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aqueduct
channels&/ or pipes built and used to carry water from a source location to a location of usage
conservation
using less of a resource so it will not used up
flood
occurs when the discharge of a stream is greater than the stream channel can carry and the water overflows the stream banks
infiltration
process of water seeping into the ground
condensation
the change of water vapor into liquid water droplets
recharge rate
how fast water from precipitation and runoff infiltrates into and refill an aquifer
water table
boundary that separates the zone of aeration and saturation; the level to which a well must be drilled in order to obtain groundwater
runoff
water that flows over the land rather than seeping unto the ground
well
a hole drilled or dug down below the water table from which water is moved to the surface
karst topography
areas with many sinkholes and few running surface streams due to limestone, dolomite, marble and gypsum bedrock
tributary
a smaller stream that flows into a larger stream
divide
imaginary line separates the watershed of one stream from the watershed of another stream
floodplain
broad, flat area along the sides of a stream that may be covered by water during times of high water
ground water
water in cracks and pores spaces in soil, regolith, & rock below Earths surface
wetland
area of land that is covered with shallow water during part of all of the year
discharge
volume of water in a stream flowing past a certain point in a given unit of time
evaporation
the change of liquid into water vapor
transpiration
evaporation of water from plants
zone of aeration
region above the water table in which the pore spaces are filled with water and air
reservoir
a man made lake
irrigation
supplying water to areas of dry land to make them more suitable for growing crops
artesian well
well that flows on its own without being pumped
aquifer
a porous and permeable layer of soil, regolith of rock from which ground water can be pumped
spring
place where water flows out of the ground
eutrophication
process in which lakes and ponds become rich in nutrients from the surrounding watershed causing algae growth and depletion of oxygen
permeability
the ability of a substance to permit water to pass through it
lake
a depression in the surface materials of a landscape that holds water
pore spaces
empty spaces in the bedrock and soil that can be filled with air or water
cavern
type of underground passage hat forms when groundwater dissolves limestone, dolomite, marble or gypsum
desalination
removal of salt from saltwater in order to make the water usable
impermeable
substance that water cannot pass through
nonpoint source
widely spread source of pollution that can not be tied to a specific point of origin
zone of saturation
region below the water table in which the pore spaces are completely filled with water
porosity
the amount of pore spaces in soil or rock
sink hole
depression on the surface cause by collapse of a ceiling of a shallow cavern
precipitation
rain, hail, snow, sleet
point source
specific source of pollution that can be identified
cone of depression
region around a well in which the water table is Iowered due to rapid removal of water from the zone of saturation
water cycle
the movement of water between plants and animals, the atmosphere, and the Earths surface and underground
water shed
an area that is drained by a river or system of rivers, a drainage basin