Wild Burrow ( Equus africanus asinus )

The Wild Burro (Equus asinus), also known as the feral donkey or ass, is a resilient equid that has become a fixture in the harsh landscapes of the desert Southwest United States. Introduced by Spanish explorers in the 1500s and later released or escaped during the mining booms of the 19th century, these animals have adapted to arid environments where few large herbivores can survive. Often viewed as both an ecological challenge and a cultural icon, wild burros are managed by agencies like the Bureau of Land Management (BLM) and U.S. Forest Service due to their impacts on native vegetation and wildlife. With their sure-footed gait and ability to endure extreme conditions, they exemplify adaptation in one of North America’s most unforgiving regions.

Wild Burrow photographed in Beatty, Nevada - Photo by James L Rathbun
Wild Burrow photographed in Beatty, Nevada – Photo by James L Rathbun

Classification

The wild burro belongs to the kingdom Animalia, phylum Chordata, class Mammalia, order Perissodactyla (odd-toed ungulates), family Equidae, genus Equus, and species asinus. Native to North Africa, where it is known as the African wild ass, the species was domesticated thousands of years ago and introduced to the Americas. In the southwestern U.S., all populations are feral, descended from domestic stock released or escaped over centuries, and are classified as herbivores and non-native mammals. They share the Equidae family with horses and zebras, exhibiting similar social and grazing behaviors but with distinct adaptations for arid survival.

Physical Description

Wild burros are sturdy, medium-sized equids, standing approximately 4 to 5 feet (1.2 to 1.5 meters) tall at the shoulder and weighing around 350 pounds (159 kg), though sizes can vary. They have a robust build with long, erect ears (up to 10 inches or 25 cm) that aid in heat dissipation and hearing, a short, upright mane, and a tail ending in a tassel. Coat colors range from gray and brown to black, often with a lighter underbelly and muzzle, and a distinctive dark dorsal stripe or shoulder cross in some individuals. Their hooves are narrow and tough, suited for rocky terrain, and they possess a digestive system efficient at extracting nutrients from low-quality forage. Key adaptations include the ability to tolerate up to 30% body weight loss in water and replenish it quickly (in as little as 5 minutes), making them exceptionally suited to desert life.

"Wanderers of the Wastelands" vintage postcard of an unknown prospector and his burros. | Courtesy of Orange County Archives.
“Wanderers of the Wastelands” vintage postcard of an unknown prospector and his burros. | Courtesy of Orange County Archives.

Behavior

Wild burros are primarily diurnal, active during the day for foraging, but shift to nocturnal patterns in hot summers to avoid midday heat, resting in shade during peak temperatures. They form small, loose social groups of 2–10 individuals, often consisting of females and young with a dominant male, though home ranges overlap without strict territorial defense. Unlike wild horses, stable female bands are less common, and males may compete for access to females. They are sure-footed, navigating steep and rocky terrain with ease, and exhibit seasonal movements: concentrating near water and riparian areas in summer for shade and hydration, then dispersing to open shrublands in cooler months. Burros communicate through braying—a loud, distinctive “hee-haw”—and body language, and they can be curious toward humans but are generally wary. Their presence can impact ecosystems by altering vegetation and competing with native species like bighorn sheep for resources.

Food Sources

As herbivores, wild burros employ a mixed feeding strategy, acting as both grazers and browsers depending on availability. Their diet primarily consists of grasses and forbs when abundant, but they readily switch to browse such as shrubs, Mormon tea (Ephedra spp.), palo verde (Parkinsonia spp.), plantain, and other desert vegetation. This adaptability allows them to thrive on low-protein, fibrous plants, with their efficient digestive systems breaking down tough material. They require access to water but derive some moisture from succulent plants. In the Mojave and Sonoran Deserts, they consume a wide variety of species, contributing to their success in barren terrains but also leading to overgrazing concerns.

