Point Lookout Sandstone

Point Lookout Sandstone
Stratigraphic range: Upper Cretaceous
Point Lookout, Mesa Verde National Park
TypeFormation
Unit ofMesaverde Group
Sub-unitsHosta Tongue
UnderliesMenefee Formation
OverliesCrevasse Canyon Formation
Thickness300 ft (91 m)
Lithology
PrimarySandstone
OtherShale
Location
Coordinates37°18′58″N 108°25′08″W / 37.316°N 108.419°W / 37.316; -108.419
RegionParadox Basin, San Juan Basin
CountryUnited States
Type section
Named forPoint Lookout
Named byA. J. Collier
Year defined1919
Point Lookout Sandstone is located in the United States
Point Lookout Sandstone
Point Lookout Sandstone (the United States)
Point Lookout Sandstone is located in Colorado
Point Lookout Sandstone
Point Lookout Sandstone (Colorado)
Stratigraphic section of formations exposed at the surface, Mesa Verde National Park, Colorado (USGS).

The Point Lookout Sandstone is a Cretaceous bedrock formation occurring in New Mexico and Colorado.

Description

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The formation consists of two informal members. The lower is a sequence of thinly bedded sandstone and shale,[1] while the upper is a massive medium- to fine-grained cross-bedded sandstone, light gray to buff in color, that is a conspicuous cliff-forming unit.[1][2] Maximum thickness is 131 meters (430 feet).[1]

The lower contact is placed at the first thin sandstone bed above the shale of the Mancos Shale. The formation is overlain by the Menefee Formation.[1]

The Point Lookout Sandstone was deposited in the Cretaceous Interior Seaway, as part of a regressive sequence as the seaway was receding. It is transitional between the marine environment of the underlying Mancos and the coastal plain environment of the overlying Menefee Formation.

Fossils

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Dinosaur remains are among the fossils that have been recovered from the formation, including a well preserved maniraptoran feather,[3] although none have yet been referred to a specific genus.[4]

The ammonite Clioscaphites vermiformis was identified in the formation.[5]

Resource geology

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Exposures of the Point Lookout Sandstone at Apache Mesa in New Mexico contain heavy mineral deposits, rich in titanium, zirconium, rare earth elements, and other valuable metals. However, the deposits are much too small to be economical to mine as of 2021. The deposits represent a beach placer deposit similar to ones seen in the southeastern U.S. Atlantic coast, southeastern Australia, and India.[6]

History of investigation

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The sandstone was first described by A. J. Collier for exposures in cliffs at Point Lookout, in Mesa Verde National Park, Montezuma County, Colorado, in the Paradox Basin,[7] and later described by Allen and Balk in 1954 as part of the Mesaverde Group in the San Juan Basin in New Mexico.[8]

See also

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Footnotes

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  1. ^ a b c d Lucas & Heckert 2005.
  2. ^ Cather 2010.
  3. ^ Williamson, T.E.; Kues, B.S.; Weissmann, G.S.; Stidham, T.A.; Yurchyk, S.L. (2009). "A feather from the Upper Cretaceous (lower Campanian) Point Lookout Sandstone, San Juan Basin, northwestern New Mexico". Cretaceous Research. 30: 547–550. doi:10.1016/J.CRETRES.2008.10.003. S2CID 128818922.
  4. ^ Weishampel, Dodson & Osmólska 2004.
  5. ^ Tschudy 1976.
  6. ^ McLemore 2017.
  7. ^ Collier 1919.
  8. ^ Allen & Balk 1954.

References

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