Tag: North Norfolk

Norfolk by UK Fossils (UKGE Group)
Read More

West Runton

West Runton brings together two very different fossil worlds: Cretaceous chalk on the shore and the much younger West Runton Freshwater Bed at the foot of the cliffs. The latter preserved a river-valley community of mammals, fish, freshwater shells and plants, including the celebrated steppe mammoth Mammuthus trogontherii. When sand has been washed away, the chalk platform reveals flints and marine fossils. Search loose beach material carefully, keep a record of each find and treat these scientifically important exposures with care. Tides, shifting sand and unstable cliffs determine what can safely be seen. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

Norfolk by UK Fossils (UKGE Group)
Read More

Hunstanton

Hunstanton’s striped Cretaceous cliffs offer a clear introduction to Norfolk’s marine fossils. Brown Carstone, the thin Red Chalk and pale Ferriby Chalk form contrasting layers, with belemnites, brachiopods, bivalves and occasional ammonites preserved in their rocks. Weathered material on the beach gives collectors a chance to examine fossils without approaching the cliff face, while the harder beds reward patient observation rather than force. The sequence also records missing intervals of geological time, so its colours tell only part of the story. Plan your visit around low tide and keep well clear of unstable cliffs and recent falls. Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

Norfolk by UK Fossils (UKGE Group)
Read More
East Runton coast, Norfolk

East Runton

At East Runton, ancient mammal remains occur beside evidence of powerful Ice Age deformation. Shelly Early Pleistocene deposits appear on the foreshore when sand is stripped away, while enormous glacially displaced chalk rafts rise within the cliffs towards Wood Hill. Loose belemnites, echinoids, bone fragments and occasional teeth make careful beach searching worthwhile, although exposure and preservation vary greatly. This is a different fossil assemblage from the famous Freshwater Bed at West Runton. Keep a precise record of where each specimen was found and explore only while the tide leaves a safe route back to East Runton Gap. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

Norfolk by UK Fossils (UKGE Group)
Read More
Overstrand coast, Norfolk

Overstrand

Overstrand’s shore is best explored for loose Chalk fossils and the changing exposures revealed when sand is washed away. Echinoids, belemnites, brachiopods and sponge remains occur in chalk and flint, while rarer mammal fossils record a much younger Pleistocene landscape. The cliffs also contain chalk rafts displaced by ice, an important reminder that the visible rocks are not always in their original order. Fossils may show both ancient features and much younger marine borings. Access is affected by coastal works and erosion, so check the current route before travelling and leave ample time to return on the falling-tide beach. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦♦♦♦

Norfolk by UK Fossils (UKGE Group)
Read More

Sheringham

Sheringham’s western foreshore is a condition-dependent fossil locality, where waves sometimes uncover Cretaceous chalk beneath the beach near the lifeboat station. Echinoids, brachiopods, oysters and occasional fish remains have been reported, but sand, shingle and seaweed can hide the rock for long periods. The shoreline also reveals how much younger sediments and glacial activity have modified an older chalk landscape. A visit works best as a careful search of loose material during suitable low-tide conditions, with realistic expectations and time to return safely. Keep the lifeboat access clear and leave unstable cliffs and attached rock undisturbed. Cretaceous, Cliffs and Foreshore, Rating: ♦♦

Norfolk by UK Fossils (UKGE Group)
Read More
Sidestrand coast, Norfolk

Sidestrand

Sidestrand’s folded glacial cliffs and displaced chalk masses preserve several very different chapters of Norfolk’s past. Loose Chalk fossils and fossil-bearing erratic pebbles can be found on the shore, while much older marine Crag and younger freshwater beds have yielded scientifically important small mammals, shells and insects. The Sidestrand Unio-bed is especially valuable for understanding the climate before the great Anglian glaciation. This is a remote, tide-dependent collecting coast rather than an easy family beach. Search only accessible loose material, keep well away from the unstable cliffs and plan the return route before walking away from an established access. Erratics (Jurassic, Cretaceous), Cliffs and Foreshore, Rating: ♦♦

Norfolk by UK Fossils (UKGE Group)
Read More

Mundesley

Mundesley combines a family seaside beach with a significant Pleistocene fossil record. Today, casual collectors are most likely to find echinoids and sponges preserved in flint, reworked onto the shore from much older deposits. The Cromer Forest-bed succession has also yielded important elephant remains and evidence of cold-climate plants, although such beds are not continuously exposed and mammal finds are uncommon. Sea defences, sand cover and changing beach levels strongly influence what can be seen. Search loose foreshore stones at a suitable low tide, enjoy the geology from a safe distance and leave protected exposures undisturbed. Pleistocene, Cretaceous, Cliffs and Foreshore, Rating: ♦♦