Decaturville crater

From Wikipedia, the free encyclopedia

The topography of the Decaturville crater is highly eroded.
The topography of the Decaturville crater is highly eroded.

The Decaturville crater, also referred to as the Decaturville Dome, is an impact crater in Missouri, United States, and is one of the 38th parallel structures.

It is 6 km in diameter and the age is estimated to be less than 300 million years (Permian or younger). The crater is exposed at the surface.

The effect that this impact had on the surrounding bedrock can be seen in a roadcut that runs along highway 5 about 16 miles north of Lebanon.

[edit] References

[edit] External links

Coordinates: 37°54′N, 92°43′W