The place where the water table meets the ground surface, and groundwater bubbles or flows out of cracks in rock openings is called a spring.

Here's a breakdown:

* Water table: The upper surface of the zone of saturation in the ground. This is where the soil and rock are completely saturated with water.

* Spring: A natural flow of groundwater that emerges from the ground. This happens when the water table intersects the surface, often in areas where the ground is fractured or porous.

* Cracks in rock openings: These provide pathways for the groundwater to reach the surface.

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