Exeter Sandstone Explained

Exeter Sandstone
Type:Formation
Period:middle Jurassic
Prilithology:Sandstone
Namedfor:Exter Post Office
Namedby:W.T. Lee
Year Ts:1902
Region:Colorado
New Mexico
Country:United States
Coordinates:36.9756°N -103.206°W
Unitof:Dockum Group
Underlies:Bell Ranch Formation
Overlies:Sheep Pen Sandstone
Thickness:24meters

The Exeter Sandstone is a geologic formation exposed in northeastern New Mexico. Its age is poorly controlled, but it is thought to have been deposited during the middle Jurassic.

Description

The formation consists of up to 24meters of white to pale pink crossbedded quartz sandstone. It unconformably overlies the Sheep Pen Sandstone and is in turn overlain by the Bell Ranch Formation. The Exeter Formation varies greatly in thickness, with the maximum thickness in synclinal valleys of the underlying Dockum Group and the formation being absent on some anticlinal crests of the Dockum Group.

The formation has long been thought to have formed in the eastern part of the Entrada Formation dune sea and thus to be correlative with the Entrada Formation, and Spencer G. Lucas and coinvestigators recommended demoting the Exeter Sandstone to member rank within the Entrada Formation. However, age control is poor on the Exeter Sandstone, and other investigators have retained the Exeter Sandstone at formation rank until the correlation becomes clearer.

History of investigation

The formation was first named by W.T. Lee in 1902 for exposures near the Exter Post Office.[1]

See also

References

Notes and References

  1. https://ngmdb.usgs.gov/Geolex/Units/Exeter_8058.html GEOLEX: "Exeter"