Cherry Canyon Formation

Coordinates: 31°53′56″N 104°46′48″W / 31.899°N 104.780°W / 31.899; -104.780
Source: Wikipedia, the free encyclopedia.
Cherry Canyon Formation
Ma
Approximate paleocoordinates
3°42′N 34°06′W / 3.7°N 34.1°W / 3.7; -34.1
RegionNew Mexico, Texas
Country United States
ExtentGuadalupe and Delaware Mountains
Type section
Named forCherry Canyon
Named byDeFord and Lloyd
Year defined1940
Cherry Canyon Formation is located in the United States
Cherry Canyon Formation
Cherry Canyon Formation (the United States)

The Cherry Canyon Formation is a

Period.[1]

Description

The formation consists mostly of cyclic marine

hiatus in deposition, marking a substantial drop in sea level, separates the Cherry Canyon Formation from the overlying Bell Canyon Formation.[4]

The Getaway Member contains carbonate debris flow beds. All three carbonate members grade into sandstone channel deposits deeper in the basin.[3]

Fossils

The formation contain abundant fish fossils, such as sharks' teeth, preserved within small

phosphatic nodules.[5] Ostracods have been identified in the Getaway Member, including Amphissites, Aurikirkbya, Ceratobairdia, Polytylites, and Roundyella.[6]

Economic resources

The Cherry Canyon Formation has been exploited for its hydrocarbon resources.

History of investigation

The unit was first designated as a formation by DeFord and Lloyd in 1940, who raised the

Delaware Mountain Formation to group rank and designed its previously informal members as formations.[9][10]

Footnotes

  1. ^ Kues and Giles 2004, p.100
  2. ^ King 1948, p.36
  3. ^ a b Kues and Giles 2004, p.124
  4. ^ Kues and Giles 2004, p.126
  5. ^ "Guadalupe Mountains National Park," Hunt, Santucci, and Kenworthy (2006); page 64.
  6. .
  7. .
  8. .
  9. ^ DeFord and Lloyd 1940
  10. ^ King 1942
Laminae in the Cherry Canyon Formation

Bibliography