Abstract: The present invention relates to a shoe sole or insole with circulation of an incorporated fluid, in which the upper surface of the shoe sole forms a chamber which is crushable under the pressure of the foot, said chamber being subdivided by slanting transverse blades having their edge independent of the deformable sheet closing said chamber and forming the lower surface of the shoe sole, this chamber communicating at the front and rear ends of the shoe sole with a chamber formed on the upper surface and closed in a tight manner by a thin sheet, both chambers being filled with a fluid, said thin sheets being welded at their periphery to the surface of a said peripheral edge.