Active serpentine mud volcanoes observed in the Mariana fore-arc provide dramatic evidence for hydration of the shallow mantle wedge by H₂O fluids derived from the subducting lithosphere (Fryer. 1996: Fryer et al., 1999).

“Well, Dominic,” Della suddenly chimed in. “Seeing as this place of yours is still under escrow, seems to me it's not really yours yet, is it?”

Diodorus Siculus says that the Gauls, who were Celts, delivered the spoils won in battle, yet reeking with blood, to their attendants: these were carried in triumph, while an epinicial song was chanted […]

He arose early in the morning.