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Blake River Megacaldera Complex

The Blake River Megacaldera Complex is a giant subaqueous caldera cluster or a nested caldera system that spans across the Ontario–Quebec border in Canada.

Structure and geographical extent
The Blake River Megacaldera Complex consists of mainly mafic to intermediate volcanic flows and less abundant felsic volcanic flows and intercalated pyroclastic rocks, which underwent three stages of major volcanic activity. • The first phase resulted in the creation of the long, wide, east-west striking Misema Caldera which has been dated to 2704–2707 Ma. It is a coalescence of at least two large mafic shield volcanoes that formed more than 2703 million years ago. • The second phase resulted in the creation of the long, wide, northwest–southeast trending New Senator Caldera which formed 2701–2704 Ma. Its formation consists of thick massive mafic sequences which has inferred to be a subaqueous lava lake during the early stages of the caldera's development. As a result, the Blake River Group is best categorized as a meganested caldera complex. ==See also==
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