West Falls Group Explained

West Falls Formation
Type:Geologic Group
Age:Frasnian
Period:Frasnian
Prilithology:Shale
Otherlithology:Black shale
Namedfor:West Falls, New York
Region:Appalachian Basin
Country:United States
Subunits:
  • Angola Shale (NY)
  • Nunda Sandstone (NY,PA)
  • West Hill Formation (NY)
  • Gardeau Formation (NY,PA)
  • Grimes Siltstone (NY)
  • Rhinestreet Formation (NY,PA)
  • Walton Formation (NY)
  • Moreland Shale (NY)
  • Millport Shale (NY)
  • Beers Hill Formation (NY)
  • Slide Mountain Formation (NY)
  • Honesdale Formation (NY)
Underlies:Java Formation
Overlies:Sonyea Group

The West Falls Group is a geologic group in the Appalachian Basin. It dates back to the Devonian period. Also stratigraphically equivalent to the Portage Group.

Description

Stratigraphy

The West Falls Group is a geologic group in New York. It dates back to the Devonian period. Also stratigraphically equivalent to the Portage Group.

The West Falls formation is bounded above by the Java Formation and below by the Sonyea Formation. It comprises the Angola Shale and Rhinestreet Shale Members. It was deposited during the Acadian Orogeny and is part of the Salina thrust sheet.[1]

Also known as the West Falls Formation in New York.

Geographic distribution

The West Falls is recognized in the subsurface from western New York to eastern Tennessee.[2]

Lithology

The predominant lithology of the West Falls Group is shale. The Rhinestreet Member can be further subdivided into two shale types: a thick, fissile black shale underlies a gray to greenish-gray shale that likely indicates a transitional environment. The Angola member is a gray to greenish-gray shale, easily distinguished by its consistent low gamma ray signature, which is typical of this shale type.[3]

Paleontology

The West Falls Formation was deposited during the Frasnian stage of the Upper Devonian. Two distinct community types are observed in the group: "a shallower water spiriferacean-rhynchonellide-bivalve species ensemble, and a deeper water assemblage of unattached epibenthic and sessile semi-infaunal brachiopods" (Sutton, McGee).[4]

Economic significance

Both members of the West Falls Formation have been assessed for oil and gas exploration. The USGS has determined that the average total organic carbon (TOC) in the Rhinestreet Shale is 0.89%; the TOC in the Angola Shale is 1.47%.[5]

The Rathbone shale field in Rathbone, Steuben County, New York was discovered in 1931. 31 wells were drilled in this field, targeting the Angola and Rhinestreet members. Of these, 24 produced natural gas, 4 were dry holes, 2 were plugged and abandoned, and one produced oil. The wells were typically 900feetto1500feetft (toft) in depth, reservoir pressure was 225lk=onNaNlk=on and flow rates ranged from 100to per day.[6]

External links

Notes and References

  1. Web site: Figure 3 . pubs.usgs.gov.
  2. Web site: Angola and Rhinestreet Shales (NYDwf;4). tin.er.usgs.gov. 2017-07-12.
  3. Web site: Open File Reports . dnr.state.oh.us.
  4. Web site: Late Devonian marine ecosystems of the lower West Falls Group in New York The Catskill Delta GeoScienceWorld Books GeoScienceWorld. specialpapers.gsapubs.org. en. 2017-07-12.
  5. Web site: NY Hill Radiation . treichlerlawoffice.com.
  6. Web site: Radiation . treichlerlawoffice.com.