Badwater Basin is the lowest point in North America and one of the defining landscapes of Death Valley National Park. At 282 feet below sea level, the basin spreads across the floor of Death Valley in an immense expanse of salt, mud, mineral crust, and temporary pools framed by some of the park’s highest mountains.
The landscape is famous for its brilliant white salt flats and geometric salt polygons, but Badwater is much more than a place to stand beside an elevation sign. It is the end point of a huge desert drainage system, the remnant of ancient lakes, a living environment for salt-tolerant organisms, and one of the best places in the park to understand how water, minerals, climate, and geology interact in an enclosed desert basin.
Across the valley, Telescope Peak rises to 11,049 feet in the Panamint Range. From Badwater, its summit is more than two vertical miles above you. Few places in North America reveal such an extraordinary difference in elevation within such a short distance.
Badwater Basin is an essential stop on a first trip to Death Valley and one of the highlights featured in our Top 10 Attractions in Death Valley National Park.
⚡ Fast Facts
| Location | Death Valley National Park, California |
| Elevation | 282 ft / 86 m below sea level |
| Significance | Lowest point in North America |
| Landscape | Salt flats, saline pools and desert basin |
| Salt Flat Area | Nearly 200 square miles |
| Main Mineral | Sodium chloride |
| Other Minerals | Calcite, gypsum and borax |
| Ancient Lake | Lake Manly |
| Major Mountain View | Telescope Peak, 11,049 ft |
| Access | Paved Badwater Road |
| Walking | Boardwalk plus optional walk onto salt flats |
| Best Season | Late fall through early spring |
| Major Hazard | Extreme heat |
| Nearest Main Visitor Hub | Furnace Creek |
🧂 The Lowest Point in North America
Badwater Basin reaches 282 feet below sea level, making it the lowest land elevation in North America.
That number becomes much easier to appreciate when you arrive.
After parking, look across Badwater Road toward the steep Black Mountains. High on the rock face is a sign marking sea level.
The marker appears surprisingly far overhead.
Standing beside the salt flats while looking upward toward where the ocean’s surface would theoretically be provides a much stronger sense of Badwater’s elevation than simply reading “-282 feet” on a map.
The landscape becomes even more dramatic when you turn west.
Across the basin, Telescope Peak rises more than 11,000 feet above sea level, creating an extraordinary vertical contrast between the lowest and highest portions of the park.
🌎 Why Is Death Valley So Low?
Badwater exists because Death Valley lies within the Basin and Range Province, a vast region where Earth’s crust has been stretched and broken by faults.
Over millions of years, large blocks of crust shifted relative to one another.
Some rose to form mountain ranges.
Others dropped to form basins.
Death Valley is one of the most dramatic results of that process.
Faulting along the eastern side of the valley helped lower the basin while the Black Mountains rose nearby. At the same time, erosion carried tremendous amounts of sediment from the surrounding mountains into the valley.
The process continues.
Death Valley is not simply an ancient depression that stopped changing long ago. Tectonic movement and erosion continue shaping the basin today.
🏔️ Telescope Peak From Badwater
Looking west from Badwater Basin, the most prominent mountains belong to the Panamint Range.
Their highest summit is Telescope Peak, at 11,049 feet.
The contrast is extraordinary.
Badwater sits 282 feet below sea level, while Telescope Peak rises more than two vertical miles above it.
The horizontal distance between the two is surprisingly small for such an enormous elevation difference.
During winter, Telescope Peak may be covered in snow while Badwater remains dry and comparatively mild.
In summer, the salt basin can experience extreme heat while the summit is considerably cooler.
That enormous elevation range is one reason Death Valley National Park contains far more ecological diversity than its name suggests.
🧂 Nearly 200 Square Miles of Salt Flats
The Badwater salt flats extend across nearly 200 square miles of the valley floor.
Visitors see only a small portion of that enormous area from the main parking lot.
The white surface stretches north and south through the lowest portions of Death Valley, sometimes looking almost like snow when seen from a distance.
It is not one solid slab of salt.
The upper surface includes layers of salt, mud, water, and other evaporite minerals that change in response to flooding, groundwater, evaporation, and weather.
Some sections form smooth polygon patterns.
Others become rough and uneven.
Still others may be temporarily covered by water after unusually heavy rainfall.
🧂 Where Does All the Salt Come From?
Badwater’s salt did not originate in one enormous deposit.
