Excerpt from Ground Water in the Meriden Area, Connecticut Exposures of the bedrock underlying the glacial material were also noted (see. Pl. II, in pocket), but the' map of bedrock geology and its structure (pl. III, in pocket) is Copied with only slight changes from geologic maps of the region. Prepared by Davis 1 and by Gregory and Robinson. 2 This map of the bedrock structure is reprodzueed with the present Ie-por-t because it Is believed that it will be of assistance to property owners and to drillers In forecasting ...
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Excerpt from Ground Water in the Meriden Area, Connecticut Exposures of the bedrock underlying the glacial material were also noted (see. Pl. II, in pocket), but the' map of bedrock geology and its structure (pl. III, in pocket) is Copied with only slight changes from geologic maps of the region. Prepared by Davis 1 and by Gregory and Robinson. 2 This map of the bedrock structure is reprodzueed with the present Ie-por-t because it Is believed that it will be of assistance to property owners and to drillers In forecasting the kind of material that will be encountered in drilling wells. Throughout the area the successive rock formations are presentin the order in which they are shown in the legend Ot Plate III. The first rock encountered at any place in the area' will: be that indicated by the color at that point on the map, and this rock is in most places successively underlain by the other formations in the order indicated in the legend. Fer example, in sinking wells in the City of Meriden the first rock reached is the lower sandstone, and this material continues for many hundred feet down to the ancient crystalline rocks, except, possibly, where it Inay be interrupted by dike rocks. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at ... 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.
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