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Updated: June 8, 2025
"This apparently is true not only of the segments of thrust surface beneath eastern Flattop, Yellow, and Chief Mountain, but also of the more deeply buried portions which appear to dip with the Algonkian strata into the syncline. While observation is not complete, it may be assumed on a basis of fact that thrust surfaces and bedding are nearly parallel over extensive areas." Geol.
We climbed out up on a bench, and across a flat, up another bench, out of the timber into the patches of snow. Here snow could be felt in the air. Water was everywhere. I saw a fox, a badger, and another furry creature, too illusive to name. One more climb brought us to the top of the Flattop Pass, about eleven thousand feet.
From the rim of the cañon, between Flattop and Hallett, I viewed the spot where I had blundered over the edge of the snow-cornice on the way to the dance. Beneath lay Tyndall glacier, its greenish ice exposed by the summer thaw. I circled the head of the cañon and climbed to the top of Hallett.
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