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a natural flow of water from underground to the surface is a/an

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Spring (hydrology)
A spring may be the result of karst topography where surface water has infiltrated the Earth's surface (recharge area), becoming part of the area groundwater. The groundwater then travels through a network of cracks and fissure—openings ranging from intergranular spaces to large caves. The water eventually emerges from below the surface, in the form of a karst springs.
A natural flow of water from an underground to the surface is a spring. 
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