greenwood, Calgary, Alberta, a neighbourhood * Greenwood, British Columbia, a city * Greenwood, Nova Scotia, a village * Greenwood, Halifax County, Nova Scotia, a community in the Halifax Regional Municipality * Greenwood, Durham Regional Municipality, Ontario * Greenwood, Renfrew County, Ontario United States * Greenwood, Arizona * Greenwood, Arkansas * Greenwood, El Dorado County, California * Greenwood, Glenn County, California * Greenwood, former name of Elk, Mendocino County, California * Greenwood Village, Colorado, a city * Greenwood, Delaware * Greenwood, Florida * Greenwood, Georgia * Greenwood, Idaho * Greenwood, Illinois * Mount Greenwood, Chicago, Illinois * Greenwood, Indiana * Greenwood, Wayne County, Indiana * G ...
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First Nations In Canada
First Nations (french: Premières Nations) is a term used to identify those Indigenous Canadian peoples who are neither Inuit nor Métis. Traditionally, First Nations in Canada were peoples who lived south of the tree line, and mainly south of the Arctic Circle. There are 634 recognized First Nations governments or bands across Canada. Roughly half are located in the provinces of Ontario and British Columbia. Under Charter jurisprudence, First Nations are a "designated group," along with women, visible minorities, and people with physical or mental disabilities. First Nations are not defined as a visible minority by the criteria of Statistics Canada. North American indigenous peoples have cultures spanning thousands of years. Some of their oral traditions accurately describe historical events, such as the Cascadia earthquake of 1700 and the 18th-century Tseax Cone eruption. Written records began with the arrival of European explorers and colonists during the Age of Dis ...
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