Horquilla Formation

Last updated
Horquilla Formation
Stratigraphic range: Pennsylvanian
Type Formation
Sub-units La Tuna Member, Berino Member, Bishop Cap Member
Underlies Earp Formation
Overlies Escabrosa Limestone, Black Prince Limestone, Paradise Formation, Helms Formation
Thickness800–3,520 ft (240–1,070 m)
Lithology
Primary Limestone
Other Shale, sandstone
Location
Coordinates 31°40′08″N110°03′58″W / 31.669°N 110.066°W / 31.669; -110.066
Region Arizona, New Mexico
Country United States
Type section
Named forHorquilla Peak, Cochise County, Arizona
Named by James Gilluly, J.R. Cooper, and J. Steele Williams
Year defined1954
Usa edcp relief location map.png
Lightgreen pog.svg
Horquilla Formation (the United States)
USA Arizona relief location map.svg
Lightgreen pog.svg
Horquilla Formation (Arizona)

The Horquilla Formation is a geologic formation exposed in southern Arizona [1] and New Mexico. It preserves fossils dating back to the Pennsylvanian.

Contents

Description

The formation is mostly thinly bedded pinkish limestone, weathering to blue-gray, with occasional thicker beds of limestone and thinner beds of shaly limestone. The thicker limestone beds typically consist mostly of fragments of crinoids. In southeastern Arizona, the formation lies on top of the Escabrosa Limestone, the Black Prince Limestone, [1] or the Paradise Formation, [2] and is overlain in turn by the Earp Formation. [1] In the Organ Mountains, the formation rests disconformably on the Helms Formation. [3] The formation varies in thickness from 800 ft (240 m) in the Chiricahua Mountains [2] to 3,450 ft (1,050 m) in the Big Hatchet Mountains. [4]

The formation is thought to have been laid down in the Horquilla Seaway, a continental shelf environment on the southwest coast of Pangaea. [3]

Fossils

The formation is highly fossiliferous. The most numerous fossils at the type section are brachiopods (such as Neospirifer , Composita , and Dictyoclostus ) and fusulinids (such as Fusulina and Fusulinella ). Crinoid stems, syringoporoid corals, and bryozoans are also common. The fossils are post-Morrowan (Moscovian to Kasimovian) in age. [1] Demosponges such as Chaetetes are found in exposures further east, in the Chiricahua Mountains [2] and Big Hatchet Mountains. [5] Exposures in the Organ Mountains include fossils of Chaetetes, Petalaxis , Fusulinella, and cordaite leaf impressions. [3]

History of investigation

The formation was first designated by James Gilluly and coinvestigators in 1954, who raised the Naco Formation to group rank and assigned its lowermost beds to the Horquilla Formation. The type section is on an eastern spur of Horquilla Peak in the Tombstone Hills of southern Arizona. [1] The formation was later mapped as far west as the Vekol Mountains [6] and as far east as the Big Hatchet Mountains in the New Mexico bootheel. [4] Spencer G. Lucas and Karl Krainer have noted the similarity of the Pennsylvanian beds of the Organ Mountains to the Horquilla Formation, and have proposed lowering the La Tuna Formation, Berino Formation, and Bishop Cap Formation to member rank within the Horquilla Formation. [3]

See also

Footnotes

References

This page is based on this Wikipedia article
Text is available under the CC BY-SA 4.0 license; additional terms may apply.
Images, videos and audio are available under their respective licenses.