Big idea (E2.1, E2.2): Igneous rocks form from cooled magma (intrusive, slow cooling, large crystals, e.g., granite) or lava (extrusive, fast cooling, fine crystals or glass, e.g., basalt, obsidian, pumice). Typical properties: hard, interlocking crystals, no sedimentary layers, no fossils.
How to help: Granite is easy to find: countertops, gravestones, landscaping stones and Canadian Shield road cuts. Ask your child to point out the crystals and guess how fast the rock cooled. In the Epsom salt model, results can vary with temperature and amount of liquid; that is fine. Ask your child to explain what happened and what they might change (A1.2).
Common difficulties:
- Mixing up magma and lava. Magma is underground; lava is at the surface.
- Thinking slow cooling makes small crystals. It is the opposite: more time, bigger crystals.
- Thinking a rock must be from a volcano to be igneous. Granite cooled underground and never erupted.
Safety: An adult handles the hot water. Obsidian (sometimes sold in rock kits) is very sharp when broken.