THE "PRE-ILLINOIAN" TILL OF SOUTHEASTERN MINNESOTA MAY ACTUALLY BE ILLINOIAN
Recent work in the Rochester area suggests that the till of the Browerville Formation, first recognized in central Minnesota, is the surface till over much of southeastern Minnesota. The type Browerville Formation is the uppermost till below the sandy till of the Wadena drumlin field, which is believed to be the earliest Wisconsinan till. No numerical dates are available at this time; wood from the Browerville till is radiocarbon-dead. The simplest interpretation of its age is Illinoian, because otherwise Minnesota had no major northwestern-source glaciation during the Illinoian.
Correlation between the type Browerville Formation and the surface till in southeastern Minnesota is by texture and by grain counts in the 1-2 millimeter size fraction. The units share a distinctive suite of marine Cretaceous clasts, dominated by limestone rather than shale. They also share a similar abundance of Paleozoic carbonate clasts. The till under the Browerville Formation in southeastern Minnesota, called the Rose Creek till, is similar to the Browerville Formation, but a bit sandier and it contains a smaller proportion of the calcareous marine Cretaceous clast assemblage. They are separated by a layer of silty sediment and a paleosol that seems to represent less than a full interglacial period. The truly pre-Illinoian till under the Rose Creek till is highly oxidized, deeply leached, and relatively thin and patchy in many places.