Capacity functions were born out of geometric. necessity, a decade and a
half ago. Plane regions had been found of arbitrarily small area, yet
with a totally disconnected boundary. Such regions seemed to defy the
very spirit of Riemann's mapping theorem. They could be mapped
conformally and univalently into a disk, with the single boundary point
at infinity being stretched into a circle. The plausible explanation of
the mystery is, of course, as follows. Under a mapping of the punctured
sphere onto a disk, an area element near the punctured point would have
to stretch more in the circular direction than in the radial direction,
and the conformality would be destroyed. But if there is a sufficiently
heavy accumulation of other boundary components, these can take over the
distortion, and the mapping of the region itself remains conformal. Such
phenomena made it an important problem to characterize pointlike
boundary components which were unstable, i.e., hid in them- selves this
power of stretching into proper continua. Standard tools such as mass
distributions, potentials, and transfinite diameters could not be used
here, as they were subject to the vagaries of the other com- ponents.
The characterization had to be intrinsic, depending only on the region
itself, in a conformally invariant manner. This goal was achieved in the
following fashion (SARlO [10, 13]).