The Magnificent Natural Rockbridge
Ohio is a land of diverse geological features. One of these features is the Natural Rockbridge. The Natural Bridge originated millions of years ago, when Ohio was under a warm inland sea. Rivers flowed into the vast body of water, carrying both fine and coarse grained sands which settled to the sea bottom. Over the centuries, the accumulating sand thickened, compressed and formed the hard sedimentary rock known as Black Hand Sandstone. Eventually, great pressure from beneath the earth's surface caused the land in eastern North America to rise, forming the Appalachian Mountains. The inland sea soon drained away, exposing the newly uncovered rock layers to steady erosions processes.
The natural bridge soon began emerging in all its grandeur. Wind, rain and percolating groundwater worked together for centuries, carving a deep cave-like recess in the softer mid portion of the Mississippian Black Hand Sandstone. Gradually, erosion forces also worked along a natural joint plane some distance behind the brink of the cliff. Over the centuries, this ongoing process has widened the crevice, and all that remains of the overhanging ledge is the narrow rock arch.
Rockbridge's natural arch or bridge is more than 100 feet long and 10 to 20 feet wide, and gracefully arches 50 feet across a ravine. It is considered the largest natural bridge in Ohio. Only the Ladd Natural Bridge in Washington County rivals it in size.
The Natural Rockbridge can be viewed by taking Trip #2, Trip #3, or Trip #4. The landmark is short two minute walk from the bank of the Hocking River. It is marked by an orange post and a state park sign.