The Great Lakes are the largest group in a chain of large lakes (including Winnipeg, Athabasca, Great Slave and Great Bear) that lies along the southern boundary of the Canadian SHIELD. From W to E the Great Lakes comprise Lakes SUPERIOR, Michigan (entirely in the US), HURON, ST CLAIR, ERIE and ONTARIO. They have a total area of approximately 246 050 km2 and drop from 183 m above sea level at Lk Superior to 74 m at Lk Ontario - the most dramatic drop occurring at NIAGARA FALLS. Lake St Clair, while not properly a "great lake," is considered part of this Laurentian chain. After withdrawal of the Palaeozoic seas, which had spread across most of the continent, there is little record of geological events in the Great Lks area between the end of the Pennsylvanian and late Tertiary periods. Although broad river valleys likely crossed the area, remnants of Tertiary erosion surfaces in Illinois and Wisconsin cannot be traced across the Great Lks, and reconstructions of preglacial drainage are uncertain. The Great Lks lie near the intersection of the Hudson Bay, Mississippi R and St Lawrence R drainage basins; because of progressive headwater capture by the Mississippi, that watershed now lies only about 10 km from parts of the southern shores of Lks Erie and Michigan, and only about 20 km from the western end of Lk Superior. Postglacial isostatic uplift continues to raise the northern shorelines of the Great Lks by about 0.4 m per century, relative to the southern shores of Lks Erie and Michigan.

The Great Lks occupy bedrock depressions that have been differentially eroded by glacial ice, and their form and location are largely controlled by structural geology. The arcuate forms of Lks Huron and Michigan have developed around the periphery of the Michigan structural basin, and the more resistant Silurian limestones and dolomites (NIAGARA ESCARPMENT) separate GEORGIAN BAY and Green Bay from the main lakes. The form of Lk Superior is largely controlled by Precambrian geology; that of Lks Erie and Ontario by trends in the underlying Appalachian geosyncline.

During the last glacial period (which lasted more than a million years) there were 4 glacial stages and, with each, the lake basins were progressively enlarged. Towards the end of the last glaciation (Wisconsin), lakes formed in front of retreating ice margins, first in the Erie and Michigan basins, and drained S to the Mississippi more than 14 000 years ago. Subsequently, a lake formed in the southern part of the Huron basin and drainage between Erie, Huron and Michigan was linked. There was also an outlet to the Hudson R (S of the Ontario basin). The Ontario basin became ice free about 12 000 years ago; Lk Superior and Georgian Bay later. The presence of ice margins caused many early lakes to form at very high levels. At one time, a single huge lake covered much of the upper Great Lks area (Superior, Michigan and Huron). As the ice melted away from the natural outlets, lake levels often dropped quickly and to extremely low levels, for example, about a 150 m drop in the Ontario basin, with the opening of the St Lawrence Valley (12 000-11 500 years ago). As a result of continued uplift during the past 10 000 years, upper lakes drainage was fully transferred (through Lks St Clair and Erie) to Lk Ontario only 4000-5000 years ago, when the Chicago outlet (Lk Michigan) closed.

The Great Lakes have, since the days of the early fur trade, provided an important transportation route to the interior of the continent, and with the opening of the ST LAWRENCE SEAWAY (1959) they became a truly international waterway.