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The Ellisdale Fossil Site is located near Ellisdale in the valley of the Crosswicks Creek, in Monmouth County, New Jersey, United States.The site has produced the largest and most diverse fauna of Late Cretaceous terrestrial animals from eastern North America, including the type specimens of the teiid lizard Prototeius stageri [1] and the batrachosauroidid salamander Parrisia neocesariensis. [2]
Ellisdale Fossil Site [Note 3] Marshalltown Formation: Cretaceous (Campanian) North America: US: New Jersey [Note 1] Ochillee Creek at Old Ochillee [Note 2] Eutaw Formation: Cretaceous: North America: US: Alabama, Georgia, Mississippi: Dinosaur, mosasaur, and pterosaur: Falls of the Ohio [Note 3] Jefferson Limestone: Devonian: North America: US ...
This list of the Cenozoic life of New Jersey contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of New Jersey and are between 66 million and 10,000 years of age.
New Jersey was ranked 13th among states where the most fossils have been found. Here are some fun facts about our state's dinosaur history. Some dino-mite facts about New Jersey's dinosaur history
This list of the prehistoric life of New Jersey contains the various prehistoric life-forms whose fossilized remains have been reported from within the US state of New Jersey. Precambrian [ edit ]
The Potomac Group is a geologic group in Delaware, Maryland, New Jersey, and Virginia. It preserves fossils dating back to the Cretaceous period . An indeterminate tyrannosauroid and Priconodon crassus , a nodosaurid , are known from indeterminate sediments belonging to the Potomac Group. [ 1 ]
Download as PDF; Printable version; In other projects Wikidata item; ... Pages in category "Fossils of New Jersey" The following 10 pages are in this category, out of ...
Hornerstown, New Jersey The Hornerstown Formation is a latest Cretaceous to early Paleocene -aged geologic formation in New Jersey . It preserves a variety of fossil remains, including those of dinosaurs, and contains direct evidence of the mass mortality that occurred at the Cretaceous-Paleogene boundary .