Places of interest in the

Death Valley Death Valley is a desert valley in Eastern California, in the northern Mojave Desert, bordering the Great Basin Desert. During summer, it is the hottest place on Earth. Death Valley's Badwater Basin is the point of lowest elevation in Nort ...

area are mostly located within

Death Valley National Park Death Valley National Park is an American national park that straddles the California–Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley, the northern section of Panamint Valley, the southern section of Eurek ...

in eastern

California California is a state in the Western United States, located along the Pacific Coast. With nearly 39.2million residents across a total area of approximately , it is the most populous U.S. state and the 3rd largest by area. It is also the m ...

Aguereberry Point

Aguereberry Point is a promontory and tourist viewpoint in the

Panamint Range The Panamint Range is a short rugged fault-block mountain range in the northern Mojave Desert, within Death Valley National Park in Inyo County, eastern California. Dr. Darwin French is credited as applying the term Panamint in 1860 during his ...

, within

in Inyo County, eastern

. The point's elevation reaches 6,433 ft and is named for Jean Pierre "Pete" Aguereberry, a Basque

miner A miner is a person who extracts ore, coal, chalk, clay, or other minerals from the earth through mining. There are two senses in which the term is used. In its narrowest sense, a miner is someone who works at the rock face; cutting, blasting ...

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 viewpoint, one can see the surrounding Panamint Range extending to the north and south;

to the east, with Furnace Creek and the

salt flats Salt flats, Salt flat, Salt Flats, or Salt Flat may refer to: Geology *Salt pan (geology), a flat expanse of ground covered with salt and other minerals *Dry lake, an ephemeral lakebed that consists of fine-grained sediments infused with alkali salt ...

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 and the United States, with a depth of below sea level. Mount Whitney, the highest poi ...

to the southeast; and Mount Charleston in Nevada far to the east.

Amargosa Chaos

USA 10789 Death Valley Luca Galuzzi 2007

The Amargosa Chaos is a series of

geological formation A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exp ...

s located in the Black Mountains in southern

. In the 1930s, geologist Levi F. Noble studied the faulting and folding in the area, dubbing it the "Amargosa chaos" due to the extreme warping of the rock. Later researchers discovered that the region had experienced substantial tension that pulled large blocks of crust apart. Modern geologists have documented four major deformational events that faulted and folded the Amargosa Chaos. The first event

metamorphosed Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causi ...

Death Valley's

Precambrian The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of th ...

basement rocks In geology, basement and crystalline basement are crystalline rocks lying above the mantle and beneath all other rocks and sediments. They are sometimes exposed at the surface, but often they are buried under miles of rock and sediment. The baseme ...

and occurred around 1,700 million years ago. The second event began while layered younger Precambrian sediments were being deposited on top of the beveled surface of older

metamorphic Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causi ...

basement rocks. This deformational event shifted the crust vertically, creating thinning and thickening of some sedimentary layers as they were being deposited. The two events responsible for the chaotic appearance of the Amargosa Chaos did not occur until over half a billion years later, during

Mesozoic The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretace ...

or Early

Tertiary Tertiary ( ) is a widely used but obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non-avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start ...

time. This third event folded the layered Precambrian and

Cambrian The Cambrian Period ( ; sometimes symbolized Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago ...

sedimentary rocks. The fourth and final event occurred quite recently, geologically speaking. This phase of deformation coincided with severe crustal stretching that created the deep valleys and high mountains of this part of the

Basin and Range Province The Basin and Range Province is a vast physiographic region covering much of the inland Western United States and northwestern Mexico. It is defined by unique basin and range topography, characterized by abrupt changes in elevation, alternating ...

. In just a few million years, during Late

Miocene The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recen ...

