Numerous and well‐preserved trackways in mid‐Cretaceous sediments of West Central Queensland, Australia, are attributed to a stampede of small to medium‐sized bipedal dinosaurs ‐ both herbivores (ornithopods) and minor‐league predators (coelurosaurs). The tracks of a single large predator (carnosaur) suggest a reason for the stampede. These trackway data permit calculation of sustained running speeds for the coelurosaurs and ornithopods.
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Thulborn et al. (1979) studied this question.
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