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  1. Fertile soils-the physical breakdown and chemical weathering of volcanic rocks have formed some of the most fertile soils on Earth.
  2. Ore deposits-Rising magma does not always reach the surface to erupt; instead it may slowly cool and harden beneath the volcano to form a wide variety of crystalline rocks (generally called plutonic or granitic rocks).
  3. Fossil fuels-Heat and pressure at depth transform the decomposed organic material into tiny pockets of gas and liquid petroleum, which then migrate through the pore spaces and larger openings in the surrounding rocks and collect in reservoirs, generally within 5 km of the Earth's surface.
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