Pliocene The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58 Artist's Drive rises up to the top of an

alluvial fan An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to semiarid climates, but a ...

fed by a deep canyon cut into the Black Mountains. Artist's Palette is an area on the face of the Black Mountains noted for a variety of rock colors. These colors are caused by the

oxidation Redox (reduction–oxidation, , ) is a type of chemical reaction in which the oxidation states of substrate change. Oxidation is the loss of electrons or an increase in the oxidation state, while reduction is the gain of electrons or ...

of different

metal A metal (from ancient Greek, Greek μέταλλον ''métallon'', "mine, quarry, metal") is a material that, when freshly prepared, polished, or fractured, shows a lustrous appearance, and conducts electrical resistivity and conductivity, e ...

s (

iron Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in ...

compounds produce red, pink and yellow, decomposition of

tuff Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock ...

-derived

mica Micas ( ) are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates. This characteristic is described as perfect basal cleavage. Mica is ...

produces green, and

manganese Manganese is a chemical element with the Symbol (chemistry), symbol Mn and atomic number 25. It is a hard, brittle, silvery metal, often found in minerals in combination with iron. Manganese is a transition metal with a multifaceted array of ...

produces purple). Called the Artist Drive Formation, the rock unit provides evidence for one of the Death Valley area's most violently explosive

volcanic A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plat ...

periods. The

-aged formation is made up of cemented gravel, playa deposits, and volcanic debris, perhaps thick.

Chemical weathering Weathering is the deterioration of rocks, soils and minerals as well as wood and artificial materials through contact with water, atmospheric gases, and biological organisms. Weathering occurs ''in situ'' (on site, with little or no movement ...

and

hydrothermal alteration Metasomatism (from the Greek μετά ''metá'' "change" and σῶμα ''sôma'' "body") is the chemical alteration of a rock by hydrothermal and other fluids. It is the replacement of one rock by another of different mineralogical and chemical co ...

cause the oxidation and other chemical reactions that produce the variety of colors displayed in the Artist Drive Formation and nearby exposures of the Furnace Creek Formation.

Badwater Basin

The Badwater Basin is a salt flat adjacent to the Black Mountains that descends to the lowest

elevation The elevation of a geographic location is its height above or below a fixed reference point, most commonly a reference geoid, a mathematical model of the Earth's sea level as an equipotential gravitational surface (see Geodetic datum § ...

North America North America is a continent in the Northern Hemisphere and almost entirely within the Western Hemisphere. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South America and th ...

at below sea level. The massive expanse of white is made up of almost pure

table salt Salt is a mineral composed primarily of sodium chloride (NaCl), a chemical compound belonging to the larger class of salts; salt in the form of a natural crystalline mineral is known as rock salt or halite. Salt is present in vast quantitie ...

. The basin is the second lowest depression in the

Western Hemisphere The Western Hemisphere is the half of the planet Earth that lies west of the prime meridian (which crosses Greenwich, London, United Kingdom) and east of the antimeridian. The other half is called the Eastern Hemisphere. Politically, the te ...

, eclipsed only by

Laguna del Carbón __NOTOC__ Laguna del Carbón ( Spanish for "coal lagoon") is a salt lake in Corpen Aike Department, Santa Cruz Province, Argentina. This salt lake is located from Puerto San Julián, within the ''Gran Bajo de San Julián'' (Great San Julián Dep ...

in Argentina at . This pan was first created by the drying-up of deep Recent Lake 2000 to 3000 years ago. Unlike at the Devils Golf Course, significant rainstorms

flood A flood is an overflow of water ( or rarely other fluids) that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are an area of study of the discipline hydrol ...

Badwater, covering the salt pan with a thin sheet of standing water. Each newly formed lake doesn't last long though, because the average rainfall is overwhelmed by a annual

evaporation Evaporation is a type of vaporization that occurs on the surface of a liquid as it changes into the gas phase. High concentration of the evaporating substance in the surrounding gas significantly slows down evaporation, such as when h ...

rate. This, the nation's greatest evaporation potential, means that even a deep, long lake would dry up in a single year. While flooded, some of the salt is dissolved, then is redeposited as clean, sparkling crystals when the water evaporates.

