Cobequid Hills
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Cobequid Hills
The Cobequid Mountains, also sometimes referred to as the Cobequid Hills, is a Canadian mountain range located in Nova Scotia in the mainland portion of the province. Geologic history Geologically, the Cobequid Mountains are considered part of the Appalachians. The range stretches from Cape Chignecto in Cumberland County in the west through to Pictou County in the east. The Cobequid Mountains trace their geologic history to the Precambrian and Devonian ages; consequently the mountains are composed of a combination of sediments, granites, and volcanic rock all of which has been crushed and folded by continental drift when this part of Nova Scotia was located at the centre of the Pangea supercontinent. Subsequent erosion over millions of years has resulted in the present-day low range of mountains and rolling hills. The part of northern Nova Scotia which contains the Cobequid Mountains is believed to have been linked with what is now northern Europe. Its collision with a section ...
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Canso, Nova Scotia
Canso is a community in Guysborough County, on the north-eastern tip of mainland Nova Scotia, Canada, next to Chedabucto Bay. In January 2012, it ceased to be a separate town and as of July 2012 was amalgamated into the Municipality of the District of Guysborough. The area was established in 1604, along with the original Port-Royal. The British construction of a fort in the village (1720), was instrumental in contributing to Dummer's War (1722–1725). The town is of national historic importance because it was one of only two British settlements in Nova Scotia prior to the establishment of Halifax (1749). Canso played a key role in the defeat of Louisbourg. Today, the town attracts people internationally for the annual Stan Rogers Folk Festival. Geography The community is located on the southern shore of Chedabucto Bay. The southern limit of the bay is at Cape Canso, a headland approximately southeast of the community. Canso is the southeastern terminus of Trunk 16, an ...
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Autumn Leaf Color
Autumn leaf color is a phenomenon that affects the normal green leaves of many deciduous trees and shrubs by which they take on, during a few weeks in the autumn season, various shades of yellow, orange, red, purple, and brown. The phenomenon is commonly called autumn colours or autumn foliage in British English and fall colors, fall foliage, or simply foliage in American English. In some areas of Canada and the United States, " leaf peeping" tourism is a major contribution to economic activity. This tourist activity occurs between the beginning of color changes and the onset of leaf fall, usually around September and October in the Northern Hemisphere and April to May in the Southern Hemisphere. Chlorophyll and the green/yellow/orange colors A green leaf is green because of the presence of a pigment known as chlorophyll, which is inside an organelle called a chloroplast. When abundant in the leaf's cells, as during the growing season, the chlorophyll's green color domi ...
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Yellow Birch
''Betula alleghaniensis'', the yellow birch, golden birch, or swamp birch, is a large tree and an important lumber species of birch native to northeastern North America. Its vernacular names refer to the golden color of the tree's bark. In the past the species name was ''Betula lutea''. ''Betula alleghaniensis'' is the provincial tree of Quebec, where it is commonly called ''merisier'', a name which in France is used for the wild cherry. Description It is a medium-sized, typically single stemmed, deciduous tree reaching tall (exceptionally to ) with a trunk typically in diameter, making it the largest North American species of birch. Yellow birch is long-lived, typically 150 years and some old growth forest specimens may last for 300 years. It mostly reproduces by seed. Mature trees typically start producing seeds at about 40 years but may start as young as 20. The optimum age for seed production is about 70 years. Good seed crops are not produced every year, and tend to be ...
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Sugar Maple
''Acer saccharum'', the sugar maple, is a species of flowering plant in the soapberry and lychee family Sapindaceae. It is native to the hardwood forests of eastern Canada and eastern United States. Sugar maple is best known for being the primary source of maple syrup and for its brightly colored fall foliage. It may also be known as "rock maple", "sugar tree", "birds-eye maple", "sweet maple", "curly maple", or "hard maple", particularly when referring to the wood. Description ''Acer saccharum'' is a deciduous tree normally reaching heights of , and exceptionally up to . A 10-year-old tree is typically about tall. As with most trees, forest-grown sugar maples form a much taller trunk and narrower canopy than open-growth ones. The leaf, leaves are deciduous, up to long and wide, palmate, with five lobes and borne in opposite pairs. The basal lobes are relatively small, while the upper lobes are larger and deeply notched. In contrast with the angular notching of the silver ...
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Geologic Fault
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ...
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Fundy Basin
The Fundy Basin is a sediment-filled rift basin on the Atlantic coast of southeastern Canada. It contains three sub-basins; the Fundy sub-basin, the Minas Basin and the Chignecto Basin. These arms meet at the Bay of Fundy, which is contained within the rift valley. From the Bay of Fundy, the Minas Basin trends northeast to Nova Scotia. Chignecto Bay runs from the Bay of Fundy northwest between New Brunswick and Nova Scotia which is separated from the waters of the Northumberland Strait by the Isthmus of Chignecto. The Fundy Basin is best known for the bay it contains. The Bay of Fundy is home to huge tidal changes and tidal bores. It is part of the system of Eastern North America Rift Basins. Approximately 220 million years ago, during the late Triassic period, the supercontinent Pangaea began to break apart. The focus of the rifting began somewhere between where present-day eastern North America and north-western Africa were joined. As the rift began to separate from mainland No ...
