2 edition of Gething Formation at Peace River Canyon, British Columbia (Report and 1 Figure). found in the catalog.
Gething Formation at Peace River Canyon, British Columbia (Report and 1 Figure).
Geological Survey of Canada.
|Series||Paper (Geological Survey of Canada) -- 68-28|
Travel info for Peace River/Alaska Highway. Trails in this area.. This region of Northern British Columbia borders Alberta to the east and both the Yukon and Northwest Territories to the north. Much of it lies on the east side of the Rocky Mountains. Rolling plains, mountains high, rushing rivers and streams and miles of forests make up the Peace River/Alaska Highway, where wilderness areas. CHETWYND, B.C. — Yet another dinosaur trackway has been discovered at a coal mine in the South Peace. The discovery was made back on August 18th by the Bru.
At Peace River Canyon rock. of the 'lower' Gething Rivers 'lower' Gething rocks are overlain by silty sedimentary rocks of the Formation, these Formation are overlain by mudstone of the Moorebar Formation. The top of the 'lower' Gething Formation is in sharp contact with a pebbly and (Ilauconitic marker unit. OCLC Number: Notes: Part of illustrative matter in pocket. Abstract in French. Description: pages illustrations 25 cm. Contents: In Pocket: Gething Formation at Peace River Canyon, British Columbia --Figure ar sections of Bullhead Group, illuminating variations in lithologies, facies and thinknesses between Bullmoose Mountain and Prophet River --Figure 8.
The most complete section is found in the type locality of the Gething Formation in the Peace River Canyon immediately downstream from the W. A. C. Bennett Dam. Relationship to other units. The Bullhead Group overlies a major regional unconformity caused by pre-Bullhead erosion. Dinosaur footprints were first discovered in the Peace River Canyon of British Columbia in (McLearn ). Expeditions by the National Museum of Canada in (Sternberg ), the Royal Ontario Museum , , ) have recovered dinosaur footprints throughout the metres of strata of the Gething Formation (Aptian-Albian.
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Gething Formation is a stratigraphic unit of Lower Cretaceous age in the Western Canada Sedimentary Basin. It is present in northeastern British Columbia and western Alberta, and includes economically important coal deposits. The formation is named for Gething Creek, a right tributary of the Peace River west of Hudson's Hope, and the nearby Gething Mountain.
It was first described by F.H. McLearn in in the Peace River Canyon. Get this from a library. The Gething Formation at Peace River Canyon, British Columbia. [Donald F Stott]. ABSTRACT. A large slab of arenaceous siltstone was collected from strata of the Gething Formation (Aptian, Lower Cretaceous) in the Peace River Canyon of northeastern British Columbia, Canada.
More than footprints between and cm in length were found on a single bedding plane within the slab. These were made by a minimum of four individuals that apparently were feeding.
Author of The Mesozoic of Middle North America, Fernie and minnes strata north of Peace River, The Gething Formation at Peace River Canyon, British Columbia, Jurassic and cretaceous stratigraphy bewtween Peace and Tetsa Rivers, Lower Cretaceous Bullhead and Fort St.
John Groups, Cretaceous rocks in the region of Liard and Mackenzie Rivers, Northwest Territories, The Cretaceous Smoky group, Rocky Mountain foothills, Alberta and British Columbia. The thickness of the Gething Form-ation in the Peace River Canyon is believed to be approximately 1, feet to 1, feet.A detailed description of the Gething Formation of the Peace River Canyon area has been published by St&t, It is the coal beds of the Gething Formation that are the objective of the coal.
explora. Monteith and Beattie Peaks Formations In and near the Peace River Canyon, the Monteith Formation has been mapped by Hughes () on Grant Knob. Although not mapped as such,ly forms part of the undifferentiated pre-Gething strata on Mount Johnson on the south side of the Peace River.
A detailed description of the Gething formation of the Peace River Canyon area has been published by Stott. It is the coal of the Gething formation that are the objective of the coal exploration being carried out in the Peace River area. Columbosauripus ungulatus Sternberg is identified from the Dunvegan Formation, Cenomanian (early Upper Cretaceous) of East Pine, northeastern British Columbia.
