Having visited the Upper Peninsula of Michigan on several occasions in the past, my wife and I are very familiar with the southern shore of Lake Superior. This coming week, we will explore its northern shore, where outcrops of ancient Precambrian rocks adorn the scenery and where a string of Ontario parks and nature preserves line the coast.
The rock strata, the youngest of which formed at least 100 million years before life crawled from the sea, are best observed along roadcuts, stream valleys and lake shores and we will surely observe many of them as we travel along the northern edge of Lake Superior.
Earth formed about 4.6 billion years ago, life evolved in the sea about 3.6 billion years ago and plate tectonics is thought to have begun by 2.5 billion years ago. Most of the rocks exposed along the North Shore of Lake Superior are 1-2 billion years old. Of course, the Great Lakes themselves are much younger, having formed during the last glacial period of the Pleistocene Epoch, the Wisconsin Glaciation, 70-10 thousand years ago (well after humans had evolved). See: Formation of the Great Lakes

