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Natural Cement
Material formed when certain minerals dissolve in water and then precipitate, binding sediment grains together into a solid mass.
Fractures
Breaks or cracks in rock caused by physical stress, often resulting in significant geological structures.
Unsaturated Zone
The layer of ground above the water table where pores are not fully saturated with water.
Water Table
The level below which the ground is completely saturated with water, marking the boundary between the unsaturated zone and the saturated zone.
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