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Boonton Formation
Stratigraphic range: Late Hettangian-Sinemurian
~197–190Ma
NewarkBasin BoontonFormation.jpg
Exposure of the Boonton Formation along a road cut in Pequannock Township, New Jersey.
Type Geological formation
Unit of Newark Supergroup
 Meriden Group
Underlies Potomac Formation
Overlies Hook Mountain Basalt
Thickness maximum of over 1,640 feet (500 m)
Lithology
Primary Sandstone, siltstone, mudstone
Other Conglomerate, evaporite
Location
Coordinates 40°54′N 74°24′W / 40.9°N 74.4°W / 40.9; -74.4
Approximate paleocoordinates 22°42′N 19°48′W / 22.7°N 19.8°W / 22.7; -19.8
Region Newark Basin of
Eastern North America Rift Basins
Extent continuous for ~30 miles (48 km) in New Jersey
Type section
Named for Boonton, New Jersey
Named by Paul E. Olsen
Year defined 1980

The Boonton Formation is a special layer of rock found in New Jersey. Think of it like a giant history book made of stone! It tells us about what the Earth was like millions of years ago. This rock layer is named after the town of Boonton, New Jersey, where scientists first studied it closely.

What is the Boonton Formation Made Of?

The Boonton Formation is mostly made of reddish-brown or reddish-purple sandstone. It also has layers of red, gray, purple, and black siltstone and mudstone. Sometimes, these layers can contain calcium carbonate or small, hard lumps called dolomitic concretions.

Scientists have found a famous fossil fish bed in a siltstone layer near the top of the formation. This layer is rich in carbonates. You can also find layers of conglomerate mixed in. These are rocks made of smaller, rounded pebbles, often from older rocks like gneiss and granite.

How Did the Boonton Formation Form?

The Boonton Formation formed a long, long time ago when the supercontinent Pangea was breaking apart. This breaking caused huge cracks in the Earth, forming basins where sediments collected. The Boonton Formation is like the very top part of another rock layer called the Passaic Formation.

The Passaic Formation mostly formed in dry places, like playas (dry lakebeds) and alluvial fans (fan-shaped deposits of sediment). This is why it's mostly red. But the Boonton Formation is different! It has many layers that are not red. This tells us that during the time the Boonton Formation was forming, there were more lakes and wetter periods.

Most rock layers in this area show a pattern of wet and dry periods, like alternating red and gray-black layers. But the lower parts of the Boonton Formation are unique. They have many different colors and textures mixed together without a clear pattern. This suggests the environment was changing a lot!

What Fossils Can You Find?

The Boonton Formation is a treasure chest for fossils! Scientists have found many amazing things here, especially fish fossils.

Fish Fossils

Near the top of the formation, you can find fossils of ancient fish. Some examples include:

  • The ray-finned fish Semionotus elegans
  • The coelacanth Diplurus longicaudatus
  • Other fish like Redfieldius and Ptycholepis

Dinosaur and Reptile Tracks

Besides fish, the Boonton Formation also has fossilized footprints! These tracks tell us about the animals that walked here millions of years ago.

  • Scientists have found tracks from plant-eating dinosaurs called ornithischians, including a type called Anomoepus.
  • You can also find footprints from other reptiles and dinosaurs, like Batrachopus and the meat-eating dinosaur Grallator.

Plant Fossils

The formation also contains fossils of ancient plants. These include:

  • Remains of conifer trees.
  • Other plant-related fossils like root structures.
  • Tiny fossilized pollen grains.

How Old is the Boonton Formation?

The Boonton Formation sits right on top of another rock layer called the Hook Mountain Basalt. This helps scientists figure out its age. It formed between about 197 and 190 million years ago. This time period is known as the late Hettangian stage and the Sinemurian stage of the Jurassic period. That's even before the famous giant dinosaurs like Tyrannosaurus rex roamed the Earth!

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