Reality is always more nuanced. That's kind of reality's deal.
> The prevailing method of estimating the length of a border (or coastline) was to lay out n equal straight-line segments of length l with dividers on a map or aerial photograph.
> the sum of the segments monotonically increases when the common length of the segments decreases. In effect, the shorter the ruler, the longer the measured border
> The result most astounding to Richardson is that, under certain circumstances, as l approaches zero, the length of the coastline approaches infinity.