Hueco Formation Explained

Hueco Formation
Type:Formation
Period:early Permian
Prilithology:Limestone
Otherlithology:Shale, sandstone
Namedfor:Hueco Mountains
Namedby:G.B. Richardson
Year Ts:1904
Region:Texas
Country:United States
Coordinates:31.953°N -106.027°W
Underlies:Wilkie Ranch Formation
Overlies:Panther Seep Formation
Thickness:5000feet

The Hueco Formation is a geologic formation in west Texas and southern New Mexico.[1] [2] [3] It preserves fossils dating back to the early Permian period.[4] [5]

Description

The formation is composed most of massive gray fossiliferous limestone with some shale and sandstone, with a thickness in excess of 5000feet. It overlies the Panther Seep Formation[6] with a slight disconformity, and its base is typically a thick biostromal limestone bed.[7] The formation unconformably underlies the Wilkie Ranch Formation.[8] It intertongues with the Abo Formation in the southern San Andres Mountains.[5]

In the Robledo Mountains, the Hueco is promoted to group rank and divided into (in ascending stratigraphic order) the Shalem Colony, Community Pit, Robledo Mountains, and Apache Dam Formations.[9] In the Hueco Mountains, the uppermost formation is the Alacran Mountain Formation.[10]

The Hueco Formation is contemporary with the Abo Formation and represents continued marine sediment deposition south of the prograding Abo deltas.[7]

History of investigation

The formation was first defined by G.B. Richardson in 1904, but mistakenly thought to be Pennsylvanian in age.[1] Nelson dated the formation as earliest Permian in the Franklin Mountains in 1940.[4] Spencer G. Lucas et al. promoted the formation to group rank in 1998.[9]

See also

References

Notes and References

  1. Richardson 1904
  2. Richardson 1908
  3. Richardson 1914
  4. Nelson 1940
  5. Bachman and Hayes 1958
  6. Kelley and Matheny 1983
  7. Kues and Giles 2004
  8. Cys 1976
  9. Lucas et al. 1998
  10. Williams 1963