A man digging the ground near a water body found that the soil was moist. As he kept digging deeper and deeper he reached a level where all the spaces between particles of soil and gaps between rocks were filled with water. The upper limit of this layer is called


The upper limit of the groundwater is known as the water table. As the man digs deeper, the level where all the spaces between particles of soil and gaps between rocks were filled with water is known as the water table.

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