Breeding

Breeding in wild burros occurs year-round, with a peak in mating from May to July, aligning with optimal forage conditions. Gestation lasts about 12 months, resulting in births primarily from May to July the following year. Females (jennies) typically produce one precocial foal (colt or filly) per pregnancy, often every other year, though annual births are possible in favorable conditions. Foals are born weighing around 50–70 pounds (23–32 kg) and can stand and nurse shortly after birth. Sexual maturity is reached as yearlings, but full breeding often begins at 2–3 years. Recruitment rates hover at 20–25%, with low natural predation contributing to population growth. During parturition, females seek cover in brush or riparian areas. Lifespan in the wild can reach 25 years, aided by few diseases or predators.

Habitat and Range

Wild burros inhabit arid and semi-arid deserts, including sagebrush, creosote bush scrub, desert riparian zones, washes, Joshua tree woodlands, and pinyon-juniper areas, from below sea level to elevations up to 8,000 feet (2,450 meters). Key requirements include access to water within 10 miles (16 km), shade for thermoregulation, and diverse vegetation for foraging. They prefer sloping, rolling terrain over steep slopes and localize around water sources in summer, with home ranges varying from 2–22 square miles (5–70 km²) based on season and resources. Their range spans the desert Southwest, including California (e.g., Mojave Desert, Death Valley), Arizona, Nevada (e.g., near Austin), New Mexico, Utah, and parts of Texas, with populations estimated at around 20,000. Managed herds exist on public lands, with ongoing conservation efforts to balance their presence with ecosystem health.

Classification

Kingdom:Animalia
Phylum:Chordata
Class:Mammalia
Order:Perissodactyla
Family:Equidae
Genus:Equus
Species:E. africanus
Subspecies:E. a. asinus

References

Artist Drive

Artist Drive is perhaps one of the most popular and scenic drives through a colorful palette of geology, located in Death Valley National Park, California. Artist drive is a one way road about nine miles long which takes just about two hour to complete provided you take the time to hike a few of the short trails. The road is a popular destination for hikers and bikers as well as motor vehicles. From the drivers perspective, the road can be quite fun to drive and it twists and turns up and down the colorful hillside.

The hills which contain burst of color were formed by volcanic deposits of different compounds such as iron oxides and chlorite, which creates a rainbow effect of color. There is no bad time to visit, however, the photographer will appreciate the warm afternoon sunlight enhancing the natural colors in the soil. The best features are on a westward facing slope which really benefits from the late hours in the day.

While the colors of the location are amazing, do not forget to turn around the allow the scenic vistas of Death Valley to take your breath away. On a visit during a three day weekend in February 2022, I was surprised by the volume of people on the route. All of the parking lanes were full and it became quite difficult photographically due to the visitors. I will say, that during this time the COVID pandemic was relaxing and it was really nice seeing people enjoying themselves outside.

Prior to becoming a National Park, Assist’s Drive and some of the nearby valley’s were a filming location for the movie Star Wars.

Artist Drive Map

The multicolored rock formations along Artist’s Drive (particularly at the famous Artist’s Palette viewpoint) in Death Valley National Park create one of the most striking natural displays in the American Southwest. These vibrant hues result from ancient volcanic activity over 5 million years ago, when eruptions deposited ash, metals, and minerals that were later altered by hydrothermal processes, chemical weathering, and oxidation.

Here are the main rock colors you’ll see splashed across the hillsides, along with the primary minerals responsible for each:

Reds, Pinks, and Oranges

These warm, fiery tones dominate many areas and often appear as bold streaks or bands. They come from iron oxides (especially hematite), which form through the oxidation of iron-rich compounds in the volcanic rocks

Yellows and Golds

Bright mustard, golden, and sunny yellow patches blend beautifully with the reds. These are also produced by various iron oxides in different stages of oxidation and weathering.

Purples and Lavenders

The cooler, softer purple and lavender shades create a dreamy contrast. These colors are caused by manganese minerals that oxidize to produce these distinctive hues.

