To cut a long story short, these buoyant early continents continued to grow and, since they were less dense than the ocean floor, proved very difficult to subduct.
Go kgaola kanelo e telele, dikontinente tse tsa pele tse di kokobetseng mo godimo ga metsi di tswelela pele go gola, ka ge di ne di sa kitlana thata go feta boalo ba lewatle fatshe, di supile di le thata go dira moselenyana o o kwa fatshe.