etluviem
and tatlings

Glacial Ar/ FE
NS a

Bedrock outcroye

AN

Borehole ae NC
om) Beas:

s

Sce/e of feet
co} 1000 2000
Contour interval 40 reet

Geological Survey, Canada.

Figure 10. Part of Cunningham creek, Cariboo district.

may be associated with this damming, but the dam could not have per-
sisted long because the materials were easily eroded. Above the broad,
flat-bottomed part of the valley the stream bends around a high rock hill
on the left side. At the bend the valley bottom is narrow and the stream

Vana AO

SS AST ITT

FRI ES

Sa