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Updated: May 16, 2025
The return ride up the Red Canyon Trail is made enjoyable by the brilliant colorings, the faultings and nonconformities of the strata, which are apparent even to the most undiscerning layman. Here the conglomerate appears above the blue limestone, while ordinarily it is found below it. The Algonkian also is largely in evidence. Across the river one may see the location of the asbestos deposits.
The condition of this body of crystalline rocks is due to the fact that they have suffered not only from the faultings, foldings, and igneous intrusions of their time, but necessarily, also, from those of all later geological ages. At present three leading theories are held as to the origin of these basal crystalline rocks.
On the plateaus separating Hance Canyon from Mineral Canyon, and the latter from Red Canyon, one can see the rare Algonkian strata to fine advantage. Numerous faultings and flexurings may be observed, and on the last mile before reaching the foot of Red Canyon, the trail leads through a great boulder bed along the brink of the gorge immediately overhanging the river. Camp is made here at night.
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