| 摘要 |
The shoe sole has an air bed effect formed by an area where a series of beads are played one above the other with each bead slightly off-set relative to the next one anddefining recesses inside. The beads pref. extend from the centre section of the sole to be slightly compressed towards the rear end section so that they cause an increase in the sole at the back. The sole is formed from an outer zone forming the wear-resistant layer (1) which is harder than the rest. An inner zone (2) is made of e.g. three beads (3a, 3b, 3c).
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