Painted Hills
"I kept waiting for the colors to be a trick of the light. They weren't. That's just what the earth looks like here."
The drive to the Painted Hills from the Willamette Valley is itself an argument for the state’s variety — you climb through the Cascades, drop into the high desert, and somewhere around the town of Mitchell you start seeing colors in the hills that make you wonder briefly if something has gone wrong with your eyes. Nothing has gone wrong. The Painted Hills are exactly what they look like: layers of volcanic ash and ancient lake sediment compressed over forty million years into striations of ochre, burgundy, black, and rust-red, the colors corresponding to different geological periods with the calm precision of a textbook illustration that has somehow been scaled to the size of a hillside.
I arrived in the late afternoon of an April day, which turned out to be accidentally perfect timing — the low angle of the sun hit the hills from the west and the colors deepened and the shallow shadows carved texture into the ridgelines and for about forty minutes I was completely unable to stop taking photographs. Then the light went flat and I stopped and just stood there in the silence. The Painted Hills are quiet in a way that feels active. There’s wind — almost always wind on this high plateau — but it’s the kind of silence that the wind happens inside of, not the kind the wind disturbs.
The John Day Fossil Beds National Monument contains three separate units — the Painted Hills, the Clarno unit (which has different geology, older, with large conglomerate formations that look like rough masonry), and the Sheep Rock unit near the town of John Day, where the Thomas Condon Paleontology Center has an actual working lab you can watch through glass walls. The fossils from this region are some of the most significant in North America — early horses the size of dogs, tapir relatives, ancient rhinoceroses, saber-toothed animals that don’t fit neatly into any category I can confidently recall. Oregon was subtropical jungle and savanna and lake shore before it was high desert, and the rock shows you that transition in colors.
The town of Mitchell, eight kilometers from the Painted Hills, has about a hundred and thirty residents and a diner where I had lunch twice on the same trip because it was the only lunch option and because the pie was genuinely excellent — a sour cherry filling with a crust that had clearly been made by hand by someone who learned from a grandmother. The motel across the road fills up when the weather is bad, which seems like the kind of weather information you should have before you go.
What makes the Painted Hills specifically affecting — as opposed to just visually interesting — is the scale. These are not dramatic cliffs or commanding peaks. They are gentle, rounded hills that look like they were inflated from below, and the colors are so unexpected in the context of a hill that your brain keeps trying to rationalize them as shadows or as something you’re misreading from a distance. Up close, on the Carroll Rim Trail above the formation, you look down on bands of color that haven’t changed since before the first human being walked anywhere near here, and the scale of that feels appropriate for a place this remote.
When to go: March through May for wildflowers and soft light. September and October are excellent — the high desert heat has passed, the crowds (such as they are) have thinned, and the autumn light on the layered colors has a warmth that the summer sun bleaches out. Avoid midsummer if you can; the plateau gets genuinely hot and the colors look better in low light.