Morse Creek Overlook

Morse Creek Overlook is a short scenic stop on Hurricane Ridge Road. Its wayside looks into a forested gorge, and a separate pillow-basalt exposure sits across the road. It’s worth a few minutes if you want a clear story of how ice and flowing water shaped this corner of Olympic. The viewpoint has a sidewalk, a low stone wall and an interpretive panel.

The panel compares today’s forested gorge with Ancient Lake Morse, which once filled the valley between Round Mountain and Blue Mountain. A continental ice sheet and glaciers from the Olympics blocked drainage; meltwater pooled here until the ice retreated and the lake drained. The panel’s side-by-side past-and-present views make that change easier to picture than a map would.

Before the glaciers redirected it, Morse Creek flowed over softer sediments between the mountains. The diverted creek cut a new path through harder volcanic rock, leaving the gorge visible from the overlook. Look from the panel to the forested valley and you’re seeing the result of that rerouted creek.

The rounded, cracked rocks at the adjoining exposure are pillow basalt, formed when lava cooled quickly underwater. The Olympic Mountains’ Crescent Formation basalts date to roughly 40–50 million years ago. NPS notes that the local rocks have few gas bubbles, consistent with lava cooling under deep-water pressure on the ocean floor.