Instead, minerals have been accumulating gradually for thousands of years.
Death Valley receives drainage from a huge surrounding watershed covering thousands of square miles.
Rain and snow falling on distant mountains begin moving downhill.
As water travels across and through rock, it dissolves small amounts of minerals.
Streams, floods, groundwater, and washes then carry those dissolved minerals toward lower elevations.
Because Death Valley is a closed basin, much of that water eventually reaches the valley floor but has no route to the ocean.
The water evaporates.
The minerals remain.
Repeat this process for thousands of years and enormous deposits of salt accumulate.
💧 Why Doesn’t the Salt Wash Away?
In most landscapes, rivers eventually carry dissolved minerals downstream to lakes or oceans.
Death Valley works differently.
It is an internally drained basin.
Water flows toward the lowest areas but does not continue through a river to the sea.
Badwater therefore acts as a kind of terminal collection point.
Minerals enter the basin much more easily than they leave.
Death Valley’s extremely dry climate intensifies the process because evaporation greatly exceeds rainfall.
Water disappears into the atmosphere while the minerals it transported stay behind.
🧂 What Kind of Salt Is at Badwater?
The largest component of the visible salt deposits is sodium chloride, the same mineral commonly known as table salt.
The basin also contains other evaporite minerals, including calcite, gypsum, and borax.
These minerals were carried into the basin through the same long-term process of weathering, runoff, groundwater movement, and evaporation.
Their presence connects Badwater with Death Valley’s famous mining history.
Borate minerals extracted elsewhere in the valley helped make Death Valley internationally known during the late nineteenth century.
Today, the salt flats are protected geological features rather than mineral resources waiting to be collected.
⬡ The Famous Salt Polygons
One of Badwater Basin’s most recognizable features is its network of geometric salt polygons.
These patterns often resemble giant white tiles separated by raised edges.
They form as groundwater and moisture move through salty sediment beneath the surface.
Water evaporates, leaving new salt crystals behind.
Crystals continue growing and expanding around existing cracks.
Over time, this process can push the edges upward into ridges, creating polygonal patterns across the surface.
The polygons are not permanent.
Rain dissolves salt.
Floods rearrange it.
Groundwater brings new minerals upward.
Evaporation creates new crystals.
The surface is continually being rebuilt.
👣 Walking Out Onto the Salt Flats
The experience changes dramatically when you leave the boardwalk area and walk farther onto the basin.
Close to the parking lot, the salt can appear rough, muddy, or heavily traveled.
Farther out, broader white expanses and more clearly developed polygon patterns often become visible.
Visitors seeking the classic Badwater salt-flat landscape should allow time to walk beyond the immediate roadside area.
A round trip of roughly 1.5 to 2 miles provides a better opportunity to see expansive polygon fields, though exact conditions vary as the salt surface changes.
There is no need to walk to the apparent middle of the basin.
The landscape is enormous, distances are deceptive, and heat exposure increases quickly.
🚶 The Boardwalk
A ramp and boardwalk lead from the parking area toward the salt pool and the edge of the basin.
This developed area provides an easy introduction to Badwater without requiring a long hike.
From here, visitors can see the saline water, salt deposits, surrounding mountains, and sea-level marker on the cliffs across the road.
Beyond the boardwalk, visitors can continue onto the salt flat itself when conditions permit.
The terrain becomes natural and increasingly uneven farther from the developed access.
💧 The Badwater Pool
Beside the boardwalk is a small spring-fed saline pool.
The water has played an important role in the origin of the name Badwater.
Despite its appearance, the pool is not poisonous.
It is simply extremely salty.
Groundwater reaches the surface along faults near the base of the Black Mountains, producing a rare aquatic environment within one of the driest regions in North America.
The pool should be observed without entering or disturbing it.
Although small compared with the enormous salt basin surrounding it, it supports specialized organisms capable of surviving conditions that would be unsuitable for most freshwater species.
🐌 Life in Bad Water
Badwater’s salty pool demonstrates that even extreme environments can support life.
A tiny endemic snail lives in this unusual habitat, while salt-tolerant plants such as pickleweed can grow near portions of the water.
The environment is difficult.
Salinity is high.
Temperatures can be extreme.
Fresh water is scarce.
Yet organisms have evolved ways to survive.
Badwater is therefore not a lifeless wasteland. It is a specialized ecosystem whose inhabitants are adapted to conditions that exclude most other species.
