At the trailhead a disused vehicle track heads due north, reaching the edge of the plateau after 0.3 miles, from where a vast tract of badlands, mud flats and washes comes into view, colored in muted shades of yellow, brown and gray. A fair proportion is overgrown, with bushes, grass and small trees but there is plenty of bare earth and exposed rock, just not so many hoodoos or other distinctive formations; the scenery is not so promising at first sight. A bushy ravine parallels the edge of the plateau to the west, separated from the main valley by a narrow ridge, while just beyond, to the north, is the wide, meandering De-Na-Zin Wash
, which splits into several tributaries to the east and north, all becoming quite deep, winding beneath unvegetated clay hills, black or yellow in color. The terrain is more uneven to the west, at the far side of the wash, while further north are many other distant escarpments and badlands, and several drainages (Hunter Wash, Alamo Wash and Willow Wash).
The most interesting region in view from the edge of the plateau near the trailhead is the uneven, eroded terrain to the northwest, about 1.2 miles away. The easiest way to reach here is first to walk west along or just below the plateau edge, over sandy land with scattered but quite large pieces of petrified wood and a few isolated hoodoos formed of orange-brown sandstone supported by white mudstone - one is especially distinctive (photo
), looking out northwards over the valley. A tributary ravine forms just south, cutting through orange, potmarked sandstone and causing the plateau to split into a narrow promontory, whose sides are easy to climb down, leading to the streambed of De-Na-Zin Wash near where the drainage makes a tight U-shaped bend.
The wash is lined on the north side by white badlands strewn with small, multicolored pebbles, beyond which, a short distance northwest, is a large basin filled with twisted, fractured rock - the uneven terrain visible from the trailhead.
In some places the white mud hills are liberally sprinkled with petrified logs, and also by strange, dark brown sandstone balls, perfectly spherical in shape, and often forming small hoodoos, supported by thin columns of the soft, underlying mudstone. The white layer is topped by a band of cream to white sandstone and then by a thicker layer of richly colored, golden-brown sandstone that has eroded into the most fantastic forms imaginable, with all kinds of complex and delicate hoodoos, narrow ravines, undulating mounds and narrow pinnacles. On top of this brown rock are massive pieces of petrified wood including many near-complete trunks, up to 100 feet long and 6 feet thick at the base, in places lying criss-cross on top of each other. The logs form caprocks, arches and thin ridges; some are fully exposed, on the surface, while others are partially buried by soil or surrounded by the sandstone. A few exposed sandstone outcrops contain holes where logs used to reside but have since eroded away - this location is unusual in that the logs are partially enclosed by harder sandstone, unlike most petrified wood in the Southwest that is found embedded in softer layers. The combination of weird, colorful rock formations and the huge petrified trees make this perhaps the single most remarkable location in the Bisti/De-Na-Zin wilderness. The basin stretches about half a mile, at the southeast corner of a 1.5 mile wide plateau that is lined on all other sides by a narrower though still interesting belt of eroded badlands. Most parts of De-Na-Zin Wash have much more scattered features, however, though there are still a fair number of large and photogenic hoodoos throughout the valley, and colorful pieces of petrified wood.