EARTH SCIENCE geology, the environment, and the universe 2008 (11)

BIG Idea Precipitation
and infiltration contribute to
groundwater, which is stored
in underground reservoirs
until it surfaces as a spring
or is drawn from a well.

10.1 Movement and
Storage of Groundwater
MAIN Idea Groundwater
reservoirs provide water to
streams and wetlands wherever
the water table intersects the
surface of the ground.

10.2 Groundwater
Weathering and Deposition
MAIN Idea Chemical weathering of limestone by water causes
the characteristic topography of
karst areas.

10.3 Groundwater Supply
MAIN Idea Water is not
always available in the quantities and in the locations where it
is needed and might be compromised by pollution.

GeoFacts
• The Strokkur geyser in Iceland
erupts every 5 to 10 minutes.
• The eruptions of Strokkur
geyser reach heights of more

than 30 m.
• There are around 1000 geysers
in the world.

250

Yvain Genevay/Geologos/CORBIS

Groundwater


Start-Up Activities
Threats to the Water Supply
Make this Foldable to summarize
the major problems that threaten
groundwater supplies.

LAUNCH Lab
How is water stored
underground?
Beneath your feet, there are vast amounts of water.
This water fills in the pore spaces and fractures in
rock and unconsolidated sediment. In this activity,
you will model groundwater storage.

STEP 1 Fold a sheet of
paper in half lengthwise.

STEP 2 Fold the sheet
in half and then into thirds.

STEP 3 Unfold and cut
along the fold lines of the
top flap to make six tabs.

Procedure
1. Read and complete the lab safety form.
2. Fill a 250-mL graduated cylinder with
fine, dry sand.
3. Fill another 250-mL graduated cylinder
with water.
4. Pour water from the second cylinder into the
sand-filled cylinder until the water level is
flush with the surface of the sand. Measure
and record the volume of saturated sand in
the cylinder.
5. Measure and record how much water is left
in the second cylinder.
6. Repeat the experiment twice using coarse
sand and clay.
Analysis
1. Describe how much water is present in the
saturated fine sand, coarse sand, and clay.
2. Calculate the ratio of water volume to the
volume of fine sand, coarse sand, and clay,
and express the value as a percentage.
3. Infer how many liters of water could be
stored in a cubic meter of each sediment.

Label the tabs

as you read.

Overuse

STEP 4

FOLDABLES Use this Foldable with Section 10.3.
As you read this section, summarize the problems that can threaten groundwater.

Visit glencoe.com to
study entire chapters online;
explore
•

Interactive Time Lines

•

Interactive Figures

•

Interactive Tables

animations:

access Web Links for more information, projects,
and activities;
review content with the Interactive
Tutor and take Self-Check Quizzes.

Section 1Chapter
• XXXXXXXXXXXXXXXXXX
10 • Groundwater 251
Doug Martin


Section 10
10.1
.1
Objectives
◗ Describe how groundwater storage
and underground movement relate
to the water cycle.
◗ Illustrate an aquifer and an
aquiclude.
◗ Relate the components of aquifers
with the presence of springs.

Review Vocabulary
hydrologic cycle: a never-ending
natural circulation of water through
Earth’s systems

New Vocabulary
infiltration
zone of saturation
water table
zone of aeration
permeability

aquifer
aquiclude
spring
hot spring
geyser

Movement and Storage
of Groundwater
MAIN Idea Groundwater reservoirs provide water to streams and
wetlands wherever the water table intersects the surface of the
ground.
Real-World Reading Link Have you ever noticed that a stream flows even

when it has not rained in a long time? Rainfall contributes to the flow in a
stream, but much of the water comes from beneath the ground.

The Hydrosphere
The water on and in Earth’s crust makes up the hydrosphere, named
after hydros, the Greek word for water. You learned about the hydrosphere in Chapter 1 in the context of Earth’s systems, including the
geosphere, hydrosphere, atmosphere, and biosphere. About 97 percent of the hydrosphere is contained in the oceans. The water contained by landmasses—nearly all of it freshwater—makes up only
about 3 percent of the hydrosphere.
Freshwater is one of Earth’s most abundant and important
renewable resources. However, of all the freshwater, between 70 and
80 percent is held in polar ice caps and glaciers. All the rivers,
streams, and lakes on Earth represent only a small fraction of Earth’s
liquid freshwater, as shown in Table 10.1. Recall from Chapter 9
that water in the hydrosphere moves through the water cycle.

