Exeter Sandstone

Last updated
Exeter Sandstone
Stratigraphic range: middle Jurassic
Steamboat Butte New Mexico.jpg
Exeter Formation capping Steamboat Butte, New Mexico, US
Type Formation
Unit of Dockum Group
Underlies Bell Ranch Formation
Overlies Sheep Pen Sandstone
Thickness24 meters (79 ft)
Lithology
Primary Sandstone
Location
Coordinates 36°58′32″N103°12′22″W / 36.9756°N 103.2060°W / 36.9756; -103.2060
Region Colorado
New Mexico
Country United States
Type section
Named forExter Post Office
Named byW.T. Lee
Year defined1902
Usa edcp relief location map.png
Cyan pog.svg
Exeter Sandstone (the United States)
USA New Mexico relief location map.svg
Cyan pog.svg
Exeter Sandstone (New Mexico)

The Exeter Sandstone is a geologic formation exposed in northeastern New Mexico. [1] Its age is poorly controlled, but it is thought to have been deposited during the middle Jurassic. [2]

Contents

Description

The formation consists of up to 24 meters (79 ft) 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. [1] 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. [2]

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, [3] [4] and Spencer G. Lucas and coinvestigators recommended demoting the Exeter Sandstone to member rank within the Entrada Formation. [5] However, age control is poor on the Exeter Sandstone, [2] and other investigators have retained the Exeter Sandstone at formation rank until the correlation becomes clearer. [6] [2]

History of investigation

The formation was first named by W.T. Lee in 1902 for exposures near the Exter Post Office. [7] [8]

See also

Footnotes

References