SUMMARYType: composite |
Geologic Background:The Maug Islands consist of three remnants of a large stratovolcano enclosing a 2.5-km-wide caldera containing a submerged central cone that rises to within 20 m of the surface. Maug is mapped as Quaternary; widespread corals and reefs support longperiod of general quiescence but do not rule out recent mild volcanic activity. Historic Activity:
Recent Activity:
Data Sources:
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ADDITIONAL INFORMATION
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Last Update: 12/12/00 |