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Hiking the Lower Metolius River Canyon

Tucked away in a nearly-forgotten corner of Deschutes National Forest, just an hour’s drive west from Culver, the hike along the Lower Metolius River follows a long-abandoned road for 3 miles over riverside terraces and through stands of old-growth incense cedars and firs. The star attraction here, though, is the local population of ospreys, a species of fish hawk that nests in the top of large snags near the river. Hikers during summer will be treated to the aerial displays of these soaring raptors, overhead and around their large stick nests.
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Photo of Boundary Springs

Boundary Springs - Source of the Rogue River

Central Oregon has its share of spring-fed rivers — the Metolius, the Cultus, the Quinn and Fall River — but none of these enters the world quite so dramatically as the Rogue River at Boundary Springs. Gushing down the hillside over colorful, moss-covered rocks and logs, these headwater springs are unique. A good 2.5-mile hiking trail starts on Forest Service land just north of Crater Lake National Park and follows the river canyon (mostly spared from an encircling 2015 wildfire) upstream to the springs across the Park boundary.
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Photo of Two Spawning Kokanees

Spawning Kokanee at Crane Prairie Reservoir

One magnificent spectacle of nature that recurs every fall in Central Oregon is the spawning of kokanee salmon in the tributary streams of local Cascade lakes. Though an introduced species, these landlocked, lake-dwelling sockeye salmon are no less impressive. Several local streams have kokanee runs in the fall, but three tributaries of Crane Prairie Reservoir — the Upper Deschutes, Cultus and Quinn Rivers — are less-visited, beautiful and easy to access. If looking for an outing on a warm, sunny day in late September or early October, these three kokanee spawning sites are worth a visit.
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Headwater Springs of Fall River

Fall River - Bellwether of Climate Change

Spring-derived streams are fairly common along the eastern slopes of the Cascade Range in Central Oregon, including the Metolius River, Cultus River, Quinn River, Brown’s Creek and Fall River. The combination of heavy precipitation along the Cascade crest, permeable volcanic bedrock, plus groundwater flow serves to recharge all of these spring-fed streams. But Fall River has been the most extensively studied as a local indicator of climate change — besides having a delightful hiking trail along its banks to explore.
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