Charcoal Kilns

The Wildrose Charcoal Kilns were completed in 1877 by the Modock Consolidated Mining Company, above Death Valley in the

, and were used to reduce pinyon and

juniper Junipers are coniferous trees and shrubs in the genus ''Juniperus'' () of the cypress family Cupressaceae. Depending on the taxonomy, between 50 and 67 species of junipers are widely distributed throughout the Northern Hemisphere, from the Arc ...

tree wood to

charcoal Charcoal is a lightweight black carbon residue produced by strongly heating wood (or other animal and plant materials) in minimal oxygen to remove all water and volatile constituents. In the traditional version of this pyrolysis process, ...

in a process of slow burning in low

oxygen Oxygen is the chemical element with the symbol O and atomic number 8. It is a member of the chalcogen group in the periodic table, a highly reactive nonmetal, and an oxidizing agent that readily forms oxides with most elements ...

. This fuel was then transported to mines in The Argus Range, 25 miles to the west, to feed

smelting Smelting is a process of applying heat to ore, to extract a base metal. It is a form of extractive metallurgy. It is used to extract many metals from their ores, including silver, iron, copper, and other base metals. Smelting uses heat and a c ...

and ore extraction operations. Although the mines themselves were worked intermittently until about 1900, there is no clear evidence that the charcoal kilns were operational after 1879. They were restored by

Navajo The Navajo (; British English: Navaho; nv, Diné or ') are a Native Americans in the United States, Native American people of the Southwestern United States. With more than 399,494 enrolled tribal members , the Navajo Nation is the largest fe ...

Indian stonemasons from

Arizona Arizona ( ; nv, Hoozdo Hahoodzo ; ood, Alĭ ṣonak ) is a state in the Southwestern United States. It is the 6th largest and the 14th most populous of the 50 states. Its capital and largest city is Phoenix. Arizona is part of the Fou ...

in 1971. The kilns were located here as the trees single-leaf pinyon pine ''(Pinus monophylla)'' and

Utah juniper ''Juniperus osteosperma'' (Utah juniper; syn. ''J. utahensis'') is a shrub or small tree native to the southwestern United States. Description The plant reaches , rarely to 9 m, tall. The shoots are fairly thick compared to most junipers, in ...

(''Juniperus osteosperma)'' dominate the landscape in the upper Panamint Mountains. Shrubs of

Mormon tea ''Ephedra'' is a genus of gymnosperm shrubs. The various species of ''Ephedra'' are widespread in many arid regions of the world, ranging across southwestern North America, southern Europe, northern Africa, southwest and central Asia, northe ...

''(Ephedra sp.)'', such as Death Valley ephedra ''(Ephedra funerea)'', are spaced between them, with other xeric sub-shrubs and

native Native may refer to: People * Jus soli, citizenship by right of birth * Indigenous peoples, peoples with a set of specific rights based on their historical ties to a particular territory ** Native Americans (disambiguation) In arts and entert ...

bunchgrass Tussock grasses or bunch grasses are a group of grass species in the family Poaceae. They usually grow as singular plants in clumps, tufts, hummocks, or bunches, rather than forming a sod or lawn, in meadows, grasslands, and prairies. As perennial ...

es. Other historic charcoal kilns in the United States include the Cottonwood Charcoal Kilns at Owens Lake, the

Piedmont Charcoal Kilns The Piedmont Charcoal Kilns in Piedmont, Wyoming, are a remnant of a once-extensive charcoal-making industry in southwestern Wyoming. The kilns were built by Moses Byrne around 1869 near the Piedmont Station along the Union Pacific Railroad. The th ...

in Wyoming, and the

Walker Charcoal Kiln The Walker Charcoal Kiln is a structure in the Prescott National Forest near the town of Walker, Arizona and situated in the vicinity of the abandoned Poland Junction Mine near the summit of Renegade Hill. It is listed on the National Register of ...

in Arizona. Wildrose Canyon has 2 campgrounds above the kilns, Thorndyke at 7,490 feet and Mahogany Flat at 7923 feet. The latter is the trail head for the hiking trail to Telescope Peak and has views to the east down to Badwater.

