thrust, forming spires and truncated columns. The heat of the molten matter so altered and disintegrated the rocks through which it was driven, that in many places these rocks have crumbled away, and have left the dykes erect in black nakedness high above the surrounding level. Such is the Aiguilhe by Le Puy, 210 feet high, to reach the summit of which a flight of steps has been hewn in the side, and on the top, in 962, Truan, Dean of Le Puy, erected a church in honour of S. Michael, and called it Seguret, The Secure Refuge; the church was consecrated in 980. Another of these obelisks is at Fay le Froid, another basaltic monolith is La Roche Rouge on the banks of the Gagne.
But sometimes the eruptive dykes are more massive, and form stone tables with precipitous sides, as at Polignac, the cradle of an illustrious family, and at Arlempdes on the Loire.
There are few crags of basalt or tufa in the Velay that are not crowned by a ruined castle, and to enumerate these would be a tedious and unprofitable task.
The last of all the volcanoes to explode was the Denise, near Le Puy, and that erupted when man was on the earth, for under the lava, in a bed of breccia or volcanic ash, was found in 1884 the skeleton of a man; another was discovered shortly after, and a third is reported to have been recently disinterred. In the case of the first of these, the man seems to have been overtaken by the shower of falling ash, to have sat down, placed his head between his knees, and held his hands over his skull to protect it, and so perished, and the rain of cinders finally enveloped and buried him. No weapons or ornaments have been found with these
