Earth:Washington Formation

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Washington Formation
Stratigraphic range: Permian
Bituminous coal (Washington Coal, Upper Pennsylvanian; Ohio)
TypeFormation
Unit ofDunkard Group[1]
Sub-unitsUpper Washington

Jollytown coal
Hundred sandstone
Upper Marietta
Washington “A” coal
Middle Washington
Lower Washington
Lower Marietta
Washington (No. 12) coal
Little Washington coal
Mannington sandstone
Waynesburg “A” coal
Waynesburg Sandstone
Elm Grove limestone

Cassville
UnderliesGreene Formation
OverliesWaynesburg Formation
Lithology
Primarylimestone, sandstone, coal
Othershale
Location
RegionOhio and West Virginia
CountryUnited States

The Washington Formation is a coal, sandstone, and limestone geologic formation located in Ohio, Pennsylvania and West Virginia.[1] It dates back to the Lower Permian period, with its base at or near the Permian/Carboniferous boundary.[2][3] The Washington formation and the Dunkard Group as a whole was deposited at a time when the continents were in the process of forming the "Super Continent" Pangaea as well as a gradual drop in sea levels.[4] The result during this period was coals being thinner and impure with high ash content. The limestones found with in the formation are exclusively freshwater deposits.

Paleofauna

The Paleo fauna of the Washington formation is considered similar to that of the Texas red beds, sharing many taxa of fish and tetrapods with the red beds. Some of the taxa listed suggest an Artinskian age [5]


Fishes

Orthacanthus

Xenacanthus

Ectosteorhachis

Dipnoa


Amphibians

Eryops


Trimerorhacis

Zatrachys

Diploceraspis

Acheloma

Synapsids

Edaphosaurus boanerges

Dimetrodon limbatus


Ophiacodon retroversus


Diadectomorpha

Diadectes

References


Template:Chronostratigraphy of Ohio Template:Chronostratigraphy of Pennsylvania Template:Chronostratigraphy of West Virginia