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The cliffs of West Runton were once part of the Cromer Forest Bed formation which is exposed at intervals along the coast of Norfolk and Suffolk, from Weybourne to Kessingland. The forest bed was formed in the Quaternary Period and dates to between 700,000 and 500,000 years ago.
Cromer Museum, Norwich Castle Museum & Art Gallery, Norfolk Collections Centre (Gressenhall Farm and Workhouse), Seaview Beach Cafe West Runton The West Runton Mammoth is a fossilized skeleton of a steppe mammoth ( Mammuthus trogontherii ) found in the cliffs of West Runton in the county of Norfolk, England in 1990. [ 1 ]
The Cromer Forest-bed Formation, sometimes known as the Cromer Forest Bed, is a geological formation in Norfolk, England. It consists of river gravels , estuary and floodplain sediments predominantly silt, sand, and muds as well as peat along the coast of northern Norfolk. [ 1 ]
At 49 miles (79 km) the road reaches the village of Beeston Regis followed by West Runton. The last village before Cromer is East Runton were the landscape of the coast is peppered with static caravans or mobile homes. The A149 now reaches the fading Victorian splendour of Cromer (52.3 miles (84.2 km)).
West Runton railway station is a stop on the Bittern Line in Norfolk, England, serving the village of West Runton.It is 28 miles 55 chains (46.2 km) down the line from Norwich and is situated between Cromer and Sheringham, the line's northern terminus.
Runton West Junction; divergence of line to North Walsham; Runton East Junction; convergence of line from North Walsham and later the Bittern Line from Norwich (via ex-GER route); Cromer Beach; opened 16 June 1887; expanded and renamed Cromer 1969; still open as part of the Bittern Line.
East Runton is a village in the civil parish of Runton in the English county of Norfolk. East Runton is located 1.3 miles (2.1 km) west of Cromer and 21.7 miles (34.9 km) north of Norwich . The village lies on the A149 coast road but most of the dwellings can be found just south of the road, nestled around the two village greens.
The stratotype for this interglacial is the Cromer Forest Bed situated at the bottom of the coastal cliff near West Runton. The Cromerian stage preceded the Anglian and Elsterian glacials and show an absence of glacial deposits in western Europe, which led to the historical terms Cromerian interglacial and the Cromerian warm period ( German ...