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"Spring chinook salmon are native to the McKenzie watershed and are the
largest common fish in the river. Historically, spring chinook spawning
and rearing areas were distributed along the main stem McKenzie up to Tamolitch
Falls, Gate Creek, Horse Creek, Lost Creek, the South Fork McKenzie, Blue River,
and the Mohawk. However, with dams affecting fish passage and temperature,
the run has been reduced from historic levels. Temperature changes have
delayed adult fish migration and decreased fry survival.
There are also concerns with the effects the hatchery fish are having on the
native run. Composition of the spring chinook run has shifted from a
wild-production run of the late 1950s to a present run heavily supported by
hatchery fish produced at the McKenzie Hatchery. The ability of the
McKenzie River spring chinook population to be self-sustaining is a
controversial issue. High quality habitat in the McKenzie River may
provide the only area in the Willamette Basin as a whole where spring chinook
are capable of self-sustaining the population."
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