Table 10.1
Location

Oceans

252 Chapter 10 • Groundwater

World’s
Water Supply
Percentage of
Total Water
97.2

Interactive Table To explore
more about Earth’s water supply,
visit glencoe.com.

Water Volume
(km3)
1,230,000,000

Ice caps and
glaciers

2.15

28,600,000

Groundwater

0.31

4,000,000

Lakes

0.009

123,000

Atmosphere

0.001

12,700

Rivers and
streams

0.0001

1200

Estimated Average
Residence Time of
Water
thousands of years
tens of thousands of
years and longer
hundreds to many
thousands of years
tens of years
nine days

two weeks


Groundwater and Precipitation
The ultimate source of all water on land is the oceans. Evaporation
of seawater cycles water into the atmosphere in the form of invisible water vapor and visible clouds. Winds and weather systems
move this atmospheric moisture all over Earth, with much of it
concentrated over the continents. Precipitation brings atmospheric
moisture back to Earth’s surface. Some of this precipitation falls
directly into the oceans and some falls on land.
Infiltration is the process by which precipitation that has fallen
on land trickles into the ground and becomes groundwater. Only a
small portion of precipitation becomes runoff and is returned
directly to the oceans through streams and rivers. Groundwater
slowly moves through the ground, eventually returns to the surface
through springs and seepage into wetlands and streams, and then
flows back to the oceans.
Reading Check Identify the ultimate source of all water on land.

Groundwater Storage
Puddles of water that are left after it rains quickly disappear, partly by
infiltrating the ground. On sandy soils, rain soaks into the ground
almost immediately. Where does that water go? The water seeps into
small openings within the ground. Although Earth’s crust appears
solid, it is composed of soil, sediment, and rock that contain countless
small openings, called pores spaces.
Pore spaces make up large portions of some of these materials. The
amount of pore space in a material is its porosity. The greater the
porosity, the easier water can flow through the material. Subsurface
materials have porosities ranging from 2 percent to more than 50

percent. For example, the porosity of well-sorted sand is 30 percent;
however, in poorly sorted sediment, smaller particles occupy some of
the pore spaces and reduce the overall porosity of the sediment, as
shown in Figure 10.1. Similarly, the cement that binds the grains of
sedimentary rocks together reduces the rocks’ porosity. Because of
the enormous volume of sediment and rock beneath Earth’s surface,
enormous quantities of groundwater are stored in the pore spaces.
■

Figure 10.1 Porosity depends on the size and variety of particles in a material.

Compare the porosities shown in each sample.

Well-sorted, large sand grains

Unsorted sand grains

Well-sorted, small sand grains

Section 1 • Movement and Storage of Groundwater

253


Soil moisture
Zone of aeration
Water table
Zone of
saturation

Stream

Normal water table
Water table during drought
■ Figure 10.2 The zone of saturation
is where groundwater completely fills all the
pores of a material below Earth’s surface.
Describe what is above the zone
of saturation.

The Zone of Saturation
The region below Earth’s surface in which groundwater completely
fills all the pores of a material is called the zone of saturation. The
upper boundary of the zone of saturation is the water table, shown in
Figure 10.2. Strictly speaking, only the water in the zone of saturation is called groundwater. In the zone of aeration, which is above the
water table, materials are moist, but because they are not saturated
with water, air occupies much of the pores.
Water movement Water in the zone of saturation and zone
of aeration can be classified as either gravitational water or capillary
water. Gravitational water is water that trickles downward as a result
of gravity. Capillary water is water that is drawn upward through
capillary action above the water table and is held in the pore spaces
of rocks and sediment because of surface tension. Capillary action
can be seen when the tip of a paper towel is dipped into water and
the water seems to climb up through the fibers of the paper towel.
The water table The depth of the water table often varies
depending on local conditions. For example, in stream valleys,
groundwater is relatively close to Earth’s surface, and thus the
water table can be only a few meters deep. In swampy areas, the
water table is at Earth’s surface, whereas on hilltops or in arid

regions, the water table can be tens to hundreds of meters or more
beneath the surface. As shown in Figure 10.2, the topography of
the water table generally follows the topography of the land above
it. For example, the slope of the water table corresponds to the
shape of valleys and hills on the surface above.
Because of its dependence on precipitation, the water table fluctuates with seasonal and other weather conditions. It rises during
wet seasons, usually in spring, and drops during dry seasons, often
in late summer.

