Plik:SIR-B Sudbury Impact Crater.jpg

SIR-B radar image of the Sudbury impact structure (elliptical because of deformation by Grenville thrusting) and the nearby Wanapitei crater (lake-filled) formed much later. The partially circular lake-filled structure on the right (east) is the 8 km (5 mi) wide Wanapitei crater, estimated to have formed 34 million years (m.y.) ago. The far larger Sudbury structure (second largest on Earth) appears as a pronounced elliptical pattern, more strongly expressed by the low hills to the north. This huge impact crater, with its distinctive outline, was created about 1800 m.y. ago. Some scientists argue that it was at least 245 km (152 mi) across when it was circular. More than 900 m.y. later strong northwestward thrusting of the Grenville Province terrane against the Superior Province (containing Sudbury) subsequently deformed it into its present elliptical shape (geologists will recognize this as a prime example of the "strain ellipsoid" model). After Sudbury was initially excavated, magmas from deep in the crust invaded the breccia filling, mixing with it and forming a boundary layer against its walls. Some investigators think that the resulting norite rocks are actually melted target rocks. This igneous rock (called an "irruptive") is host to vast deposits of nickel and copper, making this impact structure a 5 billion dollar source of ore minerals since mining began in the last century.