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At a hotspot, a plume of hot magma comes up through the mantle, causing vulcanism. At a mid-oceanic ridge, two plates move away from eachother, leaving space that is filled by magma.

Hotspots and mid-oceanic ridges can exist together at the same place, Iceland being a prime example of this. However, Hawaii, which is also a hotspot place, is nowhere near plate boundaries, so it's not a place where you would normally expect vulcanism.

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Q: What is the difference between volcanism at a hotspot and volcanism at mid-ocean ridge?
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The island of Hawaii experiences volcanism because it is located above the Mid-Pacific?

False! The island of Hawaii experiences volcanism because it is located above a hotspot in the Earth's mantle.


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Hotspots are portions of the Earth's surface that experience significant volcanism thought to be due to mantle plumes. They are normally located at a distance from plate boundaries where the majority of volcanism occurs.An example of a hotspot would be that underlying Hawaii and is responsible for the volcanism there and the creation of the Hawaiian island chain.


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This is known as a hotspot. Examples include the hotspot responsible for the Hawaiian Ridge-Emperor Seamounts chain and the one responsible for the significant volcanism of Iceland.


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hotspot volcanoes are formed away from the edge of plate boundaries. Plate boundary volcanoes are near a plate boundary


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