Sources of Sand and Gravel Sample Clauses

Sources of Sand and Gravel. Sub-bottom profiles reveal that glaciodeltaic deposits are the predominant source of sand and gravel resources within the study area. This conclusion is drawn due to several factors. Glaciodeltaic deposits are either surficially exposed or very shallowly buried by a veneer of marine sediment, making them easily accessible. The deposits are spatially continuous and in many places exceed 33 ft (10 m) thickness. The seismic characteristics and geomorphology of these deposits suggest that the sediment is predominantly sand and gravel, however, geotechnical data is critical for verifying this interpretation. Other identified deposits are deeply buried and thus inaccessible (coastal plain sediment and bedrock), have a low fraction of sand and gravel (glaciolacustrine sediment, bedrock) or require closer inspection due to the potential presence of intact paleolandscapes (paleochannels) and possible associated paleocultural sensitivity.
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