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Lee Duquette had trouble finding
this park. At first he drove right by it and went a long way on a dirt
road before he turned around and figured out that he 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 Lee
and Karen Duquette 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. But luckily
she did not get hurt since they were alone and in the middle of nowhere. |

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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,
Lee and Karen Duquette 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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