Passaic Formation

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Passaic Formation
Stratigraphic range: Upper Triassic
GoffleHill SandstoneCliff.jpg
Exposure of Passaic Formation sandstone on Goffle Hill in Hawthorne, New Jersey.
Type Geological formation
Unit of Newark Supergroup
Underlies Orange Mountain Basalt
Overlies Lockatong Formation
Thickness maximum of over 19,685 feet (6,000 m)[1]
Lithology
Primary Siltstone, Mudstone, Shale
Other Sandstone, Conglomerate
Location
Region Newark Basin of
Eastern North America Rift Basins
Extent ~200 miles (320 km) in
New York, New Jersey,
and Pennsylvania
Type section
Named for Passaic, New Jersey[1]
Named by Paul E. Olsen, 1980[1]

The Passaic Formation is a mapped bedrock unit in Pennsylvania, New Jersey, and New York. It was previously known as the Brunswick Formation since it was first described in the vicinity of New Brunswick, New Jersey. It is now named for the city of Passaic, New Jersey, which is near where its type section was described by paleontologist Paul E. Olsen.[1]

Description[edit]

The Passaic is defined as a reddish-brown shale, siltstone and mudstone with a few green and brown shale interbeds; red and dark-gray interbedded argillites near the base.[2] In New Jersey, there are conglomerate and sandstone beds within the formation.

Depositional environment[edit]

The Passaic is mostly playa and alluvial fan deposits resulting from the rifting of Pangea. The red color is often evidence that the sediments were deposited in arid conditions.[3] Interfingered with the Passaic, the Lockatong Formation are lake sediments, which were deposited during wetter climatic cycles during the late Triassic.[3] These sediments came from the northwest and contain clasts from Appalachian formations.

Fossils[edit]

Age[edit]

Relative age dating of the Passaic places it in the Late Triassic to the Early Jurassic, being deposited between 225 to 190 (±5) million years ago. It rests unconformably a top many different formations of the Appalachian Piedmont. It interfingers with the Lockatong Formation and also rests conformably atop the Stockton Formation. There are numerous diabase intrusions into the Passaic with local contact metamorphic rocks.[4]

References[edit]

  1. ^ a b c d 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.
  2. ^ Berg, T.M., Edmunds, W.E., Geyer, A.R. and others, compilers, (1980). Geologic Map of Pennsylvania: Pennsylvania Geologic Survey, Map 1, scale 1:250,000.
  3. ^ a b Faill, R.T., (2004). The Birdsboro Basin. Pennsylvania Geology V. 34 n. 4.
  4. ^ Berg, T.M., et al., (1983). Stratigraphic Correlation Chart of Pennsylvania: G75, Pennsylvania Geologic Survey, Harrisburg, Pennsylvania.

See also[edit]