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Above: Cast of a tridactyl
(three toed) print is clearly visible in the bottom right hand corner of the
photo. From a fallen block of sandstone in Burniston Bay which is between Cloughton Wyke and Scalby Bay.
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Members of the Yorkshire Geological
Society examining a cliff ledge at Cromer point at the north end of Scalby Bay. Disturbed sediments are believed to be due to
many dinosaur footprints; "dinoturbation".
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Above:Another footprint from foreshore near Cowlam Hole, Scalby Bay.
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Above:Prints (especially centre left) which appear to be
in mudstone on the underside of a fallen block of sandstone resting on
the Dogger Formation between Whitby and Saltwick Bay. The prints are infilled with sandstone. The
prints may be interpreted as "scratch marks" made by a swimming
dinosaur.
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 Left: Broad tridactyl footprints on foreshore sandstone, north of Cowlam Hole in Scalby Bay. To
aid visibility, the footprints have been outlined with chalk.
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Above: Footprints on a fallen block
of Middle Jurassic sandstone from the foreshore
in the Ravenscar area.
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