Tamolitch Falls (Blue Pool)
NF-610
Blue River, OR
A cliff-rimmed basin of impossibly clear, electric-blue water where the McKenzie River rises back to the surface after running for miles hidden beneath an old lava flow.
Along the McKenzie River Trail, deep in the Cascade foothills, the forest opens onto one of Oregon's most startling sights, a basin of water so blue it looks tinted, ringed by dark cliffs. This is the Blue Pool, formally Tamolitch Pool, sitting at the foot of a cliff that is usually bone dry. The color is not an illusion of light on green water. It comes from the extreme clarity and cold of the pool, which is fed almost entirely by springs, so that the water is scattering blue the way deep, pure water does.
The reason the cliff above the pool is dry most of the year is the strangest part of the story. The McKenzie River runs down toward this spot and then simply disappears, sinking into a porous lava flow and traveling underground for miles before welling back up to the surface here in the Blue Pool. Only in the highest water, after heavy rain or a big snowmelt, does the river top the old lava barrier and pour over the cliff as Tamolitch Falls, so most visitors see a waterfall that is not there.
What Guests Love
- The unreal turquoise-blue color of the water, so clear you can see submerged logs resting far below the surface
- The forested walk in along the McKenzie River Trail, through old-growth and past lava rock
- The strange geology of it, a river that vanishes underground and rises again in a hidden pool
- The wild, undeveloped feel, with no railings, buildings, or crowds of infrastructure
Worth Knowing
- The water is snowmelt cold year-round, dangerously so, and cliff-jumping here has caused serious injuries and deaths, so treat it as a place to look, not to leap
- There are no guardrails at the pool's rim and the rocks can be slick, so keep well back from the edge
- The trail is a real hike over rocky, root-crossed ground, so wear proper shoes rather than sandals
- It has become popular, so the trailhead lot fills on summer weekends and an early start makes a big difference
Details
Blue River, OR
Learn about Tamolitch Falls (Blue Pool)
The story of the pool
This corner of the Cascades lies within the traditional homelands of the Molalla and Kalapuya peoples, who traveled and lived along the McKenzie River corridor and the surrounding valleys for generations. Their descendants today are enrolled in tribes including the Confederated Tribes of Grand Ronde and the Confederated Tribes of Siletz Indians. The river and its high country remain part of a living cultural landscape, not merely a scenic one.
The name Tamolitch comes from the Chinook Jargon, the trade language once spoken across the region, and is usually translated as bucket, a fitting word for the deep, cliff-walled basin. The name was applied to the falls and pool in the twentieth century by a Willamette National Forest recreation engineer, drawing on that trade-language vocabulary.
The dryness of the falls owes something to human engineering as well as to geology. Upstream, a series of dams and a diversion that route much of the McKenzie's water away for hydropower means far less water reaches this reach of the old river channel than once did. As a result, water tops the lava barrier and falls over the Tamolitch cliff only during the highest flows, and for most of the year the pool is fed by the underground springs alone. The name Blue Pool has spread by word of mouth and social media in recent years, turning a quiet forest destination into one of the most sought-out short hikes in the state.
How the lava made a blue pool
The whole scene is the work of comparatively young volcanic eruptions. Not much more than a thousand years ago, lava poured from vents in the high Cascades, including the Belknap volcanoes near McKenzie Pass, and flowed down into the McKenzie's valley, burying long stretches of the river channel under fresh rock.
Lava rock is porous and riddled with cracks and tubes, so the river did what water does with porous rock, it went underground. Above the Blue Pool the McKenzie sinks into the lava and flows unseen beneath the surface for several miles, then rises again through the rock at the base of the Tamolitch cliff, filling the basin from below.
Because the water has traveled through cold rock rather than sitting in the open sun, it emerges startlingly cold and remarkably clean and clear. That clarity is exactly what produces the color, deep, transparent, cold water scatters sunlight toward the blue end of the spectrum, so the pool glows an unnatural-looking turquoise, and the pale logs and boulders resting on its floor stay visible far below the surface.
The forest and its wildlife
The walk in follows the McKenzie River Trail through classic Cascade old-growth, Douglas fir, western hemlock, and western red cedar rising over sword fern, moss, and the black, jumbled lava rock the eruptions left behind. In places the trail threads right along the water, where the McKenzie runs fast and green.
The river is prized for its cold, clean flow and holds native trout, including rainbow, cutthroat, and the increasingly rare bull trout, along with wild spring chinook salmon farther downstream. This is water clean enough and cold enough to matter to fish that many other rivers have lost.
Along the banks, watch for the American dipper, a small slate-gray songbird that bobs on midstream rocks and then walks straight into the current to feed underwater. Overhead, ospreys and belted kingfishers hunt the river, and the forest holds the usual Cascade cast of black-tailed deer, pileated woodpeckers, and, keeping well out of sight, black bear.
Season by season
Spring is when the pool is at its most vivid and when, in a high-water year, you may actually catch the rare sight of Tamolitch Falls flowing over the cliff after heavy rain or a strong snowmelt. Trails can be muddy and the water is at its coldest.
Summer is the most popular time, with warm forest air and dependable footing, though the trailhead fills early on weekends and the pool sees its heaviest visitation. The water stays icy no matter how warm the day.
Fall thins the crowds and brings a quiet, golden feel to the forest, with cool, settled days that are ideal for the hike and the river running clear.
Winter turns the trail cold and often icy, and higher elevations get snow, so the walk becomes a more serious undertaking, but the pool holds its color and the forest is at its most solitary.
Closest Boutels
The closest Boutel™ stays, so you can turn this stop into an overnight. Each is an independently owned, editorially selected place to stay.
Things to Do Near McKenzie Bridge
Sahalie and Koosah Falls
About 15 miles, a 25 minute drive
Two thundering waterfalls higher on the McKenzie, formed where the same kind of lava flow dammed the river, linked by a short forest loop trail and among the most photographed falls in the Cascades.
Clear Lake
About 18 miles, a 30 minute drive
The spring-fed headwaters of the McKenzie, so cold and clear that a submerged forest of trees drowned by an ancient lava flow still stands preserved beneath its surface.
McKenzie Pass and the lava fields
About 25 miles, a 45 minute drive (summer only)
A high, twisting scenic byway that climbs through vast black lava flows to the Dee Wright Observatory, with views of the Three Sisters and other Cascade volcanoes, open only in the snow-free months.