Greens

Vivid green sections stand out dramatically against the warmer tones. The green primarily comes from the decomposition of tuff-derived mica or weathered volcanic tuff, sometimes involving chlorite.

Overall Landscape Views

The full palette comes alive especially in late afternoon or sunset light, when the low sun angle intensifies the colors and creates dramatic shadows.

The result is a surreal, painterly landscape that looks almost too vivid to be natural — truly living up to its name as Artist’s Palette! The colors can shift subtly depending on the time of day, weather, and lighting, making every visit feel unique.

References

Zabriskie Point

Zabriskie Point is perhaps one of the best known and popular overlooks in the entire Death Valley National Park, California. The landmark is named for Christian Brevoort Zabriskie who was the Vice President of the Pacific Coast Borax Company.

Zabriskie Point bathed in warm afternoon light in Death Valley National Park - Photo by James L Rathbun
Zabriskie Point bathed in warm afternoon light in Death Valley National Park – Photo by James L Rathbun

The elevated overlook of a huge area of yellow-brown-black ancient mud lands composed of sediments from the ancient Furnace Creek Lake. A short hike from the parking lot allows is a visitor to see the expanse of the badlands. A longer hike will take the explorer down through Golden Canyon to the floor of Death National National Park. The site is best visited during the “golden hours” of warm light in the evening and mornings. The best viewing occurs at sunrise.

Zabriskie Point - Photo by James L Rathbun
Zabriskie Point – Photo by James L Rathbun

The site was made famous in popular culture by a movie from 1970 of the same name. For those of us who grew up in the 1980s, the cover of the U2 Album, The Joshua Tree features a photograph by Anton Corbijn at Zabriskie Point.

The cover of The Joshua Tree by U2 was taken in Death Valley - photograph by Anton Corbijn
The cover of The Joshua Tree by U2 was taken in Death Valley – photograph by Anton Corbijn

The only draw back with visiting this location is that it is almost always crowded during the prime months.

Zabriskie Point Map

References

Badwater Basin

Badwater Basin, located in Death Valley National Park, Inyo County, California, is the lowest point in North America, sitting at 282 feet (86 meters) below sea level. This endorheic basin spans approximately 200 square miles (518 square km) and is characterized by vast salt flats composed primarily of sodium chloride (table salt), along with calcite, gypsum, and borax. The basin features a small, spring-fed pool near Badwater Road, named “Badwater” due to its high salinity, which renders the water undrinkable. Despite this, the pool supports unique life forms, including the endemic Badwater snail, aquatic insects, and salt-tolerant plants like pickleweed. The surrounding salt flats form striking hexagonal patterns due to repeated freeze-thaw and evaporation cycles, creating a surreal, otherworldly landscape. A notable “sea level” sign on the cliffs above the basin highlights its extreme elevation, and the dramatic vertical relief to Telescope Peak (11,049 feet) in the Panamint Range, visible to the west, underscores the region’s rugged topography. The basin’s extreme heat, with summer temperatures often exceeding 120°F (49°C), and its high evaporation rate of 150 inches annually make it one of the harshest environments in the United States. Visitors can access the basin via a boardwalk from the parking lot off Badwater Road, with the best views of the salt polygons requiring a 1.5- to 2-mile roundtrip walk onto the flats.

Badwater Basin located at 282 feet below sea level in Death Valley National Park. - Photo by James L Rathbun
Badwater Basin located at 282 feet below sea level in Death Valley National Park. – Photo by James L Rathbun

History

Badwater Basin’s name originates from a story of an early prospector whose mule refused to drink from the salty pool, leading to the moniker “Badwater.” Before becoming part of Death Valley National Park, the area was an active mining region for centuries, with prospectors like Alexander “Shorty” Borden and Walter Scott exploring for valuable minerals.

