Devil’s Golf Course is one of the strangest landscapes in Death Valley National Park. Instead of rolling sand dunes or smooth white salt flats, this part of the valley floor is covered by an immense field of jagged salt formations—sharp ridges, knobs, spires, and crusts shaped by evaporation, rain, wind, and the repeated growth of salt crystals.
The surface is so rough that the name was inspired by the idea that only the devil could play golf on such a course. It is an appropriate description. What looks from a distance like a rough gray-brown field becomes much more dramatic up close, where individual salt structures rise in irregular clusters with edges hard and sharp enough to cause serious injury.
Devil’s Golf Course lies only a short distance from Badwater Basin, yet the two landscapes look surprisingly different. Badwater is famous for broad, relatively level salt flats and geometric polygons. Devil’s Golf Course reveals what happens when that same mineral-rich valley floor is uplifted, weathered, dissolved, recrystallized, and sculpted into a chaotic salt landscape.
It is one of the easiest geological attractions to combine with the destinations in our Top 10 Attractions in Death Valley National Park and makes a worthwhile stop on any trip based around Furnace Creek.
⚡ Fast Facts
| Location | Death Valley National Park, California |
| Landscape | Jagged salt pan |
| Basin | Badwater Basin |
| Elevation | Below sea level |
| Best Known For | Sharp salt pinnacles and irregular crystalline formations |
| Formation Process | Evaporation, salt crystallization, erosion and weathering |
| Access | Short unpaved road from Badwater Road |
| Main Activity | Scenic viewing and photography |
| Typical Visit | About 20–45 minutes |
| Restrooms | None at the viewpoint |
| Major Hazard | Extremely sharp, uneven salt formations |
| Best Season | Late fall through early spring |
🧂 What Is Devil’s Golf Course?
Devil’s Golf Course is part of the enormous salt pan occupying the floor of Death Valley.
At first glance, it may resemble a field of strangely shaped rocks. In reality, much of what visitors see consists of salt mixed with mud and other evaporite minerals.
The formations have been repeatedly altered by water and extreme desert weather.
Rain or floodwater dissolves portions of the salt. Intense heat evaporates moisture. New crystals form and expand. Wind and occasional rainfall further erode the exposed surface.
Over time, those processes create the rough towers, ridges, hollows, and blades visible today.
Unlike the smooth fairways implied by its name, Devil’s Golf Course may be one of the least playable landscapes imaginable.
😈 Why Is It Called Devil’s Golf Course?
The name comes from an old description suggesting the surface was so unbelievably rough that only the devil could play golf there.
The phrase captures the first impression remarkably well.
From the road, the landscape stretches outward as an almost continuous field of sharp salt formations. There are no greens, fairways, or smooth walking surfaces—only irregular chunks of crystallized salt.
The name is humorous, but visitors should not take the golf reference literally. This is a protected natural feature, and leaving golf balls, striking the formations, or treating the area as a novelty playground would damage the landscape.
The best way to experience Devil’s Golf Course is simply to stop, look closely, listen, and appreciate how ordinary salt can be transformed into such an unusual geological environment.
🌊 The Legacy of Ancient Lake Manly
The salt at Devil’s Golf Course is connected to a much larger story involving ancient lakes.
During cooler and wetter periods of the Pleistocene, Death Valley held a large lake commonly called Lake Manly.
Water flowed into the basin from surrounding mountains and distant drainage systems. Streams carried dissolved minerals with them.
Because Death Valley is an enclosed basin, the water had no outlet to the ocean.
As climate conditions became warmer and drier, evaporation increasingly exceeded the amount of water entering the valley. Lake levels fell and eventually disappeared.
The water vanished.
The minerals remained.
Over thousands of years, repeated cycles of flooding and evaporation concentrated enormous amounts of salt across the valley floor.
Devil’s Golf Course is one dramatic expression of that legacy.
💧 Why Salt Collects in Death Valley
Three ingredients help explain Death Valley’s extensive salt flats.
First, the valley receives runoff from an enormous surrounding drainage basin. Even though the desert itself is extremely dry, rain and snow falling on distant mountains eventually transport dissolved minerals downhill.
Second, Death Valley is an internally drained basin. Water reaching the lowest portions of the valley does not continue to the sea.
Third, evaporation greatly exceeds precipitation.
Temporary floodwater therefore disappears mainly through evaporation, leaving its dissolved minerals behind.
Repeat that process over thousands of years and layers of salt accumulate.
Sodium chloride—the same mineral commonly known as table salt—is abundant, but Death Valley’s evaporite deposits also contain minerals such as gypsum, calcite, and borates.
