Abstract: The secondary stratolandform is a contemporaneous surface configuration in different elevation(original stratolandform)which formed by crust deformaion and dismission later.It reflects the tendency,strength,rate of the neotectonic movement since the Quaternary.Based on this point,the mountains of Hebei Province is divided into two parts of the neotectonics,subdivided into seven subareas and twenty four of smal subareas.