254

Chapter 10 • Groundwater


Groundwater Movement
Groundwater flows downhill in the direction of the slope of the water
table. Usually, this downhill movement is slow because the water has to
flow through numerous tiny pores in the subsurface material. The tendency of a material to let water pass through it is its permeability.
Materials with large, connected pores, such as sand and gravel, have
high permeability and permit relatively high flow velocities up to
hundreds of meters per hour. Other permeable subsurface materials
include highly fractured bedrock, sandstone, and limestone.
Permeability Groundwater flows through permeable sediment
and rock, called aquifers, such as the one shown in Figure 10.3.
In aquifers, the pore spaces are large and connected. Fine-grained
materials have low permeabilities because their pores are small.
These materials are said to be impermeable. Groundwater flows so
slowly through impermeable materials that the flow is often measured in millimeters per day. Some examples of impermeable materials include silt, clay, and shale. Clay is so impermeable that a
clay-lined depression will hold water. For this reason, clay is often
used to line artificial ponds and landfills. Impermeable layers,

called aquicludes, are barriers to groundwater flow.
Flow velocity The flow velocity of groundwater depends on
the slope of the water table and the permeability of the material
through which the groundwater is moving. The force of gravity
pulling the water downward is greater when the slope of the water
table surface is steeper. Water also flows faster through a large
opening than through a small opening. The flow velocity of
groundwater is proportional to both the slope of the water table
and the permeability of the material through which the water
flows.

■ Figure 10.3 An aquifer is a layer of permeable subsurface material that is saturated
with water. This aquifer is located between two
impermeable layers called aquicludes.

Precipitation and infiltration

Aquicludes
Aquifer

Section 1 • Movement and Storage of Groundwater

255


Jon Turk/Visuals Unlimited

Figure 10.4 Springs occur when the
groundwater emerges at points where the
water table intersects Earth’s surface.

■

Springs
Groundwater moves slowly but continuously through aquifers and
eventually returns to Earth’s surface. In most cases, groundwater
emerges wherever the water table intersects Earth’s surface. Such intersections commonly occur in areas that have sloping surface topography. The exact places where groundwater emerges depend on the
arrangement of aquifers and aquicludes in an area.
Reading Check Explain how the slope of the land can affect where

groundwater emerges.

As you learned on the previous page, aquifers are permeable underground layers through which groundwater flows easily, and aquicludes
are impermeable layers. Aquifers are commonly composed of layers of
sand and gravel, sandstone, and limestone. In contrast, aquicludes,
such as layers of clay or shale, block groundwater movement. As a
result, groundwater tends to discharge at Earth’s surface where an
aquifer and an aquiclude are in contact, as shown in Figure 10.4.
These natural discharges of groundwater are called springs.
Emergence of springs The volume of water that is discharged
by a spring might be a mere trickle or it might form a stream. In some
regions called karst regions, an entire river might emerge from the
ground. Such a superspring is called a karst spring. Karst springs occur
in limestone regions where springs discharge water from underground
pathways. In regions of nearly horizontal sedimentary rocks, springs
often emerge on the sides of valleys at about the same elevation, at the
bases of aquifers, as shown in Figure 10.5. Springs might also
emerge at the edges of perched water tables. In a perched water table, a
zone of saturation that overlies an aquiclude separates it from the main
water table below. Other areas where springs tend to emerge are along

faults, which are huge fractures along which large masses of rock have
moved, and sometimes block aquifers. In limestone regions, springs
discharge water from underground pathways as karst springs.
256 Chapter 10 • Groundwater


Visualizing Springs
Figure 10.5 A spring is the result of groundwater that emerges at Earth’s surface.
Springs can be caused by a variety of situations.
Compare and contrast the origin of the four types of springs.

Sandstone

Perched water table
Layer of
impermeable clay

Water table

Spring
Spring

A spring forms where a permeable layer and impermeable layer
come together.

Sandstone

Main water
table

A layer of impermeable rock or clay can create
a perched water table. Springs can result where groundwater
emerges from a perched water table.

Water table

Water table

Cavern

Spring

Spring

lt

u
Fa

Shale

Some springs form where a fault has brought together two
different types of bedrock, such as a porous rock and a nonporous rock.

Karst springs form where groundwater weathers through limestone bedrock, and water in the underground caverns emerges
at Earth’s surface.

To explore more about springs, visit
glencoe.com.

