Glacial groundwater is located in areas where glaciers have receded, leaving behind permeable deposits of sand and gravel that can hold water. These deposits are often called moraines, and they are a common source of groundwater.
Glacial groundwater is located in areas where glaciers have receded, leaving behind permeable deposits of sand and gravel that can hold water. These deposits are often called moraines, and they are a common source of groundwater.