|
Kazabazua, Quebec
Kazabazua is a village and municipality in La Vallée-de-la-Gatineau Regional County Municipality, Quebec, Canada. The village is about halfway between Maniwaki and Hull at the intersection of Route 105 and Route 301, just west of the Gatineau River. The village and municipality are named after the Kazabazua River which passes through it. Like many other First Nations names, Kazabazua has had many spellings in English, such as Kazaluzu, Kasubasua, Cazabasua, Cazibazouis, Cazebalzuac, Cajibajouis. This word comes from the Algonquin word ''kachibadjiwan'', from ''kach'' ("hidden") and ''djiwan'' ("current"), hence it means "underground river". This name is a reflection of the local topography because the Kazabazua River disappears underground and resurfaces a few dozen metres (yards) downstream. The river then flows through rapids and passes under a natural stone bridge. The communities of Kazabazua Station, Aylwin, and Aylwin Station are also located within the municipality. G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Municipality (Quebec)
The following is a list of the types of local and supralocal territorial units in Quebec, including those used solely for statistical purposes, as defined by the Ministry of Municipal Affairs, Regions and Land Occupancy and compiled by the Institut de la statistique du Québec. Not included are the urban agglomerations in Quebec, which, although they group together multiple municipalities, exercise only what are ordinarily local municipal powers. A list of local municipal units in Quebec by regional county municipality can be found at List of municipalities in Quebec. Local municipalities All municipalities (except cities), whether township, village, parish, or unspecified ones, are functionally and legally identical. The only difference is that the designation might serve to disambiguate between otherwise identically named municipalities, often neighbouring ones. Many such cases have had their names changed, or merged with the identically named nearby municipality since t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Area Code 819
Area codes 819 and 873 are telephone area codes in the North American Numbering Plan (NANP) for central and western Quebec, Canada, including the Quebec portion of the National Capital Region, and the Hudson Strait and Ungava Bay coastlines of Quebec. Major cities in the territory include Gatineau, Sherbrooke, Trois-Rivières, Drummondville, Shawinigan, Victoriaville, Rouyn-Noranda, Val-d'Or, Magog and Mont-Laurier. The incumbent local exchange carriers in 819/873 are Bell Canada, Bell Aliant, Telus, as well as Télébec and other independent companies. From 1992 to 1997, Northwestel was also an incumbent carrier in 819, as it included former Bell Canada areas in the Northwest Territories. Area code 468 is reserved as a third area code in the region. History Ontario and Quebec were the only Canadian provinces that received assignments of multiple area codes by the American Telephone and Telegraph Company (AT&T) when the original North American area codes were created in 1947. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Algonquin People
The Algonquin people are an Indigenous people who now live in Eastern Canada. They speak the Algonquin language, which is part of the Algonquian language family. Culturally and linguistically, they are closely related to the Odawa, Potawatomi, Ojibwe (including Oji-Cree), Mississauga and Nipissing, with whom they form the larger Anicinàpe (Anishinaabeg). Algonquins call themselves Omàmiwinini (plural: Omàmiwininiwak) or the more generalised name of Anicinàpe. Though known by several names in the past, such as ''Algoumequin'', the most common term "Algonquin" has been suggested to derive from the Maliseet word (): "they are our relatives/allies." The much larger heterogeneous group of Algonquian-speaking peoples, who, according to Brian Conwell, stretch from Virginia to the Rocky Mountains and north to Hudson Bay, was named after the tribe. Most Algonquins live in Quebec. The nine recognized status Algonquin bands in that province and one in Ontario have a combined ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Champlain Sea
The Champlain Sea (french: Mer de Champlain) was a prehistoric inlet of the Atlantic Ocean into the North American continent, created by the retreating ice sheets during the closure of the last glacial period. The inlet once included lands in what are now the Canadian provinces of Quebec and Ontario, as well as parts of the American states of New York and Vermont. Origins The mass of ice from the continental ice sheets had depressed the rock beneath it over millennia. At the end of the last glacial period, while the rock was still depressed, the Saint Lawrence and Ottawa River valleys, as well as modern Lake Champlain, at that time the Lake Vermont, were below sea level and flooded with rising worldwide sea levels, once the ice no longer prevented the ocean from flowing into the region. As the land gradually rose again, in the process known as isostatic rebound, the sea coast gradually retreated to its current location. The sea lasted from about 13,000 years ago to about ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Arch
