Book Description

Excerpt from Stratigraphy of Unconsolidated Sediments in the Southern Part of Lake Michigan Underlying the Lake Michigan Formation is a series of glacial lacustrine deposits, including sand, sandy pebbly clay, silt, and clay pebble conglomerate. These deposits are more compact, coarser grained, and contain less water than those of the Lake Michigan Formation. They show the direct effect of nearby glaciers. The glacial-lacustrine deposits are assigned to the Carmi Member of the Equality Formation and overlie glacial tills that are assigned to the wadsworth Member of the Wedron Formation. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.