Natural AttractionHickman Natural Bridge
133-ft Navajo Sandstone arch—erosion in action beneath Capitol Reef.

The Bentonite Hills display softly-contoured, banded ridges in shades of gray, red, purple, maroon, brown, and green—layers within the Jurassic Brushy Basin shale member of the Morrison Formation. These ancient mudstones were deposited as mud, silt, fine sand, and volcanic ash in warm, shallow lakes and swamps approximately 150 million years ago. The distinctive popcorn-like surface texture results from bentonite clay (altered volcanic ash) repeatedly absorbing water, swelling, and then cracking as it dries—a weathering process still active today. Access requires high-clearance 4-wheel-drive vehicles via Hartnet Road, and the fragile surface is easily damaged; every footprint and tire track leaves scars that take years to heal.
Geological Formation
5,500 ft
High-clearance 4-wheel-drive vehicle required
Softly rounded, multicolored banded hills in shades of gray, red, purple, maroon, brown, and green. Composed of Brushy Basin shale member of the Morrison Formation from the Jurassic period.
Softly-contoured, banded hills with visible color gradations in gray, red, purple, maroon, brown, and green. The distinctive popcorn-like surface texture created by bentonite clay (altered volcanic ash) expanding and contracting through water-absorption cycles.
Composed entirely of bentonite clay (altered Jurassic volcanic ash) from the Morrison Formation. The distinctive fine popcorn-like surface texture develops from ongoing cycles of clay absorbing water, swelling, and then cracking as it dries. This weathering process is geologically active today.
Spring (April-May) and fall (September-October) offer ideal combinations of reliable road access, comfortable temperatures, and excellent photography light. Summer heat is intense and afternoon thunderstorms frequently render clay roads impassable. Winter is generally passable but less reliable after snow.
Bentonite clay becomes extremely slick and gummy when wet—travel becomes difficult or impossible. Roads are impassable during and after rain. Never venture off the main road; the surface is easily damaged and scars take years to heal. High-clearance vehicles only. No services or emergency help nearby. Afternoon thunderstorms are common in summer. Call 435-425-3791 before visiting for current road conditions.
Composed entirely of bentonite clay (altered Jurassic volcanic ash) from the Morrison Formation. The distinctive fine popcorn-like surface texture develops from ongoing cycles of clay absorbing water, swelling, and then cracking as it dries. This weathering process is geologically active today.
Visible Jurassic Morrison Formation (Brushy Basin shale member) represents ancient depositional environment—mud, silt, sand, and volcanic ash deposited in warm lakes and swamps approximately 150 million years ago. Bentonite clay (altered volcanic ash) provides mineralogical insight into past volcanism and hydrothermal alteration. Active weathering process visible: clay swelling and cracking cycles create distinctive surface texture and demonstrate ongoing erosion and landscape modification.
From the Capitol Reef park area, head north toward Cathedral Valley. Take Hartnet Road, which branches from the main park access routes and leads directly through the Bentonite Hills. The location is outside the main park boundary on Bureau of Land Management land.
None; there are no official trails through the Bentonite Hills. The site is accessed via scenic drive only.
No trails connect to the Bentonite Hills. The site is accessed via scenic drive only.
Drive along Hartnet Road through the heart of the Bentonite Hills for continuous panoramic views. Pullouts along the road provide vantage points for observing the surrounding colored badlands and capturing the full sweep of colors.
Early morning or late afternoon golden-hour light enhances the subtle color gradations and surface texture. Wide-angle compositions capture the full sweep of colored ridges. Clear blue skies amplify the hues; cloudy conditions mute them. Include sky above badlands for scale.
The entire drive along Hartnet Road offers photography opportunities. Best compositions emphasize the color gradations across the face of the hills. Golden hour (sunrise/sunset) brings out subtle colors and surface texture details.
Unknown; remote location with sparse vegetation and harsh clay terrain supports limited visible wildlife.
Afternoon thunderstorms common in summer. Flash flood risk in washes. Bentonite roads become impassable when wet. High winds can occur. Check weather forecast before visiting.
Cathedral Valley, Fluted Wall Viewpoint, Navajo Dome Viewpoint, Temple of the Sun and Temple of the Moon, Capitol Reef National Park's Scenic Drive, Waterpocket District
None at the location. Nearest services (food, lodging, fuel, supplies) are in Torrey, Utah. Capitol Reef Visitor Center provides information and restrooms.
Accessible only by high-clearance 4-wheel-drive vehicles via Hartnet Road. Unpaved dirt surface. Road becomes impassable when wet. No wheelchair access. No developed trails. Cross-country travel not recommended due to fragile, easily-scarred surface.
Remote location with no services, restrooms, or emergency infrastructure. Requires high-clearance vehicle and careful driving. Children must stay on or very near the main road at all times—no wandering off-road. Bring ample water and snacks; summer heat is intense. Not recommended for very young children, elderly visitors with mobility challenges, or anyone uncomfortable driving in remote, undeveloped areas without cell service.
None at the Bentonite Hills. Nearest facilities (visitor center, restrooms, water, supplies, lodging) are at Capitol Reef Visitor Center or in Torrey, Utah.
" Visitors appreciate the unique geological colors and remote setting. Experiences are largely positive for those adequately prepared with high-clearance vehicles and supplies. Road conditions are the primary concern; wet weather can unexpectedly close access. The fragile surface and complete lack of services require self-sufficiency and advance planning."
Yes. High clearance 4-wheel drive is usually necessary to access the Bentonite Hills via Hartnet Road. Standard vehicles risk getting stuck or damaged.
Yes. Bentonite clay becomes extremely slick and gummy when wet. Roads are impassable during and after rain until they dry completely.
No. There are no official trails. Stay on the main road to protect the fragile surface—footprints and tire tracks leave scars that take years to heal.
No permit is required. The Bentonite Hills are located on Bureau of Land Management land outside Capitol Reef's park boundary.
Call 435-425-3791 (press 1 for information, then 4 for road conditions) before your visit to confirm access.
Cell service is unreliable or unavailable in this remote area. Don't rely on it for emergencies. Tell someone your travel plans before visiting.
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