Top Attractions in Death Valley National Park

Badwater Basin

Badwater Basin is an endorheic basin in Death Valley National Park, Death Valley, Inyo County, California, noted as the lowest point in North America, with an elevation of 282 ft below sea level. Mount Whitney, the highest point in the contiguous 48 United States, is only 84.6 miles to the north west. The site itself consists of a small spring-fed pool of "bad water" next to the road in a sink; the accumulated salts of the surrounding basin make it undrinkable, thus giving it the name. The pool does have animal and plant life, including pickleweed, aquatic insects, and the Badwater snail. Adjacent to the pool, where water is not always present at the surface, repeated freeze–thaw and evaporation cycles gradually push the thin salt crust into hexagonal honeycomb shapes. The pool is not the lowest point of the basin: the lowest point is several miles to the west and varies in position, depending on rainfall and evaporation patterns. The salt flats are hazardous to traverse, and so the sign marking the low point is at the pool instead. The basin was considered the lowest elevation in the Western Hemisphere until the discovery of Laguna del Carbón in Argentina at −344 ft .

Devil's Golf Course

The Devils Golf Course is a large salt pan on the floor of Death Valley, located in the Mojave Desert within Death Valley National Park. The park is in eastern California. It was named after a line in the 1934 National Park Service guide book to Death Valley National Monument, which stated that "Only the devil could play golf" on its surface, due to a rough texture from the large halite salt crystal formations.

Scotty's Castle

Scottys Castle is a two-story Mission Revival and Spanish Colonial Revival style villa located in the Grapevine Mountains of northern Death Valley in Death Valley National Park, California, U.S.. "Scottys Castle" is named for gold prospector Walter E. Scott, although Scott never owned it, nor is it an actual castle.

Furnace Creek

Furnace Creek is a census-designated place in Inyo County, California, United States. The population was 24 at the 2010 census, down from 31 at the 2000 census. The elevation of the village is 190 feet below sea level. The Visitor Center, Museum, and headquarters of the Death Valley National Park are located at Furnace Creek. Furnace Creek is surrounded by a number of Park Service public campgrounds. Two of the Parks major tourist facilities, the Furnace Creek Inn and Furnace Creek Ranch, are located here. The Furnace Creek Golf Course attached to the Ranch claims to be the lowest in the world, at 214 feet below sea level. Most of the lodging is closed in the summer, when temperatures can surpass 125 °Fbut the golf course remains open; the resort went so far as to establish a summer tournament in 2011 called the Heatstroke Open, which drew a field of 48. There is also a restaurant, cafe, store, and gas station in Furnace Creek village. The Furnace Creek Airport is located about 0.75 miles west of the park headquarters.

Zabriskie Point

Zabriskie Point is a part of Amargosa Range located east of Death Valley in Death Valley National Park in California, United States noted for its erosional landscape. It is composed of sediments from Furnace Creek Lake, which dried up 5 million years ago—long before Death Valley came into existence.

Darwin Falls

Darwin Falls is a waterfall located on the western edge of Death Valley National Park near the settlement of Panamint Springs, California. Although there exists a similarly named Darwin Falls Wilderness adjacent to the falls, the falls themselves are located in and administered by Death Valley National Park and the National Park Service. There are several falls, but they are mainly divided into the upper and lower with a small grotto in between. At a combined 80 feet, it is the highest waterfall in the park. The canyon is walled by dramatic plutonic rock. Darwin Creek is one of the four perennial streams in three million-acre Death Valley National Park. Darwin Falls and Creek are fed by the Darwin Wash, which is in turn fed by the volcanic tableland of the Darwin Bench between the Inyo Mountains and the Argus Range. The small, narrow valley where the creek and falls are located features a rare collection of riparian greenery in the vast desert and is home to indigenous fauna such as quail. The falls themselves support several small fern gullys. Darwin Falls, the Darwin Falls Wilderness, the nearby town of Darwin, California, and all other areas named "Darwin" in the vicinity are named after Dr. Darwin French, a local rancher, miner, and explorer.

Telescope Peak

Telescope Peak is the highest point within Death Valley National Park, in the U.S. state of California. It is also the highest point of the Panamint Range, and lies in Inyo County. From atop this desert mountain one can see for over one hundred miles in many directions, including west to Mount Whitney, and east to Charleston Peak. The mountain was named for the great distance visible from the summit.

The Racetrack

The Racetrack is a scenic dry lake feature with "sailing stones" that inscribe linear "racetrack" imprints. It is located above the northwestern side of Death Valley, in Death Valley National Park, Inyo County, California, U.S..

Leadfield

Leadfield was an unincorporated community, and historic mining town in Inyo County, California. It is now a ghost town. It is located in Titus Canyon in the Grapevine Mountains, east of Death Valley in Death Valley National Park. Leadfield lies at an elevation of 4,058 ft . It is on the National Register of Historic Places.

