The forest fire model is a reaction-diffusion model where energy, in the fo
rm of trees, is injected uniformly, and burned (dissipated) locally. We sho
w that the spatial distribution of fires forms a geometric structure where
the fractal dimension varies continuously with the length scale. In the thr
ee-dimensional model, the dimensions vary from zero to three, proportional
with In(l), as the length scale increases from l similar to 1 to a correlat
ion length l = xi. Beyond the correlation length, which diverges with the g
rowth rate p as xi proportional to p(-2/3), the distribution becomes homoge
neous; We suggest that this picture applies to the "intermediate range" of
turbulence where it provides a natural interpretation of the extended scali
ng that has been observed at small length scales. Unexpectedly, it might al
so be applicable to the spatial distribution df luminous matter in the univ
erse. In the two-dimensional version, the dimension increases to D = 1 at a
length scale l similar to 1/p, where there is a crossover to homogeneity,
i.e., a jump from D = 1 to D = 2.