For more about life in extreme park environments, visit our Wildlife & Plants hub.
🐴 How Badwater Got Its Name
A popular story explains that an early surveyor arrived at the spring with his mule.
The animal refused to drink.
The surveyor supposedly marked the location as having “bad water.”
The water was not poisonous—it was simply too salty for the mule.
Whether every detail of the story happened exactly as later retellings describe is less important than the name it produced.
“Badwater” became permanently attached to one of the most famous places in Death Valley.
Ironically, the small pool that inspired the name exists within a landscape where any naturally occurring water is remarkable.
🌊 Ancient Lake Manly
The modern salt basin is the descendant of a much wetter landscape.
During cooler periods of the Pleistocene, a large lake occupied Death Valley.
Today it is generally known as Lake Manly.
At various times, the lake was many miles long and hundreds of feet deep.
Streams and rivers carried water into the basin from a much larger regional drainage system than exists today.
As the climate became warmer and drier, incoming water declined while evaporation increased.
The lake shrank.
Eventually, the permanent body of water disappeared, leaving behind sediments and increasingly concentrated minerals.
Today’s Badwater salt flats are part of that long transition from lake to desert basin.
🌧️ When Lake Manly Returns
The ancient Lake Manly is gone, but temporary lakes still appear at Badwater after unusually heavy rainfall.
When enough water runs into the basin faster than it can evaporate, a shallow lake can spread across parts of the salt flat.
Recent storms have demonstrated just how dramatically the landscape can change.
A place normally associated with brilliant white salt can suddenly contain broad stretches of water reflecting the Panamint Mountains.
These modern temporary lakes are sometimes informally called Lake Manly, after their ancient predecessor.
They should not be confused with the much larger prehistoric lake.
Modern flooding is temporary. Eventually, evaporation removes the water and salt flats reappear.
🌧️ How Flooding Changes the Salt
Floodwater does more than cover the salt.
It reshapes it.
Salt dissolves back into the water.
Mud and sediment arrive from surrounding mountains.
Existing polygons may disappear.
As the water evaporates, minerals crystallize again.
A surface that looked rough before a flood may later appear brighter and smoother.
New patterns develop.
Dust that accumulated over previous years may be washed away.
This continual cycle is why Badwater should not be viewed as a finished landscape.
It is actively changing every time water reaches the basin.
☀️ Why Badwater Is So Hot
Badwater lies at the bottom of a deep desert basin surrounded by high mountains.
Its extremely low elevation is one ingredient in Death Valley’s famous heat.
Air descending into the valley becomes compressed and warms.
The surrounding mountains create strong rain shadows, limiting moisture.
Clear skies allow intense solar radiation to reach the ground.
The valley floor absorbs that energy and radiates heat.
During summer, the result can be extraordinary.
Temperatures around central Death Valley routinely reach dangerous levels, while surface temperatures exposed to direct sun can be even hotter.
🌡️ Summer at Badwater Basin
Summer requires extreme caution.
Badwater is one of the lowest, hottest, most exposed locations in the park.
There is almost no shade once you walk beyond the parking area.
A trip that feels easy during winter can become dangerous under summer conditions.
During extreme heat, limit your time away from an air-conditioned vehicle and avoid walking far onto the salt flats.
Carry abundant drinking water even for a short visit.
Heat illness can develop quickly, and the dazzling salt surface provides almost no protection from the sun.
A planned walk to distant salt polygons is never worth risking heat stroke.
🥵 The Salt Reflects Heat & Light
Badwater can feel particularly intense because the pale salt reflects sunlight while the surrounding terrain radiates heat.
Visitors are exposed from above and below.
Sunglasses can make a major difference on bright days.
A hat, sunscreen, long lightweight clothing, and adequate water are also useful.
Footwear matters as well.
The salt surface may be rough, muddy beneath a thin crust, or broken by irregular holes and ridges.
Closed-toe walking shoes are much better suited to the environment than bare feet.
🍂 Best Time to Visit
For most travelers, November through March provides the most comfortable conditions.
Cooler weather allows visitors to spend more time walking across the salt flats without the extreme heat that defines summer.
Late autumn and early spring can also be excellent, although temperatures may rise quickly.
Winter mornings can feel surprisingly cool, particularly before sunlight reaches the entire basin.
Weather varies substantially from year to year, so visitors should check the current forecast rather than assuming Death Valley is always hot.