Dante's View

From Dante's View one can see the central part of Death Valley from a vantage point above sea level. From here

can be seen, which contains the lowest dry point in North America.

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 hundre ...

can also be seen from here which is above sea level. This is the greatest topographic relief in the conterminous U.S. The mountain that Dante's View is on is part of the Black Mountains which along with the parallel

across the valley from what geologists call a horst and the valley that is called a

graben In geology, a graben () is a depressed block of the crust of a planet or moon, bordered by parallel normal faults. Etymology ''Graben'' is a loan word from German, meaning 'ditch' or 'trench'. The word was first used in the geologic conte ...

. These structures are created when the surface of the earth is under extensional, or a pulling force. The crust responds to this force by sending a large and long roughly v-shaped block of crust down which forms the bedrock of the valley floor (see Basin and Range).

Darwin Falls

Darwin Falls is a waterfall located on the western edge of Death Valley National Park near the settlement of Panamint Springs, California. There are several falls, but they are mainly divided into the upper and lower with a small grotto in between. 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.

Devil's Golf Course

The Devil's Golf Course is a large salt pan on the floor of Death Valley. It was named after a line in the 1934

National Park Service The National Park Service (NPS) is an agency of the United States federal government within the U.S. Department of the Interior that manages all national parks, most national monuments, and other natural, historical, and recreational properti ...

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.

Lake Manly Lake Manly was a pluvial lake in Death Valley, California, covering much of Death Valley with a surface area of during the so-called "Blackwelder stand". Water levels varied through its history, and the chronology is further complicated by act ...

once covered the valley to a depth of . The salt in the Devil's Golf Course consists of the minerals that were dissolved in the lake's water and left behind in the

when the lake evaporated. With an elevation several feet above the valley floor at Badwater, the Devil's Golf Course remains dry, allowing weathering processes to sculpt the salt there into complicated formations. Through exploratory holes drilled by the Pacific Coast Borax Company, prior to Death Valley becoming a national monument in 1934, it was discovered that the salt and gravel beds of the Devil's Golf Course extend to a depth of more than . Later studies suggest that in places the depth ranges up to . Devil's Golf Course can be reached from Badwater Road via a gravel drive, closed in wet weather. It should not be confused with an actual

golf course A golf course is the grounds on which the sport of golf is played. It consists of a series of holes, each consisting of a tee box, a fairway, the rough and other hazards, and a green with a cylindrical hole in the ground, known as a "cup". ...

in Furnace Creek, also in Death Valley.

Eureka Valley and Sand Dunes

Between the

Last Chance Range The Last Chance Range of California is located near the Nevada state line in eastern Inyo County in the United States The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country ...

and Saline Mountains is the

Eureka Valley. Sand dunes cover 3 square miles (8 km²) of Eureka Valley, rising 680 feet (207 m) as one of North America's tallest dunes. As sand moves down the dune face it produces a booming noise, known as

singing sand Singing is the act of creating musical sounds with the voice. A person who sings is called a singer, artist or vocalist (in jazz and/or popular music). Singers perform music (arias, recitatives, songs, etc.) that can be sung with or without ...

phenomenon, due to the small grain size and loose, dry packing. Endemic species include the Eureka Dune Grass, the Eureka Evening Primrose and the Shining Locoweed.

