1-10 OF 10 RESULTS FOR

Necoslie River

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 February 1997
Canadian Journal of Earth Sciences (1997) 34 (2): 200–208.
...A. Plouffe; H. Jetté Abstract At two sites in central British Columbia, sediments with dispersed organic matter, underneath Fraser Glaciation deposits, are interpreted as nonglacial deposits of Middle Wisconsinan age (Olympia Nonglacial Interval). At Necoslie River, undated sand with dispersed...
Image
Location of the study area in British Columbia (shaded). The box delineates...
Published: 01 May 2001
Fig. 1. Location of the study area in British Columbia (shaded). The box delineates Fig.  2 . Sites referred in the text (▲) where sediments of the Olympia Nonglacial Interval are exposed include: 1, Babine Lake ( Harington et al. 1974 ); 2, Chuchi Lake ( Harington et al. 1996 ); 3, Necoslie
Image
Maps showing (A) approximate distribution of Cache Creek Terrane in souther...
Published: 01 May 2001
, eastern limit of Cordilleran deformation; FSJ, Fort St. James; P, Mt. Pope; N, Necoslie River; V, Vancouver. Base maps for A and B after Gabrielse et al. ( 1992 ) and Bellefontane et al. (1995), respectively.
Journal Article
Published: 04 May 2001
Canadian Journal of Earth Sciences (2001) 38 (4): 551–578.
... of the mountain; between Stuart and Pinchi Lakes; and between Necoslie River and Spad Lake (Figs.  1 , 2 ). Locally, the limestone shows bedding generally defined by accumulations of limestone fragments and bioclasts (crinoids and fusulinaceans). Some of these accumulations may be debris flows and turbidites...
FIGURES | View All (12)
Journal Article
Published: 01 May 2001
Canadian Journal of Earth Sciences (2001) 38 (4): 733–749.
... pollen (65%), mainly Artemisia (32%) and Poaceaew (31%), with lesser tree and shrub pollen (34%), mainly Pinus (13%), Betula (12%), and Picea (6%). A similar assemblage but with less Pinus and Picea tree pollen was found in subtill fluvial sediments at the Necoslie River site, located about 20...
FIGURES | View All (7)
Journal Article
Published: 01 May 2001
Canadian Journal of Earth Sciences (2001) 38 (4): 719–731.
...Fig. 1. Location of the study area in British Columbia (shaded). The box delineates Fig.  2 . Sites referred in the text (▲) where sediments of the Olympia Nonglacial Interval are exposed include: 1, Babine Lake ( Harington et al. 1974 ); 2, Chuchi Lake ( Harington et al. 1996 ); 3, Necoslie...
FIGURES | View All (9)
Journal Article
Published: 01 May 2001
Canadian Journal of Earth Sciences (2001) 38 (4): 751–765.
... the Necoslie River (200 km northeast; Plouffe and Jetté 1997 ) and Chelaslie Arm of the Nechako Reservoir (10 km southwest; Levson et al. 1998 , 1999 ; see Fig.  1 for location). At all three sites, fine sands containing finely disseminated organics within stratified silts and clays underlie advance-phase...
FIGURES | View All (10)
Journal Article
Published: 01 May 2001
Canadian Journal of Earth Sciences (2001) 38 (4): 535–550.
..., eastern limit of Cordilleran deformation; FSJ, Fort St. James; P, Mt. Pope; N, Necoslie River; V, Vancouver. Base maps for A and B after Gabrielse et al. ( 1992 ) and Bellefontane et al. (1995), respectively. ...
FIGURES | View All (12)
Journal Article
Published: 01 November 2023
Journal of Paleontology (2023) 97 (6): 1161–1191.
... during 1983 field work with E.T. Tozer in the Toad–Liard River area. Follow-up fieldwork along the Alaska Highway by the present authors in 2011 yielded supplementary collections from locations that underpin parts of the standard Canadian ammonoid biochronology (Tozer, 1967 , 1994 ). Upper Anisian...
FIGURES | View All (15)
Journal Article
Published: 07 January 2016
Canadian Journal of Earth Sciences (2016) 53 (3): 304–320.
.... 1997 . Middle Wisconsinan sediments and paleoecology of central British Columbia: sites at Necoslie and Nautley rivers . Canadian Journal of Earth Sciences , 34 : 200 – 208 . 10.1139/e17-016 . Reimer , P.J. Bard , E. Bayliss , A. Beck , J.W. Blackwell , P.G. Ramsey...
FIGURES | View All (9)