🌅 Sunrise
Badwater can be beautiful around sunrise.
Early light reaches the high Panamint Range while the basin remains partly in shadow.
The salt flats gradually brighten as sunlight moves across the valley.
Temperatures are also generally at their lowest near this time.
Photographers often benefit from arriving before direct sunlight reaches the salt because softer light preserves details that can disappear under harsh midday glare.
A calm morning after unusual rainfall can be especially striking if standing water reflects the surrounding mountains.
🌇 Sunset
Sunset produces a different atmosphere.
The Panamint Range blocks the sun to the west, allowing much of the basin to fall into shadow before the sky itself becomes dark.
Warm light may remain on the mountains while the salt flats turn cooler in color.
Because Badwater lies at the base of the Black Mountains, direct sunlight disappears from parts of the basin earlier than visitors might expect.
Stay through twilight for subtler colors and a quieter atmosphere.
Bring a light if you plan to walk far from the parking area.
🌌 Badwater After Dark
The immense open basin offers spectacular views of the night sky.
Away from major urban areas, Death Valley’s darkness allows thousands of stars to become visible.
The white salt can provide an excellent foreground for night photography.
Moonlight creates a particularly unusual scene.
A bright moon can illuminate the salt flats enough to reveal mountain outlines and surface textures, while a moonless night provides darker conditions for observing the Milky Way.
Visitors exploring after dark should remain aware of navigation. The parking area can become difficult to locate once you walk far onto an almost featureless basin.
📷 Photographing Badwater Basin
Badwater offers two very different photographic approaches.
Wide compositions emphasize the enormous scale of the salt flats and surrounding mountain ranges.
Closer images focus on geometric salt polygons, crystalline textures, cracks, and patterns.
A low camera position can make polygon ridges appear much larger and create strong lines leading toward the Panamint Mountains.
Sunrise and sunset usually produce more interesting shadows than midday.
After rainfall, reflections may create entirely different compositions.
Never break or rearrange salt formations for a photograph.
The surface will change naturally without human help.
🪧 Find the Sea-Level Sign
One of the simplest things to do at Badwater is turn around.
Visitors naturally look west across the salt flat, but the Black Mountains immediately east of the parking area contain one of the site’s best interpretive features.
High on the mountainside is a SEA LEVEL sign.
The distance between that sign and the basin floor visually represents the depth of Badwater below the ocean’s surface.
It is an easy feature to miss if you arrive focused entirely on the salt.
Once you see it, the meaning of 282 feet below sea level becomes much more tangible.
🏔️ Badwater & Dante’s View
Dante’s View provides one of the best complementary experiences to Badwater Basin.
At Badwater, you stand at the bottom of Death Valley looking toward the mountains.
At Dante’s View, you stand more than a mile above the salt flats in the Black Mountains and look down across the basin.
Visiting both creates an extraordinary sense of scale.
The parking area at Badwater becomes almost impossible to distinguish from above.
The huge salt flats appear as a narrow white strip.
The Panamint Range that towered over you from the basin becomes part of a much larger panorama.
If possible, include both on your Death Valley itinerary.
🧂 Badwater vs. Devil’s Golf Course
Devil’s Golf Course lies nearby and is part of the same broader salt basin, but the two sites look remarkably different.
Badwater is best known for broad flats and geometric salt polygons.
Devil’s Golf Course consists of rough, jagged salt formations that rise above the surface in chaotic ridges and pinnacles.
Badwater feels expansive.
Devil’s Golf Course feels textured and hostile.
Visiting both provides a much better understanding of what salt can do when water, evaporation, groundwater, and weather act on different parts of the same basin.
🏜️ Badwater vs. Mesquite Flat Sand Dunes
Mesquite Flat Sand Dunes show another completely different Death Valley landscape.
Badwater is dominated by salt and mud deposited at the lowest point of an enclosed basin.
Mesquite Flat is built from sand transported and sculpted by wind.
The two sites also challenge a common misconception about deserts.
Death Valley is not one enormous field of dunes.
Most of the park consists of mountains, gravel fans, canyons, playas, salt flats, and rocky terrain.
Sand dunes occupy only a relatively small portion.
🌄 Badwater vs. Zabriskie Point
Zabriskie Point overlooks colorful badlands carved into ancient sediments.
Badwater lies on the flat basin floor below the surrounding mountain ranges.
