When the earth's surface got significantly colder around 2 million years ago during the Cenozoic Era, glaciers formed. The glaciers of the Pleistocene Epoch (Ice Age) slowly made their way southward after forming in Eastern and Central Canada.
As they moved, glaciers carved and shaped the rock and ground in Illinois. They picked up sediments and deposited them elsewhere. This is a form of till. Till is a type of drift deposited directly by glaciers. Drift is all deposits of earth and rock materials moved by glacial activity.
Glaciers also carried ginormous slabs of rock which, when the glaciers melted, piled up and created moraines. Moraines are arc-shaped ridges formed when till piles up along a glacier's edge.
Also, when glaciers melted, they created rivers, streams and other bodies of water. These "rivers" carried outwash. Outwash is sorted and stratified sediments deposited by meltwater flowing away from a glacier.
Over the Quaternary Period of geological time (past 1.6 million years), many glaciers formed. These were called glacial episodes. There were about 125,000 years in between each episode called "warm" periods or the Yarmouth. The deep weathered zone called the Yarmouth Geasol formed during these "warm" periods.