The authors have studied the surface features and structural state of the feldspar from the Holocene volcanic eruptive rock on the Tianfeng profile using data from observations under scanning electron microscope and analysis of X-ray diffraction. On this profile black pumice appears at the top and darkgrey pumice is present at the bottom. The result shows that the feldspar in these pumice rocks has fresh surface, with slightly weathering for individual cases, and occasionally seen as non-crystalline floc of varied thickness at concaves on its grain surface.