This paper reviews the origins and geological history of the Galápagos Islands. The islands arose from a ‘hot-spot’. The oceanic crust on which the islands are built can be no more than 10 million years old, and the islands themselves have been in existence at least 3.3 million years. The Galápagos are among the most active volcanic groups in the world, and the physical nature of the islands is dominated by lava structures of various ages, including lava tubes or tunnels, which have been of particular interest to biologists. Weathering of the rock to produce soil has generally been slow, particularly in the drier parts.
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Tom Simkin (1984) studied this question.
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