Tag: North Norfolk

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Mundesley

Mundesley was once an important site for Cromer Forest Bed material, with a number of large vertebrate specimens being found from foreshore deposits. Today, the sea defence prevents this bed from being washed out, although the occasional bone can turn up. However, erratic fossils, mostly of flint echinoids and sponges, can be found. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦

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Sidestrand

The cliffs from Trimingham to Sidestrand are some of the most spectacular glacial formations along the northern Norfolk coast. These tall, rapidly eroding cliffs here display an array of various colours from the sands, tills and clays. Fossils are mostly Jurassic and Cretaceous erratics. Erratics (Jurassic, Cretaceous), Cliffs and Foreshore, Rating: ♦♦

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East Runton

East Runton is the best location for mammal remains from the Pastonian Stage interglacial. It also is one of the only locations where you can see younger Pleistocene beds below huge chalk cliffs. The chalk was transported here during the ice age and is spectacular to see. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

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Sheringham

Near the lifeboat station on the foreshore, chalk is exposed during scouring conditions. Corals and shark remains have been found at this location at these times, although scouring only happens a few times a year. If you do visit during favourable conditions, you should find some nice specimens. Cretaceous, Cliffs and Foreshore, Rating: ♦♦

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Overstrand

Overstrand is a foreshore collecting location. Chalk is exposed during low tide, especially during scouring conditions or winter/spring months. The chalk is highly fossiliferous, yielding many echinoids, sponges and molluscs. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

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West Runton

This is the location of the famous ‘West Runton Elephant’ find. From the West Runton Fresh Water Bed, mammal and fish remains are common, along with freshwater shells. On the foreshore, during scouring tides, the chalk yields echinoids and sponges. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

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Hunstanton

The famous red and white cliffs of Hunstanton are visited by thousands of people each year simply to see this spectacular natural geological feature. The Red Rock and White Lower Chalk are rich in fossils including echinoids, fish, sharks’ teeth, bivalves and brachiopods, ammonites and more. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