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Woss Lake
Woss, also commonly known as Woss Lake after the nearby lake of the same name, is a small village in the Nimpkish Valley, located southeast of Port McNeill and north of Campbell River on Highway 19, in northeastern Vancouver Island, British Columbia, Canada. The estimated population of Woss and the Nimpkish Valley is 200. The town of Woss lies about 3 km north of Woss Lake, a long, narrow lake stretching about 10 km in a primarily north-south direction with a maximum width of about one km, the southern portion of which is part of Woss Lake Provincial Park. Woss is a member municipality of the Regional District of Mount Waddington, which also includes Alert Bay, Port Alice, Port McNeill, Hyde Creek, Coal Harbour, Holberg, Malcolm Island, Quatsino and Port Hardy. Woss has regular telephone service, and acquired cellular phone services in early 2016. Woss had one elementary school for many years, that was closed up after its 2015-2016 school year. Until the mid 1960s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Designated Place
A designated place (DPL) is a type of community or settlement identified by Statistics Canada that does not meet the criteria used to define municipalities or population centres. DPLs are delineated every 5 years for the Canadian census as the statistical counterparts of incorporated places such as cities, towns, and villages. Though lacking separate municipal government, DPLs otherwise physically resemble incorporated places. They are created by provincial or territorial governments for the purpose of providing data for settled concentrated populations that are identifiable by name but are not legally incorporated under the laws of the province/territory in which they are located. The boundaries of a DPL therefore have no legal status, and not all unincorporated communities are necessarily granted DPL status. Some designated places may have a quasi-governmental status, such as a local services board in Ontario or an organized hamlet in Saskatchewan. Others may be formerly uninc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal Harbour, British Columbia
Coal is a combustible black or brownish-black sedimentary rock, formed as stratum, rock strata called coal seams. Coal is mostly carbon with variable amounts of other Chemical element, elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous (Pennsylvanian (geology), Pennsylvanian) and Permian times. Many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maritime Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, 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 planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, 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 volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, 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 flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granodiorite
Granodiorite () is a coarse-grained (phaneritic) intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. The term banatite is sometimes used informally for various rocks ranging from granite to diorite, including granodiorite. Composition According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. A greater amount of plagioclase would designate the rock as tonalite. Granodiorite is felsic to intermediate in composition. It is the intrusive igneous equivalent of the extrusive igneous dacite. It contains a large amount of sodium (Na) and calcium (Ca) rich plagioclase, potassium feldspar, quartz, and minor amounts of muscovite mica as the lighter colored mineral components. Biotite and amphiboles often in the form of hornblende are more abundant in granodiorite than in granite, giving it a more distinct two-toned or overall darker appearan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pluton
In geology, an igneous intrusion (or intrusive body or simply intrusion) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and compositions, illustrated by examples like the Palisades Sill of New York and New Jersey; the Henry Mountains of Utah; the Bushveld Igneous Complex of South Africa; Shiprock in New Mexico; the Ardnamurchan intrusion in Scotland; and the Sierra Nevada Batholith of California. Because the solid country rock into which magma intrudes is an excellent insulator, cooling of the magma is extremely slow, and intrusive igneous rock is coarse-grained (phaneritic). Intrusive igneous rocks are classified separately from extrusive igneous rocks, generally on the basis of their mineral content. The relative amounts of quartz, alkali feldspar, plagioclase, and feldspathoid is particularly important in classifying intrusive igneous rocks. Intrusions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Englewood Railway
Englewood Railway was a logging railroad on northern Vancouver Island, Canada. Headquartered in Woss, British Columbia, the line ran from Vernon Lake, through Woss, and past Nimpkish Lake Provincial Park to Beaver Cove. It was the last operating logging railroad in North America. After 100 years of use, railway operations ceased on November 7, 2017, following a deadly derailment in April of that year. History The demand for wood products during the First World War led to the construction of a pulp mill, sawmill, shingle mill and community at Beaver Cove by ''Beaver Cove Lumber & Pulp Limited'' in 1917, which in turn brought about large-scale railway logging operations in the lower Nimpkish Valley. The active logging company was ''Wood & English'' (owned by the ''Nimpkish Timber Company'') which established a logging camp ('Camp 8', later 'Nimpkish') and logging railway at the head of Nimpkish Lake. The logs cut from this area were hauled by an isolated logging railway, dumped ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beaver Cove, British Columbia
Beaver Cove is a small coastal community on Northern Vancouver Island, located on the cove of the same name. It is located at the mouth of the Kokish River, southeast of Port McNeill and up the inlet from Telegraph Cove. Background It is the northern terminus of the Englewood Railway, which is named via that of the Wood & English Logging Company, whose former logging camp, now abandoned, was Englewood, on the other side of Beaver Cove from today's community. Also nearby, to the northeast on the southeast shore of Beaver Cove, is the community of Kokish. See also *Beaver Cove (other) Beaver Cove may refer to: * Beaver Cove, Maine, U.S. * Beaver Cove (British Columbia), a cove on Vancouver Island, Canada ** Beaver Cove, British Columbia Beaver Cove is a small coastal community on Northern Vancouver Island, located on the co ... References Populated places in the Regional District of Mount Waddington Unincorporated settlements in British Columbia { ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port Hardy, British Columbia
Port Hardy is a district municipality in British Columbia, Canada located on the north-east end of Vancouver Island. Port Hardy has a population of 4,132 as of the last census (2016). It is the gateway to Cape Scott Provincial Park, the North Coast Trail and the BC Marine Trail, located on the northernmost tip of Vancouver Island. The community has access to various outdoor activities, such as kayaking, caving, scuba diving, nature viewing, surfing, saltwater rapids, fishing and camping. Port Hardy's twin city is Numata, Japan. Name Port Hardy was named after Vice-Admiral Sir Thomas Masterman Hardy, who served as the captain of ''HMS Victory''. He served at the Battle of Trafalgar when Horatio Nelson died in his arms. Demographics In the 2021 Census of Population conducted by Statistics Canada, Port Hardy had a population of 3,902 living in 1,791 of its 1,984 total private dwellings, a change of from its 2016 population of 4,132. With a land area of , it had a population ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
