Painted Hills โ€” rock formation
Image by Gruendercoach from Pixabay

Painted Hills

  • 2 min read
  • 44.661ยฐ N 120.273ยฐ W

Interesting facts

  • On 21 August 2017 the path of totality of the Great American Eclipse passed directly over the Painted Hills, darkening them for about two minutes.
  • The striped beds belong to the Big Basin Member, the oldest division of the John Day Formation, which built up over some 20 million years.
  • The mudstones here preserve leaves of more than a hundred tree species and imprints of over fifty kinds of seeds, cones and nuts.
  • The colour cycling recorded in the hills spans roughly 34 to 28 million years ago, a window of about six million years.
  • Scattered black flecks on the slopes are manganese oxide, distinct from the darker seams of lignite left by ancient vegetation.
  • The clays contain a dozen elements, among them aluminium, silicon, iron, magnesium, manganese and titanium, whose shifting proportions produce the different hues.
  • The monument, and the river beside it, take their name from John Day, a Virginia fur trapper who was robbed and stranded near the river's mouth in the early 1800s.
  • The Painted Hills are counted among the Seven Wonders of Oregon, a list of the state's signature natural landscapes.
  • The wider John Day fossil country has yielded abundant remains of early horses, camels and rhinoceroses from the same ancient epochs.

Why it is worth it

The Painted Hills look less like geology than like a bolt of striped cloth thrown over the high desert of central Oregon. Rounded, almost bare mounds are banded in brick red, ochre, gold and charcoal, and the bands are not a surface stain but a record of climate laid down layer by layer. Most of what you see is volcanic ash that drifted roughly a hundred miles east from eruptions in the ancestral Cascades beginning some 35 million years ago, settling here and weathering into clay over the following several million years, as the warm, wet world of the late Eocene cooled into the drier Oligocene.

Each colour corresponds to a different chapter of that change. The deep reds are fossil soils formed in humid spells, rich in oxidised iron and aluminium; yellower bands record drier intervals; the dark streaks are lignite, the compressed remains of plant matter; and the soft greys are mudstone, siltstone and shale. The slopes carry almost no vegetation, so the stripes stay exposed, and the light keeps rewriting them: flat and pastel at midday, saturated and almost glowing in the low sun of morning and evening. Fossils are scarce here compared with the rest of the monument, though leaf impressions of redwood, alder, fig and cinnamon relatives have been found in the shales.

The hills are one of three units of John Day Fossil Beds National Monument, alongside Sheep Rock and Clarno, and cover a little over 3,100 acres. Five short trails each start from their own parking area. The Painted Hills Overlook trail gives the classic wide view of the main ridge; the Painted Cove trail crosses a boardwalk through a small amphitheatre of crumbly red and yellow mounds you can see up close; Red Scar Knoll and Leaf Hill are brief loops; and the Carroll Rim trail, the only demanding one, climbs about 400 feet to a panorama over the whole unit. The soil crust is easily scarred and footprints remain for years, so staying on the paths matters more here than almost anywhere.

Getting there

The unit lies about 9 miles (14 km) northwest of the small town of Mitchell, off U.S. Highway 26. From the highway, take Burnt Ranch Road for about 6 miles, then turn left onto Bear Creek Road at the unit entrance; directional signs lead to each trailhead. The nearest larger town is Redmond, roughly 84 km away in a straight line, and the closest airport is Roberts Field (RDM), Redmond, at a similar distance. The area is remote with few services, so arrive with fuel and water.

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From the encyclopaedia

The Painted Hills is a geologic site in Wheeler County, Oregon that is one of the three units of the John Day Fossil Beds National Monument along with Sheep Rock and Clarno. It totals 3,132 acres (12.67ย km2) and is located 9 miles (14ย km) northwest of Mitchell, Oregon. The Painted Hills are listed as one of the Seven Wonders of Oregon. The layers of color for which the site is named can be traced back to cycling periods of wet and dry climate conditions associated with the transition from the Eocene epoch to the cooler, more temperate Oligocene epoch. The different layers of colors are due to the soil being composed of a combination of mudstone, siltstone, shale and lignite.

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