Panamint City

Panamint City is a ghost town in the Panamint Range, near Death Valley, in Inyo County, California, USA. It is also known by the official Board of Geographic Names as Panamint. Panamint was a boom town founded after silver and copper were found there in 1872. By 1874, the town had a population of about 2,000. Its main street was one mile long. Panamint had its own newspaper, the Panamint News. Silver was the principal product mined in the area. The town is located about three miles northwest of Sentinel Peak. According to the National Geographic Names Database, NAD27 latitude and longitude for the locale are 36°07′06″N 117°05′43″W, and the feature ID number is 1661185. The elevation of this location is identified as being 6,280 feet AMSL. The similar-sounding Panamint Springs, California, is located about 25.8 miles at 306.4 degrees off true north near Panamint Junction.

Rhyolite, Nevada

Rhyolite is a ghost town in Nye County, in the U.S. state of Nevada. It is in the Bullfrog Hills, about 120 miles northwest of Las Vegas, near the eastern edge of Death Valley. The town began in early 1905 as one of several mining camps that sprang up after a prospecting discovery in the surrounding hills. During an ensuing gold rush, thousands of gold-seekers, developers, miners and service providers flocked to the Bullfrog Mining District. Many settled in Rhyolite, which lay in a sheltered desert basin near the regions biggest producer, the Montgomery Shoshone Mine. Industrialist Charles M. Schwab bought the Montgomery Shoshone Mine in 1906 and invested heavily in infrastructure, including piped water, electric lines and railroad transportation, that served the town as well as the mine. By 1907, Rhyolite had electric lights, water mains, telephones, newspapers, a hospital, a school, an opera house, and a stock exchange. Published estimates of the towns peak population vary widely, but scholarly sources generally place it in a range between 3,500 and 5,000 in 1907–08. Rhyolite declined almost as rapidly as it rose. After the richest ore was exhausted, production fell. The 1906 San Francisco earthquake and the financial panic of 1907 made it more difficult to raise development capital. In 1908, investors in the Montgomery Shoshone Mine, concerned that it was overvalued, ordered an independent study. When the studys findings proved unfavorable, the companys stock value crashed, further restricting funding. By the end of 1910, the mine was operating at a loss, and it closed in 1911. By this time, many out-of-work miners had moved elsewhere, and Rhyolites population dropped well below 1,000. By 1920, it was close to zero. After 1920, Rhyolite and its ruins became a tourist attraction and a setting for motion pictures. Most of its buildings crumbled, were salvaged for building materials, or were moved to nearby Beatty or other towns, although the railway depot and a house made chiefly of empty bottles were repaired and preserved. From 1988 to 1998, three companies operated a profitable open-pit mine at the base of Ladd Mountain, about 1 mile south of Rhyolite. The Goldwell Open Air Museum lies on private property just south of the ghost town, which is on property overseen by the Bureau of Land Management.

Skidoo

Skidoo was an unincorporated community in Inyo County, California. The geographical location of the old town site lies at an elevation of 5,689 feet . Skidoo is a virtual ghost town located in Death Valley National Park. It is on the National Register of Historic Places.

Keane Wonder Mine

The Keane Wonder Mine and mill is an abandoned mining facility located within Death Valley National Park in Inyo County, California. It is located in the Funeral Mountains east of Death Valley and Furnace Creek, California

Furnace Creek Inn and Ranch Resort

The Furnace Creek Inn and Ranch Resort is a privately owned luxury resort in Furnace Creek, on private land within the boundaries of Californias Death Valley National Park. It is operated by Xanterra. The Inn at Furnace Creek is a member of Historic Hotels of America, the official program of the National Trust for Historic Preservation.

Titus Canyon

Titus Canyon is a deep, narrow gorge cut into the steep face of the Grapevine Mountains of the Mojave Desert, within Death Valley National Park in southeastern California and southwestern Nevada. The canyon features limestone rock formations, petroglyphs, and native plants and wildlife.

Eagle Borax Works

The Eagle Borax Works in Death Valley, California was established near Bennetts Well in 1882 by Isidore Daunet, J.M. McDonald, M. Harmon and C.C. Blanch to mine the borate deposits that Daunet discovered there in 1880. The partnership established the first borax works in the valley. Partly refined borax was hauled to Daggett, California through the Panamint Valley using 12-mule teams hauling two wagons. The extraction business operated until 1884 when problems mounted and Daunet took his own life. The property eventually passed to the U.S. Borax Company, which kept it as a mining reserve, then to Borax Consolidated, Ltd. in 1922. The property was sold to the Death Valley Hotel Company in 1956, and finally to the National Park Service. Little remains of the structures but ruins. The works originally included a boiler, a tank for dissolved borax, and open tanks for crystallization of the borax. A stone building stood nearby to house the workers. The boiler fire box remains, along with an earth mound at the site of the building.