The landscapes could hardly look more different, yet water plays a major role in both.
Flash floods carve Zabriskie’s gullies.
Floods and groundwater help shape Badwater’s salt flats.
A first-time visitor can experience both locations in the same day, moving from deeply eroded hills to an almost perfectly flat mineral basin.
🥾 Badwater vs. Golden Canyon
Golden Canyon is the better choice for visitors looking for a conventional hike.
Its routes wind through badlands toward Red Cathedral, Gower Gulch, and Zabriskie Point.
Badwater is more open.
There is no canyon directing your route and no summit to reach.
The experience is primarily about walking onto the salt, understanding the extreme elevation, and appreciating the enormous surrounding landscape.
During cool weather, combining both provides an excellent balance between hiking and sightseeing.
🪨 Badwater vs. The Racetrack
The Racetrack is another dry-basin landscape, but reaching it requires a long journey over a rough backcountry road.
Badwater is reached by paved road and is one of the easiest major destinations to visit.
The Racetrack is known for clay playa and rocks that occasionally move under rare combinations of water, ice, and wind.
Badwater is defined by enormous evaporite deposits and salt polygons.
Both landscapes reveal what happens when water enters a desert basin but has no route to the sea.
🚗 Getting to Badwater Basin
Badwater Basin lies along Badwater Road, approximately 17 miles south of Furnace Creek.
Under normal conditions, the drive takes about half an hour.
The road is paved and suitable for ordinary passenger vehicles.
The route passes several other major Death Valley attractions, making Badwater easy to include in a central-valley sightseeing day.
Storms and flash floods can occasionally damage roads, so current conditions should always be checked after significant rainfall.
🅿️ Parking
A paved parking area sits directly across from the salt basin.
Spaces accommodate ordinary vehicles as well as larger buses and RVs.
Badwater is extremely popular, particularly during the winter visitor season, so the parking area can become busy.
If the lot is full, wait for a legal parking space rather than damaging roadside terrain.
Visitors arrive and depart frequently, so turnover is usually steady.
♿ Accessibility
Badwater Basin is one of the more accessible major natural attractions in Death Valley.
Accessible parking is provided, and a ramp leads toward the boardwalk and salt pool.
The developed portion offers views of the basin without requiring a long walk.
Beyond the boardwalk, the surface becomes natural salt terrain.
Conditions vary and may include rough crust, holes, mud, and uneven formations.
Visitors with mobility limitations can still experience the extraordinary elevation and broad landscape from the developed viewing area.
🚻 Facilities
Vault toilets are available at the parking area.
There is no drinking water, restaurant, fuel, or visitor center at Badwater Basin.
The main nearby services are at Furnace Creek.
Fill water containers and obtain supplies before heading down Badwater Road.
That is especially important during warm weather, even if you expect to spend only a short time at Badwater.
🐕 Pets
Pets are not permitted on Death Valley hiking trails, including the route onto the Badwater salt flats.
They also should never be left in a vehicle during warm or hot weather.
Interior vehicle temperatures can rise rapidly in Death Valley’s intense sun.
Travelers with pets should review current park regulations and identify appropriate roads or developed areas where animals may be allowed before arriving.
🚫 Don’t Drive Onto the Salt Flats
Vehicles must remain on established roads.
The salt surface can look hard enough to support a vehicle, but its upper crust is relatively thin in places.
Beneath it may be wet mud.
Tire tracks can break through the crust and leave scars that remain visible for a long time.
Off-road driving also damages fragile salt formations and protected park resources.
The vast openness of Badwater does not mean the basin is an unrestricted driving area.
Explore it on foot from established access points.
🧂 Don’t Collect the Salt
Leave salt crystals where they formed.
Although sodium chloride itself is common, Badwater’s salt formations are protected natural resources inside a national park.
Removing crystals gradually diminishes the landscape, particularly at a destination visited by large numbers of people.
Do not break polygons, carve names into the crust, construct piles, or carry salt away.
The best souvenir is a photograph.
👟 Watch Your Step
The salt flats can look smoother than they are.
Polygon ridges create uneven footing.
Thin crust may conceal softer mud beneath it.
Holes and cracks can occur in the surface.
Wear sturdy shoes and pay attention while walking.
The farther you travel from the boardwalk, the more natural the terrain becomes.
After flooding, conditions can be especially variable.
