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Locality 5 Cambell Hollow &Steele Hollow, McKean County, Pennsylvania, USA
Mindat.org Locality Page | McKean County, Pennsylvania, USA |
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Lat/Long (Decimal) | 41.8167,-78.2833 |
Co-ordinates Derivation | based on political unit |
Given Location | Pennsylvania, United States |
Mindat.org Region (for given coordinates) | McKean County, Pennsylvania, USA |
Collections
Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
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DeLong Quarry | Arnold C. A. (1932) | Conewango - Pocono | Arnold (1932, p. 52): "The lower ten or twelve feet of rock exposed in the quarry consists of hard massive sandstone cracked in various directions. Above this lies a bed, two feet or less thick, consisting of yellow mud and sand." | sandstone | 372.2 - 358.9 Ma Late/Upper Devonian |
Port Allegany | Pocono | sandstone | 379.5 - 360.7 Ma Late/Upper Devonian | ||
Locality 5 Cambell Hollow &Steele Hollow | Arnold C. A. (1939) | Oswayo sandstone | Arnold (1939,p.276): Sandstones overlie the Cattaraugus red beds | sandstone | 382.7 - 358.9 Ma Late/Upper Devonian |
Recorded Fossils
Accepted Name | Hierarchy | Age |
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Archaeopteris sp. genus | Plantae : Aneurophytophyta : Archaeopteridopsida : Archaeopteridales : Archaeopteridaceae : Archaeopteris | 382.7 - 358.9 Ma Late/Upper Devonian |
Callixylon sp. genus | Plantae : Aneurophytophyta : Archaeopteridopsida : Archaeopteridales : Archaeopteridaceae : Callixylon | 382.7 - 358.9 Ma Late/Upper Devonian |
Lepidostrobus sp. genus | Plantae : Tracheophyta : Lycopodiopsida : Lepidodendraceae : Lepidostrobus | 382.7 - 358.9 Ma Late/Upper Devonian |
Rhacopteris sp. genus | Plantae : Tracheophyta : Rhacopteris | 372.2 - 358.9 Ma Late/Upper Devonian |
Sigillaria sp. genus | Plantae : Sigillariaceae : Sigillaria | 372.2 - 358.9 Ma Late/Upper Devonian |
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!