THE STRATIGRAPHIC APPROACH TO HYDROGEOLOGIC AND GEOTECHNICAL INVESTIGATIONS
Choosing a suitable groundwater monitoring zone in a sequence of glacial deposits is often complicated by the difficulty in determining which sand-and-gravel bodies are discontinuous and which are sufficiently continuous to constitute a preferential contaminant pathway. Upland glacial settings in the Midwestern United States are typically underlain by a sequence of fine-grained glacial sediments deposited by successive glacial advances. Stratified sand and gravel may occur at various stratigraphic positions within this fine-grained succession. Laterally extensive sand-and-gravel units are most likely to occur between the deposits of different glacial advances. The key to determining a suitable groundwater monitoring zone thus depends on the ability to determine the boundary between different glacial advances in these successions of primarily fine-grained deposits. Unfortunately, use of the Unified Soil Classification System (USCS) as the means for classifying and differentiating fine-grained units in glacial settings is often inadequate because different fine-grained stratigraphic units typically classify as the same in the USCS. Other properties must be recognized and described to provide suitable information for recognizing and correlating fine-grained glacial stratigraphic units, including sedimentary structure and secondary weathering zone properties. In certain situations, it may be important to select a drilling method that provides adequate sample recovery and high quality samples.