The Nuvvuagittuq Greenstone Belt formed approximately 3.77 billion years ago in northeastern Quebec, Canada, though some studies suggest origins as early as 4.3 billion years ago. This volcano-sedimentary sequence contains metamorphosed mafic volcanic rocks and chemical sedimentary rocks that likely represent ancient oceanic crust. Geochemical evidence indicates the rocks underwent hydrothermal alteration by seawater. The belt contains some of Earth's oldest known rocks and chemical signatures that may indicate early life or prebiotic processes.