The most common method of how fossils formed is once an animal or plant dies, it falls to the ground, and is covered by sediment. This is often sediments brought from water. Of the vast amount of prehistoric life that died, it is only a tiny amount that has survived the fossilisation process. The conditions when the majority of life died were just not right at that time, to preserve them.
Belemnites (Belemnitida) were squid-like animals belonging to the cephalopod class of the mollusc phylum, and therefore related to ammonites of old, as well as to modern squids, octopuses and nautiluses. Now extinct, their fossils are […]
Widemouth Bay contains a number of popular holiday parks, situated with easy access to the sandy beach. This is a well-known tourist hot-spot, especially for surfers, yet few realise that it has spectacular geological features and yields a variety of Upper Carboniferous fossils. Carboniferous, Cliffs and Foreshore, Rating: ♦♦♦
Cloughton Wyke is an excellent location for finding plant remains. The beds are rich in a variety of flora and collecting is fairly easy. Bivalves can also be found here, along with trace fossils, such as ripple marks and burrows. Jurassic, Cliffs and Foreshore, Rating: ♦♦♦