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