The chemical composition of the magma in the first four eruptions in the Sundhnúkagígar crater row on the Reykjanes Peninsula suggests that the magma comes from several magma chambers or vents that are close to each other at a depth of about five kilometers.
The chemical composition of the magma in the first four eruptions in the Sundhnúkagígar crater row on the Reykjanes Peninsula suggests that the magma comes from several magma chambers or vents that are close to each other at a depth of about five kilometers.
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