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Shield volcanoes are lower in elevation and usually not exposive, such as Kilauea, which has been constantly 'erupting' since the 80s.

Composite volcanoes (aka stratovolcano) are large, usually somewhat cone shaped and appear dormant/extinct until an explosive eruption.

Examples are Krakatoa (awesome example), Vesuvius, Pinatubo, Rainier, St Helens and many more.

Shield volcanoes typically occur on mid-oceanic 'hot spots' while composites/stratovolcanoes occur on tectonic plate boundaries. The "ring of fire" around the pacific plate has many strato/composite volcanoes and Hawaii's Kilauea is in the center on a 'hot spot'

*Skylla*

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13y ago

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