The Painted Hills unit of John Day Fossil Beds National Monument occupies roughly 3,000 acres in Wheeler County near the community of Mitchell, approximately 3.5 hours east of Portland via US-26. The site preserves layered bentonite clay hills formed from ancient volcanic ash deposits that have weathered over 33 million years into horizontal bands of red, gold, black, and tan. The colors result from varying mineral concentrations: iron oxides produce the deep reds and yellows, while manganese and carbon compounds create the dark bands. Color intensity shifts dramatically with moisture, time of day, and season — after rain the saturated clays appear almost luminous; in dry summer light the tones are more subdued but the geometric banding is more precise. Five short trails totaling about 3 miles access the main formations without requiring strenuous hiking. The Painted Hills Overlook Trail (0.5 miles) climbs a short rise to a sweeping view of the main color sequence. The Carroll Rim Trail (1.6 miles round trip, moderately strenuous) ascends to a ridge offering the widest panorama of the unit. The Painted Cove Trail (0.25 miles, paved) is an accessible loop around the base of a densely colored small hill. The Leaf Hill Trail accesses Eocene plant fossil beds where ancient specimens have been excavated over more than a century of paleontological work. A seasonal visitor center provides geological and paleontological context. Mitchell, 9 miles away, offers limited food and lodging; staying near Prineville or Bend allows access to the Painted Hills and the Thomas Condon Paleontology Center in Fossil within a single day.
Good to know
- Hours
- Open daily dawn to dusk; visitor center 9 AM–5 PM
- Best time
- April–May (rain activates color richness) and late October (dry colors vivid in low light)
Location
32651 OR-19, Mitchell, OR 97750
44.6616, -120.2683 View on map
Highlights
- 33-million-year-old volcanic clay hills with layered red, gold, black, and tan mineral bands
- Carroll Rim Trail: best panoramic vantage point across the entire Painted Hills unit
- Painted Cove Trail: paved 0.25-mile accessible loop through the most intensely colored hill
- Color richness shifts dramatically with moisture — rain activates colors that dry conditions subdue
- Leaf Hill: Eocene plant fossil beds from one of North America's richest plant fossil sites
Tips for visiting
- Visit in the golden hour before sunset or the first hour after sunrise for the most vivid color contrast
- April and May offer damp post-rain conditions that activate the colors most intensely
- Stay on marked trails at all times — bentonite clay is extremely fragile and footsteps cause lasting visible damage
- No food or water is available at the site; Mitchell has a general store 9 miles away
- The site has no entry fee or reservation requirement at any time of year
- Combine a Painted Hills visit with the Clarno and Sheep Rock units of John Day Fossil Beds for a full geological day
When to visit
April and May offer the best color intensity after winter moisture. The golden hour around sunset and the first hour of morning light provide the most dramatic color contrast; midday flat light diminishes the visual impact.
Accessibility
The Painted Cove Trail is a paved 0.25-mile accessible loop around the base of the main colored hill, suitable for wheelchair users. The Painted Hills Overlook Trail is unpaved gravel and not fully accessible. Accessible parking and restrooms are available at the main trailhead.
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Frequently asked questions
How long does a visit to the Painted Hills take?
Completing all five short trails takes 2–3 hours. The overlook and Painted Cove trails can be covered in under an hour for those short on time. The scenic drive through the unit adds another 30 minutes.
Is the Painted Hills site accessible for children and seniors?
Yes. The Painted Cove Trail is paved and suitable for wheelchair users. The Overlook Trail is short and suitable for most visitors. Carroll Rim is more demanding but manageable for fit walkers of any age.
What causes the colors in the Painted Hills?
The colors result from minerals in ancient volcanic ash deposits. Iron oxides create the red and yellow bands; manganese and carbon compounds produce the dark layers. Moisture intensifies all colors significantly after rain.