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how are volcanic islands formed?
by the subduction of oceanic crust at the sea floor
by ocean-ocean convergence at the sea floor
by mantle plumes or hot spots erupting underneath moving plates
by continent-continent convergence over open ocean
Brief Explanations
- Analyze each option:
- Option 1: Subduction of oceanic crust at the sea floor mainly forms features like ocean trenches and volcanic arcs near continents, not volcanic islands in the middle of oceans typically.
- Option 2: Ocean - ocean convergence at the sea floor forms volcanic arcs (like island arcs) but the formation mechanism of most volcanic islands (like Hawaii) is different.
- Option 3: Mantle plumes or hot spots erupting underneath moving plates: A hot spot is a region of the mantle that is unusually hot. As the tectonic plate moves over the hot spot, the magma from the hot spot erupts onto the ocean floor, building up over time to form a volcanic island. For example, the Hawaiian Islands are formed this way.
- Option 4: Continent - continent convergence over open ocean is not a valid process for forming volcanic islands as continent - continent convergence leads to mountain building (like the Himalayas) and occurs on land or at continental margins, not over open ocean.
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C. by mantle plumes or hot spots erupting underneath moving plates