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Escarpment
An escarpment is a steep slope or long cliff that forms as a result of faulting or erosion and separates two relatively level areas having different elevations. The terms ''scarp'' and ''scarp face'' are often used interchangeably with ''escarpment''. Some sources differentiate the two terms, with ''escarpment'' referring to the margin between two landforms, and ''scarp'' referring to a cliff or a steep slope. In this usage an escarpment is a ridge which has a gentle slope on one side and a steep scarp on the other side. More loosely, the term ''scarp'' also describes a zone between a coastal lowland and a continental plateau which shows a marked, abrupt change in elevation caused by coastal erosion at the base of the plateau. Formation and description Scarps are generally formed by one of two processes: either by differential erosion of sedimentary rocks, or by movement of the Earth's crust at a geologic fault. The first process is the more common type: the escarpment is a t ...
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Northumberland Strait
The Northumberland Strait (French: ''détroit de Northumberland'') is a strait in the southern part of the Gulf of Saint Lawrence in eastern Canada. The strait is formed by Prince Edward Island and the gulf's eastern, southern, and western shores. Boundaries The western boundary of the strait is delineated by a line running between North Cape, Prince Edward Island and Point Escuminac, New Brunswick while the eastern boundary is delineated by a line running between East Point, Prince Edward Island and Inverness, Nova Scotia. Hydrography The Northumberland Strait varies in depth between 17 and 65 metres, with the deepest waters at either end. The tidal patterns are complex; the eastern end has the usual two tides per day, with a tidal range of 1.2 to 1.8 metres, while the western end effectively has only one tide per day. The strait's shallow depths lend to warm water temperatures in summer months, with some areas reaching 25° C, or 77° F. Consequently, the strait is repo ...
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Dalhousie Mountain
__NOTOC__ Dalhousie Mountain is a Canadian peak in the Cobequid Mountains and the highest elevation point in Pictou County, Nova Scotia. Located north of Trunk 4 west of Salt Springs, the peak is accessible by vehicle using gated roads and is topped by wind turbines and a forest fire surveillance tower. Wind farm The Dalhousie Mountain Wind Farm was constructed in 2009 at a cost of $130 million and consists of 34 wind turbines with an installed capacity of 51 MW. The turbines are clustered in the vicinity of Dalhousie Mountain as well as on the peak itself. The wind farm is owned by RMSenergy Ltd and is operated as Dalhousie Mountain Wind Farm Operating Limited Partnership. See also * List of highest points of Canadian provinces and territories This is a list of the highest points of the Canadian provinces and territories, by height. ;Notes *Fairweather Mountain is the officially gazetted name, but Mount Fairweather is the common usage. Mount Fairweather is on the boundar ...
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Nuttby Mountain
Nuttby Mountain is a Canadian peak in the Cobequid Mountains and at 360.6 metres is one of the highest elevation points on the mainland portion of Nova Scotia. Its longstanding claim to be the highest peak was disproven in 2017 when it was discovered that Higgins Mountain near Folly Lake is 363.7 metres and an unnamed peak near Hart Lake is 365.02 metres. Located west of Route 311 in Colchester County some 20 km north of Truro, the peak is accessible by vehicle using a gated road and is topped by telecommunication towers. A fire lookout tower stood there from 1937 to 2013. A 45-megawatt wind farm was constructed on a 400-acre site on the mountain in 2010. As of 2017 Nova Scotia Power owned 22 Enercon E82 turbines on the site with a total capacity of 50.6 MW. See also * List of highest points of Canadian provinces and territories * Nuttby, Nova Scotia Nuttby is a community in Colchester County, Nova Scotia Nova Scotia ( ; ; ) is one of the thirteen provinces ...
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Higgins Mountain
__NOTOC__ Higgins may refer to: People * Higgins (surname), including list of people with the surname (see also Ó hUiginn) Places * Higgins, Australian Capital Territory, a suburb in the Canberra district of Belconnen * Higgins, North Carolina, populated place in Yancey County, North Carolina, USA * Higgins, Texas, city in Lipscomb County, Texas, USA * Higgins Township, Michigan, USA * Higgins Beach, small beach in Maine, USA * Higgins Field, a World War II airbase on the northern tip of Cape York Peninsula in Queensland, Australia * Higgins Lake, in Michigan, USA * Division of Higgins, Australian Electoral Division in Victoria Other * Higgins (dog), trained dog actor in ''Benji'' and ''Petticoat Junction'' * Higgins boat, or LCVP, a landing craft used in amphibious warfare * Higgins Industries, a US firm that manufactured the Higgins boat * Higgins project, an open source framework for user-centric identity management * Higgins Armory Museum, in Worcester, Massachusetts, ...
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