Trip Planning and Safety
Vehicle and foot travel in the southern part of the park can be light to moderate, depending on the time of year, so be prepared for the unexpected. If you have problems, help may not arrive for hours or even days. Carry plenty of water, food, gas, adequate clothing, a shovel, and emergency supplies. Cell phone reception is usually poor to nonexistent. Cool or cold temperatures will accompany sudden summer storms or an unexpected night out in the backcountry. Daytime temperatures in the summer may top 100 °F (37.8°C) and winter highs may stay below freezing, so dress and plan accordingly. Your safety is your responsibility.
Hiking in the Waterpocket District
Explore the southern Waterpocket District by foot.
Capitol Reef offers two free primitive campgrounds in more remote parts of the park.
Your safety is your responsibility. Ask about the latest weather conditions at the visitor center.
Loop-The-Fold Driving Tour
Most visitors to the southern part of the park drive the 124-mile (199 km) loop, or various sections of it. Drive time is generally 4-6 hours.
Highways 24 and 12 and the first 10 miles (16.1 km) of the Notom-Bullfrog Road (from the junction with Highway 24) are paved.
Notom-Bullfrog/Burr Trail Road to Lake Powell (at Bullfrog Marina)
The Burr Trail Road south from the Burr Trail Road junction remains unpaved for another 10.8 miles (17.3 km) to Eggnog Junction. From there it continues another 22.8 miles (36.7 km) to Bullfrog Marina at Glen Canyon National Recreation Area (NRA). The road to Lake Powell is paved from from Eggnog junction south to the boundary of Glen Canyon NRA. The access road to Halls Creek Overlook is located along this section of road and is marked by signs. Halls Creek Overlook Road usually requires high clearance four-wheel drive. Within Glen Canyon NRA, there is a section of unpaved road at Bullfrog Creek Crossing. The road from Capitol Reef to Bullfrog is normally in good condition, with the exception of the Bullfrog Creek Crossing which is occasionally impassable due to deep water, cut banks, and mud.
Loop the Fold Distances - Clockwise
All distances are from the Capitol Reef Visitor Center (VC), traveling in a clockwise direction
Loop the Fold Distances - CounterclockwiseAll distances are from the Capitol Reef Visitor Center (VC), traveling in a counterclockwise direction
A drive south along the Notom-Bullfrog Road offers views of the Waterpocket Fold's unique geology. The monocline, or one-sided uplift of the Earth's crust, is a premier example of the bending and folding of rock layers. The Waterpocket Fold is notable for its great length of multiple layers of exposed and carved colorful sedimentary rock. The monocline extends from Thousand Lake Mountain in the north to Lake Powell in the south.
Crustal pressure reactivated an ancient buried fault deep within the Earth, causing the overlying sedimentary rock layers to uplifted and folded. Today this monocline appears as a steep slope that ends in an abrupt cliff line. The east side of the Fold is tilted as much as 60% from the normal horizontal which caused accelerated stream erosion to occur. An estimated 7,000 feet (2,134 m) of overlying rock has been eroded away since the formation of the Fold, 60 million years ago. The west side, or escarpment face, is a near vertical cliff line and a formidable barrier to travel.
Geological features provide a source of park names. The vast expanse of white Navajo Sandstone atop the sloped side of the monocline is dotted with numerous natural tanks or potholes that collect rain water, contributing the name "Waterpocket" Fold. Navajo Sandstone domes resemble the Capitol building, hence the name "Capitol." Many early prospectors were former sailors who likened the vertical cliffs of Wingate Sandstone to a barrier common in nautical travel: a "Reef."
As you travel along the Notom-Bullfrog Road you will be driving through Strike Valley, which runs parallel to and on the east side of the Waterpocket Fold. The Burr Trail Road crosses through the Fold via a series of steep switchbacks. Both roads offer an outstanding viewing platform for this geologic wonder and of the Henry Mountains to the east. Enjoy your visit to this land of extraordinary rock formations...it's time well spent!
Last updated: March 31, 2020