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The Connecticut River Valley trackways are the fossilised footprints of a number of Early Jurassic dinosaurs or other archosauromorphs from the sandstone beds of Massachusetts and Connecticut. The finding has the distinction of being among the first known discoveries of dinosaur remains in North America.
One of the footprints at the Dinosaur Footprints Reservation. As the name implies, fossil footprints are this park's main attraction. They were formed during the Early Jurassic period (approximately 200 million years ago) when what is now the Connecticut River Valley was a subtropical region filled with lakes and swamps.
Dinosaur footprints and trackways are found in at least 50 localities in the Glen Rose, primarily at the top of the Upper Glen Rose and a smaller number at the top of the Lower Glen Rose. [30] The most famous of these sites is the Paluxy River site in Dinosaur Valley State Park near the town of Glen Rose, Texas, southwest of Fort Worth.
The direct association of the drawings with dinosaur fossil tracks is unique and may shed more light on rock art importance, meaning and significance, according to Radosław Palonka, an associate ...
The Paluxy River, also known as Paluxy Creek, is a river in the U.S. state of Texas.It is a tributary of the Brazos River.It is formed by the convergence of the North Paluxy River and the South Paluxy River near Bluff Dale, Texas in Erath County and flows a distance of 29 miles (47 km) before joining the Brazos just to the east of Glen Rose, Texas in south central Somervell County.
The dinosaur footprints of Connecticut and those of neighboring Massachusetts have sometimes been regarded as composing a single continuous site. [5] Other reptiles and amphibians left trace fossils in Connecticut as well as dinosaurs. [4] At least 13 species in seven ichnogenera of non-dinosaurian Mesozoic reptile footprint are known from the ...
The Purgatoire River track site, also called the Picketwire Canyonlands tracksite, is one of the largest dinosaur tracksites in North America. [1] The site is located on public land of the Comanche National Grassland , along the Purgatoire ("Picketwire") River south of La Junta in Otero County, Colorado .
The St. Mary River Formation is a geologic formation of Late Cretaceous (71.9-67 Ma [3]) age of the Western Canada Sedimentary Basin in southwestern Alberta and northwesternmost Montana. [ 4 ] [ 5 ] It was first described from outcrops along the St. Mary River by George Mercer Dawson in 1883, and it takes its name from the river.
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