— a limestone wave that runs twelve miles long.
“A twelve-mile-long limestone escarpment that rises almost a thousand feet above the meadow at its base. The walk in from the Benchmark trailhead takes most of two days, with no road within twenty miles of the wall itself. Hikers who reach Spotted Bear Pass see the cliff face turn copper for the last half hour before the sun drops behind it.
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The Chinese Wall is a Madison Limestone escarpment running roughly twelve miles along the Continental Divide inside the Bob Marshall Wilderness in northwest Montana. The wall rises about a thousand feet above the basin floor at the head of the White River drainage. There is no road access; the shortest approach from the Benchmark trailhead on the east side covers about twenty-six miles one way, putting most hikers two days from the cliff base.
The wall is part of the Sawtooth Range, an overthrust belt where Mississippian-age Madison Limestone was shoved east during the Lewis and Clark uplift and tilted into a near-vertical face. The pale grey rock holds fossil crinoid stems and brachiopods from a Paleozoic seafloor more than 340 million years old. Sun moving across the face through an afternoon turns it from bone-white at noon to deep copper in the last hour, with shadows tracking down chutes carved by spring runoff.
Few places in the lower forty-eight stay this far from a road. The Bob Marshall Wilderness covers about 1.5 million acres with no motorised access, and the basin below the wall is a full day's walk from the nearest trailhead at Benchmark on the east or Holland Lake on the west. Outfitters from Augusta still pack the meadows by mule string. Most nights at the base of the wall the only sound is wind off the Divide and elk moving through the timber.