Section 1 • Movement and Storage of Groundwater

257


Eruption of geyser

Heat

Heat
Hot water

Figure 10.6 A geyser is a type of hot
spring from which very hot water and vapor
erupt at the surface.
Identify the origin of a geyser.
■

Section 10.1

Temperature of springs People usually think of spring
water as being cool and refreshing. But the temperature of groundwater that is discharged through a spring is generally the average
annual temperature of the region in which it is located. Thus,
springs in New England have year-round temperatures of about
10°C, while further south, springs in the Gulf states have temperatures of about 20°C.
Compared to air temperatures, groundwater is generally colder
in the summer and warmer in the winter. However, in some
regions around the world, springs discharge water that is much
warmer than the average annual temperature. These springs are
called warm springs or hot springs, depending on their temperatures. Hot springs are springs that have a temperature higher than

that of the human body, which is 37°C.
There are thousands of hot springs in the United States. Most of
them are located in the western United States in areas where the
subsurface is still hot from nearby igneous activity. A number of
hot springs also occur in some eastern states. These hot springs
emerge from aquifers that descend to tremendous depths in
Earth’s crust and through which deep, hot water rises. The water
is hot because temperatures in Earth’s upper crust increase by an
average of 25°C for every km of depth.
Among the most spectacular features produced by Earth’s
underground thermal energy in volcanic regions are geysers,
shown in Figure 10.6. Geysers are explosive hot springs. In a geyser, water is heated past its boiling point, causing it to vaporize. The
resulting water vapor builds up tremendous pressure. This pressure
is what fuels the eruptions. One of the world’s most famous geysers,
Old Faithful, is located in Yellowstone National Park, Wyoming.

Assessment

Section Summary

Understand Main Ideas

◗ Some precipitation infiltrates the
ground to become groundwater.

1.

◗ Groundwater is stored below the
water table in pore spaces of rocks
and sediment.

2. Illustrate how the relative positions of an aquifer and aquiclude can result in the
presence of a spring.

◗ Groundwater moves through permeable layers called aquifers and is
trapped by impermeable layers
called aquicludes.

4. Analyze the factors that determine flow velocity.

◗ Groundwater emerges from the
ground where the water table intersects Earth’s surface.

6. Infer why it is beneficial for a community to have an aquiclude located beneath
the aquifer from which it draw its water supply.

MAIN Idea

Explain how the movement of groundwater is related to the water

cycle.

3. Describe how the water in hot springs gets hot.

Think Critically
5. Differentiate between porosity and permeability in subsurface materials.

Earth Science
7. Develop a set of guidelines in which you describe where you would be most likely
to find groundwater.

258 Chapter 10 • Groundwater

Self-Check Quiz glencoe.com


Section 1 0 . 2
Objectives
◗ Explain how groundwater dissolves
and deposits rocks and minerals.
◗ Illustrate how caves form.
◗ Describe how the features of karst
topography shape the landscape.

Groundwater Weathering
and Deposition
MAIN Idea Chemical weathering of limestone by water causes the
characteristic topography of karst areas.

Review Vocabulary

Real-World Reading Link You might have seen an old gravestone, statue, or

hydrolysis: chemical reaction of
water with other substances

sculpture that has been weathered by acidic water. Similar processes form limestone caves underground.

New Vocabulary
cave

sinkhole
karst topography
stalactite
stalagmite

■

Figure 10.7 Carbonic acid has

dissolved large portions of this limestone. This resulting formation is the
Stone Forest in China.

Carbonic Acid
Acids are aqueous solutions that contain hydrogen ions. Most
groundwater is slightly acidic due to carbonic acid. Carbonic acid
forms when carbon dioxide gas dissolves in water and combines
with water molecules. This happens when precipitation falls
through the atmosphere and interacts with carbon dioxide gas or
when groundwater infiltrates the products of decaying organic
matter in soil. As a result of these processes, groundwater is usually
slightly acidic and attacks carbonate rocks, especially limestone.
Limestone mostly consists of calcite, also called calcium carbonate,
which reacts with any kind of acid. The results of this reaction over
time are shown in Figure 10.7. This process occurs above ground
and below ground.

