— — the worn-down tooth of an older mountain.
“An eroded shield volcano whose summit pinnacle stands above the lodgepole and lava fields of central Oregon. Visible from the Cascade Lakes Highway and from Highway 20 as drivers crest Santiam Pass. The Mount Washington Wilderness around it holds some of the youngest lava flows in the state. From the studio.
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Mount Washington stands at 7,795 feet in the central Oregon Cascades, in Linn and Deschutes counties. It is the deeply eroded remnant of a shield volcano that last erupted hundreds of thousands of years ago, with the harder volcanic plug at its core left exposed as a steep summit pinnacle. The peak gives its name to the 54,278-acre Mount Washington Wilderness, which spans the Willamette and Deschutes National Forests and sits between Santiam Pass to the north and McKenzie Pass to the south.
The wilderness around the peak is one of the most heavily lava-covered landscapes in Oregon. Belknap Crater and Little Belknap, just south near McKenzie Pass, sent flows across the area as recently as about 1,500 years ago, and the basalt fields visible from the Dee Wright Observatory on Highway 242 are the result. The summit pinnacle itself is composed of erosion-resistant basaltic andesite. The first recorded ascent was in 1923 by a Mazamas party.
The standard climb leaves the Pacific Crest Trail at Big Lake and ascends the north ridge, gaining about 3,400 feet over roughly five miles one way. The upper pitches are class-four to low-fifth rock on loose volcanic stone, and most parties rope up and carry a small rack. Day-hikers without climbing experience usually stop at the saddle below the pinnacle. The wilderness permit is free and self-issued at the trailhead. The route is generally climbable from July through September.