Furnace Creek

Furnace Creek is a spring, oasis, and village that sits on top of a remarkably symmetrical

. The main visitor center of the park is located here as well as the Oasis at Death Valley resort complex. Controversy surrounds the use of Furnace Creek water to support the resort (complete with a swimming pool) and nearby facilities, including a

. The scarce springs and surrounding lush oases support thriving

plant Plants are predominantly photosynthetic eukaryotes of the kingdom Plantae. Historically, the plant kingdom encompassed all living things that were not animals, and included algae and fungi; however, all current definitions of Plantae exclu ...

communities and attract a wide variety of animals. As the resort grew, the

marsh A marsh is a wetland that is dominated by herbaceous rather than woody plant species.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p Marshes can often be found a ...

es and

wetland A wetland is a distinct ecosystem that is flooded or saturated by water, either permanently (for years or decades) or seasonally (for weeks or months). Flooding results in oxygen-free (anoxic) processes prevailing, especially in the soils. The p ...

s around it shrank. The highest temperature in North America was recorded at Furnace Creek Ranch (134 °F or 57 °C). The Furnace Creek Fault runs through this part of Death Valley.

Hells Gate

Hells Gate is a point of interest located in

, at the intersection of Daylight Pass Road and Beatty Road. There is a parking area and hiking paths.

Mesquite Flat Sand Dunes

Death Valley Mesquite Flats Sand Dunes 2013

The Mesquite Flat Sand Dunes are at the northern end of the valley floor and are nearly surrounded by mountains on all sides. Due to their easy access from the road and the overall proximity of Death Valley to Hollywood, these dunes have been used to film sand dune scenes for several movies including films in the Star Wars series. The largest dune is called Star Dune and is relatively stable and stationary because it is at a point where the various winds that shape the dunes converge. The depth of the sand at its crest is but this is small compared to other dunes in the area that have sand depths of up to deep. The primary source of the dune sands is probably the Cottonwood Mountains which lie to the north and northwest. The tiny grains of

quartz Quartz is a hard, crystalline mineral composed of silica ( silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical ...

and

feldspar Feldspars are a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. The most common members of the feldspar group are the ''plagioclase'' (sodium-calcium) felds ...

that form the sinuous sculptures that make up this dune field began as much larger pieces of solid rock. In between many of the dunes are stands of

creosote bush ''Larrea tridentata'', called creosote bush and greasewood as a plant, chaparral as a medicinal herb, and ''gobernadora'' (Spanish for "governess") in Mexico, due to its ability to secure more water by inhibiting the growth of nearby plants. In S ...

and some

mesquite Mesquite is a common name for several plants in the genus '' Prosopis'', which contains over 40 species of small leguminous trees. They are native to dry areas in the Americas. They have extremely long roots to seek water from very far under gr ...

on the sand and on dried mud, which used to cover this part of the valley before the dunes intruded (mesquite was the dominant plant here before the sand dunes but creosote does much better in the sand dune conditions).

Mesquite Spring

Mesquite Spring is located in the northernmost part of Death Valley. This part of the valley has numerous cotton top cactus, blister beetles and '' cholla cactus''. On the alluvial fan above the springs there are 2-3 thousand year old petroglyphs from the extinct Mesquite Spring culture. The petroglyphs here are made possible because many of the rocks in these arid conditions have desert varnish on them. This particular form of desert varnish takes 10,000 years to make 1/100th of an inch of varnish and is deposited by a certain type of

bacteria Bacteria (; singular: bacterium) are ubiquitous, mostly free-living organisms often consisting of one Cell (biology), biological cell. They constitute a large domain (biology), domain of prokaryotic microorganisms. Typically a few micrometr ...

that collects the

and

clay Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay par ...

needed to make the varnish. Also, since varnish is created at a predictable rate, it is possible to date petroglyphs based on the amount of re-varnishing that has taken place since the marks were made. Varnish does not normally form on carbonate rocks because their surfaces weather too easily. In a wash near some of the petroglyphs there is a

fault scarp A fault scarp is a small step or offset on the ground surface where one side of a fault has moved vertically with respect to the other. It is the topographic expression of faulting attributed to the displacement of the land surface by movement a ...

that exposes some

fanglomerate Conglomerate () is a clastic rock, clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix (geology), matrix of finer-grained sediments, such as ...

which is a type of sedimentary rock which looks like

concrete Concrete is a composite material composed of fine and coarse aggregate bonded together with a fluid cement (cement paste) that hardens (cures) over time. Concrete is the second-most-used substance in the world after water, and is the most wid ...

with large rocks intermixed. In fact it is lithified alluvial sediment.

