

Using geochemical data to determine tectonic uplift Time Frame - 1 hour Advanced PreparationBarrier reef islands surrounding the coastlines of the New Georgia Islands represent a stage in the sequence of atoll formation proposed by Charles Darwin in 1842. Barrier reefs and atolls form as coral reefs anchored to volcanic islands grow upward to keep pace with actual rising sea level, or apparent sea level rise due to subsidence of the islands. Emergent barrier reefs also exist on the New Georgia Islands the islands reaching up to 25 meters above sea level. Their presence indicates the interruption of Darwin’s predicted subsidence sequence in the formation of atolls by tectonic uplift, which has raised these coral reefs above sea level to create islands capped by a series of coral reef terraces. Indeed, earthquakes provide evidence that the recently active spreading center (Gizo Ridge) is now subducting beneath the New Georgia Islands generating tectonic uplift. The presenter/teacher will review the following information before doing this exercise.
Materials
Procedure
|