Zhejiang is located at the East Asiatic continental margin, and is situated in the contact belt between the Jiangnan block and the Cathaysian block. Structural and magmatic activities, especially the Mesozoic magmatic ones, are extremely intensive, which form massive granitoids. The granitoids constitute materials of granite landform in Zhejiang Province. The Zhejiang granite landforms may be classified into the granitic peak cluster, granitic hill, granite nubbin and collapse pile landforms and so on. Taking the Daming mountain, Tiantai mountain, the Putuo mountain, the Fugai mountain etc. as the examples, the characteristics of the above granite landforms and their forming processes are analyzed, and the factors such as prospects of rocks, the structure and the climate which influence the development and evolution of granite landform are discussed as well.