Mount Michael and the other volcanoes of the South Sandwich Islands are the result of ongoing subduction of the
South American Plate beneath the
South Sandwich Plate along the
South Sandwich Trench. As the oceanic slab descends, it releases water and other volatiles that lower the melting point of the overlying mantle wedge. This process generates basaltic to basaltic-andesitic magmas that ascend through thin oceanic crust and build the
island arc volcanoes. Mount Michael is one of the most active volcanoes of the South Sandwich Islands. The subduction system consists of the eastern side of the broader
Scotia Arc, consisting of arcs, ridges, and microplates. This links the
South Atlantic Ocean and
Southern Ocean. There is also active
back-arc rifting behind the South Sandwich Islands. The active crater rises from an older
caldera. Due to its southern latitude, the volcano is almost entirely covered by ice and snow. == Volcanic activity ==