🧂 Why Devil’s Golf Course Looks Different From Badwater Basin
Visitors often wonder why nearby Badwater Basin looks relatively smooth while Devil’s Golf Course resembles a frozen ocean of jagged salt.
The answer involves differences in the salt surface and the ways water, crystallization, and erosion have acted upon it.
Badwater’s most famous areas frequently display broad salt polygons. Moisture rises through the salty mud, evaporates, and deposits crystals along cracks. Repeated growth can push the edges of polygons upward into distinctive ridges.
At Devil’s Golf Course, the surface has been weathered into much rougher formations.
Water dissolves exposed salt and later evaporates. Crystals expand and grow. Rain and wind reshape the surface. Continued weathering creates the serrated pinnacles that distinguish the area.
Both landscapes are part of the same immense salt basin, yet small differences in surface conditions can produce dramatically different results.
That contrast is one reason it is worth visiting both places rather than assuming one salt-flat stop is enough.
🪨 Is It Really Rock Salt?
Much of the strange terrain is composed of rock salt, or halite, mixed with mud and other minerals.
Halite is the mineral form of sodium chloride.
In a kitchen, salt appears as tiny crystals. At Devil’s Golf Course, the same basic mineral occurs in massive natural deposits that have accumulated, dissolved, recrystallized, and hardened over long periods.
The result feels much more like rough stone than loose salt.
That hardness can surprise visitors.
Some projections are strong enough to cause deep cuts if someone falls onto them, while other sections remain fragile enough to break when stepped on.
This unusual combination—hard enough to injure you yet delicate enough to damage—is one reason walking extensively across the formations is discouraged.
👂 Listen to the Salt
Devil’s Golf Course is interesting not only to look at but also to listen to.
During changing temperatures, visitors may hear faint popping or pinging sounds coming from the salt.
These sounds occur as salt crystals expand and contract in response to heating and cooling.
On a quiet day, particularly when there are few vehicles or people nearby, the sounds can be surprisingly noticeable.
It creates an unusual experience: a landscape that appears completely still is actually undergoing tiny physical changes around you.
The salt pan is not a dead or frozen surface.
It continues responding to temperature, moisture, flooding, and evaporation.
☀️ Extreme Heat Shapes the Landscape
Death Valley’s intense heat is central to the formation and continued evolution of its salt environments.
Water entering the basin does not remain for long under normal conditions.
Strong sunlight and extremely dry air cause rapid evaporation, leaving dissolved minerals behind.
Summer temperatures on the valley floor can exceed 120°F, creating conditions in which evaporation becomes especially intense.
Temperature swings also influence individual crystals.
Salt expands and contracts as conditions change, gradually contributing to cracking and fragmentation.
The landscape may look permanent from a human perspective, but it is constantly being altered at a small scale.
🌧️ What Happens When It Rains?
Rain can dramatically transform Death Valley’s salt pan.
Water flowing from surrounding mountains may temporarily spread across the basin floor, dissolving surface salts and carrying additional minerals into low areas.
When the water eventually evaporates, salt recrystallizes.
Heavy rainfall can produce temporary lakes in portions of Death Valley, as has occurred repeatedly in modern times.
These flooding events can erase some existing salt patterns while creating entirely new surfaces.
The phenomenon provides an important reminder that Death Valley’s salt flats are not ancient relics that stopped changing thousands of years ago.
The landscape is still active.
🌊 Temporary Lakes in Death Valley
After unusually heavy storms, visitors may encounter something that appears completely out of place in Death Valley: water stretching across the desert floor.
Temporary lakes can form within Badwater Basin when rainfall and runoff arrive faster than evaporation can remove them.
Historically, this modern temporary water has sometimes been informally referred to as Lake Manly, after the much larger prehistoric lake.
Reflections of the Panamint Range in standing water can create spectacular scenes, but flooding also affects roads and access to attractions such as Devil’s Golf Course.
Visitors should never assume that a road open during one Death Valley trip will remain open after the next major storm.
Checking current conditions is particularly important in this park.
🏔️ A Basin Surrounded by Mountains
Devil’s Golf Course becomes even more impressive when viewed in the context of the mountains surrounding it.
To the west rises the Panamint Range, including 11,049-foot Telescope Peak.
The Black Mountains rise along the eastern side of the valley.
Between them lies the deep structural basin of Death Valley.
This enormous difference in elevation is central to the park’s character.
The valley floor continues to sink along faults while surrounding mountain blocks rise and erode.
Material washed from those mountains gradually accumulates below.
Some of the sediment and salt beneath Badwater Basin extends thousands of feet below the visible surface.