Mosaic Canyon

Mosaic Canyon is a canyon in the north western mountain face of the valley which is named after a stream-derived

breccia Breccia () is a rock composed of large angular broken fragments of minerals or rocks cemented together by a fine-grained matrix. The word has its origins in the Italian language, in which it means "rubble". A breccia may have a variety of ...

sediment with angular blocks of dolomite in a pebbly matrix. The entrance to Mosaic Canyon appears deceptively ordinary, but just a walk up the canyon narrows dramatically to a deep slot cut into the face of Tucki Mountain. Smooth, polished

marble Marble is a metamorphic rock composed of recrystallized carbonate minerals, most commonly calcite or dolomite. Marble is typically not foliated (layered), although there are exceptions. In geology, the term ''marble'' refers to metamorphose ...

walls enclose the trail as it follows the canyon's sinuous curves. The canyon follows faults that formed when the rocky crust of the Death Valley region began stretching just a few million years ago. Running water scoured away at the fault-weakened rock, gradually carving Mosaic canyon. Periodic flash floods carry rocky debris (sediment) eroded from Mosaic Canyon and the surrounding hillsides toward the valley below. At the canyon mouth water spreads out and deposits its sediment load, gradually building up a large wedge-shaped

that extends down toward Stovepipe Wells. This canyon was formed through a process of

cut and fill In earthmoving, cut and fill is the process of constructing a railway, road or canal whereby the amount of material from cuts roughly matches the amount of fill needed to make nearby embankments to minimize the amount of construction labor. ...

which included periodic erosive floods followed by long periods of deposition and uplift. But due to the uplift when the next flood hit the area it would deeply cut the streambed which forms stairstep-shaped banks. Mosaic Canyon promontory, Death Valley

Mosaic Canyon's polished marble walls are carved from the Noonday Dolomite and other Precambrian

carbonate rock Carbonate rocks are a class of sedimentary rocks composed primarily of carbonate minerals. The two major types are limestone, which is composed of calcite or aragonite (different crystal forms of CaCO3), and dolomite rock (also known as dolosto ...

s. These rock formation began as

limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...

deposited during Late

(about 850-700 million years ago) when the area was covered by a warm sea. Later addition of

magnesium Magnesium is a chemical element with the symbol Mg and atomic number 12. It is a shiny gray metal having a low density, low melting point and high chemical reactivity. Like the other alkaline earth metals (group 2 of the periodic ta ...

changed the limestone, a rock made of calcium carbonate, to dolomite, a calcium-magnesium carbonate. The dolomite was later deeply buried by younger sediment. Far below the surface, high pressure and temperature altered the dolomite into the

metamorphic rock Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock ( protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, caus ...

, marble. The Noonday Dolomite has since been tilted from uplift. Mosaic Canyon was named for a rock formation known as the Mosaic Breccia.

Breccia Breccia () is a rock composed of large angular broken fragments of minerals or rocks cemented together by a fine-grained matrix. The word has its origins in the Italian language, in which it means "rubble". A breccia may have a variety of ...

is an Italian word meaning ''gravel''. This formation is composed of angular fragments of many different kinds of parent rock, and it can be seen on the floor of the canyon just south of the parking area.

Natural Bridge Canyon

Natural Bridge Canyon is found on the east side of the park and is one of the few canyons with an official trailhead. Located south of the Artist's Drive scenic loop, the canyon contains a natural stone bridge, accessible after a fifteen-minute walk from the parking area.

Panamint Valley

The Panamint Valley basin runs between the

to the east and Argus and Slate ranges to the west for 65 miles (105 km). It has a width of about 10 miles (16 km). It is an

endorheic basin An endorheic basin (; also spelled endoreic basin or endorreic basin) is a drainage basin that normally retains water and allows no outflow to other external bodies of water, such as rivers or oceans, but drainage converges instead into lakes ...

that can form a lake after heavy rain. Airspace above the valley is part of the Panamint Military Operating Area, restricted to US military use. The ghost town of Ballarat had 400 residents at the turn of the 20th century when mines were active in the area.

