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Results of a geochronological and paleomagnetic investigation of the volcanic island of Mauritius are reported.
Potassium-argon dates indicate that the main shield volcano was built subaerially between about 7.8 and 6.8 m.y. Some evidence is presented for caldera formation following the construction of the volcanic shield.
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Profound erosion subsequently destroyed much of the volcano, leaving only peripheral steep-sided massifs.
Lavas of the Younger Volcanic Series were erupted from about 3.5 m.y. ago, flooding the denuded stumps of the shield volcano.
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This activity was intermittent and a hiatus is recognized from about 2 to 0.7 m.y.