Earth:Schnebly Hill Formation

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Short description: Dark red sandstone, the major component of the red rocks of Sedona, Arizona
Schnebly Hill Formation
Stratigraphic range: 286–273 Ma
[1]
Bell Rock Top.jpg
Bell Rock, Sedona
Thickness800 feet (240 m) to 1,000 feet (300 m)
Lithology
PrimarySandstone
Location
RegionColorado Plateau
CountryUnited States
Type section
Named forSedona Schnebly
LocationArizona
Thickness at type section800 feet (240 m) to 1,000 feet (300 m)

The Schnebly Hill Formation is a section of red bed deposits found at the Colorado Plateau, near Sedona, Arizona. It is a dark red sandstone, from 800 feet (240 m) to 1,000 feet (300 m) thick. It lies between Coconino Sandstone and the older Hermit Formation.[2] It is near the Supai Group.[3]

The source of the name "Schnebly" is Sedona Schnebly, after whom the city of Sedona, Arizona, was named.[4]

Geology

The formation traces to the Permian Age.[5][6]

The formation is the most prominent layer of the red rocks of the Sedona area due the presence of hematite – iron-oxide, frankly, rust – giving the sandstone a red color. The Schnebly Hill Sandstone formation comprises three sections:

  • the Bell Rock member,
  • the Fort Apache member, and
  • the Sycamore Pass member.[7]

See also

Sedona-area rocks

  • Bell Rock
  • Capitol Butte
  • Cathedral Rock
  • Courthouse Butte
  • Red Rock State Park
  • Slide Rock State Park

Local geology

Local interest

  • Cottonwood, Arizona
  • Honanki
  • Jerome, Arizona
  • Jerome State Historic Park
  • Chapel of the Holy Cross
  • Oak Creek Canyon
  • Palatki Heritage Site
  • Slide Rock State Park

References

External links and references