Racetrack Playa

Racetrack Playa is a seasonally dry lake (playa) located in the northern part of the Panamint Mountains that is famous for rocks that mysteriously move across its surface. During periods of heavy rain, water washes down from nearby mountain slopes onto the playa, forming a shallow, short-lived lake. Most of the so-called 'sailing stones' are from a nearby high hillside of dark dolomite on the south end of the playa. Similar rock travel patterns have been recorded in several other playas in the region but the number and length of travel grooves on The Racetrack are notable. Racetrack stones only move once every two or three years and most tracks last for just three or four years.

Rainbow Canyon

Rainbow Canyon is a canyon near the western edge of the park. It is commonly used by the United States Military for fighter jet training and is frequented by photographers who, from the canyon rim, are able to photograph jets flying beneath them.

Red Cathedral

Red Cathedral is a geological formation located between highways 178 and 190. Formed of steep cliffs, it is composed of red colored oxidized rocks and is visible from Zabriskie point and the Golden Canyon trail.

Saline Valley

Salt Creek

Much of Salt Creek is usually dry at the surface and covered by a bright layer of salt which was created by many flooding and subsequent evaporation of water that periodically flows at the surface. Over time the small amount of solutes in the water accumulate to form this linear salt pan. Another part of salt creek runs with brackish water year-round. It is here that the last survivor of Lake Manly resides; the Death Valley pupfish.

Saratoga Springs

Saratoga Springs () is a desert oasis located in southern

. 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 (2.7 ha) in area, making the site the third largest

in the park. The pools provide habitat for several

endemic Endemism is the state of a species being found in a single defined geographic location, such as an island, state, nation, country or other defined zone; organisms that are indigenous to a place are not endemic to it if they are also found else ...

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 Bulrush is a vernacular name for several large wetland grass-like plants *Sedge family (Cyperaceae): **''Cyperus'' **'' Scirpus'' **''Blysmus'' **''Bolboschoenus'' **'' Scirpoides'' **'' Isolepis'' **'' Schoenoplectus'' **'' Trichophorum'' * T ...

and saltgrass. The springs were probably named in 1871 by the

Wheeler Survey The Wheeler Survey, carried out in 1872-1879, was one of the "Four Great Surveys" conducted by the US government after the Civil War primarily to document the geology and natural resources of the American West. Supervised by First Lieutenant (lat ...

after the resort town of

Saratoga Springs, New York Saratoga Springs is a city in Saratoga County, New York, United States. The population was 28,491 at the 2020 census. The name reflects the presence of mineral springs in the area, which has made Saratoga a popular resort destination for over 2 ...

, 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 Gold is a chemical element with the symbol Au (from la, aurum) and atomic number 79. This makes it one of the higher atomic number elements that occur naturally. It is a bright, slightly orange-yellow, dense, soft, malleable, and ductile me ...

and

silver Silver is a chemical element with the symbol Ag (from the Latin ', derived from the Proto-Indo-European ''h₂erǵ'': "shiny" or "white") and atomic number 47. A soft, white, lustrous transition metal, it exhibits the highest electrical ...

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 Talc, or talcum, is a clay mineral, composed of hydrated magnesium silicate with the chemical formula Mg3Si4O10(OH)2. Talc in powdered form, often combined with corn starch, is used as baby powder. This mineral is used as a thickening agent a ...

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.

