Which two mantle hot spots are located at midocean ridges

the answer is Yellowstone and Iceland

Explanation:

number 1

Iceland, the Azores, and the Galápagos are examples of these “hotspot” islands—so named because they are believed to form above small regions scattered around the earth where unusually hot rocks rise from deep inside the mantle layer.

Mid-ocean ridges are formed when a divergent boundaries are pushed apart, creating rift valleys and eventually ridges on the ocean floor where magma wells up to form new crust and forms a mid-ocean ridge. They occur at plate boundaries.

Hot spots are spots where a tectonic plate is moving over a mantle plume and are responsible for creating islands like Hawaii and volcanoes like Yellowstone. They occur in the middle of tectonic plates.

The main differences between hot spots and mid-ocean ridges are, what mid-ocean ridges create at the bottom of the ocean and hotspots create at the top of the ocean; and mid-ocean ridges occur at the edges of tectonic plates while hot spots occur in the middle of tectonic plates.

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