The Calvin Impact Structure, located in Cass County, Michigan, is 8.5 km in diameter. It is not exposed to the surface. The structure dates from the Ordovician, about 450 million (+- 10) years ago.
Diagnostic Evidence For This Crater
The impact origin of each location listed on this website has been supported by unambiguous diagnostic evidence of hypervelocity impact that has been reported in a scientific (usually peer reviewed) context. Without such evidence, a geological structure is not a confirmed impact crater. This section, which is included for each crater on this website, is not an exhaustive list of such published evidence, but is meant to demonstrate that appropriate work has been done for each listing.
Nature of diagnostic evidence:
Other reported evidence: morphology, 'microbreccia,' iron oxide and iron sulfide microspherules, single sets of planar fractures in a percentage of quartz grains.
Other related publications:
Donofrio, R.R., 1998, North American impact structures hold giant field potential: Oil and Gas Journal, v. 96/19.
R. L. Milstein. Geology of the Calvin Impact Structure, Cass County Michigan
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