000	00000nam##2200000za#4500
001	9.615187
003	CaOODSP
005	20230131161134
007	ta
008	150406|2000||||xxc|||||     f|0| 0 eng|d
020	|a0-660-18170-3
022	|a0068-7626
040	|aCaOODSP|beng
043	|an-cn---
086	1 |aM42-554E
110	2 |aGeological Survey of Canada.
245	10|aQuaternary geology of the Fort Fraser and Manson River map areas, central British Columbia / |cby Alain Plouffe.
260	|aOttawa - Ontario : |bNatural Resources Canada. |c2000.
300	|a62p. : |bfigs., illus., maps, references ; |c28 cm. + |emaps.
490	1 |aBulletin|x0068-7626|v554
500	|a"The Fort Fraser and Manson River map areas were last glaciated during the Late Wisconsinan Fraser Glaciation. Quaternary sediments predating this event are rare. The oldest deposits identified are oxidized sand and gravel, which locally contain placer gold. Stratigraphic evidence of a pre-Fraser glaciation was found at one site. Sediments of the Olympia Nonglacial Interval have been identified at three sites. Paleoecological reconstruction indicates climatic conditions cooler than at present for at least part of that nonglacial interval."--Abstract.
520	3 |aThe Fort Fraser and Manson River map areas were last glaciated during the Late Wisconsinan Fraser Glaciation. Quaternary sediments predating this event are rare. The oldest deposits identified are oxidized sand and gravel, which locally contain placer gold. Stratigraphic evidence of a pre-Fraser glaciation was found at one site. Sediments of the Olympia Nonglacial Interval have been identified at three sites. Paleoecological reconstruction indicates climatic conditions cooler than at present for at least part of that nonglacial interval.--Abstract
546	|aRésumés en français
563	|aSoftcover
590	|a00-46|b2000-11-17
690	07|aSedimentology|2gcpds
690	07|aGeology|2gcpds
720	1 |aPlouffe, Alain
830	#0|aBulletin,|x0068-7626|v554|w(CaOODSP)9.514768