Description
Surficial hydrogeological materials show the distribution of sediment deposited in glacially influenced environments. Most drinkable groundwater resources in Canada occur in shallow surficial-sediment aquifers. Surface sediments, such as gravel, sand, silt and clay, or mixed sediments, are an important control on vegetation patterns and surface-water recharge to aquifers. In addition, areas with significant thicknesses of sand and gravel-large moraines and buried valleys-often host prolific aquifers.
Resources
| Name | Format | Description | Link |
|---|---|---|---|
| Download the English JP2 File through HTTP | Unknown | Open resource | |
| Download the English ZIP (PDF,JPG) file through HTTP | ZIP | Open resource | |
| Download the French JP2 File through HTTP | Unknown | Open resource | |
| Download the French ZIP (PDF, JPG) File through HTTP | ZIP | Open resource |