Remote sensing dynamic monitoring was conducted along the shoreline and the tidal bank in Chuanshan Peninsula. Being the outside strand of Hangzhou Bay, Chuanshan peninsula is very complex in such aspects as dynamic condition, sediment transport, sedimentary process and morphological evolution. Based on large quantities of remote sensing data and topographic data, this paper studied the evolution of the shoreline and the tidal bank in Chuanshan peninsula since 1964. The results show that the tidal bank in Chuanshan peninsula has experienced varied evolutionary processes. The west part has moved outward for 3 050 m, with the velocity of 82.4 m/a, while the east part has only experienced slow change. The silting of the west bank mainly occurred between 1955 and 1963 and between 1977 and 1982.