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Hawaii currently sits above an area of the mantle known as a hotspot. The mantle, or the part of the planet directly below the crust is made of a hot, dense material called peridotite. The Earth's mantle moves and is akin to a thick, viscous liquid such as syrup, due to trapped primordial heat and the radioactive decay of naturally occuring elements this thick, viscous fluid is hot and convects - sending plumes of hotter material up towards the crust while cooler material sinks down towards the core.

Hawaii sits directly above one of these plumes, as do other volcanic hotspots such as Yellowstone, the Canary Islands and Reunion. Over geologic time sustained volcanic activity has built the islands from the seafloor upwards, and over millions of years as the crust moves over the hotspot, new islands are created while others fall dormant.

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