“…Though the ECCLIP is generally considered to be a product of the Galápagos plume, other authors however, based on paleomagnetic reconstructions, suggest that the ECCLIP originated 2,000 km east of the Galápagos hotspot, and may thus not be derived from the same mantle plume (Boschman et al., 2014). On the other hand (Shellnutt et al., 2021), goes further as to suggest that the Triassic volcanic rocks of Wrangellia of western North America (more than 3,000 km away from present‐day Galápagos) were generated from a Pacific mantle plume source. Their paleogeographic constraints, thermal estimates, and geochemistry suggests that it is possible that the Galápagos hotspot generated the volcanic rocks of Wrangellia and the Caribbean plateau or, more broadly, that the eastern Pacific (Panthalassa) Ocean was a unique region where anomalously high thermal conditions either periodically or continually existed from at least ∼230 Ma to the present day.…”