What appears to be a flat desert floor is actually the top of an enormous accumulation of material filling a continually evolving geological basin.
🌎 The Basin and Range Province
Death Valley lies within the Basin and Range Province, a region where Earth’s crust has been stretched and broken into large fault-bounded blocks.
Some blocks have risen to create mountain ranges.
Others have dropped to form valleys.
Death Valley represents one of the most dramatic examples of this process.
Movement along faults near the Black Mountains continues to lower portions of the basin, while erosion steadily transports material down from higher elevations.
The result is a landscape shaped by two seemingly opposite processes at once: tectonic activity creates relief while erosion tries to fill it in.
Devil’s Golf Course occupies the lowest part of that geological system.
🧂 Salt Is Still Forming
It is tempting to think of the Death Valley salt pan as a deposit left behind once when an ancient lake disappeared.
The process is actually ongoing.
Every flood has the potential to carry additional dissolved minerals into the basin.
Water evaporates.
More crystals remain.
Existing salt dissolves and forms again elsewhere.
Wind brings dust onto the surface.
Mud accumulates beneath the salt crust.
Crystals grow and break.
The salt pan is therefore continually being recycled rather than simply sitting unchanged on the valley floor.
Devil’s Golf Course is one stage in that ongoing cycle.
🚗 Getting to Devil’s Golf Course
Devil’s Golf Course is reached from Badwater Road, south of Furnace Creek.
A short unpaved side road leads west toward a small parking area at the edge of the salt formations.
The road is relatively short compared with Death Valley’s true backcountry routes, but conditions can change after flooding.
Washouts, mud, loose gravel, and storm damage can temporarily affect access.
Check current Death Valley road conditions before driving there, especially after significant rain.
Unlike the remote journey to The Racetrack, Devil’s Golf Course normally fits easily into a day of sightseeing along Badwater Road.
🗺️ Combining Devil’s Golf Course With Nearby Attractions
Devil’s Golf Course is particularly convenient because several major Death Valley attractions lie nearby.
A trip south from Furnace Creek can include Golden Canyon, Artist’s Drive, Devil’s Golf Course, and Badwater Basin without requiring huge detours.
That makes the area ideal for first-time visitors.
A typical day might begin at Zabriskie Point, continue south along Badwater Road, stop at Devil’s Golf Course and Badwater Basin, and return through Artist’s Drive later in the day.
For a broader itinerary, see our Top 10 Attractions in Death Valley National Park.
⏰ How Long Do You Need?
Most visitors need only 20 to 45 minutes at Devil’s Golf Course.
There is no long developed hiking trail to complete.
The main experience involves stopping at the parking area, examining the salt formations, taking photographs, and appreciating the surrounding mountains.
Visitors particularly interested in geology or photography may want to stay longer.
That short visit makes Devil’s Golf Course easy to include even on a busy Death Valley sightseeing day.
Its visual impact is much greater than the amount of time required to see it.
🥾 Do You Need to Hike?
No significant hike is necessary.
The salt formations begin almost immediately beyond the parking area, and excellent views are available without walking deeply onto the rough surface.
In fact, wandering far across the formations is generally unnecessary and can be hazardous.
Anyone who does step beyond the parking area should move very carefully.
There is no smooth trail through the salt field.
Each step may involve irregular surfaces, deep gaps, unstable crystals, or extremely sharp projections.
For visitors primarily interested in hiking, better options are available elsewhere in Death Valley through the routes in our Trails & Hiking collection.
⚠️ Why Walking on the Salt Can Be Dangerous
The salt formations can be razor-sharp.
A slip or fall that would produce a scrape on an ordinary trail can result in significant cuts at Devil’s Golf Course.
The surface is also extremely uneven.
Deep gaps can occur between formations, while apparently stable surfaces may crumble under pressure.
The safest approach is to appreciate the landscape close to the parking area rather than attempting to cross large sections of it.
Closed-toe shoes with sturdy soles are a much better choice than sandals if you plan to step onto the salt.
Children should be supervised closely.
♿ Accessibility
Devil’s Golf Course can be appreciated without walking onto the salt field.
Views are available directly from the parking area, making the attraction more accessible to visitors who cannot negotiate rough terrain.
The parking area itself is gravel rather than a fully developed paved overlook, and there are no designated accessible parking spaces.
There are also no restrooms at Devil’s Golf Course.
The closest facilities are in the Badwater Basin area a short drive away.
Visitors with specific accessibility needs should review current National Park Service guidance when planning the stop.
🚻 Facilities
Devil’s Golf Course is a simple roadside attraction rather than a developed visitor complex.
There is no visitor center.
There is no drinking water.
There are no restrooms.
