Isoclinal folding within Cambrian Puncoviscana Formation metaturbidites likely occurred during mid to Late Cambrian time.

Sigma clasts and S-C fabrics occur within ultramylonitic shear zones in Ordovician granitoids in the core of the Cachi Range. This shear zone records a normal sense of displacement and may reflect extensional collapse of an Ordovician orogen.

This minor fault propagation fold south of La Poma accommodated ~30 m of reverse-sense structural relief.

Overturned angular unconformity in an overturned footwall syncline at the eastern margin of the Cachi Range. This is a thick-skinned style of deformation and, coupled with (U-Th)/He-zircon results, demonstrates that fault-propagation folding (not slip across discrete faults) was the major mechanism for the formation of structural relief in the region.