A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, rivers or weathering ( subaerial processes). Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over geologic time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on opposite sides of the formation beneath the relatively harder stratum, or caprock, above it. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, thus creating an arch. The erosional processes exploit weaknesses in the softer rock layers making cracks larger and removing material more quickly than the caprock; however, the caprock itself continues to er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grossular Garnet
Grossular is a calcium-aluminium species of the garnet group of minerals. It has the chemical formula of Ca3Al2(SiO4)3 but the calcium may, in part, be replaced by ferrous iron and the aluminium by ferric iron. The name grossular is derived from the botanical name for the gooseberry, ''grossularia'', in reference to the green garnet of this composition that is found in Siberia. Other shades include cinnamon brown (cinnamon stone variety), red, and yellow. Grossular is a gemstone. In geological literature, grossular has often been called ''grossularite''. Since 1971, however, use of the term grossularite for the mineral has been discouraged by the International Mineralogical Association. Hessonite Hessonite or "cinnamon stone" is a common variety of grossular with the general formula: Ca3Al2Si3O12. The name comes from the grc, ἣσσων (hēssōn), meaning ''inferior''; an allusion to its lower hardness and lower density than most other garnet species varieties. It has a chara ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grenville Orogeny
The Grenville orogeny was a long-lived Mesoproterozoic mountain-building event associated with the assembly of the supercontinent Rodinia. Its record is a prominent orogenic belt which spans a significant portion of the North American continent, from Labrador to Mexico, as well as to Scotland. Grenville orogenic crust of mid-late Mesoproterozoic age (c. 1250–980 Ma) is found worldwide, but generally only events which occurred on the southern and eastern margins of Laurentia are recognized under the "Grenville" name. These orogenic events are also known as the Kibaran orogeny in Africa and the Dalslandian orogeny in Western Europe. Timescale The problem of timing the Grenville orogeny is an area of some contention today. The timescale outlined by Toby Rivers in 2008 is derived from the well-preserved Grenville Province and represents one of the most detailed records of the orogeny. This classification considers the classical Grenville designation to cover two separate oro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gatineau River
The Gatineau River (french: Rivière Gatineau, ) is a river in western Quebec, Canada, which rises in lakes north of the Baskatong Reservoir and flows south to join the Ottawa River at the city of Gatineau, Quebec. The river is long and drains an area of . While it has been said that the river's name comes from Nicolas Gatineau (sometimes spelled Gastineau), a fur trader who is said to have drowned in the river in 1683, the original inhabitants, the Algonquin Anicinabek, assert that the name comes from their language. The name they give the river is "''Te-nagàdino-zìbi''", which means "The River that Stops ne's Journey. Geography The geography of the area was altered with the construction of the Baskatong Reservoir, and it is still possible to travel upstream on the Gatineau and reach a point where a small portage leads to the headwaters of the Ottawa River. The Ottawa River then flows northwest and turns south where it eventually flows more easterly and connects with th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quebec Route 301
Route 301 is an provincial highway located in the Outaouais region in western Quebec. The route serves as a direct connection between the Pontiac region and the Upper Gatineau region. The 82-kilometer route runs from the end of Ontario Highway 653 near Portage-du-Fort and joins Route 148 for a stretch up to Campbell's Bay where it continues eastward and ends in Kazabazua at the junction of Route 105. Municipalities along Highway 301 * Portage-du-Fort * Bryson * Litchfield * Campbell's Bay * Thorne * Otter Lake * Alleyn-et-Cawood * Kazabazua Major intersections See also * List of Quebec provincial highways References External links Provincial Route Map (Courtesy of the Quebec Ministry of Transportation) Route 301on Google Maps 301 __NOTOC__ Year 301 (Roman numerals, CCCI) was a common year starting on Wednesday (link will display the full calendar) of the Julian calendar. At the time, it was known as the Year of the Consulship of Postumius and Nepotia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quebec Route 105
Route 105 is a north-south highway in Quebec, Canada. It runs from Hull, Quebec, Hull (now part of Gatineau), where it is known as Boulevard Saint-Joseph (until the limits with Chelsea, Quebec, Chelsea), to Grand-Remous, Quebec, Grand-Remous where it ends at Quebec Route 117, Route 117. Route 105 runs mostly in the Gatineau River valley, where it is characterized by twisty and hilly sections. Besides Hull, the only other significant town along the route is Maniwaki, Quebec, Maniwaki. Originally part of the former Route 11, it was renumbered to 105 in the 1970s, and runs parallel to Quebec Autoroute 5, Autoroute 5 in the Gatineau area. Municipalities along Route 105 * Gatineau * Chelsea, Quebec, Chelsea * La Pêche, Quebec, La Pêche (''Wakefield, Quebec, Wakefield / Alcove, Quebec, Alcove / Farrellton, Quebec, Farrellton'') * Low, Quebec, Low * Kazabazua, Quebec, Kazabazua * Wright, Quebec, Wright * Gracefield, Quebec, Gracefield * Bouchette, Quebec, Bouchette * Messines, Quebe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Karst")
