[112a] what it is now. For as it is now, the action of a single night of extraordinary rain has crumbled it away and made it bare of soil, when earthquakes occurred simultaneously with the third of the disastrous floods which preceded the destructive deluge in the time of Deucalion.1 But in its former extent, at an earlier period, it went down towards the Eridanus and the Ilissus, and embraced within it the Pnyx; and had the Lycabettus as its boundary over against the Pnyx2; and it was all rich in soil and, save for a small space, level on the top.
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