Zabriskie Quartzite

Zabriskie Quartzite
Stratigraphic range: Lower Cambrian [1]
TypeGeologic formation
UnderliesCarrara Formation
OverliesWood Canyon Formation
Thickness0–2,000 feet (0–610 m)[1]
Lithology
PrimaryQuartzite
Location
RegionInyo County, California, Nye County, Nevada
CountryUnited States
Type section
Named forZabriskie Point

The Zabriskie Quartzite is a Cambrian Period geologic formation of the northern Mojave Desert, in Inyo County, California and Nye County, Nevada.[2][3]

It is named for its occurrence at Zabriskie Point, located on the eastern slopes of Death Valley in Death Valley National Park.[2]

Geology

The lower unit is defined by the Resting Springs Member, the upper unit by the Emigrant Pass Member.[3]

It overlies the Wood Canyon Formation, and underlies the Carrara Formation.[4]

The Quartzite is mostly massive arid granulated due to shearing, in beds 0.5–2 feet (15–61 cm) thick within the park,[2] and up to 984 feet (300 m) elsewhere.[4]

Paleobiota

The Zabriskie Quartzite contains a wealth of Skolithos trace fossils, although no other fossils have been reported from this formation, despite the underlying and overlying formations containing fossil material.[1]

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Ichnogenera

Genus Species Notes Images
Skolithos[1]
  • Skolithos sp.
Burrows.

See also

References