High cliffs with tilted strata create an optical illusion that the river is beginning a sharp descent, but the mellow flow tells the truth.
2.
Geologists consider Mount Rundle to be a classic example of a mountain cut in dipping layered rocks, with the tilted strata giving the mountain its shape.
3.
Though this surface is typically a plane, differential erosion of the tilted strata of the Unkar Group left resistant beds of the upper layer Cardenas Basalt and the middle layer Shinumo Quartzite as ancient hills, called monadnocks.
4.
Though this surface is typically a plane, differential erosion of the tilted strata of the Unkar Group left resistant beds of the Cardenas Basalt and Shinumo Quartzite as ancient hills, called monadnocks, that are up to high.
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