Scotty's Castle

Shoreline Butte

This desert

butte __NOTOC__ In geomorphology, a butte () is an isolated hill with steep, often vertical sides and a small, relatively flat top; buttes are smaller landforms than mesas, plateaus, and tablelands. The word ''butte'' comes from a French word me ...

was once an island in a lake that filled Death Valley several times during the

Pleistocene The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in ...

ice age An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and gre ...

s. Scientists call all manifestations of this large body of water

. There are different horizontal linear features on the northeast flank of the butte that are ancient shorelines from this lake. It takes some time for waves to gnaw away terraces like the ones seen on Shoreline Butte, so these benches provide records of times when the lake level stabilized long enough for waves to leave their mark on the rock. The highest strandline is one of the principal clues that geologists use to estimate the depth of the lake that once filled Death Valley. Shorelines of ancient Lake Manly are preserved in several parts of Death Valley, but nowhere is the record as clear as at Shoreline Butte. Several lakes have occupied Death Valley since the close of the Pleistocene epoch 10,000 years ago, but these younger lakes were quite shallow compared to Lake Manly (See Badwater and Devils Golf Course above).

Teakettle Junction

At the junction where the unimproved road from Ubehebe Crater meets roads to the Racetrack Playa and Hunter Mountain (), there is a sign reading "Teakettle Junction." While the origin of the name is unknown, it has become a tradition for visitors to attach teakettles to the sign with messages written on them.

National Park Service ranger National Park Service rangers are among the uniformed employees charged with protecting and preserving areas set aside in the National Park System by the United States Congress and the President of the United States. While all employees of the ag ...

s will sometimes remove a number of teakettles when there are too many. The rock at the junction includes the bedrock sandstone of the Eureka Quartzite strata.

Telescope Peak

Telescope Peak is the highest point within Death Valley National Park and was named for the great distance visible from the summit – 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. Its summit rises above Badwater Basin, the lowest point in Death Valley at .

Titus Canyon

Titus Canyon is a narrow gorge in the Grapevine Mountains near the eastern boundary of

. It features megabreccia and other rock formations, petroglyphs, and wildlife of various kinds, including bighorn sheep. Along the road to the canyon stands Leadfield, a

ghost town Ghost Town(s) or Ghosttown may refer to: * Ghost town, a town that has been abandoned Film and television * ''Ghost Town'' (1936 film), an American Western film by Harry L. Fraser * ''Ghost Town'' (1956 film), an American Western film by All ...

dating to the 1920s.

Ubehebe Crater

Ubehebe Crater is the largest of more than a dozen of in the

Ubehebe Craters The Ubehebe Craters are a volcanic field in the northern Death Valley of California, consisting of 14–16 volcanic crater, craters in a area. The largest of the craters is the wide and deep Ubehebe Crater. Many of the craters, though, are par ...

field. As groundwater exploded into steam due to the heat of magma underneath, an empty pit was left behind and the debris spread around the field. Erosion over the millennia since the eruption revealed multi-colored stripes on the crater walls dating to the

. Visitors can hike on trails to the bottom or around the rim.

Ventifact Ridge

Ventifact Ridge is a part of a

basalt Basalt (; ) is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon. More than 90 ...

ic lava flow. The rocks on its exposed and barren ridge are famous for being shaped by wind erosion and are called ventifacts. Sharp edges of ventifacts called ''Kanters'' are formed when two or more facets (planar surfaces) intersect. Open grooves in the ventifacts are called flutes. Most of the holes in the basalt are vesicles that were formed when gas escaped from the cooling lava. Some of these have been expanded or even merged by sandblasting. Non-stop winds on this ridge are concentrated and compressed at the top of the hill and are very fast as a result. These strong winds pick-up dust and sand (mostly from the two closest alluvial fans), which literally sand-blast exposed surfaces. Winds strong enough for sandblasting come from the north and the south.

References

*''Geology Underfoot in Death Valley and Owens Valley'', Sharp, Glazner (Mountain Press Publishing Company, Missoula; 1997)
USGS: Death Valley National Park Virtual Geology Field Trip
{{DEFAULTSORT:Places Of Interest In The Death Valley Area * * * Geography of San Bernardino County, California Geography of Inyo County, California Tourist attractions in San Bernardino County, California Tourist attractions in Inyo County, California