Lake Warren was a proglacial lake that formed in the Lake Eriebasin around 12,700 years before present when Lake Whittlesey dropped in elevation. Lake Warren is divided into three stages: Warren I, Warren II, and Warren III, each defined by the relative elevation above sea level.
Origin
Lake Warren followed Lake Wayne. It covered the basin of Lake Erie, part of Lake Huron, including Saginaw Bay and the lowland, which separates Lake Huron from Lake Erie. It included a part of the Lake Ontario basin and the lowland between Lakes Ontario and Erie. Lake Warren included the Saginaw basin and the Huron-Erie basin. Its outlet was through the Grand River to Lake Chicago. The beach stands at above sea level west of the hinge line, unaffected by the isostatic rebound. It is marginally above the outlet, at. Lake Warren was preceded by a lower stage, which had its outlet through the Mohawk valley. Lake Warren came into existence its waters were raised from Lake Wayne by advancing ice front. The ice both compacted the area where the melt water could be held, raising the water level, while blocking the lower outlet from Lake Wayne.
Size
Lake Warren was about half the size of the present day Lake Erie, lying in the southern half of the basin.
Beach
The beach rises to the north of the Grand River outlet at per mile until it reaches near Gladwin. It is also nearly on the point of the "Thumb" in Huron county north of Bad Axe. The beach is horizontal from Lenox, in St. Clair county, around the west end of Lake Erie, then along the south shore through Ohio to the Pennsylvania line, a distance of. Between there and Batavia, New York, it rises in the next. The beach marks a lake level which lasted a considerable period of time, shorter than either the Arkona or the Lake Whittlesey durations. The delta deposits are not as extensive as Lake Arkona. Its shore deposits vary, where the lakebed was till or gravelly material, a gravelly beach was formed. Where the lakebed was sandy it is a sandy ridge.
Lakes Warren and Wayne
The relatively strong but discontinuous multiple sand and gravel beach ridges occurring as close as 40 feet and as much as 100 feet below the Whittlesey strand line in western New York (between are correlated with Glacial Lake Warren. These ridges occur at the foot of the Allegheny Plateau. They are frequently associated with deltas. The ridges are well developed in a few areas well beyond the Plateau in the Lakes Erie and Ontario lowlands. In many cases, the ridges and deltas are underlain by silts of Lake Whittlesey lakebed.