Ubehebe Craters

The Ubehebe Craters are an isolated group of overlapped maars in the Cottonwood Mountains, beyond the upper end of Death Valley, in Inyo County, California, U.S. They were formed during a period of phreatic eruptions along a fault line in Death Valley National Park. The youngest volcanic feature is Ubehebe Crater. Immediately south of Ubehebe Crater lies Little Hebe Crater, the second oldest maar in the Ubehebe Craters volcanic field.

Aguereberry Point

Aguereberry Point is a mountain viewpoint in Death Valley National Park in Inyo County, California, United States. The points elevation reaches 6,433 ft and is named for Jean Pierre "Pete" Aguereberry, a Basque miner who was born in 1874, emigrated from France in 1890, and lived at and worked the nearby Eureka Mine from 1905 to his death in 1945. From this point on the Panamint Range, one can view the surrounding Panamints extending to the north and south, Mount Charleston to the east, Furnace Creek and the salt flats of Badwater Basin.

Dante's View

Dantes View is a viewpoint terrace at 1,669 m height, on the north side of Coffin Peak, along the crest of the Black Mountains, overlooking Death Valley. Dantes View is about 25 km south of Furnace Creek in Death Valley National Park. Dante's View was also used for panoramic shots of Mos Eisley during the filming of Star Wars.

Gindarja Springs

Gindarja Springs is an alignment of depressions that consists of three large indentations aligned in a northwesterly direction within the Racetrack playa area of Death Valley, USA. Two are completely within the Racetrack playa and the third is on the edge. All three are associated with significant vegetation.

Saratoga Springs

Saratoga Springs is a desert oasis located in southern Death Valley National Park in California. The wetland lies at the southern tip of the Ibex Hills, on the floor of Death Valley and just northeast of the Amargosa River. Several springs overflow into pools totaling 6.6 acres in area, making the site the third largest marsh in the park. The pools provide habitat for several endemic species, including the Saratoga Springs pupfish. Other rare species present include the Amargosa tryonia snail, the Amargosa springsnail, the Saratoga Springs belostoma bug, the Amargosa naucorid bug, and the Death Valley June beetle. Plant life includes common reeds, bulrush and saltgrass. The springs were probably named in 1871 by the Wheeler Survey after the resort town of Saratoga Springs, New York, and were an important water source for the twenty-mule teams of the 1880s. The area saw a failed nitrate rush in 1902, and similarly unsuccessful attempts to mine gold and silver in the middle part of the decade. The Pacific Nitrate Company arrived in 1909 and built a small camp, but left within a few years. From the 1930s through the 1960s the springs provided water for the successful talc mines in the nearby Ibex Hills. Except for two partially collapsed stone structures, little evidence remains of human habitation at the spring. A dirt road provides access to an overlook of the area, but human entry into the wetland itself is prohibited in order to the protect the sensitive habitat.

Funeral Mountains

The Funeral Mountains are a short, arid mountain range in the United States along the California-Nevada border approximately 100 mi west of Las Vegas. The mountains are considered a subrange of the Amargosa Range that form the eastern wall of Death Valley. The crest of the range is within Death Valley National Park. The range is separated from the Grapevine Mountains to the northwest by the narrow Boundary Canyon and is separated from the Black Mountains by Furnace Creek Wash on the southwest and from the Greenwater Range at the narrow Travertine Point on the south. The broad flats of the Amargosa Desert lie across the border to the northeast in Nevada. The highest point in the range is Pyramid Peak, at 6703 ft . The first movement of Ferde Grofes Death Valley Suite is a symphonic musical portrayal of pioneer settlers drudging through the dry craggy peaks of the Funeral Mountains.

Amargosa Desert

The Amargosa Desert is located in Nye County in western Nevada, United States, along the California-Nevada border. It is largely coincident with the geographic Amargosa Valley. The desert is named after the Amargosa River, so-named for the Spanish word for bitter because of the bitter taste of the water.

Amargosa Range

The Amargosa Range is a mountain range in Inyo County, California and Nye County, Nevada. The 110-mile range runs along most of the eastern side of California's Death Valley, separating it from Nevada's Amargosa Desert. The U-shaped Amargosa River flows clockwise around the perimeter of the range, ending 279 feet below sea level in the Badwater Basin. The mountain range is named after the Amargosa River, so-named for the Spanish word for bitter because of the bitter taste of the water. In order from north to south, the Grapevine Mountains Grapevine Peak), the Funeral Mountains, and the Black Mountains form distinct sections. Many of Death Valley National Park's most well-known features, such as Zabriskie Point and Artists Drive are located in or are part of the Amargosa Range.

