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The two RV Gypsies had trouble
finding this park. At first they drove right by it and went a long way
on a dirt road before they turned around and figured out that they had
driven past the park. Lee Duquette was not very happy. The small parking
lot just off the road access was full of cars with bicycles on them.
Then the two RV Gypsies walked across a small wooden bridge that crossed
Driftwood Creek. The bridge was not in the best of shape, because the
part people walk on had dips that made Karen Duquette trip. |
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Below: A short
interpretive trail gave glimpses of Driftwood Creek and led to a cliff-face
exposure of Eocene shales that were deposited in an inter-montane lake. |
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Below: After a short walk,
the two RV Gypsies came to the end of the trail and a big hill that
was blocked off. The hill of shales was interbedded with volcanic ash
beds, the result of area volcanoes that were erupting throughout the
life of the Eocene lake that produced the shales. Preserved within the
shale formations were plant, animal and insect species that inhabited
the area over 50 million years ago. Pieces were laid out on a railing
for examination by visitors. |
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Below; The BC Parks management
plan for Driftwood Canyon Provincial Park lists these conservation attributes:
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internationally-significant Eocene fossil beds: most northerly site in North America with fossilized Eocene insects; fossils also include ancestral salmon, trout and suckers, including Eosalmo driftwoodensis;
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site of ongoing paleontological research;
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remnant Bulkley Basin Ecosection (high priority, underrepresented ecosection) SBSdk (dry cool sub-boreal spruce subzone; underrepresented biogeoclimatic subzone).
Limited personal fossil collecting was originally permitted in Driftwood
Canyon Park, and the site has been listed in several tourism and rock
collection guides as a place to visit for this activity.However,
this activity is no longer allowed here.
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