An usual method to determine the coastal change over the period of several years to hundreds years is to compare the pictorial materials which are available. Among them, maps, aerial photographs and satellite images are the most commonly applied. All pict6orial materials convcey certain amount of errors and the material is not usable when the error involved is larger than the amount of change of the target features. The main aim of this study is, with Huatrung coast of the eastern Taiwan as a cast, to illustrate the availability and limitation of pictorial materials when tackling with the topic of coastal change of which the coast changes less dramatic.