Ground-fed describes a water source, typically a body of water like a lake, river, or wetland, that receives its primary water supply from groundwater. This means the water originates underground, seeping upwards and outwards to replenish the surface water. The process often involves an aquifer, a subterranean layer of rock or sediment that holds and transmits groundwater. ground-fed water bodies are typically characterized by relatively stable water levels and temperatures, as groundwater is less susceptible to rapid fluctuations compared to surface water sources like rainfall. They can also be distinguished by their specific mineral composition, which is often richer in dissolved minerals depending on the geology the water has passed through. The ecosystems that rely on ground-fed water are frequently highly specialized because the specific conditions the water provides promote them. Groundwater is the hidden source that can provide crucial stability and resource in the environment.
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