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Death Valley

 

Death Valley

(NASA image)
Death Valley is a deep arid basin in the northern Mojave Desert of southern California in the United States, extending for approximately 140 mi (225 km) along the California-Nevada border approximately 100 mi (160 km) west of Las Vegas. Famous for its brutal extremes of heat, the valley floor at Badwater Basin is the location of the lowest point in the Western Hemisphere (N36° 13.961' W116° 46.700'), at 282 feet (86 m) below sea level. The entire valley is located within Death Valley National Park.

The valley is located southeast of the Sierra Nevada range in the Great Basin. It is bounded on the east by the Grapevine Mountains, Funeral Mountains, and Amargosa Range. It is bounded on the west by the Cottonwood Mountains and the Panamint Range. The geological configuration is considered one of the best examples of the Basin and Range configuration.

The valley radiates extreme amounts of heat, allowing for temperatures that are among the hottest on earth. The hottest temperature recorded in the U.S., and the second hottest in the world, was 134°F (56.6°C) at Greenland Ranch near the valley on July 10, 1913. The valley receives less than 2 in (5 cm) of rain annually. The Amargosa River and Furnace Creek flow through the valley, disappearing into the sands of the valley floor.

While there is very little rain in Death Valley, the valley is prone to flooding during heavy rains, because the soil is unable to absorb the bulk of the water. The runoff can produce dangerous flash floods. In August 2004 such flooding occurred, causing two deaths and shutting down the national park.

During the late Pleistocene, the valley was indundated by prehistoric Lake Manly. The valley received its name in 1849 during the California gold rush by emigrants who sought to cross the valley on their way to the gold fields. During the 1850s, gold and silver were extracted in the valley. In the 1880s borax was discovered and extracted by mule-drawn wagons.

For a detailed examination of the geology and other features of the valley, see Death Valley National Park

Native population


Death Valley is home to the Timbisha tribe, who have inhabited the valley for at least the past 1000 years. Some families still live in the valley at Indian Village. The name of the valley, tümpisa, means 'rock paint' and refers to the valley as a source of red ochre paint. Another village in the valley was located in Grapevine Canyon near the present site of Scotty's Castle. It was called maahunu, the meaning of which is uncertain although hunu means 'canyon'. See Timbisha Language.

Composition and occurrence of salts in Death Valley


(green crescent feature) at the far right, and the sand dunes near Stove Pipe Wells at the center. (NASA image)


Mineral


Composition


Known or probable occurrence


Halite


NaCl


Principal constituent of chloride zone and of salt-impregnated sulfate and carbonate deposits.


SyIvite


KCI


With halite.


Nahcolite


NaHCO3


Not yet identified; might be found in wintertime as efflorescence or trona or thermonatrite in carbonate zone in Cottonball Basin.


Trona


Na3H(CO3)22H2O


Carbonate zone of Cottonball Basin, especially in marshes.


Thermonatrite


Na2CO3·H2O


Questionably present on floodplain in Badwater Basin, would be expected in marshes of carbonate zone in Cottonball Basin.


Natron


Na2CO3·10H2O


Not yet identified but may be expected, especially In winter, immediately following rains or periods of high discharge at marshes in carbonate zone in Cottonball Basin.


Pirssonite


Na2Ca(CO3)2·2H2O


Not yet identified, may be expected in environments where gaylussite would be dehydrated.


Gaylussite


Na2Ca(CO3)2·5H2O


Carbonate zone and floodplain in Badwater Basin.


Calcite


CaCO3


Occurs as clastic grains in sediments underlying salt pan and as sharply terminated crystals in clay fraction of carbonate zone and in sediments underlying sulfate zone.


Magnesite


MgCO3


Obtained in artificially evaporated brines from Death Valley; not yet identified in salt pan; may be expected in carbonate zone of Cottonball Basin.


Dolomite


CaMg(CO3)2


identified only as a detrital mineral; may be expected in carbonate zone.


Northupite


and/or


Tychite


Na3MgCl(CO3)

 


Na6Mg2(SO4)·(CO3)4


An isotropic mineral, having index of refraction in the range of Northupite and Tychite, has been observed in saline facies of sulfate zone in Cottonball Basin.


Burkeite


Na6(CO3)(SO4)2


Sulfate zone in Cottonball Basin.


Thenardite


Na2S04


Common in all zones in Cottonball Basin and in sulfate marshes in Middle and Badwater basins.


Mirabilite


Na2S04·10H2O


Occurs on floodplains in Cottonball Basin immediately following winter storms.


Glauberite


Na2Ca(SO4)2


Common on floodplains except in central part of Badwater Basin; sulfate zone in Cottonball Basin.


Anhydrite


CaSO4


As layer capping massive gypsum I mile north of Badwater. Possibly also as dry-period efflorescence on floodplains.


Bassanite


2CaSO4·H2O


As layer capping massive gypsum along west side of Badwater Basin and as dry-period efflorescence in floodplains.


Gypsum


CaS04·2H2O


In sulfate caliche, layer in carbonate zone, particularly in Middle and Badwater basins, in sulfate marshes and as massive deposits in sulfate zone.


Hexahydrite


MgS04·6H2O


Not yet identified but might he expected as dehydration product of epsomite in chloride zone on floodplains.


Epsomite


MgS04·7H2O


Not yet identified; probably will he found as efflorescence on floodplains following storms or floods would dehydrate to hexahydrite during dry periods.


Bloedite


Na2Mg(SO4)2·4H2O


Questionably present in efflorescence on floodplain in chloride zone.


Polyhalite


K2Ca2Mg(SO4)4·2H2O


Questionably present on floodplain in chloride zone.


Barite


BaS04


Not yet identified but probably will be found in carbonate zone and as clastic grains in sediments underlying salt pan.


Celestite


SrSO4


Found with massive gypsum.


Schairerite


Na3(SO4)(F,Cl)


Not yet identified, might he expected in Cottonball Basin or east side of Middle Basin.


Sulfohalite


Na6ClF(SO4)2


Not yet identified, might he expected in Cottonball Basin or east side of Middle Basin.


Kernite


Na2B4O7·5H2O


Possibly present in Middle Basin in surface layer of layered sulfate and chloride salts.


Tincalconite


Na2B4O7·10H2O


Probably occurs as dehydration product of borax.


Borax


Na2Mg(SO4)2·4H2O


Floodplains and marshes in Cottonball Basin.


Inyoite


Ca2B6O11·13H2O


Questionably present (X-ray determination but unsatisfactory) in floodplain in Badwater Basin.


Meyerhofferite


Ca2B6O11·7H2O


Found in all zones in Badwater Basin and in rough silty rock salt in Cottonball Basin


Colemanite


Ca2B6O11·5H2O


Questionably present (X-ray determination but unsatisfactory) in floodplain in Badwater Basin.


Ulexite


NaCaB5O9·8H2O


Common in floodplain in Cottonball Basin; known as "cottonball"


Proberite


NaCaB5O9·5H2O


A fibrous borate with index of refraction higher than ulexite occurs on dry areas in Cottonball Basin following hot dry spells and in surface layer of smooth silty rock salt.


Soda niter


NaNO3


Weak, but positive chemical tests obtained locally.

References

  • U.S. Geological Survey Professional Paper 494, Hunt, C.B., and Mabey, D.R., 1966, General geology of Death Valley, California (adapted public domain table)[1]



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