Manicouagan Crater in northern Canada is one of the oldest impact craters known [
http://antwrp.gsfc.
]. Formed about 200 million years ago, the present day terrain supports a 70-kilometer diameter hydroelectric reservoir [
http://www.ilec.or.
] in the telltale form of an annular lake [
http://epod.usra.ed
]. The crater itself has been worn away by the passing of glaciers [
http://www.glacier.
] and other erosional processes. Still, the hard rock at the impact site has preserved much of the complex impact structure [
http://antwrp.gsfc.
] and so allows scientists a leading case to help understand large impact features [
http://www.lpi.usra
impacts.html ] on Earth [
http://antwrp.gsfc.
] and other [
http://antwrp.gsfc.
] Solar System bodies. Also visible above is the vertical fin of the Space Shuttle Columbia [
http://www.nasa.gov
orbiters/orbiterscol .html ] from which the picture was taken in 1983.
Explanation
Manicouagan Crater in northern Canada is one of the oldest impact craters known [
http://antwrp.gsfc.
]. Formed about 200 million years ago, the present day terrain supports a 70-kilometer diameter hydroelectric reservoir [
http://www.ilec.or.
] in the telltale form of an annular lake [
http://epod.usra.ed
]. The crater itself has been worn away by the passing of glaciers [
http://www.glacier.
] and other erosional processes. Still, the hard rock at the impact site has preserved much of the complex impact structure [
http://antwrp.gsfc.
] and so allows scientists a leading case to help understand large impact features [
http://www.lpi.usra
impacts.html ] on Earth [
http://antwrp.gsfc.
] and other [
http://antwrp.gsfc.
] Solar System bodies. Also visible above is the vertical fin of the Space Shuttle Columbia [
http://www.nasa.gov
orbiters/orbiterscol .html ] from which the picture was taken in 1983.
Explanation