Scotty's Castle

In the northern part of the park near Scotty's Castle, this giant crater was formed by volcanic activity. Walking trails lead into and around the crater, but be warned - going down into the crater is a difficult undertaking, and it may be best to enjoy the view from the top.

An unimproved road into Death Valley that begins just west of Beatty (the road to Titus canyon heads north from the normal paved route from Beatty into Death Valley). Titus canyon is narrow, deep and spectacular. Due to narrowness, parts of this road are one-way, so you really need to start from the east end of the road. You don't need an off-road vehicle for this, normal cars should do fine, but don't bring the RV.

Tucked away in the north part of the park, accessible only by tens of miles of dirt road, these are the second tallest dunes in the United States. Don't let their out-of-the-way location deter you from visiting, however. The solitude only adds to the otherworldliness of the wind-swept sands, the highly rare Eureka Grass blades grasping for life in the dry mounds, and the panoramic view of the colorful Last Chance and Saline Ranges which flank the dunes on either side. Best route is around the park, CA 190 to US 395 north through Lone Pine.

In the backcountry near the Racetrack Playa, this signpost is decorated with numerous tea kettles and makes for a rather odd sight in the vast desert.

A popular hiking destination. While accessible only by a long, sandy road followed by a technical rock crawl through a wash, this hike is worth the headache (or fun) of getting to the base of the trail. Before you go, consult rangers about the location of various petroglyphs along the canyon walls. Though a fair few have been vandalized, many are in pristine condition.

As with many points of interest within the park, this one is not easily accessible. The main route consists of 27 mi of dirt road, beginning at the Ubehebe Crater in the northern part of the park. However, the effort is well-rewarded with a site of twilight-zone proportions. The Plestiocene-era lake bed, nearly 3 mi long and 1 mi wide, is so flat that it once used as a landing strip for drug smugglers. But the Racetrack is most famous for its "moving rocks": boulders whose erratic tracks remain visible for years. Though their movement has been tracked with GPS, no adequate explanation for it has been found. In the spring months, brine shrimp - which hibernate when the water dries up, only to emerge months or even years later - are sometimes visible in the muddy puddles here.