Tephra layers from Mount Takahe have also been found at Dome C, Dome F, Mount Waesche, Siple Dome and elsewhere in Antarctica. Volcanic eruptions at Mount Takahe lack the pyroclastic flow deposits observed in other large explosive eruptions. The thickness of the Byrd ice core tephras attributed to Mount Takahe suggested that the eruptions were not large, but later research has indicated that large Plinian eruptions also occurred.