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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 constant movement of the plate stops volcanoes from erupting, but it also allows new volcanoes to be formed. Loâihi seamount, an active volcano south of Kilauea, is the firstborn from the countless eruptions and plate movements. Each island in Hawaii is composed of an active volcano. The Big Island, which is the largest of the Hawaiian Islands, is home to five major volcanoes, including Mauna Loa, the largest volcano on Earth. Aside from the eight major islands, the Hawaiian archipelago is also composed of islets, atolls and underwater seamounts in the North Pacific Ocean.