Hawaii isn’t a permanent paradise—it’s an island chain on a one-way trip across the Pacific.
In this video, we explore how plate tectonics and mantle hotspots are moving Hawaii northwest toward Tokyo at roughly 3 inches (7-8 cm) per year. As the islands drift away from their magma source, they cool, erode, and sink. In approximately 80 million years, Hawaii will collide with Japan's deep subduction trench, being dragged directly into Earth’s mantle rather than merging with the land.
Learn the fascinating geological timeline of Oahu, Kauai, and the future of our planet's crust.
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Tags: #hawaii #PlateTectonics #geology #Volcano #sciencefacts #GeologicalHistory #EarthFacts