Harmony Borax Works

The Harmony Borax Works is located in Death Valley at Furnace Creek Springs, then called Greenland. It is now located within Death Valley National Park in Inyo County, California. It is on the National Register of Historic Places.

Ashford Mill

Ashford Mill is a former mining town settlement in Inyo County, California. It was located in Death Valley, at an elevation of 121 feet below sea level. The place is now protected ruins within Death Valley National Park. The original mill at the site was built in 1914 by brothers named Ashford. The ore was processed here from the Golden Treasure Mine 5 miles to the east in the Amargosa Range, and processed for further smelting.

Chloride City

Chloride City is a ghost town in Inyo County, California, USA. It is located 8.5 miles north-northeast of Beatty Junction, at an elevation of 4,770 ft . The former settlement is now in Death Valley National Park. The town was established in 1905 when the Bullfrog, Nevada, gold discovery brought people into the area. The ghost town contains numerous adits, dumps, and the grave of James McKay, of whom nothing is known. The town also holds the remains of three stamp mills.

Rainbow Canyon

Rainbow Canyon is a canyon located in Lincoln County, Nevada. It is also the location of the Rainbow Canyon Rock Art Site, which contains paintings that are around 10,000 years old. Additionally, due to its location near training ranges, it is known as an excellent location for low-level aviation photography.

Eureka Valley Sand Dunes

The Eureka Valley Sand Dunes are located in the southern part of Eureka Valley, in northern Inyo County in eastern California, in the southwestern United States. Although covering an area of only 3 square miles, the dunes rise approximately 680 feet above the surrounding valley floor, making them one of the highest dune fields in North America. Eureka Valley is a basin and range structural valley oriented northwest-southeast and enclosed by the Last Chance Range to the east and the Saline Range to the west. The Eureka Dunes themselves are located in the southeastern most tip of the valley and trend north-south, parallel to Last Chance Range. According to a USGS survey map, the surrounding mountain ranges contain rocks that date back to the Mississippian and Cambrian periods while the surficial deposits on the valley floor are made up mainly of alluvium dating to the Quaternary period. They are also classified as booming sand dunes, one of only about forty worldwide. Accessed via a gravel road in Eureka Valley, the dunes became part of the Death Valley National Park as part of its expansion in 1994. Foot travel in the dunes is permitted, but vehicle access is prohibited. A primitive campground is located at the north end of the dune field. Morphology The Eureka Dunes are an example of a complex-linear dune- the main ridge is a static linear dune but there are active star dunes formations superimposed on the linear dune A linear dune has alternating slip faces on opposite sides of the crest. This means it both sides of the dune have similar slopes and wind must have come from both the northern and southern ends of the valley. Star dunes have "arms" radiating off of a central crest that change direction as the wind direction changes. Little is known about the past of the Eureka Dunes and its development. The sand source is unknown, although some scientists believed that it originated from an ancient lake at the northern end of the valley. Booming The unique booming characteristic of the Eureka Dunes is caused by the relative motion of moving sand grains. The sound has been compared to moans, hums, drums, and, in the case of Eureka, a distant propeller plane. Most researchers agree that the average sand grain size should be smaller than 300 µm, well-sorted with no dusty material, dry and in low humidity, loosely packed, and each sand grain should be spherical and smooth The booming sound occurs when a sheet of sand avalanches down the slip face, exciting the sand grains. The friction between these grains creates an acoustic air wave that emits an audible sound. Other Information The Eureka Dunes are the home of several unique plant species. The Eureka Dune Grass, the Eureka Evening Primrose, and the Shining Locoweed are only found in this area. Visitors to the dunes may also experience other unique aspects of these dunes, other than the booming. In wet weather, patterns can be seen in the sand that reveals the diverse sources, and the complex Aeolian process by which these dunes are formed (and re-formed- sources and processes that are not yet fully understood. Sand dunes also exist in Death Valley near Stovepipe Wells. The Eureka Dunes share regional characteristics with the Kelso Dunes in the Mojave Desert.

Ubehebe Crater

Ubehebe Crater is a large volcanic crater of the Ubehebe Craters volcanic field in the northern half of Death Valley, in Death Valley National Park, California, USA.

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Top Attractions in Death Valley National Park

Badwater Basin

Devil's Golf Course

Scotty's Castle

Furnace Creek

Zabriskie Point

Darwin Falls

Telescope Peak

The Racetrack

Leadfield

Panamint City

Rhyolite, Nevada

Skidoo

Keane Wonder Mine

Furnace Creek Inn and Ranch Resort

Titus Canyon

Eagle Borax Works

Ubehebe Craters

Aguereberry Point

Dante's View

Gindarja Springs

Saratoga Springs

Funeral Mountains

Amargosa Desert

Amargosa Range

Harmony Borax Works

Ashford Mill

Chloride City

Rainbow Canyon

Eureka Valley Sand Dunes

Ubehebe Crater

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