When surface cracks on continuous casted slab were observed by a micro
scope, internal oxidation layers were sometimes present along the crac
ks. These layers that were called subscales were paid attention. The s
ubscale was formed in steam atmosphere in laboratory for considering o
f the generated mechanism of the surface crack. The results are summar
ized as follows, (1)The subscale was the internal oxidation layer wher
e the generated rate of scale was greatly reduced. (2)The thickness of
the subscale depended on the temperature and the time, and that was c
alculated by the internal oxidation theory. (3)The type and the diamet
er of particles in the subscale also depended on the temperature. (4)T
herefore, the surface crack formed temperature and position in the con
tinuous easter were able to decide by the observation of the subscale.