Dissolution by Groundwater
The process by which carbonic acid forms and dissolves calcite,
can be described by three simple chemical reactions.
In the first reaction, carbon dioxide (CO2) and water (H2O)

combine to form carbonic acid (H2CO3), as represented by the following equation.
CO2 + H2O → H2CO3
In the second reaction, carbonic acid splits into hydrogen ions
(H+) and bicarbonate ions (HCO3–). This process is represented by
the following equation.
H2CO3 → H+ + HCO3–
In the third reaction, the hydrogen ions (H+) react with calcite
(CaCO3) and form calcium ions (Ca2+) and bicarbonate ions
(HCO3–).
CaCO3 + H+ → Ca2+ + HCO3–
Section 2 • Groundwater Weathering and Deposition 259
Michele Burgess/Index Stock


The resulting calcium ions (Ca2+) and bicarbonate ions are then
carried away in the groundwater. Eventually, they precipitate, which
means they crystallize out of the solution, somewhere else. Precipitation occurs when the groundwater evaporates or when the carbon
dioxide gas leaves the water. The processes of dissolving, called dissolution, and precipitation of calcite both play a major role in the formation of limestone caves, such as those shown in Figure 10.8.

Figure 10.8 Groundwater dissolution
and precipitation result in a variety of features
in caves.
Identify which chemical reactions might
be at work.
■

Caves A natural underground opening with a connection to Earth’s
surface is called a cave or a cavern. Some caves form three-dimensional mazes of passages, shafts, and chambers that stretch for many
kilometers. Some caves are dry, while some contain underground
streams or lakes. Others are totally flooded and can be explored only

by cave divers. Mammoth Cave in Kentucky, shown in Figure 10.8,
is composed of a series of connected underground passages.
Most caves are formed when groundwater dissolves limestone.
The development of most caves begins in the zone of saturation just
below the water table. As groundwater infiltrates the cracks and
joints of limestone formations, it gradually dissolves the adjacent
rock and enlarges these passages to form an interconnected network
of openings. As the water table is lowered, the cave system becomes
filled with air. New caves then form beneath the lowered water table.
If the water table continues to drop, the thick limestone formations
eventually become honeycombed with caves. This is a common
occurrence in limestone regions that have been uplifted by tectonic
forces.

Carlsbad Caverns, New Mexico
260

Chapter 10 • Groundwater

(l)Fritz Polking/Visuals Unlimited, (r)Adam Jones/Visuals Unlimited

Reading Check Explain how most caves form.

Mammoth Cave, Kentucky


■ Figure 10.9 Karst topography is
characterized by a landscape of sinkholes
formed by dissolution of limestone.
Identify what controls the rate

of dissolution of bedrock in karst
topography.

Karst topography Figure 10.9 shows some of the surface features produced by the dissolution of limestone bedrock. One of the
main features is a sinkhole—a depression in the ground caused by the
collapse of a cave or by the direct dissolution of limestone by acidic
water. Another type of feature, called a disappearing stream, forms
when a surface stream drains into a cave system and continues flowing
underground, leaving a dry valley above. Disappearing streams sometimes reemerge on Earth’s surface as karst springs.
Limestone regions that have sinkholes and disappearing streams
are said to have karst topography. The word karst comes from the
name of a region in Croatia where these features are especially well
developed. Prominent karst regions in the United States are located
in Kentucky, Indiana, Florida, and Missouri. The Mammoth Cave
region in Kentucky has karst topography that contains tens of
thousands of sinkholes.
In karst areas, sinkholes proliferate, grow, and eventually join to
form wide valleys. Most of the original surface has been dissolved,
with the exception of scattered mesas and small buttes. The rate of
the dissolution process varies greatly among locations, depending
on factors such as humidity and soil composition. In humid areas,
where there is more precipitation, more water infiltrates areas of
porous soil, and dissolves the limestone in the subsurface.

Figure 10.10 Stalactites are dripstones produced by a buildup of minerals
precipitated from groundwater.

■

Groundwater Deposits

Calcium ions eventually precipitate from groundwater and form new
calcite minerals. These minerals create spectacular natural features.
Dripstones The most remarkable features produced by groundwater are the rock formations called dripstone that decorate many
caves above the water table, as shown in Figure 10.10. These formations are built over time as water drips through caves. Each
drop of water hanging on the ceiling of a cave loses some carbon
dioxide and precipitates some calcite. A form of dripstone, called a
stalactite, hangs from the cave’s ceiling like icicles and forms gradually. As the water drips to the floor of the cave, it may also slowly
build mound-shaped dripstone called stalagmites.
Section 2 • Groundwater Weathering and Deposition 261
(t)Lloyd Homer/GNS Science, (b)Albert J. Copley/Visuals Unlimited


Sheila Terry/Photo Researchers

■ Figure 10.11 Hard water
contains high concentrations of
minerals., which leave precipitates in household water pipes
such as this one.
Identify one of the likely
precipitates in this pipe.

