| Seastacks at Rialto Beach in Olympic National Park. During
the last ice age of the Pleistocene Epoch, sea level was more than 300 feet
lower than it is today. When the glaciers started melting about 15,000 years ago, sea
level began to rise, and shorelines migrated landward. Wave erosion
is constantly carving away at the shore leaving behind more resistant rocks
as sea stacks offshore. |