chapter 10: ground water review designed by: meghan e. dillner
TRANSCRIPT
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Chapter 10: Ground water Review
Designed by:Meghan E. Dillner
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ReviewLESSON 10.1 VOCABULARY
100 200 300 400 500
LESSON 10.2 VOCABULARY
100 200 300 400 500
LESSON 10.3 VOCABULARY
100 200 300 400 500
MIXED VOCABULARY
100 200 300 400 500
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BONUS QUESTION!
If answered correctly, this question is worth…
1,000 EXTRA POINTS!
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How much of the hydrosphere is contained in
the oceans?
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97%
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Permeable under ground layer through which groundwater
flows relatively easily.
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AQUIFER
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Process by which precipitation that has fallen on land surfaces enters the ground and becomes groundwater.
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INFILTRATION
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Ability of a material to let water pass through, which
is high in material with large, well-connected pores and low in material with few
pores or small pores.
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PERMEABILITY
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Percentage of open spaces between
grains in a rock; is heightened in well sorted sediments
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POROSITY
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Upper boundary of the zone of saturation that
rises during wet seasons and drops during dry
periods
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WATER TABLE
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Underground opening connected to Earth’s
surface, usually formed when groundwater
dissolves limestone
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CAVE
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Irregular topography with sinkholes, sinks, and
sinking streams caused by groundwater
dissolution of limestone
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KARST TOPOGRAP
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Depression in Earth’s surface formed when a cave collapses or bedrock is dissolved
by acidic rain
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SINKHOLE
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Cone-shaped or cylindrical dripstone deposit of calcium
carbonate that hangs like an icicle from a cave’s
ceiling
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STALACITE
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Mound-shaped dripstone deposit of calcium
carbonate that forms on a cave’s floor beneath a
stalacite
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STALAGMITE
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Fountain of water that spurts above the land
surface when a well taps a deep, confined aquifer containing water under
pressure
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ARTESIAN WELL
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Difference between the water level in a
pumped well and the original water-table
level
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DRAWDOWN
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Explosive hot spring that erupts
regularly
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GEYESER
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Thermal spring with temperatures
higher than that of the human body
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HOT SPRING
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Process by which water from
precipitation and runoff is added to the
zone of saturation
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RECHARGE
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Depth below Earth’s surface where all the pores of a material
are completely filled with groundwater
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ZONE OF SATURATION
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A type of limestone found in dripstone
formations
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TRAVERTINE
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Natural discharge of groundwater at Earth’s
surface where an aquifer and an aquiclude come
in contact
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SPRING
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Deep hole drilled or dug into the ground to reach a reservoir
of groundwater
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WELL
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The Greek word for water
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hydros
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