The Decorah lies above the Platteville Limestone and below the Cummingsville Formation in the sedimentary sequence that formed from the shallow sea that covered central North America during Ordovician Time.

[1] The Spechts Ferry member is organic-rich and suggests a large influx of terrigenous sediment during deposition.

The Ion Member, present in the southern Decorah in Iowa, is characterized by alternating beds of shale and limestone.

Where it crops out in the Upper Midwest, especially in the Twin Cities, the Decorah is a popular stratum for amateur fossil collecting.

It contains trilobites, brachiopods, horn corals, gastropods, crinoids, and large numbers of bryozoans.