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Florenceville-Bristol
Florenceville-Bristol is a town in the northwest part of Carleton County, New Brunswick, Canada. The town is located on the banks of the Saint John River. As of 2016, the population was 1,604. History Florenceville was originally known as Buttermilk Creek. In 1855 it was renamed Florenceville to honour Florence Nightingale, the famous Crimean War nurse. Florenceville was on the west side of the Saint John River and there the first post office and commercial section of the village was situated. In later years East Florenceville, previously known as Buckwheat Flats, became the commercial centre with five grocery stores and several other small businesses. There is a small strip mall along with several convenience stores and restaurants. The former village of ''Bristol'' is located on the Saint John River, in Carleton County, New Brunswick, Canada, approximately 5 kilometres north of Florenceville. It was named after the city of Bristol, England. The name replaced Kent Stat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carleton County, New Brunswick
Carleton County (2016 population 26,220) is located in west-central New Brunswick, Canada. The western border is Aroostook County, Maine, Aroostook County, Maine, the northern border is Victoria County, New Brunswick, Victoria County, and the southeastern border is York County, New Brunswick, York County from which it was formed in 1831. The Saint John River (New Brunswick), Saint John River bisects the western section of the county. The Southwest Miramichi River flows through the eastern section of the county. Potato farming is a major industry. The scenic town of Hartland, New Brunswick, Hartland is home to the longest covered bridge in the world. Transportation Major Highways * * * * * * * * * * * * * * * * * * * * Census subdivisions List of communities in New Brunswick, Communities There are five incorporated municipalities within Carleton County (listed by 2016 population): First Nations There is one First Nations reserve in Carleton County, the Woodstock_First_Na ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carleton North High School
Carleton North High School is a high school located in Florenceville-Bristol, New Brunswick. Carleton North High School is in the Anglophone West School District and one of the last schools in New Brunswick that participated in the New Brunswick Potato Picking Week.http://cnhs.nbed.nb.ca/ See also * List of schools in New Brunswick * Anglophone West School District Anglophone West is a Canadian school district in New Brunswick. Anglophone West is an Anglophone district operating 70 public schools (gr. K-12) in York, Carleton, Victoria, Madawaska and Queen's counties. Current enrollment is approximate ... References Schools in Carleton County, New Brunswick High schools in New Brunswick {{NewBrunswick-school-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
French Fries
French fries (North American English), chips (British English), finger chips ( Indian English), french-fried potatoes, or simply fries, are '' batonnet'' or ''allumette''-cut deep-fried potatoes of disputed origin from Belgium and France. They are prepared by cutting potatoes into even strips, drying them, and frying them, usually in a deep fryer. Pre-cut, blanched, and frozen russet potatoes are widely used, and sometimes baked in a regular or convection oven; air fryers are small convection ovens marketed for frying potatoes. French fries are served hot, either soft or crispy, and are generally eaten as part of lunch or dinner or by themselves as a snack, and they commonly appear on the menus of diners, fast food restaurants, pubs, and bars. They are often salted and may be served with ketchup, vinegar, mayonnaise, tomato sauce, or other local specialities. Fries can be topped more heavily, as in the dishes of poutine or chili cheese fries. French fries can be made from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Florenceville Bridge
The Florenceville Bridge is a wooden covered bridge combined with a steel trusses which crosses the Saint John River at Florenceville, New Brunswick, Canada. Built in 1907, the 46.9 metre (154 foot) bridge has one wooden Howe truss span, four steel through trusses and one plate girder span. The bridge evolved from a five span uncovered Burr Truss bridge built in 1885. One Burr span was converted to a covered Howe truss and in 1907 the others were converted to steel thru trusses. See also * List of bridges in Canada This is a list of bridges and viaducts in Canada, including those for pedestrians and vehicular traffic. Historical and architectural interest bridges There are only a few covered bridges left in Canada compared to all those that were built in t ... References Road bridges in New Brunswick Transport in Carleton County, New Brunswick Buildings and structures in Carleton County, New Brunswick Bridges over the Saint John River (Bay of Fundy) Bridges com ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2021 Canadian Census
The 2021 Canadian census was a detailed enumeration of the Canadian population with a reference date of May 11, 2021. It follows the 2016 Canadian census, which recorded a population of 35,151,728. The overall response rate was 98%, which is slightly lower than the response rate for the 2016 census. It recorded a population of 36,991,981, a 5.2% increase from 2016. Planning Consultation on census program content was from September 11 to December 8, 2017. The census was conducted by Statistics Canada, and was contactless as a result of the COVID-19 pandemic in Canada. The agency had considered delaying the census until 2022. About 900 supervisors and 31,000 field enumerators were hired to conduct the door-to-door survey of individuals and households who had not completed the census questionnaire by late May or early June. Canvassing agents wore masks and maintained a physical distance to comply with COVID-19 safety regulations. Questionnaire In early May 2021, Statistics Can ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gabbro
Gabbro () is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is chemically equivalent to rapid-cooling, fine-grained basalt. Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism. Due to its variant nature, the term ''gabbro'' may be applied loosely to a wide range of intrusive rocks, many of which are merely "gabbroic". By rough analogy, gabbro is to basalt as granite is to rhyolite. Etymology The term "gabbro" was used in the 1760s to name a set of rock types that were found in the ophiolites of the Apennine Mountains in Italy. It was named after Gabbro, a hamlet near Rosignano Marittimo in Tuscany. Then, in 1809, the German geologist Christian Leopold von Buch used the term more restrictively in his descri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ... [...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] |
Saint John River (Bay Of Fundy)
The Saint John River (french: Fleuve Saint-Jean; Maliseet-Passamaquoddy: ''Wolastoq'') is a long river that flows from Northern Maine into Canada, and runs south along the western side of New Brunswick, emptying into the Atlantic Ocean in the Bay of Fundy. Eastern Canada's longest river, its drainage basin is one of the largest on the east coast at about . A part of the border between New Brunswick and Maine follows 130 km (80 miles) of the river. A tributary forms 55 km (35 miles) of the border between Quebec and Maine. New Brunswick settlements through which it passes include, moving downstream, Edmundston, Fredericton, Oromocto, and Saint John. It is regulated by hydro-power dams at Mactaquac, Beechwood, and Grand Falls, New Brunswick. Hydronym Samuel de Champlain visited the mouth of the river on the feast day of John the Baptist in 1604 and renamed it the Rivière Saint-Jean or Saint John River in English. Many waterways in the system retain their origi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Union of Geological Sciences, Intern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
