Yant Flat can be reached from the west starting at St George though part of the route is rather rough, so the best approach is from the east, beginning at Leeds along I-15. From the interstate exit, the Silver Reef Road (later Oak Creek Road) winds past scattered houses for a few miles then enters the Dixie National Forest, where the surface changes to gravel. A notice advises that camping is permitted in designated sites only, a restriction which applies just for the next few miles. The road climbs steeply at first, crossing a high ridge then dropping back down, round the heads of several canyons including Yankee Doodle Hollow, then flattens out as it reaches Yant Flat, where the surface is clayish, and rutted from being driven over when wet. A suitable parking spot for visiting the cliffs is 10.4 miles from Leeds, at a minor crossroads; right is an active ATV track, while left is a disused track, now just a trail. Parking is limited as the main road is quite narrow and has no verges. The surrounding land is flat, covered by typical pinyon-juniper pine forest, dotted with desert plants including yucca, agave, cholla, opuntia and echinocereus. The track/path - apparently known as Anna'a View Point Trail
- heads south towards the plateau edge, reaching it after 1.3 miles. The land falls away steeply hereabouts but is more undulating further east. Faint paths follow the rim in both directions.
The exposed red rocks extend several miles east to west, spanning 500 feet or more of elevation, though the best area appears to be from the end of the trail a mile or so southeast. Lower down the ground is much less steep, more overgrown and has smaller erosive features. The main section is characterized by domes and cones, cliffs and ledges, and U-shaped gullies, with all surfaces generally quite smooth, though crossed by thin, parallel ridges and grooves due to the underlying cross-bedding. Some areas have neat hexagonal patterns. In a few places, the predominantly light-colored sandstone is interrupted by small, jagged intrusions of much darker rocks, resembling partly buried dinosaur bones. The wavy color patterns range in scale from thin parallel lines just a fraction of an inch apart to broad, curving bands several feet wide. Most colors seem somewhat faded however; there are few really bright patches. The cliffs face southeast so are best visited in the morning.