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Most hotspot volcanoes are basaltic (e.g., Hawaii, Tahiti). As a result, they are less explosive than subduction zone volcanoes, in which water is trapped under the overriding plate. Where hotspots occur in continental regions, basaltic magma rises through the continental crust, which melts to form rhyolites.n geology, the places known as hotspots or hot spots are volcanic regions thought to be fed by underlying mantle that is anomalously hot compared with the surrounding mantle. They may be on, near to, or far from tectonic plate boundaries. Currently, there are two hypotheses that attempt to explain their origins.
chain. The oldest islands are the furthest to the West from the hot spot. As the Pacific Plate moves, newer islands form. Hawaii is the youngest island and it is still being formed today; thus, Hawaii is currently at the hot spot location. Students are given ages for three of the islands: Kauai, Molokai and Hawaii. With the scale on the map, they can figure out the distances between each island and the hot spot.