The entropy spectrum method is applied to self-affine fractal profiles. Fir
st, the profile created by a generalized multiaffine generator is decompose
d into many subsets having their own topological entropies. The entropy spe
ctrum and H-q (the qth Hurst exponent) of its profile is calculated exactly
. For each subset, D-D (divider dimension) and D-B (box dimension) are also
calculated. The relation D-B = 2 - H-q=1 is obtained for the remaining sub
set after infinite iteration of the generator. Next, the entropy spectrum o
f fractional Brownian motion (FBM) traces is examined and obtained as a poi
nt spectrum. This implies that a variety of lengths of segments in FBM trac
es is caused not by intrinsic inhomogeneity or mixing of the Hurst exponent
s but by only the trivial fluctuation. Namely, there are no fluctuations in
singularity or in topological entropy. Finally, a real mountain range (the
Hida mountains in Japan) is also analyzed by this method. Despite the prof
ile of the Hida mountains having two Hurst exponents, the entropy spectrum
of its profile becomes a point spectrum again. [S1063-651X(99)10901-2].