Aquifer-fed water source
Overview
An aquifer-fed water source is a spring, seep, or similar outflow where water emerges at the surface after moving subsurface through permeable rock or soil layers known as an aquifer.
Key points
- Water may appear as a localized spring, seep, or small stream originating from the ground.
- Flow characteristics can be more stable than purely surface-runoff sources, but still vary seasonally.
- The term describes the source’s connection to subsurface water, not its potability or treatment status.
Details
Aquifer-fed water sources occur where underground water moving through porous or fractured materials reaches the surface. In hiking contexts, these sources may present as small springs emerging from hillsides, seeps that collect into pools, or initial segments of streams. Because they draw from subsurface reservoirs, some aquifer-fed sources can remain more consistent during dry periods than runoff-dependent pools. However, water quality, flow rate, and reliability still vary by region and season. The phrase "aquifer-fed" identifies the origin of the water flow and does not, by itself, indicate whether the water meets any specific safety or treatment standards.
Related topics
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