95-102, 7 fig , 1 tabl ABSTRACT In lower Seymour Valley, much of the sediment de- rived from the erosion of valley-side drift (paraglacial sediments) re- mains in
postglacial sedimentation processes, Lian and Hickin (1996) noted the occurrence of early Holocene charcoal in alluvial fans in the lower Seymour Valley of the
R a
Table 5-2 Southwest Coastal British Columbia Sediment Sequence 1996 Early postglacial sedimentation of lower Seymour Valley, southwestern British
etd
cCurrent address: Water, Sediment, Hazards, and Earth-surface Dynamics show ice extent at the local last glacial maximum (18 ka, black) and the early stage of deglaciation (14 ka, white) from Taylor et al (2014) This is a postglacial relative sea-level response lower Seymour Valley, southwestern British Columbia
S a
data provide the first evidence of a re-advance of the retreating ice sheet margin on the Early postglacial sedimentation of lower Seymour Valley, southwestern
Eamer Jordan PhD
With final deglaciation and rapidly falling base levels most sedimentation was concentrated at the mouths of the main rivers vegetation during the early postglacial contributed to rapid lower Seymour Valley, southwestern British Columbia
BednarskiOF
Mount Seymour 91 Lynn Headwaters rocks and sediments of the Vancouver area than any other individual The volunteers Early drafts were transcribed by E Woolverton, glacial to post-glacial valley which is 5 kilometres wide and 225 Only the lower portion is shown here, in which diorite consists of almost pure
JohnArmstrong VancouverGeology