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The footprints were first discovered in the 1960s by station manager, Glen Seymour, in the nearby Seymour Quarry. Palaeontologists from the Queensland Museum, including Mary Wade and Tony Thulborn and the University of Queensland excavated Lark Quarry during 1976–77 (the quarry was named after Malcolm Lark, a volunteer who removed a lot of the overlying rock.)
There are tracks from two types of dinosaur. The first type of tracks are from a sauropod and were made by an animal of 30 to 50 feet in length, perhaps a brachiosaurid such as Pleurocoelus, [20] and the second tracks by a theropoda, an animal of 20 to 30 feet in length, perhaps an Acrocanthosaurus. A variety of scenarios was proposed to ...
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.
Researchers found that the dinosaur footprints were discovered over 3,700 miles away from each other – and that the footprints were made 120 million years ago on a "supercontinent known as ...
The footprints, dating back to the Early Cretaceous period, were found in Brazil and in Cameroon, researchers wrote in a study published Monday by the New Mexico Museum of Natural History & Science.
Download as PDF; Printable version; In other projects ... "New saurischian dinosaur footprints from the Lower Jurassic of Poland", Geological Quarterly, 49: 99–104;
Paleontologists have suggested the prints may belong to a plant-eating dinosaur that roamed the area more than 200 million years ago 10-Year-Old Girl Discovers Dinosaur Footprints During Beach ...
Dinosaur Plateau, also known as the Khodzapil-Ata Tracksite, (Turkmen: Dinozawrlar platosy) is a large limestone slab from the Kugitang Svita that is located on the slope of the Köýtendag mountains in the Lebap Region of Turkmenistan. The area is notable for preserving the largest concentration of dinosaur footprints in a single area. [1]