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Fig. 6.1 Location of study area with outline of Lake Barlow-Ojibway (
inset
) and surficial geology
(Source: Agterberg and Banerjee
1969
, Fig. 1)
extends uninterruptedly across the Hudson Bay - St. Lawrence divide (Fig.
6.1
).
More detailed geological background with references to earlier work is given in
Agterberg and Banerjee (
1969
). It is mentioned here that individual varves can be
traced laterally from their proximal (northern) end to distal (southern) end succes-
sively changing from sandy through silty to diamictic facies (Fig.
6.2
). In the
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