Sometimes stalactites and stalagmites grow together to form dripstone columns. Increasingly, researchers are finding abundant and
varied microorganisms associated with dripstone formations in caves.
It is possible that these organisms play an important role in the deposition of at least some of the materials found in caves.
Hard water You are probably aware that tap water contains various dissolved solids. While some of these materials are added by
water treatment facilities, others come from the dissolution of minerals in soils and subsurface rock and sediment. Water that contains
high concentrations of calcium, magnesium, or iron is called hard
water. Hard water is common in areas where the subsurface rock is
limestone. Because limestone is made of mostly calcite, the groundwater in these areas contain significant amounts of dissolved calcite.
Hard water used in households can sometimes cause problems. Just

as calcite precipitates in caves, it can also precipitate in water pipes,
as shown in Figure 10.11, and on the heating elements of appliances. Over time, deposits of calcite can clog water pipes and render
some electrical appliances useless.

Section 10.2

Assessment

Section Summary

Understand Main Ideas

◗ Groundwater dissolves limestone
and forms underground caves.

1.

◗ Sinkholes form at Earth’s surface
when bedrock is dissolved or when
caves collapse.

2. Identify the acid that is most common in groundwater.

◗ Irregular topography caused by
groundwater dissolution is called
karst topography.
◗ The precipitation of dissolved
calcite forms stalactites and stalagmites in caves.

MAIN Idea Analyze how limestone is weathered, and identify the features that

are formed as a result of this dissolution.

3. Illustrate in a series of pictures how caves are formed.
4. Examine Why is hard water more common in some areas than others?

Think Critically
5. Compare and contrast the formation of stalactites and stalagmites.
6. Analyze how you might be able to tell an area of karst topography on a topographic map.

Earth Science
7. Explain how subsurface limestone is related to karst topography.

262

Chapter 10 • Groundwater

Self-Check Quiz glencoe.com


Section 1 0 . 3

Groundwater Supply

Objectives
◗ Explain how groundwater is withdrawn from aquifers by wells.
◗ Describe the major problems that
threaten groundwater supplies.

MAIN Idea Water is not always available in the quantities and
in the locations where it is needed and might be compromised

by pollution.

Review Vocabulary

Real-World Reading Link If you have a bank account, can you withdraw

runoff: water flowing downslope
along Earth’s surface

as much money as you want? Of course not. Like a bank account, groundwater
can be withdrawn, but only in the amount that has been deposited there.

New Vocabulary
well
drawdown
recharge
artesian well

Wells
Wells are holes dug or drilled into the ground to reach an aquifer.
There are two main types of wells: ordinary wells and artesian wells.

■ Figure 10.12 Overpumping from one well
or multiple wells can result in a cone of depression
and a general lowering of the water table.

Well

Ordinary wells The simplest wells are those that are dug or
drilled below the water table, into what is called a water-table

aquifer, as shown in Figure 10.12. In a water-table aquifer,
the level of the water in the well is the same as the level of the
surrounding water-table. As water is drawn out of a well, it is
replaced by surrounding water in the aquifer.
Overpumping occurs when water is drawn out of the well at a
rate that is faster than that at which it is replaced. Overpumping of
the well lowers the local water level and results in a cone of depression around the well, as shown in Figure 10.12. The difference
between the original water-table level and the water level in the
pumped well is called the drawdown. If many wells withdraw
water from a water-table aquifer, the cones of depression can overlap and cause an overall lowering of the water table, causing shallow wells to become dry. Water from precipitation replenishes the
water content of an aquifer in the process of recharge. Groundwater recharge from precipitation and runoff sometimes replaces
the water withdrawn from wells. However, if withdrawal of groundwater exceeds the aquifer’s recharge rate, the drawdown increases
until all wells in the area become dry.

Well

Water table
Before heavy pumping

Well

Dry
well

Dry
well

Cone
ssion
of depre

Lowered water table
After heavy pumping
Section 3 • Groundwater Supply

263


■ Figure 10.13 An artesian aquifer contains water under pressure.
Identify the features that cause the primary difference between an ordinary well
and an artesian well.

