Charlevoix crater
The Charlevoix impact structure is a large eroded meteorite impact structure in the Charlevoix region of Quebec, Canada. Only part of the impact structure is exposed at the surface, the rest lying beneath the Saint Lawrence River.Description
The original impact structure is estimated to have been in diameter and the age of the impact is estimated to be 450 ± 20 million years. The projectile was probably a stony asteroid, at least in diameter, and weighing an estimated. The Mont des Éboulements, situated in the exact centre of the impact structure, is interpreted as the central uplift, a consequence of elastic rebound. The impact structure is classified as a multi-ringed basin with a central uplift.
The impact origin of Charlevoix impact structure was first realized in 1965 after the discovery of many shatter cones in the area. Other evidence for impact includes planar deformation features in quartz and feldspar grains.
In contrast to the surrounding craggy Laurentian Mountains, the impact structure is relatively smooth and flat, which has facilitated human settlement. Today, 90% of the people of Charlevoix live within this impact structure.
