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Muskwa River
The Muskwa River flows through northern British Columbia, Canada. It is a major tributary of the Fort Nelson River - part of the Mackenzie River system. The river rises at Fern Lake in the Bedaux Pass in the Northern Rocky Mountains. From there, it flows generally east, then north, and then east again to meet with the Fort Nelson River just east of the town of Fort Nelson. The river drops approximately , its course taking it down the Rocky Mountain foothills through sub-alpine and boreal forest to meander across the forest and muskegs of the vast Liard River plains. From mouth to headwater, prominent tributaries include the Prophet River, Tuchodi River, and Gathto Creek. Much of the upper portions of this wilderness river and its watershed are located in the Northern Rocky Mountains Provincial Park, which is part of the larger Muskwa-Kechika Management Area. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort Nelson, British Columbia
Fort Nelson is a community in northeast British Columbia, Canada, within the Northern Rockies Regional Municipality (NRRM). It held town status prior to 6 February 2009, when it amalgamated with the former Northern Rockies Regional District to form the NRRM, becoming its administrative centre. The NRRM is the first regional municipality in the province. The community lies east of the northern Rocky Mountains in the Peace River region along the Alaska Highway at Mile 300. The town is approximately a four hour drive from the nearest urban centre, Fort St. John, but could potentially take six hours under winter driving conditions. The Alaska Highway both north and south of Fort Nelson is most often very well plowed in the winter and offers scenic views year round. According to the 2016 Canadian Census, the population was 3,366, a drop of 5.5% from the 2011 Census. History Fort Nelson, named in honour of the British naval hero Horatio Nelson, 1st Viscount Nelson, was establish ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort Nelson Country
A fortification is a military construction or building designed for the defense of territories in warfare, and is also used to establish rule in a region during peacetime. The term is derived from Latin ''fortis'' ("strong") and ''facere'' ("to make"). From very early history to modern times, defensive walls have often been necessary for cities to survive in an ever-changing world of invasion and conquest. Some settlements in the Indus Valley civilization were the first small cities to be fortified. In ancient Greece, large stone walls had been built in Mycenaean Greece, such as the ancient site of Mycenae (famous for the huge stone blocks of its 'cyclopean' walls). A Greek ''Towns of ancient Greece#Military settlements, phrourion'' was a fortified collection of buildings used as a military garrison, and is the equivalent of the ancient Roman, Roman castellum or English language, English fortress. These constructions mainly served the purpose of a watch tower, to guard certa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of British Columbia
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tetsa River
Tetsa River is a river in northeastern British Columbia, Canada. It heads in the Northern Rocky Mountains Provincial Park, and flows northeast and then east into the Muskwa River. In the area around Tetsa River grows mainly pine forests. The area around Tetsa River is almost uninhabited, with less than two inhabitants per square kilometre. Highway 97 / Alaska Highway [Baidu] |
Chischa River
Chischa River is a river in Canada. It is located in the province of British Columbia, in the central part of the country, 3500 km west of the capital, Ottawa. In the area around the Chischa River grows mainly Pine tree, pine forests. The area around Chischa River is almost uninhabited, with less than two inhabitants per square kilometre. The neighbourhood is part of the boreal climate zones. Annual average temperature is -1 °C. The warmest month is July, when the average temperature is 14 °C, and the coldest is January, with-16 °C.[ Chischa River] hos [ GeoNames.Org (cc-by)]; post uppdaterad 2006-01-18; databasdump nerladdad 2015-12-29 References {{authority control Rivers of British Columbia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fern Lake (British Columbia)
Fern Lake is an alpine lake in Larimer County, Colorado, United States. It is a major source for the Big Thompson River The Big Thompson River is a tributary of the South Platte River, approximately 78 miles (123 km) long, in the U.S. state of Colorado. Originating in Forest Canyon in Rocky Mountain National Park, the river flows into Lake Estes in the town .... External links * Lakes of Rocky Mountain National Park Lakes of Larimer County, Colorado {{Colorado-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peace River (Canada)
The Peace River (french: links=no, rivière de la Paix) is a river in Canada that originates in the Rocky Mountains of northern British Columbia and flows to the northeast through northern Alberta. The Peace River joins the Athabasca River in the Peace-Athabasca Delta to form the Slave River, a tributary of the Mackenzie River. The Finlay River, the main headwater of the Peace River, is regarded as the ultimate source of the Mackenzie River. The combined Finlay–Peace–Slave–Mackenzie river system is the 13th longest river system in the world. History The regions along the river are the traditional home of the Danezaa people, called the Beaver by the Europeans. The fur trader Peter Pond is believed to have visited the river in 1785. In 1788 Charles Boyer of the North West Company established a fur trading post at the river's junction with the Boyer River. In 1792 and 1793, the explorer Alexander Mackenzie travelled up the river to the Continental Divide. Mackenzie refe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muskwa Formation
The Muskwa Formation is a stratigraphical unit of Frasnian age in the Western Canadian Sedimentary Basin. It takes the name from Muskwa River, and was first described in the Western National Gas Fort Nelson a-95-J/94-J-10 well by F.F. Gray and J.R. Kassube, in 1963. Lithology The Muskwa Formation is composed of bituminous shale. Pyrite is a common accessory mineral. Gas production Gas is produced from the Muskwa Formation shales in the Horn River Basin in the Greater Sierra oil field in north-eastern British Columbia. Horizontal drilling and fracturing techniques are used to extract the gas from the low permeability shales (see ''Shale gas''). Distribution The Muskwa Formation occurs in northern Alberta, north-eastern British Columbia and in the southern part of the Northwest Territories, and typically has a thickness of . Relationship to other units The Muskwa Formation is a sub-unit of the Horn River Formation; it is conformably overlain by the Fort Simpson Formation and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Unit
A stratigraphic unit is a volume of rock of identifiable origin and relative age range that is defined by the distinctive and dominant, easily mapped and recognizable petrographic, lithologic or paleontologic features (facies) that characterize it. Units must be ''mappable'' and ''distinct'' from one another, but the contact need not be particularly distinct. For instance, a unit may be defined by terms such as "when the sandstone component exceeds 75%". Lithostratigraphic units Sequences of sedimentary and volcanic rocks are subdivided the basis of their shared or associated lithology. Formally identified lithostratigraphic units are structured in a hierarchy of lithostratigraphic rank, higher rank units generally comprising two or more units of lower rank. Going from smaller to larger in rank, the main lithostratigraphic ranks are Bed, Member, Formation, Group and Supergroup. Formal names of lithostratigraphic units are assigned by geological surveys. Units of formation or hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Rocky Mountains Provincial Park
Northern Rocky Mountains Provincial Park is a provincial park in British Columbia, Canada. It is located in the north-eastern part of the province, 90 km south-west from Fort Nelson and it is bordered to the north by the Alaska Highway. Access is mostly done by boat, aircraft, on horseback or by hiking. At 6,657.1 km2, it is the largest protected area in the Muskwa-Kechika Management Area , Muskwa-Kechika Management Area and the third largest provincial park in British Columbia. The park borders to the north-west and |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