The species was originally reported from the Gething Formation, Albian (late Lower Cretaceous) of Peace River canyon, British Columbia. A detailed description of the Gething Formation of the Peace River Canyon area has been published by Stott, It is the coal beds of the Gething Formation that are the objective of the coal exploration activities being carried out in the Peace River area.
The northeastern British Columbia deposits are in the Foothills and Plains coalfields, together known as the Peace River coalfields. The Foothills coalfield extends for km along the eastern flank of the Rocky Mountains. The coals are distributed through a stratigraphic interval of more than m, and are hosted by five Lower Cretaceous units, the most important of which are the Gates Formation (Fort St.
John Group) and the Gething Formation. feature of the Gething formation. The thickness of the- Gething formation in the Peace River Canyon area is believed to be approximately '.A detailed description of the Gething formation of the Peace River Canyon area has been published by Stott.
The Peace River Formation is 60 feet (20 m) thick on average. The formation has different extents at different stages, with the Paddy Member present only in the Peace River Country in northern Alberta south of Clear Hills, while the Cadotte Member and the Harmon Member occur in both Alberta and north-eastern British Columbia.
Physiography. Type specimen: NMCa footprint. Its type locality is miles upstream from Gething's mine, Peace River Canyon, which is in an Albian terrestrial sandstone/coal in the Gething Formation of Canada. Ecology: ground dwelling carnivore.
Northeastern British Columbia has a long history of vertebrate footprint discoveries and research dating back as early as the s. Initially, the majority of the research attention went to the large-scale in situ track exposures in the Gething Formation (Lower Cretaceous: Aptian/Albian) exposed along the Peace River Canyon near the town of Hudson’s Hope (Sternberg, ; Currie, ).
Type specimen: BCPMPMA P (now RTMP), a footprint. Its type locality is north shore, Peace River Canyon, which is in an Aptian terrestrial siltstone in the Gething Formation of Canada. Ecology: ground dwelling carnivore.
Its type locality is 2 miles upstream from Gething's mine, Peace River Canyon, which is in an Albian terrestrial sandstone/coal in the Gething Formation of Canada.
Ecology: ground dwelling herbivore Full reference: C. Sternberg. Dinosaur tracks from Peace River, British Columbia. National Museum of Canada Bulletin the head of Peace River canyon, 20 miles below Gold Bar, by way of Gething Creek and mentioned above.
the area, but this trail was probably almost completely destroyed by the forest fires vicinity of the Peace River. This formation has been intensively studied by E’. McLearn, British Columbia.” sion, but fossils are common, and. Type specimen: NMCa footprint.
Its type locality is miles upstream from Gething's mine (B), Peace River Canyon, which is in an Albian terrestrial sandstone/claystone in the Gething Formation of Canada. Ecology: ground dwelling carnivore.
The Peace River (French: rivière de la Paix) is a 1,kilometre-long (1, mi) river in Canada that originates in the Rocky Mountains of northern British Columbia and flows to the northeast through northern Peace River joins the Athabasca River in the Peace-Athabasca Delta to form the Slave River, a tributary of the Mackenzie Finlay River, the main headwater of the.
site was unprecedented for British Columbia for its size as well as the the Gaylard Member of the Gething Formation, which were deposited footprint sites from the Peace River Canyon near.
The first vertebrate ichnofauna from the Cretaceous was described in by C.M. Sternberg, based on specimens collected from the Peace River Canyon in northeastern British Columbia.Head east from Chetwynd and drive over the Kiskatinaw Bridge, one of the only timber trestle bridges still in use in British Columbia.
It is also one of the most unusual, curving nine degrees along its metre (foot) length. Kiskatinaw Provincial Park, situated right beside the bridge, provides tent sites for camping and river access.Abstract. Fragmentary but associated dinosaur bones collected in from the Pine River of northeastern British Columbia are identified here as originating from an ankylosaur.
The specimen represents only the second occurrence of dinosaur skeletal material from the Cenomanian Dunvegan Formation and the first from Dunvegan outcrops in the province of British Columbia.