The Grandview Monocline and its subsidiary normal fault exposed in the southern wall of Miners Spring Canyon; the fold axis and fault trace a path nearly parallel to the trend of the cliff, the fault intersecting the plane of the cliff face at the vertical gash exploited by a tall pouroff left-of-center, lower layers of Redwall are distinctly folded downward to the left (eastward) as they pass the fault trace along the base of the Redwall cliff.