Lead Camp Limestone

The Lead Camp Limestone is a geologic formation in the San Andres Mountains of New Mexico. It preserves fossils dating back to the middle Pennsylvanian.[1][2]

Lead Camp Limestone
Stratigraphic range: Pennsylvanian
TypeFormation
UnderliesPanther Seep Formation
OverliesLake Valley Limestone, Sandia Formation
Thickness320–861 ft (98–262 m)
Lithology
PrimaryLimestone
OtherShale
Location
Coordinates32.7337°N 106.5746°W / 32.7337; -106.5746
RegionNew Mexico
CountryUnited States
Type section
Named forLead Camp Canyon
Named byBachman and Myers
Year defined1969
Lead Camp Limestone (the United States)
Lead Camp Limestone (New Mexico)

Description

The Lead Camp Limestone consists of 75% medium- to dark-gray cherty limestone and 21-24% calcareous shale. The base of the formatino contains minor sandstone and conglomerate. The limestone forms prominent cliffs capping the southern San Andres Mountains. The total thickness is 320–861 feet (98–262 m).[1] The formation rests unconformably on the Lake Valley Limestone to the south and conformably on the Sandia Formation to the north.[2]

Deposition began in the late Morrowan (Bashkirian) to the south, spread to the north in the Atokan (early M0scovian, and continued into the Missourian(Kasimovian) Age.[2]

Fossils

The formation contains marine fossils in the calcareous shale beds. It contains fusilinids characteristic of the middle Pennsylvanian.[2]

History of investigation

The formation was first defined by Bachman and Myers in 1969, for exposures near the confluence of Lead Camp and San Andres Canyons.[1]

See also

Footnotes

  1. Bachman and Myers 1969
  2. Kues and Giles 2004

References

  • Bachman, George O.; Myers, Donald A. (1969). "Geology of the Bear Peak area, Dona Ana County, New Mexico". U.S. Geological Survey Bulletin. 1271-C. doi:10.3133/b1271C.
  • Kues, B.S.; Giles, K.A. (2004). "The late Paleozoic Ancestral Rocky Mountain system in New Mexico". In Mack, G.H.; Giles, K.A. (eds.). The geology of New Mexico. A geologic history: New Mexico Geological Society Special Volume 11. pp. 95–136. ISBN 9781585460106.
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