Recharge area
Artesian
wells

Pressure surface
Water table

Impe

Impermeab

rmea

Sandstone

le layer

ble la

yer

Artesian wells An aquifer’s area of recharge is often at a higher
elevation than the rest of the aquifer. An aquifer located between aquicludes, called a confined aquifer, can contain water that is under pressure. This is because the water at the top of the slope exerts
gravitational force on the water downslope, as you will learn in the
Problem-Solving Lab on this page. An aquifer that contains water
under pressure is called an artesian aquifer. When the rate of recharge
is high enough, the pressurized water in a well drilled into an artesian
aquifer can spurt above the land surface in the form of a fountain
known as an artesian well. The level to which water in an open well
can rise is called its pressure surface, as shown in Figure 10.13.
Similarly, a spring that discharges pressurized water is called an
artesian spring. The name artesian is derived from the French province of Artois, where such wells were first drilled almost 900 years ago.

PROBLEM-SOLVING Lab
Make a Topographic
Profile
Aquifer Data

How does water level vary in an artesian well?
Artesian aquifers contain water under pressure.
The table provides data about an artesian aquifer for three sites that are spaced 100 m apart
along a survey line. It shows the following: elevations of the land surface, the water table, the
upper surface of the aquiclude on top of the
artesian aquifer, and artesian pressure surface.
Analysis
1. Plot the elevation data on a graph with the
sites on the x-axis and the elevations on the
y-axis.
2. Make a topographic profile of the survey

line from Site 1 to Site 3. Use a heavy line to
indicate land surface.

264

Chapter 10 • Groundwater

Site

Surface
Elevation
(m)

Water
Table
Elevation
(m)

Aquiclude
Elevation
(m)

Pressure
Surface
(m)

1

396

392

388

394

2

394

390

386

393

3

390

388

381

392

Think Critically
2. Analyze What are the depths of the water levels in the three wells before they are pumped?
3. Evaluate what would happen if a well were
drilled into the confined aquifer at Site 3.

4. Consider At what sites could there be an
artesian well?


An important artesian aquifer in the United States
is the Ogallala Aquifer, which underlies the Great
Plains. This aquifer delivers water to a huge area
stretching from South Dakota to Texas. The recharge
areas of the Ogallala Aquifer are located in the Black
Hills and the Rocky Mountains.

Threats to Our Water Supply
Freshwater is Earth’s most precious natural resource.
Human demands for freshwater are enormous, because
it is essential for life. Water is also used extensively in
agriculture and industry. Figure 10.14 shows freshwater usage in the United States. Groundwater supplies
much of this water.
Reading Check Summarize why freshwater is Earth’s
most precious natural resource.

Estimates of water supplies are the result of a
dynamic equilibrium between various factors. These factors include the amounts of precipitation and infiltration,
the surface drainage, the porosity and permeability of
subsurface rock or sediment, and the volume of groundwater naturally discharged back to the surface. Several of
these factors vary naturally over time, and several can be
affected by human activities. Changes to groundwater
supplies can lead to environmental issues such as a lowered water table, subsidence, and pollution.

U.S. Water Use

Power
generation
48%

Irrigation
35%

Municipal
11%

Private wells
less than 1%
Industrial
5%

■ Figure 10.14 Municipal water and private wells
supply your daily water needs.
Identify how you are involved with water use in
each of the other areas.

Model an Artesian Well
How does an artesian well form? What causes the water to rise above the ground surface?
Procedure
1. Read and complete the lab safety form.
2. Half fill a plastic shoe box or other container with sand. Add enough water to saturate the sand.
Cover the sand completely with a 1- or 2-cm layer of clay or a similar impermeable material.
3. Tilt the box at an angle of about 10°. Use a book for a prop.
4. Using a straw, punch three holes through the clay, one near the low end, one near the middle,
and one near the high end of the box. Insert a clear straw through each hole into the sand below.
Seal the holes around the straws.

Analysis

1.
2.
3.
4.

Observe the water levels in the straws. Where is the water level the highest? The lowest?
Identify the water table in the box.
Analyze Where is the water under greatest pressure? Explain.
Predict what will happen to the water table and the surface if the water flows from one of the
straws.

Section 3 • Groundwater Supply

265


Careers In Earth Science

Hydrogeologist Earth scientists
who map groundwater are called
hydrogeologists. They use field
methods, maps, and aerial photographs to determine where groundwater is located. To learn more
about Earth science careers, visit
glencoe.com.

