Ringbone Formation

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Ringbone Formation
Stratigraphic range: Campanian
~84–71  Ma
Type Geological formation
Underlies Hidalgo Formation
Overlies Mojado Formation
Thickness7,500 feet (2,300 m)
Lithology
Primary Mudstone
Other Sandstone
Location
Coordinates 31°57′32″N108°27′50″W / 31.959°N 108.464°W / 31.959; -108.464
Approximate paleocoordinates 39°18′N80°42′W / 39.3°N 80.7°W / 39.3; -80.7
Region New Mexico
Country United States
Type section
Named forRingbone Ranch
Named byS.G. Lasky
Year defined1938
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Ringbone Formation (the United States)
USA New Mexico relief location map.svg
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Ringbone Formation (New Mexico)

The Ringbone Formation is a Campanian geologic formation in southwestern New Mexico. [1] [2]

Contents

Description

The base of the formation is a conglomerate with boulders up to 2.5 feet (0.76 m) in diameter. The bulk of the formation is dark shale with minor sandstone and black limestone. The upper beds are tuffaceous sandstone with minor black limestone. A basalt flow and an andesite breccia are present in the upper beds. [1] The total thickness is about 7,500 feet (2,300 m). The formation interfingers with the underlying Mojado Formation and is overlain by the Hidalgo Formation. [3]

Fossils

The formation contains fossils of the gastropod Physa , [2] [4] the palm Sabal , and other fossils consistent with Campanian age. [3]

Dinosaur remains of tyrannosaurs and hadrosaurs are among the fossils that have been recovered from the formation. [5] These include possible remains of Albertosaurus [6] and a hadrosaur tail skin impression. [7]

History of investigation

The formation was first named as the Ringbone Shale by Lasky in 1938 for outcrops near Ringbone Ranch in the Little Hatchet Mountains. [1] Zeller renamed the unit as the Ringbone Formation in 1970. [3]

See also

References

  1. 1 2 3 Lasky 1938.
  2. 1 2 Hayes 1970.
  3. 1 2 3 Zeller 1970.
  4. Basabilbazo 2000, p. 207.
  5. Weishampel, Dodson & Osmólska 2004, pp. 517–607, "Dinosaur distribution.".
  6. Lucas, Basabilvazo & Lawton 1990.
  7. Anderson et al. 1998.

Bibliography