Feltville Formation

{{Infobox rockunit

| name = Feltville Formation

| period = Hettangian

| age = Hettangian
~{{Geological range|199|196}}

| image = 2ndWatchungMountain_FeltvilleFormation.jpg

| type = Geological formation

| prilithology = Sandstone, siltstone, mudstone

| otherlithology = Limestone

| namedfor = Deserted Village of Feltville, New JerseyOlsen, P.E., 1980. The Latest Triassic and Early Jurassic Formations of the Newark Basin (Eastern North America, Newark Supergroup): Stratigraphy, Structure, and Correlation. New Jersey Academy of Science Bulletin, v. 25, no. 2, p. 25-51.

| namedby = Paul E. Olsen

| year_ts = 1980

| region = Newark Basin of
Eastern North America Rift Basins

| caption = Exposure of Feltville Formation sandstone beneath a ledge of Preakness Basalt on Preakness Mountain in New Jersey.

| unitof = Newark Supergroup
 Meriden Group

| underlies = Preakness Basalt

| overlies = Orange Mountain Basalt

| thickness = maximum of {{convert|1,968|ft|m|-1}}

| extent = continuous for ~{{convert|40|mi|km}} in New Jersey,
with outliers present in
New Jersey, New York
& Pennsylvania

| coordinates = {{coord|40.8|N|74.3|W|display=inline,title}}

| paleocoordinates = {{coord|21.4|N|20.7|W|display=inline}}

| map = {{Location map+ | United States#New Jersey

| relief = 1

| width = 250

| float = center

| places =

{{Location map~ | United States#New Jersey

| lat_deg = 40.8

| lon_deg = -74.3

| mark = Blue pog.svg

| marksize = 12

}}

}}

}}

The Feltville Formation is a mapped bedrock unit primarily in New Jersey, with one known outlier in Pennsylvania and another one in New York. It is named for the Deserted Village of Feltville in Watchung Reservation, New Jersey, which is near where its type section was described by paleontologist Paul E. Olsen.

Description

The Feltville Formation is composed of red, gray, and white sandstone of varying grain thickness, as well as red, gray, and black siltstone and calcareous mudstone. Sandstone/siltstone layers tend to be alternatingly massive and cross-bedded. Black to white carbonaceous limestone layers exist near the base of the formation.[https://mrdata.usgs.gov/geology/state/sgmc-unit.php?unit=NJJf%3B5 Mineral Resources Online Spatial Data – Feltville Formation, New Jersey]. U.S. Geological Survey. Accessed July 23, 2010. Additionally, pebbles and cobbles of quartz are embedded within layers of sandstone and siltstone that interfinger with the Feltville Formation near Oakland, New Jersey.

= Depositional environment =

The Feltville Formation can be characterized as a continuation of the Passaic Formation, which is mostly playa and alluvial fan deposits resulting from the rifting of Pangea. The primarily red color of this formation is often evidence that the sediments were deposited in arid conditions.Faill, R.T., (2004). The Birdsboro Basin. Pennsylvania Geology V. 34 n. 4. However, the Feltville Formation differs from the Passaic Formation in that it contains a more significant portion of non-red layers, which were laid down by deep lakes present during wetter periods.Schlische, Roy W. [http://geology.rutgers.edu/103web/Newarkbasin/NB_text.html Geology of the Newark Rift Basin] {{Webarchive|url=https://web.archive.org/web/20210604164004/https://geology.rutgers.edu/103web/Newarkbasin/NB_text.html |date=2021-06-04 }}. Department of Geological Sciences, Rutgers University, Piscataway, NJ. Accessed July 23, 2010.

= Fossils =

Fish fossils, commonly those of the ray-finned Semionotus, can be found in limestone layers within the formation. In other layers, indeterminate fossil ornithischian tracks have been noted,Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. along with additional reptile and dinosaur prints. Fossil plant remains, as well as root structures and pollen, are also found in the formation.

Age

The Feltville Formation rests conformably above the Orange Mountain Basalt and below the Preakness Basalt, placing its deposition somewhere between approximately 199 and 196 million years ago during the early Jurassic stage known as the Hettangian.

Economic geology

The Feltville Formation was once mined for freestone, as indicated by a historical work detailing quarrying operations at the base of Preakness Mountain in New Jersey.Gordon, Thomas Francis. A Gazetteer of the State of New Jersey – Comprehending a General View of its Physical and Moral Condition, together with a Topographical and Statistical Account of its Counties, Towns, Villages, Canals, Railroads, &c. Published by D. Fenton, 1834. [https://books.google.com/books?id=BnIFAAAAQAAJ&pg=RA1-PA8 Available via Google Books]

See also

References

{{Reflist}}

= Bibliography =

  • {{citation |last1=Weishampel |first1=David B. |author2-link=Peter Dodson |last2=Dodson |first2=Peter |author3-link=Halszka Osmólska |last3=Osmólska |first3=Halszka |year=2004 |title=The Dinosauria, 2nd edition |url=https://books.google.com/books?id=vtZFDb_iw40C |publisher=Berkeley: University of California Press |pages=1–880 |accessdate=2019-02-21 |isbn=0-520-24209-2 |author1-link=David B. Weishampel }}

{{Geology of the Newark Basin}}

Category:Geologic formations of New Jersey

Category:Geologic formations of New York (state)

Category:Geologic formations of Pennsylvania

Category:Hettangian Stage

Category:Jurassic geology of New Jersey

Category:Sandstone formations of the United States

Category:Siltstone formations of the United States

Category:Mudstone formations of the United States

Category:Alluvial deposits

Category:Ichnofossiliferous formations

Category:Paleontology in New Jersey

Category:Paleontology in New York (state)

Category:Paleontology in Pennsylvania

Category:Limestone formations of the United States