There is no food or fuel.
Most visitors will use services around Furnace Creek before traveling south along Badwater Road.
Carry water even when planning only short stops. Death Valley’s extreme dryness and heat can make dehydration a concern much faster than visitors expect.
🌡️ Visiting in Summer
Summer is the most challenging season for visiting Devil’s Golf Course.
Temperatures on the valley floor can become dangerously high.
Because the attraction requires only a short walk from the vehicle, it may still be possible to view during hot weather, but visitors should minimize exposure during extreme conditions.
Remain close to a functioning air-conditioned vehicle.
Carry abundant water.
Wear sun protection.
Avoid wandering far across the salt.
Do not treat a short distance from the parking lot as evidence that heat cannot become dangerous.
In Death Valley, serious heat illness can develop quickly.
🍂 Best Time to Visit
For most visitors, late fall through early spring offers the most comfortable conditions.
Cooler daytime temperatures make it much more pleasant to spend time examining the salt formations and exploring nearby attractions.
Winter can bring cold mornings despite Death Valley’s reputation for heat.
Spring temperatures rise quickly, while autumn gradually becomes more comfortable as the extreme summer heat fades.
The attraction itself changes subtly with moisture, recent flooding, sunlight, and crystal growth, so there is no single season in which the formations always look exactly the same.
🌅 Best Time of Day
Early morning and late afternoon usually provide the most interesting light.
When the sun is low, shadows emphasize the rough texture of individual formations.
Midday light tends to flatten those details and can make the landscape appear more uniformly pale.
Late afternoon can be particularly attractive when warm light reaches the surrounding mountains.
Photographers should remember that the salt formations are part of a protected landscape.
A better angle is never worth breaking crystals or risking injury.
📷 Photography Tips
The great photographic challenge at Devil’s Golf Course is conveying texture.
A wide landscape image can show how far the salt formations extend, while closer compositions reveal individual ridges and crystals.
Low-angle light helps tremendously.
Including the Panamint Range in the background provides a sense of scale and connects the salt field to the wider Death Valley landscape.
Rather than walking far out to find an untouched foreground, work carefully around durable areas near established access.
The rough salt itself provides almost endless patterns without requiring much movement.
👂 Stop and Listen
One of the easiest things to miss is the sound of the salt.
Turn off the car.
Stand quietly.
When conditions are right, faint pops, pings, and cracking noises may come from the formations as crystals respond to temperature changes.
The sounds are subtle and easy to lose beneath voices, vehicles, or wind.
Hearing them changes the character of the place.
The salt field no longer seems like a static collection of rocks.
It becomes an active mineral surface responding to the desert environment in real time.
🌱 Does Anything Live Here?
The salt pan itself is an extremely difficult environment for most plants and animals.
High salinity, extreme heat, limited fresh water, and intense solar exposure create conditions few organisms can tolerate.
However, Death Valley as a whole supports far more life than its name suggests.
Plants and animals occupy nearby springs, alluvial fans, mountains, canyons, dunes, and other habitats where conditions are less extreme.
Even hypersaline environments can support specialized microorganisms.
The relative biological emptiness of Devil’s Golf Course therefore contrasts sharply with surprisingly rich ecosystems elsewhere in the park.
Explore more of those environments through our Wildlife & Plants hub.
🧂 Devil’s Golf Course vs. Badwater Basin
These two attractions are close together, but they are not interchangeable.
Badwater Basin is the place to experience the broad scale of the salt flat and stand at the lowest point in North America. Visitors can walk outward across relatively level areas and see the famous polygonal salt patterns.
Devil’s Golf Course is about texture.
Its surface is rough, jagged, chaotic, and difficult to cross.
Badwater emphasizes space.
Devil’s Golf Course emphasizes structure.
Visiting both provides a much better understanding of Death Valley’s salt landscape than seeing either location alone.
🪨 Devil’s Golf Course vs. The Racetrack
The Racetrack is another dry-lake landscape in Death Valley, but it differs dramatically from Devil’s Golf Course.
The Racetrack is famous for its exceptionally flat clay playa and stones that occasionally move across the surface under rare icy conditions.
Devil’s Golf Course consists primarily of rough salt formations and requires only a short side trip from Badwater Road.
The Racetrack requires a demanding backcountry drive.
The two places show opposite expressions of enclosed desert basins: one remarkably flat and smooth, the other extraordinarily rough.
🌊 Devil’s Golf Course vs. a Normal Salt Flat
The word salt flat can create the expectation of a smooth, white plain.
Devil’s Golf Course challenges that image.
Salt deposits do not always remain level.
Water can dissolve them unevenly.
