DeskrifansLongshore drift at work, Dungeness - geograph.org.uk - 1006936.jpg
English: Longshore drift at work, Dungeness The succession of shingle ridges that form the Dungeness peninsula are the result of thousands of years of longshore drift. This is caused by the waves constantly hitting the beach at an oblique angle and rolling along it, moving the shingle as it does so.
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a ranna – a dhasskrifa, lesranna ha treuskorra an ober
a gemyska – a aswiwa an ober
Yn-dann an ragselyow a syw:
askrifans – Res yw dhywgh ri askrifans gwiw, provia kevren dhe'n lecyans, ha meneges mar peu chanjyow gwrys. Hwi a yll gul hemma yn fordh resonus a vynnowgh, mes ny yllir y wul yn fordh a broffo synser an lecyans dh'agas skoodhya po agas devnydh.
ranna kehaval – Mar kwrewgh hwi chanjya, treusfurvya po drehevel war an ober ma, res yw dhywgh lesranna agas kevrohow yn-dann an keth lecyans hag an derowel, po lecyans kesplegadow.
== {{int:filedesc}} == {{Information |description={{en|1=Longshore drift at work, Dungeness The succession of shingle ridges that form the Dungeness peninsula are the result of thousands of years of longshore drift. This is caused by the waves constantly
An restren ma a's teves kedhlow keworransel, dres lycklod keworrys dhyworth an kamera bysyel po an skanyer devnydhys rag hy gwruthyl po hy bysya. Mars yw chanjys an restren dhyworth hy studh gwredhek, possybyl yw na veu nebes manylyon nowedhys.