The Potomac River is suggested to have a subterranean counterpart, raising questions about the presence of large, unnoticed freshwater aquifers. The interaction between surface rivers and groundwater is complex, with aquifers either feeding rivers or vice versa, depending on location and seasonal variations. Groundwater does not flow through underground rivers; instead, it moves through pore spaces and fractures in rock formations. It is possible for groundwater to flow perpendicular to surface rivers. The discussion also touches on the Colombia River Basalts as a notable example of a deep igneous aquifer, though details about the deepest aquifers remain uncertain.