The hot spot volcanic activity is not dependent on the subduction and melting of oceanic crust. The hot spot simply appears to be a non-moving place in the Earth's mantle where heat rises from the interior.
If you are talking ac, then a spot of frost.If you are talking ac, then a spot of frost.
Subduction (I believe that's what you meant) occurs at CONVERGENT boundaries, where two plates collide and the less dense one remains and the denser one sinks. An example of subduction is two oceanic plates colliding. Oceanic plates contain mainly basalt, which is dense. The oceanic plate closer to a heat source (hot spot, volcano) would remain in place while the denser plate sinks (cold water is denser than hot water so it sinks) below the other. When an oceanic plate and a continental plate collide, the oceanic plate sinks because granite (what continental plates are composed of mainly) is less dense than basalt, therefore the oceanic plate would sink. However, when two continental plates collide, because both plates are made of granite and are not very dense, they push and shape the land into mountains.
the g spot is the place when stimulated causes an orgasm.
Neptune. It's Great dark spot resembles that of Jupiter's Great Red Spot.
Japan formed as a result of a subduction zone.
hot spot
Krakatoa is not associated with a hot spot. It is associated with a subduction zone.
Mount Fuji is not associated with a hot spot. It is associated with a subduction zone.
Kilauea is a result of a hot spot, not subduction. It is located on the Big Island of Hawaii, which sits over a volcanic hot spot in the Earth's mantle. This hot spot produces magma that rises to the surface, causing the formation of volcanoes like Kilauea. In contrast, subduction involves one tectonic plate sliding beneath another, leading to different volcanic activity.
ls it formed due to a hot spot or a plate boundary Komagatake
Vesuvius is a explosive subduction volcano, not a hot spot volcano.
No. Stromboli is associated with a subduction zone.
yes, it is it is not a divergent or hot spot
Mount Vesuvius was formed by subduction. It is located at a convergent boundary where the African Plate subducts beneath the Eurasian Plate. The intense pressure and heat generated by this subduction process led to the formation of the volcano.
The Cinnamon Butte is a volcanic feature located in the Cascade Range of Oregon, and it is associated with a hot spot. This region is characterized by volcanic activity resulting from the upwelling of molten rock from deep within the Earth, rather than from tectonic plate interactions typical of subduction zones. Thus, Cinnamon Butte is primarily linked to a hot spot rather than a subduction zone.
Normally a trench develops, marking the area of subduction.