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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.
The Hawaiian islands are the result of a hot spot beneath the Pacific Plate. Hot material rises from deep within the mantle and collects beneath the lithosphere.Some of it rises through the crust and erupts at the surface, forming volcanoes. Those volcanoes gradually build up into islands.he Hawaiian islands are the result of a hot spot beneath the Pacific Plate. Hot material rises from deep within the mantle and collects beneath the lithosphere.