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Portland Formation
Stratigraphic range: Hettangian-Sinemurian
~199–195Ma
Type Geological formation
Unit of Newark Supergroup
Sub-units Turners Falls Sandstone & Mount Toby Formation
Lithology
Primary Sandstone
Other Mudstone, siltstone, limestone
Location
Coordinates 42°18′N 72°30′W / 42.3°N 72.5°W / 42.3; -72.5
Approximate paleocoordinates 24°00′N 18°36′W / 24.0°N 18.6°W / 24.0; -18.6
Region Connecticut, Massachusetts
Country  USA
Extent Deerfield & Hartford Basins

The Portland Formation is a geological formation in Connecticut and Massachusetts in the northeastern United States. It dates back to the Early Jurassic period. The formation consists mainly of sandstone laid down by a series of lakes (in the older half of the formation) and the floodplain of a river (in the younger half). The sedimentary rock layers representing the entire Portland Formation are over 4 kilometres (2.5 mi) thick and were formed over about 4 million years of time, from the Hettangian age (lower half) to the late Hettangian and Sinemurian ages (upper half).

In 2016, the paleontologist Robert E. Weems and colleagues suggested the Portland Formation should be elevated to a geological group within the Newark Supergroup (as the Portland Group), and thereby replacing the former name "Agawam Group". They also reinstated the Longmeadow Sandstone as a formation (within the uppermost Portland Group); it had earlier been considered identical to the Portland Formation.

Vertebrate paleofauna

Dinosaur coprolites located in Massachusetts, USA. Ornithischian tracks located in Massachusetts and Connecticut, USA. Theropod tracks located in Massachusetts and Connecticut, USA. Prosauropod tracks located in Massachusetts and Connecticut, USA.

Dinosaurs
Genus Species Location Stratigraphic position Material Notes Images
Anchisaurus A. polyzelus
  • Connecticut
  • Massachusetts
Anchisaurus NT.jpg
Podokesaurus P. holyokensis Connecticut Partial postcranial skeleton. All known remains of this species have been destroyed.
Podokesaurus restoration.jpg
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