Decaturville crater

From Wikipedia, the free encyclopedia
Jump to: navigation, search
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.[1]

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

Coordinates: 37°54′N 92°43′W / 37.9°N 92.717°W / 37.9; -92.717


Personal tools
Namespaces

Variants
Actions
Navigation
Interaction
Toolbox
Print/export