The basin’s geological history spans millions of years, shaped by tectonic activity, erosion, and climatic shifts since at least the Pleistocene epoch (possibly up to 3 million years ago). During wetter periods, streams from surrounding mountains filled Death Valley, forming Lake Manly, which at its peak was 80 miles long and up to 600 feet deep. As an endorheic lake with no outlet, Lake Manly’s evaporation led to hypersalinity, leaving behind thick salt deposits (95% sodium chloride) that form the basin’s iconic crust, ranging from 3 to 60 inches thick. Periodic flooding from rare rainstorms temporarily revives Lake Manly, as seen in 2005 and 2023, but the water quickly evaporates, redepositing clean salt crystals. The region’s geological cycles, influenced by the nearby San Andreas Fault and the Colorado River’s alluvial deposits, have created a dynamic landscape of evaporating and reforming lakes over the Quaternary Period.

Despite its arid appearance, Death Valley sits atop one of the world’s largest aquifers, a remnant of these ancient water systems. Badwater Basin also holds historical significance for Native American settlements, which utilized the desert’s resources, and for 19th-century explorers and settlers who braved its harsh conditions during westward expansion.

Today, it remains a popular tourist destination, drawing visitors to its stark beauty and geological wonders, with the Badwater Ultramarathon challenging athletes in its extreme environment.

Badwater 135

Badwater is host to the starting line for the Badwater 135, an ultra-marathon for the ultra-crazy. The marathon starts at Badwater and runners, run, jog, and walk over one hundred and thirty miles to the Mount Whitney Portal Campground. Over the course of about two days, the runners gain over 14,600 feet in total elevation and this is done in the heat of midsummer just to make it interesting.

Summary

NameBadwater Basin
LocationDeath Valley National Park, California
Latitude, Longitude36.250278, -116.825833
Elevation-282 feet
OtherRound Trip Length: 1 mile (1.6km) to edge of salt flat
Round Trip Time: 40 minutes
Dificulty: Easy 
Elevation Gain: Flat
Trail Type: Boardwalk then route, out and back 
Location: Badwater Road, 30 minutes (17 miles/27km) south of Furnace Creek
Parking: Paved parking lot with large spaces for RVs and buses
Closest Restroom: Vault toilet located in parking lot
Route: An ADA accessible ramp leads down to a wooden boardwalk. The walking surface is firm and wide beyond the boardwalk. 

Badwater Basin Map

References

Furnace Creek Campground

Furnace Creek Campground is located at -200 below sea level in Death Valley National Park, California. The campground is the most popular in the Death Valley and reservations are strongly recommended. The campground is located just off Highway 190 near Furnace Creek.

Borax Wagons near Furnace Creek Campground, Death Valley National Park, California
Borax Wagons near Furnace Creek Campground, Death Valley National Park, California

Furnace Creek Campground is the lowest in the park in terms of elevation, and located near the hottest measured temperature on the plant. Close to a lot of amenities , such as a store, borax museum & gas station, this campground offers a central location to scout out and explore Death Valley. All of the campsites feature tables, fire rings, water and flush toilets. This is a wonderful location for sky gazers who seek a clear night sky with little light pollution.

Death Valley frequently experiences temperatures over 120° F and in addition to holding the all time hottest temp (134° F – July 10, 1913) Death Valley routinely records some of the hottest days on the planet year after year. All to frequently, a visitor will die in this area due to the very extreme heat, plan your trip with care and mind the heat. One more that one occasion, I have been in the park with the temperature being north of 125° F.

Artist Drive, Badwater and Zabriskie Point and all located a short drive from this little oasis. The local gas station is always a quick stop for us when we drive by, so we can star in horror at the high price of fuel, which is typically $2 per gallon higher than outside of the National Park.

Campground Summary

NameFurnace Creek Campground
LocationFurnace Creek, Death Valley National Park, California
Latitude, Longitude36.463188,-116.8710673
Elevation-200 feet
Number of Sites136
Amenties

Furnace Creek Campground Map

References