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E. Sci. Ch. 14

AB
aquifera body of rock through which large amounts of water can flow and in which much water can be stored
porositythe amount/percentage of open spaces in a given volume of a rock
sortingthe amount of uniformity in the size of the particles, or grains, in rock
permeabilityhow freely water passes through the open spaces in it
impermeablewater cannot flow through it
zone of saturationthe layer of ground where all the pores are filled with water
water tablethe upper surface of the zone of saturation
zone of aerationthe zone that lies between the water table and the earth's surface
capillary fringethe bottom region of the zone of aeration, just above the water table
artesian formationa sloping layer of permeable rock sandwiched between two layers of impermeable rock and exposed at the ground surface
hot springhot groundwater that rises to the surface before cooling
mud potsweathered rock around a hot spring that mixes with the hot water to form liquid clay that bubbles at the surface
geyserhot springs that erupt periodically
hard waterwater that contains large amounts of dissolved minerals
soft waterwater that contains few dissolved minerals
sinkholecircular depression caused when the roof of a cavern collapses
stalactitecone-shaped calcite deposit suspended from the ceiling of a cavern
stalagmitecone-shaped calcite deposit built up from the floor of a cavern
karst topographyregions where the effects of the chemical weathering due to ground water are clearly visible at the surface


Mrs. Bitley

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