Final answer:
Large-scale confining bends can result in folding, uplift, faulting, and subsidence.
Step-by-step explanation:
In large-scale confining bends, several geological processes can occur as a result. These include folding of the rock layers, where the layers are bent or curved due to the compressional forces. Another process is uplift, which is the upward movement of rock layers, often as a result of tectonic activity. Additionally, faulting can occur, where there is a fracture or break in the rock layers, resulting in movement along the fault line. Subsidence may also happen, which is the downward motion of land caused by various factors such as soil compaction or extraction of natural resources.