This paper relates first to the changes brought about in glass solids bounded by plane surfaces, by exposure to high temperatures, the main object of the paper being to elucidate the changes which have taken place in vitreous, and once vitreous, rocks by comparing the phenomena of natural devitrification with similar phenomena effected by artificial means. The first case considered is that of a piece of thick plate glass which has been totally devitrified under conditions described in detail in the paper. In the roughly broken specimen the fractured surface sufficiently reveals the fact that crystallisation has taken place throughout the mass, while other specimens subsequently described by the authors demonstrate beyond question that the crystallisation has started at the surfaces and has travelled inwards. In this particular specimen the crystallisation has advanced from the different surfaces until the various sets of crystals have arrested one another in very definite planes, whose traces are clearly perceptible on a fractured surface.