A Gazebo in the Gorge?

Look above to the rim on the opposite side of the gorge for the Adirondack-style gazebo precariously perched on a pinnacle of bedrock. This pinnacle was formed as a result of “architectural jointing,” meaning the rock was eroded along two vertical rockfaces that intersect at nearly 90-degree angles. The rock of these vertical faces was weakened, or fractured, by compression dating back millions of years when the Appalachian Mountains were forming.