Fig. 4

Schematic diagram of the Euclidean volume scaling of the diffusive avalanche boundaries, visualized as circles or spheres in the three Euclidean space dimensions S = 1,2,3. The Euclidean length scale x of subcubes decreases by a factor 2 in each step (xi = 2 − i,i = 0,1,2), while the number of subcubes increases by ni = (2i)S, defining a probability of for each avalanche size with size xi.
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