A dike is a type of geological formation that typically occurs when magma intrudes into existing rock layers and then solidifies. In the context of the Grand Canyon, the dike would have formed after the sandstone layers formed and before erosion revealed the canyon wall. This means the correct answer is:
after the sandstone formed and before erosion revealed the canyon wall.
This sequence of events indicates that the sandstone layers were already in place when the dike intrusion occurred, and the subsequent erosion then exposed both the sandstone and the dike in the canyon walls.