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The Calvert Formation is a geologic formation in Maryland, Virginia, and Delaware. It preserves fossils dating back to the early to middle Miocene epoch of the Neogene period . It is one of the three formations which make up the Calvert Cliffs , all of which are part of the Chesapeake Group .
Calvert Cliffs State Park is a public recreation area in Lusby, Calvert County, ... Fossils from the Calvert Formation, Zone 10, Calvert Co., MD (Miocene)
This group contains one of the best studied fossil record of Neogene oceans in the world. Professional Paleontologists and amateur fossil hunters alike collect from this group intensely. The Calvert Cliffs stretch the length of Calvert County, Maryland and provide the best continuous stretch of the Calvert, Choptank, and St. Marys Formations.
That makes the tooth about a half-inch longer than the one found Christmas Day by a 9-year-old girl at Maryland’s Calvert Cliffs State ... solved by using preserved bite marks on Arizona fossil.
Calvert Cliffs State Park [Note 2] Calvert Formation: Miocene: North America: US: Maryland: Middle Miocene Climate Transition and Middle Miocene disruption: Goodsell Ridge, Isle La Motte (Lake Champlain) [Note 2] Chazy Formation: Ordovician: North America: US: Vermont: Early Reef: bryozoa, corals, stromatoporoids: Chuckanut Drive, south of ...
Flag Ponds Nature Park is a nature preserve located in Lusby, Maryland along the Chesapeake Bay in Calvert County, Maryland. It is operated by the Calvert County Department of Natural Resources. The park includes nature trails and a beach for swimmers. Fossil shark's teeth eroded from the Calvert Cliffs formation may be collected on the beach ...
It is visible within the Calvert Cliffs State Park where it is exposed in cliffs. Located on the western shore of the county, Calvert Cliffs are famous for their fossil deposits and are a popular collecting location of marine vertebrates, shark teeth, birds as well as fresh water and marine turtles and tortoises.
Pictured is a lump of 66-million-year-old vomit found on the Cliffs of Stevns, a geological site on the Danish island of Zealand that is comprised of a 15 km-long fossil-rich coastal cliff.