Manicouagan Impact
Structure, Quebec
Posted December 6, 2001
download large image (591 KB, JPEG) acquired June 1, 2001
The large
annular lake in this image represents the remnants of one of the largest impact
craters still preserved on the surface of the Earth. Lake Manicouagan in
northern Quebec, Canada, surrounds the central uplift of the impact structure,
which is about 70 kilometers in diameter and is composed of impact-brecciated
(relativley large pieces of rock embedded in finer grained material) rock.
Glaciation and other erosional processes have reduced the extent of the crater,
with the original diameter estimated at about 100 kilometers. This natural-color
image of the region was acquired by the Multi-angle Imaging Spectroradiometer's
(MISR's) nadir (vertical-viewing) camera on June 1, 2001.
The impact
that formed Manicouagan is thought to have occurred about 212 million years
ago, toward the end of the Triassic period. Some scientists believe that this
impact may have been responsible for a mass extinction associated with the loss
of roughly 60% of all species. It has been proposed that the impact was created
by an asteroid with a diameter of about 5 kilometers. The lake is bounded by
erosion-resistant metamorphic and igneous rocks, and shock metamorphic effects
are abundant in the target rocks of the crater floor. Today Lake Manicouagan
serves as a reservoir and is one of Quebec's most important regions for
Atlantic salmon fishing.
NASA
image courtesy NASA/GSFC/LaRC/JPL, MISR
Team.
from
NASA's Earth Observatory, http://earthobservatory.nasa.gov |

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