The black, hole-riddled stones of island stone walls, the speckled sparkling stone of a school's front steps, and the smooth white stone of a museum statue were all made in different ways. By how they formed, rocks are split into igneous rock, cooled and hardened magma; sedimentary rock, grains that piled up and were pressed hard; and metamorphic rock, existing rock changed by great heat and pressure. So looking at a rock's grain size, whether it has layers, and whether it has stripes lets you work out how it was made. Pick each rock with the buttons to see where it sits in the cycle, then compare how it forms and what it looks like in the lower picture.
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