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Shield volcanoes are found along divergent plate boundaries where two plates pull apart and lava flows into the gap to form a volcano.

Shield volcanoes are also formed at hot spots. A hot spot is an area of persistent volcanic activity. Hot spots originate at unusually hot areas of the mantle-core boundary. Overlying mantle melts forming plumes of magma that rise and penetrate the crust forming volcanoes. Hawaii, Iceland, and Yellowstone are examples of hot spots. The trace of a hot spot appears as a chain, such as an island chain. As the overlying plate moves one volcano off the hot spot, another is formed. The Hawaiian Island Chain is an example.

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