This paper summarizes the results of numerous investigations on the structure, surfaceproperties and flotation behaviour of chrysocolla. Until the late sixties, chrysocolla was considered to be a hydrated copper silicate without fixed mineral composition. Recent articles, however, have revealed that chrysocolla is a definite mineral having an orthorhombic unit cell and a characteristic fibrous structure. The results reported by various researchers seem to indicate that mobile superficial copper ions. as well as the silica skeleton, are responsible for the similarities observed in the surface properties of all chrysocolla samples which prevail in spite of the well known differencesin composition of chrysocolla specimens. The equilibrium diagram for the system copper oxide-silica-water has been introduced as a valuable tool for predictingthe surface propertiesofchrysocolla. However, the conditioning pH is the most critical parameter which determines the surface characteristicsand the flotation behaviour of chrysocolla. It has been recognized that this mineralis a microporous solid whose naturecan be considerably alteredby heal treatment around 550'C. This so-called "thermal activation of chrysocolla" could result in the crystallization ofindividual surface oxides and/or the sintering of the rnicroporcs, which in turn significantly enhances the flotation response of copper silicate. Studies of the sulfidization of malachite and chrysocolla have revealed that the sulfidization process produces different sulfide surfaces on natural and thermally activated chrysocolla. It is only in the latter case that the superficial filmexhibits the same electrochemical properties as the surface of sulfidized malachite.'