New Hawaiian Island
12 million years hence

The Hawaiian hotspot, the volcanic center of the Hawaiian archipelago, will remain active for many millions of yesars in the future. The continuous movement of magma to the surface has led to the eruption of more seamounts, which over time will mature into islands. The next island to surface, located to the southeast of the island of Hawai'i, originated with a seamount named Lō'ihi. Now, 12 million years in the future, it is approximately in the middle of the remaining island chain.

The tropical seas around Lō'ihi are lush with coral reefs, though these are not the same coral reefs of the Holocene; they are descended from the few deeper-sea corals that survived. Fish and squid froth around these reefs, and these are preyed upon by sharks, seabirds, and swimming mongooses. The beaches on Lō'ihi are combed by the semiaquatic wharf rats, and the rats are in turn preyed upon by flightless owls.

Lō'ihi stolas Notter Wharf rat
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