Peace River Geology Page The peace river 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 flows into the slave river, a tributary of the mackenzie river. the mackenzie is the 12th longest river in the world, preceded by the mekong and followed by the niger river. The peace river arch (pra) is a large cratonic uplift in northwestern alberta and northeastern british columbia. it is one of only a few large scale tectonic elements in the western canada sedimentary basin that has significantly disturbed the phanerozoic cover of the craton. the structure has influenced the location of oil and gas.
Chapter 28 Geological History Of The Peace River Arch Alberta Peace river. peace river, 1,923 km long, is one of the principal tributaries of the mackenzie river system. the name of the river refers to a settlement between cree and dane zaa (beaver) warring parties around 1781 at peace point at the lower portion of the river. the dane zaa word for the river is unchaga, meaning “big river”; the cree. Chapter 28 geological history of the peace river arch 431 devonian onian and cambrian . hope fort st. 435 . 436 . 437 . created date: 10 22 2008 1:15:47 pm. June 14, 2014. the finlay river is a 402 km long river in north central british columbia flowing north and thence south from thutade lake in the omineca mountains to williston lake, the impounded waters of the peace river formed by the completion of the w.a.c. bennett dam in 1968. prior to this, the finlay joined with the parsnip river to form. The peace river region is located in a complex structural setting within the western canadian sedimentary basin (wcsb; fig. 1). several large scale fault and graben structures (identified as.
Chapter 28 Geological History Of The Peace River Arch Alberta June 14, 2014. the finlay river is a 402 km long river in north central british columbia flowing north and thence south from thutade lake in the omineca mountains to williston lake, the impounded waters of the peace river formed by the completion of the w.a.c. bennett dam in 1968. prior to this, the finlay joined with the parsnip river to form. The peace river region is located in a complex structural setting within the western canadian sedimentary basin (wcsb; fig. 1). several large scale fault and graben structures (identified as. The peace river arch in northwestern alberta and northeastern british columbia is a cratonic uplift that was formed at a high angle to the passive margin during the late proterozoic. the arch was an asymmetrical structure, with major uplift along an east west trending fault zone at its northern edge. Bulletin of canadian petroleum geology vol. 38a (1990), r 4 24 the peace river arch in northwestern alberta and northeastern british columbia is a cratonic uplift that was formed at a high.
Comments are closed.