— — the ridge that lets the colour breathe.
“A short, steep climb out of the Painted Hills Unit of John Day Fossil Beds. Roughly 1.6 miles round-trip, about 400 feet up, on a path that leaves the parking lot and keeps gaining until the whole banded basin opens below. The hills hold their best red after a light rain, when the claystone darkens and the gold band between layers reads sharper. Most people skip the rim and stay on the boardwalks below. from the studio
Each tile is finished by hand in our Knoxville studio. Artwork is slowly infused into the ceramic surface under high heat and pressure, and rests beneath a thin glossy finish. The colour lives in the surface, not on top of it.
Pick any four 4-inch tiles — National Parks you've been to, a Smokies set, the four seasons of one place. $ for a set of , cork-backed, ready to live on the table.
Carroll Rim Trail sits in the Painted Hills Unit of John Day Fossil Beds National Monument, in Wheeler County, Oregon, about nine miles northwest of the town of Mitchell. The trailhead is off Bear Creek Road, opposite the main Painted Hills overlook. The route gains roughly 400 feet over about three-quarters of a mile to the rim, then returns the same way, for a round-trip near 1.6 miles. The hills below are claystone layers laid down between roughly 39 and 33 million years ago, recording the cooling climate of the late Eocene through early Oligocene.
The reds, golds, and blacks on the slopes below come from iron and manganese oxides in volcanic ash weathered over millions of years. The bands shift with moisture: dry claystone reads pale and chalky, and the same hill after rain turns a darker, deeper red. The bright yellow horizon between two red bands tracks an ancient shift in soil chemistry rather than a single eruption. From Carroll Rim the layering reads as a long horizontal record across the basin, harder to see from the boardwalks at ground level.
The Painted Hills Unit is open daily, sunrise to sunset, with no entrance fee. The trail is exposed, with no shade and no water on route, so morning or late afternoon in spring and autumn read best. Summer afternoons in the John Day basin regularly run above 90°F. The colour reads strongest after a light rain or under low, raking light near sunset. Pets, drones, and off-trail walking on the hills are prohibited; the claystone crust is fragile and damage is visible for years.