Around 250 million years ago, the earth's crust began to shift along the belt and molten rock from the mantle was pushed up through narrow cracks in the sandstone.
Kwalomu ka 250 wa mamiliyo wa malembe lawa yanga hundza, crust ya misava yisungule ku ku famba nyana hile tlhelo ka belt na ribye ra molten endzhaku kaloko mantle yitava yi tlakusiwile kuya e henhla hilaha kunga pandzekela misava endzeni ka sandstone.