Crystals grow in cracks.
Moisture moves through mud beneath the surface.
Temperature changes expand and contract minerals.
Rain and wind erode exposed formations.
Over time, a once flatter salt surface can become a complicated field of pinnacles and ridges.
That is what makes this site so valuable for understanding desert geology. It shows that even seemingly simple salt deposits can evolve into elaborate landforms.
🏜️ A Landscape That Is Still Changing
Death Valley often appears timeless, but Devil’s Golf Course demonstrates that change is ongoing.
Every rainstorm alters the salt.
Every flood dissolves and redistributes minerals.
Every period of evaporation encourages new crystal growth.
Temperature changes fracture existing structures.
Wind removes small particles.
Meanwhile, tectonic processes continue shaping the entire basin.
The changes may be difficult to notice during a half-hour visit, but return after enough time and the details will not be identical.
Devil’s Golf Course is better understood as an active geological process than as a finished geological object.
🚫 Protecting the Salt Formations
The rough surface may look indestructible, but many formations are surprisingly fragile.
Climbing on them can break crystals.
Repeated footsteps can damage distinctive structures.
Driving beyond established roads can leave tracks that persist for years.
Avoid collecting salt or mineral pieces.
Everything within the national park should remain where it formed.
The best rule is simple: look closely without trying to modify what you see.
Future visitors deserve to experience the same strange landscape.
🚙 Check Road Conditions First
The access road to Devil’s Golf Course is unpaved and can be affected by storms.
Death Valley regularly experiences flash flooding capable of damaging roads throughout the park.
Even routes that are normally easy can close temporarily.
Mapping apps may not always reflect current park conditions.
Before heading south from Furnace Creek, check the National Park Service’s latest road and weather information.
This becomes particularly important following monsoon storms, atmospheric rivers, or other significant rainfall events.
For broader preparation advice, visit our National Park Travel & Planning hub.
🗺️ A Good Death Valley Day Trip
Devil’s Golf Course works best as part of a larger day around the central and southern valley.
Start around sunrise at Zabriskie Point.
Continue toward Furnace Creek and then south along Badwater Road.
Visit Badwater Basin, followed by Devil’s Golf Course and the colorful hills along Artist’s Drive.
Depending on the season and available time, add a hike in Golden Canyon or finish the day with panoramic views from Dante’s View.
This itinerary moves through badlands, salt flats, mountains, canyons, and mineral-colored hills without requiring the remote backcountry driving needed to reach places like the Racetrack.
🌄 Is Devil’s Golf Course Worth Visiting?
Yes—especially because it requires relatively little time.
Devil’s Golf Course may not be the first Death Valley attraction most travelers recognize by name, but there are few other landscapes quite like it.
Badwater Basin is grander.
Zabriskie Point is more colorful.
Mesquite Flat Sand Dunes fit the traditional image of a desert more closely.
But Devil’s Golf Course is strange.
The entire valley floor seems to have hardened into a violent frozen sea of salt.
Walk carefully toward the edge, look closely at the crystal structures, and listen for faint cracking sounds as the salt responds to the heat.
It is an excellent reminder that some of Death Valley’s most interesting landscapes reveal themselves not through enormous size but through the details beneath your feet.
🌵 Why Visit Devil’s Golf Course?
Devil’s Golf Course tells the geological story of Death Valley in a remarkably compact area.
Ancient lakes once occupied the basin.
Mountains supplied minerals.
Water carried those minerals toward the lowest point.
Climate became hotter and drier.
Lakes disappeared.
Salt accumulated.
Floods returned temporarily.
Water dissolved the surface again.
Evaporation created new crystals.
Wind, rain, and heat transformed those deposits into the jagged landscape visible today.
The result looks almost alien, yet every formation comes from ordinary natural processes working over extraordinary spans of time.
That is what makes Devil’s Golf Course such a worthwhile stop in Death Valley National Park.
It is not simply a field of salt.
It is a landscape still being built, dissolved, broken, and rebuilt by the desert.
🔗 Related Articles
- Death Valley National Park
- Top 10 Attractions in Death Valley National Park
- Furnace Creek
- The Racetrack
- U.S. National Parks
- Trails & Hiking
- Wildlife & Plants
- National Park Travel & Planning
📚 Sources & Further Reading
- National Park Service — Devil’s Golf Course
- National Park Service — Death Valley National Park
- National Park Service — Death Valley Salt Flats
- National Park Service — Death Valley Geology
- National Park Service — Death Valley Faults
- National Park Service — Death Valley Current Conditions
- National Park Service — Death Valley Safety
- National Park Service — Sightseeing & Hiking Accessibility
