Contact: Ben Norman
Caption: This movie is a simple 0 m to -210 m geographical loop sequence at 5 m increments. Important features are the substantial gaps between Galapagos' "core" islands even at -100 m. However, below c. -130 m the various islands begin coalescing.
Credit: Video from: "Exploring the combined role of eustasy and oceanic island thermal subsidence in shaping biodiversity on the Galápagos" by Jason R. Ali and Jonathan C. Aitchison from the Journal of Biogeography.
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Related news release: How have changing sea-levels influenced evolution on the Galapagos Islands?