The alternating geology of mudstones, shales and sandstones tell us that the
environment was not static but changed back and forth over time and one finds a
number of shell beds within the rock. These are notable at the Avicula and
Pecten Seams and at the boundary between the
Redcar Mudstone and the
Staithes Sandstone Formations.
The images below are arranged roughly in chronographic order the highest
being the youngest fossils above the Main Seam and the lowest being the oldest
in the Redcar Mudstone
These are not however the only fossils found near Staithes they are the most
predominant. In 1968 part of an Ichthyosaur was found but before that a number
of Plesiosaur were uncovered by the Alum mining.
Other types of fossils, known as trace fossils, notably Rhizocorallium
burrows are common in the Main Seam whilst fossilised wood in the form of
Lignite or Jet has been mined here for many hundred of years.