Further south, on both sides of the continent, from latitude 41 degrees to the southernmost extremity, we have the clearest evidence of former glacial action, in numerous immense boulders transported far from their parent source.
Hegorago kontinentearen alde bietan, 41°ko latitudetik hego ertzeraino, antzinako glaziarearen eraginaren frogarik nabarienak ditugu beren sorlekutik urrun eramaniko hainbat eta hainbat harkosko eskergatan.