Fraser Lowland

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Journal Article
Published: 01 April 1985
Canadian Journal of Earth Sciences (1985) 22 (4): 498-505.
... episode when this part of the Fraser Lowland was ice free between the Coquitlam and Vashon ice advances.The beetle assemblage from Mary Hill Quadra sediments probably indicates that a bog environment existed at that time; however, the lack of specific identifications precludes detailed paleoclimatic...
Journal Article
Published: 01 December 1982
Canadian Journal of Earth Sciences (1982) 19 (12): 2288-2296.
...Stephen R. Hicock; Richard J. Hebda; John E. Armstrong Abstract Pollen and macrofossil evidence from two sites in northwestern Fraser Lowland reveals that Abies lasiocarpa – Picea cf. engelmannii forest and parkland grew there about 18 000 years ago under cold humid continental conditions. Taxus...
Journal Article
Published: 01 May 1982
Canadian Journal of Earth Sciences (1982) 19 (5): 899-906.
...Stephen R. Hicock; Keith Hobson; John E. Armstrong Abstract Three recently radiocarbon-dated tusk segments from eastern Fraser Lowland indicate Pleistocene proboscideans (probably mammoths) lived there between 22 700 and 21 400 years ago during early Fraser (for the Fraser Lowland) ice advance...
Journal Article
Published: 01 September 1981
Canadian Journal of Earth Sciences (1981) 18 (9): 1443-1451.
... years BP, during the Fraser Glaciation (late Wisconsin) and prior to the main Vashon glacial maximum at about 14 500 years BP. The drift was deposited in short pulses by valley and piedmont glaciers fluctuating into the Fraser Lowland from the Coast Mountains to the north and Cascade Mountains...
Series: GSA Field Guide
Published: 01 January 2014
DOI: 10.1130/2014.0038(05)
EISBN: 9780813756387
... in relative sea level in the Fraser Lowland from ~180 m (600 ft) at the end of the Everson interval to near present sea level. Following emergence of the Fraser Lowland, a lobe of the CIS advanced from the Fraser Canyon near Sumas to Bellingham during the Sumas Stade. As the ice retreated, at least eight end...
FIGURES | View All (39)
Series: GSA Field Guide
Published: 01 January 2007
DOI: 10.1130/2007.fld009(02)
EISBN: 9780813756097
... to southern British Columbia. The Everson deposits are characterized by vast areas of massive, poorly sorted stony silt and clay commonly containing marine shells. At Bellingham Bay and elsewhere in the Fraser Lowland, Deming sand is overlain by massive, poorly sorted, Bellingham glaciomarine drift...
FIGURES | View All (35)