To the east of Malahide town centre is a small beach on which it is easy to find loose carboniferous fossils and limestone pebbles containing beautifully preserved crinoids, bryozoans, bivalves, corals and brachiopods. The pebbles are washed out from exposures along the local coastline, including foreshore platforms found between Malahide and nearby Portmarnock.Carboniferous, Foreshore, Rating: ♦♦♦♦♦
North of Portmarnock, on the east coast of Ireland to the east of Dublin, is a short stretch of coastline with abundant exposures of Carboniferous rocks in foreshore platforms, containing beautifully preserved crinoids, bryozoans, bivalves, corals and brachiopods. The cliffs and platforms are protected, but many pebbles are washed out from the exposures along the coastline between Malahide and nearby Portmarnock.Carboniferous, Foreshore, Rating: ♦♦♦♦
Southeast of Waterford and southwest of Wexford is the Hook Head peninsula, which is remarkable for the abundant, beautifully preserved Carboniferous fossils, at its furthest reach by the Hook Lighthouse. The outcrops around Hook Head consist of abundant exposures of Lower Carboniferous rocks in foreshore platforms, containing beautifully preserved crinoids, bryozoans, bivalves, corals and brachiopods. The cliffs and platforms are protected, but many loose fragments can be found containing significant numbers of jumbled fossils of all types, with superbly preserved detail.Carboniferous, Foreshore, Rating: ♦♦♦♦
Ten kilometres northwest of Ballycastle in Co. Antrim is White Park Bay. Successive layers of rock yield Mesozoic fossils including ammonites, belemnites and Gryphaea. However, the cliffs and platforms are protected, but many loose blocks containing fossils and some washed out fossils can be found. The beach is also known as one of the few places in the world to have “singing sand” – when conditions are right, the extremely fine sand vibrates to make a humming noise. The location is also known as a historic manufacturing hub for flint axes and arrow heads, due to the abundance of flint nodules found in the cliffs, with artefacts dating back as far as 8,000 BC. The landscape also features passage tombs looking out over the sea, where, on a clear day, the coast of Scotland can be seen.Cretaceous, Jurassic, Foreshore, Rating: ♦♦♦
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: ♦♦♦