Feltville Formation: Difference between revisions
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==Age== |
==Age== |
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The Feltville Formation rests conformably above the [[Orange Mountain Basalt]] and below the [[Preakness Basalt]], placing its |
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]]. |
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==Economic Uses== |
==Economic Uses== |
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Revision as of 23:21, 23 July 2010
| Feltville Formation | |
|---|---|
Stratigraphic range: | |
 Exposure of Feltville Formation sandstone beneath a ledge of Preakness Basalt on Preakness Mountain in New Jersey. | |
| Type | Geological formation |
| Unit of | Newark Supergroup |
| Underlies | Preakness Basalt |
| Overlies | Orange Mountain Basalt |
| Thickness | maximum of 1,968 feet (600 m)[1] |
| Lithology | |
| Primary | Sandstone, Siltstone, Mudstone |
| Other | Limestone |
| Location | |
| Region | Newark Basin of Eastern North America Rift Basins |
| Extent | continuous for ~40 miles (64 km) in New Jersey, with outliers present in New Jersey & Pennsylvania. |
| Type section | |
| Named for | Deserted Village of Feltville, New Jersey[1] |
| Named by | Paul E. Olsen, 1980[1] |
The Feltville Formation is a mapped bedrock unit primarily in New Jersey, with one known outlier in Pennsylvania. 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.[1]
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.[1][2] Additionally, pebbles and cobbles of quartz are embedded within layers of sandstone and siltstone that interfinger with the Feltville Formation near Oakland, New Jersey.[2]
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.[3] 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.[4]
Fossils
Fish fossils, commonly those of the ray-finned Semiontus, can be found in limestone layers within the formation.[1] In other layers, indeterminate fossil ornithischian tracks have been noted [5], along with additional reptile and dinosaur prints. Fossil plant remains, as well as root structures and pollen, are also found in the formation.[1]
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 Uses
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.[6]
See also
References
In-line citations
- ^ a b c d e f g Olsen, 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.
- ^ a b Mineral Resources Online Spatial Data – Feltville Formation, New Jersey. U.S. Geological Survey. Accessed July 23, 2010.
- ^ Faill, R.T., (2004). The Birdsboro Basin. Pennsylvania Geology V. 34 n. 4.
- ^ Schlische, Roy W. Geology of the Newark Rift Basin. Department of Geological Sciences, Rutgers University, Piscataway, NJ. Accessed July 23, 2010.
- ^ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
- ^ 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. Available via Google Books
Additional references
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.
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