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Mahantango Formation
Stratigraphic range: Givetian, ~387Ma
Mahantango Formation Rt522 PA.jpg
Outcrop of the Mahantango on Rt. 522, Fulton County, Pennsylvania
Type Geological formation
Unit of Hamilton Group
Sub-units See: Description
Underlies Harrell Shale and West Falls Formation
Overlies Marcellus Formation
Lithology
Primary Shale
Other Limestone, Siltstone
Location
Region Appalachian Basin of
eastern North America
Extent Maryland, New Jersey, New York, Ohio, Pennsylvania, Virginia, and West Virginia
Type section
Named for Mahantango Creek

The Mahantango Formation is a special type of rock layer found in Pennsylvania, West Virginia, and Maryland. It formed a very long time ago, during the Devonian Period. This rock layer gets its name from the North branch of the Mahantango Creek in Pennsylvania. It's part of a bigger group of rocks called the Hamilton Group. Below it, you'll find another rock layer called the Marcellus Formation. In some parts of Pennsylvania, the lower sections of the Mahantango Formation are also known as the Montebello Formation.

What is the Mahantango Formation Made Of?

The Mahantango Formation is mostly made of gray, brown, and olive-colored siltstone and shale. These rocks often show "coarsening-upward cycles." This means the rock layers start with finer grains at the bottom and get coarser (bigger grains) as you go up.

Where is the Mahantango Formation Found?

USGS 2006 1237 table2 Stratigraphy Middle Devonian
The different rock layers in the Appalachian Basin during the Devonian Period.

The Mahantango Formation usually sits right on top of the Marcellus Formation. Above it, you might find a rock layer called the Tully Limestone.

The Mahantango Formation can be split into four main parts, called "members":

  • Tully Limestone: This part is a shale that contains many fossils. It helps separate the Mahantango from the Hamilton Group.
  • Sherman Ridge: This section has olive-gray claystone and siltstone. It also has layers of fine sandstone that get coarser as you go up. Many fossils are found here.
  • Montebello Sandstone: This part is made of olive-gray sandstone with coarse to fine grains. It's mixed with siltstone and claystone and also shows coarsening-upward cycles. Fossils are common.
  • Fisher Ridge: This section includes silty claystone, siltstone, and very fine-grained sandstone. It's sometimes called the Dalmatia or Turkey Ridge.

The Sherman Ridge and Fisher Ridge parts often form ridges in the landscape. In south-central Pennsylvania, the Mahantango also includes other sections like the Clearville, Frame, Chaneysville, and Gander Run Members.

Amazing Fossils Found in the Mahantango Formation

Phacops-enrolled
An enrolled Phacops rana fossil found in the Mahantango Formation in Pennsylvania. You can see its special schizochroal eye.

The Mahantango Formation is famous for its many marine (ocean) fossils. These fossils tell us about the ancient sea life that lived there millions of years ago. You can find:

Brachiopods

  • Athyris
  • Chonetes
  • Mucrospirifer
  • Protoleptostrophia
  • Tropidoleptus

Trilobites

  • Basidechenella
  • Dipleura
  • Eldredgeops (used to be called Phacops)
  • Greenops

Bivalves

  • Grammysioidea
  • Grammysia
  • Leiopteria
  • Modiomorpha
  • Orthonota

Corals

  • Pleurodictyum
  • Trachypora

Gastropods

  • Bembexia
  • Crenistriella
  • Cyclonema
  • Glyptotomaria
  • Loxonema
  • Platyceras

Cephalopods

  • Tornoceras
  • Agoniatites
  • Spyroceras
  • Michelinoceras
  • Bactrites

How Old is the Mahantango Formation?

Scientists use special methods to figure out the age of rock layers. The Mahantango Formation formed during the Middle Devonian period. This was about 392 to 385 million years ago! It sits directly on top of the Marcellus Formation shale. Above it, you'll find the Trimmers Rock Formation and Harrell Shale. In 2012, scientists Read and Erikson confirmed that the formation in Virginia belongs to a specific time within the Devonian called the Givetian Stage.

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