An episode of mountain-building (orogeny) associated with the assembly of the ancient supercontinent Rodinia. The Grenville orogeny occurred at the end of the Precambrian around 1300-1000 million years ago along the southeastern margin of the then North American continent. The Gatineau Hills are the local remnants of these deeply eroded and highly uplifted mountains.
Épisode de soulèvement de montagnes (orogenèse) associé à la mise en place de l’ancien supercontinent de la Rodinia.