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https://doi.org/10.1787/55831c5b-en
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https://doi.org/10.1038%2Fsrep40624
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https://doi.org/10.1038%2Fnature13472
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https://doi.org/10.5670%2Foceanog.2024.501
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https://doi.org/10.1038/srep44095
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https://doi.org/10.1139%2Fp63-094
If there are convection currents in the Pacific region and if the upper parts of these cells move faster than the central parts, sources of lava within the slower moving cores could give rise to linear chains of progressively older volcanic piles such as the Hawaiian Islands