Weathering zonation of steep slopes of welded tuff characterized by obsidian lenses and systematic cracks were estimated based on styles of weathering conditions and rebound values of Schmidt rock hammer on artificially excavated slopes. Although horizontal microcracks and the slice-shaped fragments that are separated by them are notable within the weathered rocks, the zone of weathering as a whole is quite concordant with natural slopes. No elongation of crack planes under weathering is recognized. The weathered condition changes outward from fresh and massive to disintegrated condition through brecciated zones. These zonations were also confirmed by the distribution of rebound values of the Schmidt rock hammer.
This is due to the lack of brittle behavior usually characteristic of welded tuff. Cracks do not elongate during the process of weathering, and the rate of weathering of each intact rock body is greater than that of crack extension. Consequently, thickness and the dip angle of weathered zones of slopes may be important factors, even in welded tuffs.