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Footprints dating back 120 million years show where dinosaurs were able to cross between land that's now part of two different continents. Matching dinosaur footprints found more than 3,700 miles ...
Download as PDF; Printable version; In other projects ... Location; Coordinates ... (2005), "New saurischian dinosaur footprints from the Lower Jurassic of Poland ...
Theropod footprint at the Purgatoire River dinosaur track site, Picket Wire Canyonlands, Colorado, U.S.A. Interp Panel 1 Interp Panel 2 Interp Panel 3 The Purgatoire River track site , also called the Picketwire Canyonlands tracksite , is one of the largest dinosaur tracksites in North America . [ 1 ]
Grallator (GRA-lə-tor) is an ichnogenus (form taxon based on footprints) which covers a common type of small, three-toed print made by a variety of bipedal theropod dinosaurs. Grallator-type footprints have been found in formations dating from the Early Triassic through to the early Cretaceous periods.
A team of researches, led by Southern Methodist University (SMU) paleontologist Louis L. Jacobsfound over 260 matching sets of Early Cretaceous dinosaur footprints in Brazil and Cameroon ...
The tracks were originally created about 621 miles apart over a thin sandstone layer of silt and mud on the former supercontinent Gondwanan, which later separated and formed the south Atlantic Ocean.
Ripple marks preserved in sandstone at Dinosaur Footprints. A dirt path leads from the reservation entrance to the footprints. Besides the clearly formed dinosaur tracks, visitors can see imprints left by prehistoric plants, invertebrate trace fossils and delicate ripple marks of an ancient pool preserved in stone near the river's west bank.
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.)
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