If the salt surface looks wet or unstable, avoid damaging it simply to reach a particular photographic location.
🗺️ A Badwater Road Day Trip
Badwater Basin fits naturally into one of the best sightseeing routes in Death Valley.
Start with sunrise at Zabriskie Point or a cool-weather morning hike through Golden Canyon.
Continue south from Furnace Creek along Badwater Road.
Stop at Devil’s Golf Course before continuing to Badwater Basin.
On the return trip, explore Artist’s Drive and Artist’s Palette.
Later in the day, drive into the Black Mountains for sunset at Dante’s View.
This route combines some of the park’s best badlands, salt landscapes, mineral colors, and mountain panoramas without requiring backcountry driving.
⏰ How Long Should You Spend at Badwater?
A short visit can take about 30 minutes.
That provides enough time to see the pool, walk along the boardwalk, photograph the elevation sign, and step onto the salt.
Allow an hour or more if you want to walk farther onto the basin toward better-developed polygon formations.
Sunrise, sunset, or photography visits may take longer.
Badwater does not require a lengthy hike to appreciate, but visitors who walk beyond the immediate parking area usually gain a much stronger impression of its enormous scale.
🌡️ Check Conditions Before Visiting
Death Valley is a dynamic environment.
Flash floods can close roads.
Temporary lakes can cover portions of the salt flat.
Extreme heat can make walking unsafe.
Storms may leave mud, debris, or damaged infrastructure.
Always check current National Park Service conditions before relying on an itinerary created weeks or months earlier.
This is particularly important after major storms.
For broader trip preparation, visit our National Park Travel & Planning hub.
♻️ Protecting Badwater Basin
Badwater looks harsh enough to survive almost anything.
It is actually surprisingly fragile.
Salt crystals are easily crushed.
Vehicle tires can break through the crust.
Foot traffic can leave long-lasting marks in wet areas.
The small saline pool supports specialized life found in an extremely limited habitat.
Stay out of the water.
Keep vehicles on designated roads.
Leave salt formations undisturbed.
Pack out trash.
Follow closures when flooding or restoration work requires them.
A place does not need trees and lush vegetation to be environmentally sensitive.
🌄 Is Badwater Basin Worth Visiting?
Absolutely.
Badwater is not simply famous because it holds an elevation record.
The setting itself is extraordinary.
A nearly white mineral basin stretches between dark mountain ranges.
A sea-level marker hangs improbably high on the cliffs behind you.
Across the valley, Telescope Peak rises more than two vertical miles above where you stand.
Beneath your feet are layers of salt accumulated through thousands of years of runoff and evaporation.
In the small spring-fed pool nearby, specialized organisms survive water too salty for most animals to drink.
The landscape is simultaneously barren and active.
Water arrives.
Lakes briefly form.
Salt dissolves.
The water evaporates.
Crystals grow again.
Badwater is always changing.
🌵 Why Visit Badwater Basin?
Few places summarize Death Valley as effectively as Badwater Basin.
It contains geological extremes, extreme climate, unexpected water, specialized wildlife, ancient lake history, brilliant mineral landscapes, and some of the largest elevation contrasts in North America.
Stand on the salt and look east toward the sea-level marker.
Then turn west toward Telescope Peak.
You are standing below the elevation of the ocean between mountains high enough to hold winter snow.
The white surface around you is the residue of water that traveled from those surrounding mountains, carrying minerals downhill until it reached a basin with nowhere else to go.
The water vanished.
The salt stayed.
That simple cycle, repeated again and again over thousands of years, created one of the most distinctive landscapes in Death Valley National Park—and one of the essential places to experience on any first visit.
🔗 Related Articles
- Death Valley National Park
- Top 10 Attractions in Death Valley National Park
- Furnace Creek
- Devil’s Golf Course
- Golden Canyon
- Zabriskie Point
- Dante’s View
- Mesquite Flat Sand Dunes
- The Racetrack
- U.S. National Parks
- Wildlife & Plants
- National Park Travel & Planning
📚 Sources & Further Reading
- National Park Service — Badwater Basin
- National Park Service — Salt Flats
- National Park Service — Death Valley Geology
- National Park Service — Natural Features & Ecosystems
- National Park Service — Death Valley Wildlife
- National Park Service — Sightseeing & Hiking Accessibility
- National Park Service — Death Valley Safety
- National Park Service — Current Conditions
- National Park Service — Death Valley National Park
