RECOGNITION OF LACUSTRINE SEQUENCES IN NORTHEAST ILLINOIS AND THEIR IMPLICATIONS FOR INTERPRETATIONS OF FLUCTUATIONS OF THE LAKE MICHGIAN LOBE MARGIN: HAVE WE OVERLOOKED ALLOSTRATIGRAPHY?
Parts of both sequences are interpreted to have been deposited in so-called Glacial Lake Milwaukee. Sequence 1 can be considered an offlap and is interpreted to be comprised of coalesced deltas or subaqueous fans, ranging in thickness from 0 to 150 ft (45m) and extends from the Fox River lowland in the west to the area of the eastern edge of the Valparaiso moraine to the east. The eastern, ice-proximal slope of the Valparaiso moraine coincides with the eastern most buried ice-contact face of sequence 1. However, the sequence is completely buried and has no surface expression. Sequence 2, which forms the Valparaiso, Tinley, and Lake Border moraines, can be considered an onlap, both overlies and insets sequence 1, and ranges in thickness from 0 to 200 ft (60m).
Differentiation of these sequences and recognition of their internal facies is based upon recognition of bounding surfaces, making them allostratigraphic units. The contact between sequence 1 and sequence 2 is typically within lake sediment and recognized by a contrast in depositional environments. The sediments at top of sequence 1 are typical of an ice-proximal lake environment and the sediments at the bottom of sequence 2 are typical of an ice-distal lake environment. Coarse facies of sequence 1 are used as an aquifer, so facies distribution has become a focus of three-dimensional mapping efforts.