Jump to content

Conestoga Formation

From Wikipedia, the free encyclopedia
Conestoga Formation
Stratigraphic range: Middle Cambrian to Early Ordovician
Thick-bedded crystalline limestone passing into finely laminated slaty limestone typical of the Conestoga, in quarry 1 mile northwest of Bellemont.
Typesedimentary, metamorphic
OverliesVintage Dolomite
Lithology
Primarylimestone
Otherphyllite, conglomerate
Location
RegionPennsylvania
CountryUnited States
Type section
Named byKnopf and Jonas (1923)
Folded micaceous marble of Conestoga Formation, in a quarry a half-mile northwest of Quarryville
Basal Conestoga (slate and limestone conglomerate), unconformably overlying Vintage Dolomite, Bellemont Quarry

The Conestoga Formation is a geologic formation in Pennsylvania.

Description

[edit]

Light-gray, thin-bedded, impure, contorted limestone having shale partings; conglomeratic at base; in Chester Valley, includes micaceous limestone in upper part, phyllite in middle, and alternating dolomite and limestone in lower part.[1]

Type section

[edit]

Named from outcrops along Conestoga River, Lancaster County, Pennsylvania.

References

[edit]
  1. ^ Conestoga Formation, USGS Mineral Resources On-Line Spatial Data