ⓘ Trout River Formation. The Trout River Formation is a stratigraphical unit of Late Devonian age in the Western Canadian Sedimentary Basin. It takes the name fro ..

                                     

ⓘ Trout River Formation

The Trout River Formation is a stratigraphical unit of Late Devonian age in the Western Canadian Sedimentary Basin.

It takes the name from the Trout River, and was first described on the banks of the river, 35 kilometres 22 mi upstream from the Mackenzie River, by C.H. Crickmay in 1953.

                                     

1. Lithology

The Trout River Formation is composed bedded limestone top, silty limestone and shale middle, silty limestone and calcareous siltstone base.

Brachiopod and coral paleo-fauna can be found in outcrops.

                                     

2. Distribution

The Trout River Formation reaches a maximum thickness of 91 metres 300 ft. It occurs in the District of Mackenzie in outcrop and dips south into the Fort Nelson area in north-eastern British Columbia.

                                     

3. Relationship to other units

The Trout River Formation is conformably overlain by the Tetcho Formation and disconformably overlays the Kakisa Formation. In its western extent, it overlies and grades into the Fort Simpson Formation.

It is equivalent to the Sassenach Formation in the central Alberta Rockies, with the Graminia Formation in central Alberta, the Crowfoot Formation in southern Alberta, the Torquay Formation in Saskatchewan and Lyleton Formation in Manitoba.

                                     
  • gives the name to the Trout River Formation a stratigraphical unit of the Western Canadian Sedimentary Basin. The Trout River originates in Sambaa K e at
  • Mackenzie River and was first described in outcrop on the banks of the Trout River by H.R. Belyea and D.J. McLaren in 1962. The Kakisa Formation is composed
  • the Imperial Island River No. 1 well located south of Trout Lake by H.R. Belyea and D.J. McLaren in 1962. The Tetcho Formation is composed of fine grained
  • River, a tributary of the Mackenzie River and was first described in the banks of the Trout River north of Trout Lake, Northwest Territories, at Table
  • Simpson Formation is overlain by the Jean Marie Member of the Redknife Formation in its eastern reaches, and progressively by the Kakisa Formation Trout River
  • Trout River is a small rural fishing village located on the southern coastal edge of Gros Morne National Park in Newfoundland. Trout River was settled
  • empties again. Trout Pond and its sinkhole are karst features. They are underlain by strata of Tonoloway Limestone and the Helderberg Formation The facilities
  • Poudre River contains abundant populations of self - sustaining wild trout The vast majority of trout that live within the river system are brown trout The
  • of Trout Run are over rock of the Catskill Formation The stream s upper reaches lie over the Huntley Mountain Formation The lower reaches of Trout Run
  • these formations guide local prospectors to ammolite deposits. The Oldman River contains fish species such as rainbow trout cutthroat trout bull trout brown
  • Mauch Chunk Formation occurs in this valley. The valley is known as Brush Valley. A dam known as the Trout Run Dam Number 4 is located on Trout Run. As of


                                     
  • Carolina, is located in the Southern Nantahala Wilderness. Coleman River is a designated trout stream, and a portion of it is further designated by the Wildlife
  • Trout Creek Hill is a small Pleistocene basaltic shield volcano in Washington, United States. Located in Skamania County, Trout Creek Hill rises to an
  • of trout It was designated as an American Heritage River in 1997. The Lackawanna River begins at the confluence of the East Branch Lackawanna River and
  • Department in Inland Fisheries and Wildlife stocks the river with brook trout and brown trout Pleasant River is the only known brook floater habitat in southern
  • Migratory Fishery, as well as Class A Wild Trout Waters. A total of 13 species, including brook trout and brown trout inhabit the creek. Lewis Creek begins
  • branches, the South Thompson River and the North Thompson River The river is home to several varieties of Pacific salmon and trout The area s geological history
  • clear. Chalk streams are popular with fly fishermen who fish for trout on these rivers Chalk is a highly porous and permeable rock and rain falling onto
  • quality of life, and economic vitality of the Jefferson River watershed. Trout Unlimited - Trout Unlimited s mission is to conserve, protect and restore
  • sea trout shad, perch, American eels, stripped bass, mackerel, herring, brook trout speckled trout minnows and smelts. Consequently, the river is popular
  • branched bur - reed. Freshwater fish, found include specifically the brown trout grayling and bullhead. To support the fish population there is a rich diversity
                                     
  • short river once supported relatively large stocks of salmon, sea trout and brown trout but their populations have dwindled since the 1940s. The River Yealm
  • Juniata River 2 km northeast of Bellwood, Pennsylvania Blue Rock, and other large outcroppings, in the Smoke Hole Canyon of eastern West Virginia Trout Pond
  • sandstone cliff formation Seneca Creek is popular destination for anglers, hikers, and backpackers. In 1999 it was named one of the 100 best trout streams in
  • The Trout Creek Mountains are a remote, semi - arid Great Basin mountain range mostly in southeastern Oregon and partially in northern Nevada in the United
  • entirely over sandstone rocks of the Clarens Formation The Kraai is fishable, containing rainbow trout brown trout and smallmouth yellowfish. In 1881 a sandstone
  • Kase Run, Mauses Creek, and Sechler Run. Mahoning Creek is designated as a Trout - Stocking Fishery and a Migratory Fishery for part of its length and as a
  • sharing the same habitat as imported trout species and living in an area between the Olifants and the Keurbooms River Although in South Africa this relatively
  • The Horn River Formation also Horn River Shale is a stratigraphic unit of Devonian early Givetian to late Frasnian age in the Western Canadian Sedimentary
  • Pennsylvania Wild Trout Waters Natural Reproduction PDF p. 46, retrieved April 5, 2015 93.9j. Drainage List J. Susquehanna River Basin in Pennsylvania


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