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-Confined groundwater builds up high hydrostatic pressure |
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-Forms when groundwater dissolves the soluble rock layers and they collapse |
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-Depression in the water table around a well |
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-Energy produced from Earth's internal heat |
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-Hot springs which periodically eject hot water and steam with tremendous force |
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-All subsurface water trapped in pores |
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-Springs where the water temperate is higher than 37 degrees celcius |
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-Hot water -Heated by magma or Earth's geothermal gradient |
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-Develops by groundwater erosion |
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-The capacity to transmit fluids |
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-Percentage of a material's total volume that is pore space |
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-Depressions in the ground formed by the dissolution of the underlying soluble rocks -Or collapse of a cave roof |
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-When percolating water reaches water or an impermeable layer, it flows laterally |
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-Top of the zone beneath the surface in which the pores are filled with water |
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-Openings made by digging or drilling down into the zone of saturation |
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-When water initially infiltrates the ground, most of the pores are filled with air |
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-Underlying the Zone of Aeration is a zone in which the pores are filled with water |
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