Final answer:
The sedimentary layers at Capitol Reef are tilted due to the Waterpocket Fold, a monocline formed by the Laramide Orogeny, which caused an ancient buried fault to reactivate and the west side to shift upwards, tilting the layers.
Step-by-step explanation:
The sedimentary layers at Capitol Reef are tilted due to geological activity associated with the Waterpocket Fold, a classic monocline formed during the Laramide Orogeny. This major mountain-building event reactivated an ancient buried fault, causing movement along the fault which shifted the west side upwards relative to the east side. This process lifted the sedimentary rock layers and created a distinctive tilt. Other regions like the Grand Canyon, Zion National Park, and the Colorado Plateau were also affected by uplift, but they often display a more uniform 'layer cake' appearance because their uplift was relatively even, unlike the dramatic tilting observed at Capitol Reef.