Overview

This moderately strenuous, 4.0-mile loop involves a 1-mile walk up Golden Canyon, (a picturesque, narrow, and geologically interesting canyon), a steep 1.0-mile hike up and over badland mud hills to Gower Gulch, and a pleasant 2.0-mile hike down Gower Gulch through mud hills and towering conglomerate cliffs back to the Golden Canyon trailhead. There is a short, 3rd-class pour-over near the bottom of Gower Gulch to downclimb.

This hike starts on the Golden Canyon Nature Trail. There are 10 numbered posts in Golden Canyon, so be sure to pick up a brochure at the Visitor Center or the trailhead so you can read about the local geology while hiking up the canyon.

Link to map.

Watch Out

Other than the standard warnings about hiking in the desert, ...this hike is pretty safe, but stay out of the canyon (and off the mudhills) if it is raining or threatens to rain because of flash flood dangers. There is a pour-over in the lower end of Gower Gulch that is an easy 3rd-class downclimb, but the rock is water-polished and slick, plus it is covered with dust and gravel, so there is greater than usual risk if slipping. There are several open mine shafts along this route; it is never safe to enter old mines.

While hiking, please respect the land and the other people out there, and please try to Leave No Trace of your passage. Also, this is a fairly long hike, so be sure to bring the 10 Essentials.

Getting to the Trailhead

This hike is located along Badwater Road in Death Valley National Park, about 2-1/2 hours northwest of Las Vegas. From town, drive out to Death Valley, pay the entrance fee, and then drive to the Golden Canyon Trailhead. Park here; this is the trailhead.

For a change of scenery, consider starting the hike at the Zabriskie Point Trailhead.

The Hike

From the Golden Canyon Trailhead (Table 2, Waypoint 1), the trail immediately enters and ascends a narrow canyon with colorful walls, ripple marks in the rocks, and other evidence of wetter conditions in the past. Follow the Golden Canyon Nature Trail for 1.0 miles (about 30 minutes) to a trail junction at Trail Marker #10 (Wpt. 2). For details on this section of the hike, see the description of the Golden Canyon Trail.

At the trail junction, a sign indicates that Red Cathedral is to the northeast (left; straight up the main canyon) and that Zabriskie Point and Gower Gulch are to the southeast (right; up a side canyon). Head southeast and follow the narrow trail up into the eroded mudhills. Markers along this section of trail indicate which gullies to follow. The trail runs steeply and more or less directly towards the northwest corner of Manly Beacon, and there are some great views of the Red Cathedral cliffs. The trail then cuts southward under the sheer west face of Manly Beacon and runs out to a saddle on the southwest flank of the beacon (Wpt. 4).

This saddle, 0.4 miles from Golden Canyon, marks the high point on the route. From the saddle, there are spectacular views of the badlands and mesquite flats in floor of Death Valley to the north and of badlands and mountains to the south. Even without shade, this is a great place to stop for lunch.

From the saddle, the trail drops steeply through the mudhills heading southeast. Along this section of the trail, you get well beyond Manly Beacon and can look back to see that the brick-red Red Cathedral cliffs continue to the south behind Manly Beacon and off towards Zabriskie Point. After about 0.3 miles, you get to another signed trail junction (Wpt. 5). The fork to the east (left; uphill) runs up to Zabriskie Point, while the fork to the southwest (right; downhill) runs down to Gower Gulch.

Taking the southern fork towards Gower Gulch, the trail follows a relatively wide canyon with a firm base as it runs downhill through low mud hills. This canyon has no markings and you wouldn't know that it was a route, but just stay in the main canyon. In the lower part of this little canyon, the hard gravel wash surface has eroded to form a tiny slot canyon (3 inches wide and 10 inches deep); it looks like a new slot canyon getting started in the old canyon. After about 0.3 miles, the canyon ends at the edge of Gower Gulch (Wpt. 6). This is another signed trail junction; heading upstream leads to Zabriskie Point, while downstream leads back to the Golden Canyon trailhead.

From this junction, head westward (right) and down Gower Gulch. The gray gravel in the wash contrasts nicely with the pale yellow badlands, and there is enough dirt mixed in the gravel to make the surface hard and easy to walk on. The vegetation in the wash is sparse, mostly desert holly and prickly penstemon, but it is lush compared to the mudhills.

Hiking down Gower Gulch, you can see places where water has eroded the edges of the mudhills revealing the underlying sedimentary layers. It seems that the surface erodes and covers the hills with mud, making them look soft and rounded. There also seems to places where a volcanic conglomerate or pyroclastic rubble is mixed into the mud; makes you wonder if volcanic rocks were blasted into the ancient lake. The mudhills survived the eons because they were capped by basalt flows, and in places you can see the remains of the basalt cap on ridges south of the gulch.

After another 0.6 miles, you leave the mud hills and get into conglomerate rocks that form the lower portion of Gower Gulch and Golden Canyon (there are some sedimentary layers here too). At this point, you arrive at the borax mining area (Wpt. 7) where several mine shaft penetrate the sides of the canyon and an old road runs way up the hillside north of the wash. From the bottom of the canyon, you can't see any structures.

Just downstream from the mines, the canyon walls are polished conglomerate rocks with green cliffs, and there are ripple marks in some red rocks along the canyon wall. About 0.3 miles below the mining area, you arrive at the Gower Gulch pour-over (Wpt. 8), a 10-ft pour-over in the polished conglomerate rock. It is an easy 3rd-class scramble to get down the pour-over; there are some shorter scramble-downs in this section of the canyon too.

Below the pour-over, you can see a fairly new erosion channel cut into the old alluvial fan with great contrast between new (bright gray) and old (dark and desert varnished) alluvium. The new channel has 6- to 10-ft high sidewalls that keep the newer flows tightly concentrated and flowing all the way out into bottom of the valley.

After taking in the view, the route runs northward across ledges until reaching the gentle slopes on the floor of Death Valley. From there, the route continues wandering northward across the tops of several little alluvial fans to the Golden Canyon trailhead (Wpt. 01), which is about 0.8 miles north of the pour-over.