ðə klˈɪfs ʌv wˈɛst ɹˈʌntən wɜː wˈʌns pˈɑːɹt ʌvðə kɹˈoʊmɚ fˈɔːɹɪst bˈɛd fɔːɹmˈeɪʃən wˌɪtʃ ɪz ɛkspˈoʊzd æɾ ˈɪntɚvəlz ɐlˈɔŋ ðə kˈoʊst ʌv nˈɔːɹfək ænd sˈʌfək, fɹʌm wˈeɪboːɹn tə kˈɛsɪŋɡlənd.
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.