Site Survey Methodology :
1) to ensure high potential areas were examined thoroughly and
2) to insure survey coverage and examine geomorphologic processes.
Surface site visibility within the study area is
considered to be poor to good depending on surrounding flora and land form
features. In areas deemed to be poor the main factor limiting site visibility
was the dense heath community of plants. These grasses, shrubs, flowers
and litter mat obscure archaeological materials (see figure 6).


On areas with active erosion such as ridge tops, edges of run-off channels, along side trails and the edges of ephemeral ponds, site visibility is fair to good. It was in these fair to good contexts where sites have been found (see figure 7).

At the extreme of this is the area affected by glacial ice expansion. Rapid ice retreat left behind large areas of bare and uninhabitable rock and cinder flat sediments. Without any nearby resources and being covered by ice more than once these areas were unlikely to have archaeological remains (see figure 8).

Upon identification, the extent of each site was
determined by the surface scatter of artifacts and the nature of the land
form it is located on. Sites were "mapped in" using a Garmin G.P.S. II
plus system. In addition sites were "tied into" land forms and trails using
the compass and pace method. The results were plotted on 1:50,000 and 1:25,000
scale maps (see attached site forms in appendix 1). Each site was photographed
with slide film. Each site was assessed with respect to its overall heritage
significance. Details of site investigations are found in section 3.0.
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Survey Results