Overuse Groundwater supplies can be depleted. If groundwater is
pumped out at a rate greater than the recharge rate, the groundwater
supply will decrease and the water table will drop. This is happening to

the Ogallala Aquifer. Its water, used mostly for irrigation, is being
withdrawn at a rate much higher than the recharge rate.
Subsidence Another problem caused by the excessive withdrawal
of groundwater is ground subsidence—the sinking of land. The volume of water underground helps support the weight of the soil, sediment, and rock above. When the height of the water table drops, the
weight of the overlying material is increasingly transferred to the
aquifer’s mineral grains, which then squeeze together more tightly.
As a result, the land surface above the aquifer sinks.
A dramatic example of subsidence can be seen along parts of the
Gulf coast of Texas, where heavy usage of groundwater over many
decades resulted in a wide-scale drop in the ground level. In a region
of 12,000 km2, the average subsidence was 15 cm, while some areas
dropped by as much as 3 m. This has presented flooding hazards for
much of the coastal region.
Pollution in groundwater In general, the most easily polluted groundwater reservoirs are water-table aquifers, which lack a
confining layer above them. Confined aquifers are affected less frequently by local pollution because they are protected by impermeable barriers. When the recharge areas of confined aquifers are
polluted, however, those aquifers can also become contaminated.
Reading Check Identify which kind of aquifer is more vulnerable to

pollution.

Sources of groundwater pollution include sewage from faulty
septic tanks and farms, landfills, and other waste disposal sites.
Pollutants usually enter the ground above the water table, but they
eventually infiltrate to the water table. In highly permeable aquifers, pollutants can spread quickly in a specific direction, such as
toward the wells shown in Figure 10.15.
■ Figure 10.15 Pollutants can spread
rapidly through a highly permeable aquifer.
Note how the polluted well has drawn the
pollution toward it as it has withdrawn
water from the water table.

Unpolluted
well

Faulty
septic
tank

Water
table

Coarse sandy
gravel
Polluted water
Polluted well

266 Chapter 10 • Groundwater

Sand


Chemicals Because chemicals dissolved and transported with

VOCABULARY

groundwater are submicroscopic in size, they can travel through
the smallest pores of fine-grained sediment. For this reason, chemicals such as arsenic can contaminate any type of aquifer. The
chemicals generally move downslope from a source in the form of
a pollution plume, which is a mass of contaminants that spreads
through the aquifer. Once chemical contaminants have entered

groundwater, they cannot be easily removed. In the GeoLab at the
end of the chapter, you will learn more about how geologists predict the risks of chemical contamination of groundwater based on
a region’s topography.

ACADEMIC VOCABULARY
Transport
to move from one place to another
Airplanes transport packages across the
country.

Reading Check Explain why chemicals such as arsenic can contami-

nate any kind of aquifer.

Sewage, landfills, and other waste disposal sites can include a
variety of contaminants. Chemical contaminants can be leached,
meaning dissolved by infiltrating groundwater. When chemical
and biological contaminants enter the groundwater, they flow
through the aquifer at the same rate as the rest of the groundwater.
Over time, an entire aquifer can become contaminated and toxic to
humans. Aquifers are particularly vulnerable to pollution in humid
areas where the water table is shallow and can more easily come in
contact with waste.
Salt Not all pollutants are toxic or unhealthful in and of themselves.

For example, ordinary table salt is used to season food, but water is
undrinkable when its salt content is too high. In like manner, groundwater is unusable after the intrusion of salt water. Salt pollution is one
of the major threats to groundwater supplies, especially in coastal
areas, where the intrusion of salt water into groundwater is a major
problem. In coastal areas, salty seawater, which is denser than freshwater, underlies the groundwater near Earth’s surface, as shown in

Figure 10.16. The overpumping of wells can cause the underlying
salt water to rise into the wells and contaminate the freshwater aquifer.
■

Figure 10.16 Freshwater aquifers can become contaminated with salt water.

Identify how overpumping can cause the underlying salt water to rise
in wells.

Interactive Figure To see an animation of salt
water contamination, visit glencoe.com.

Before pumping

After pumping
Ocean

Ocean
Overpumping
well

Water table
Fresh groundwater
Salt water

Water
table

Fresh
groundwater

Salt water

Section 3 • Groundwater Supply

267


Table
10.2

Groundwater
Pollution Sources

Infiltration from fertilizers
Leaks from storage tanks
Drainage of acid from mines
Seepage from faulty septic tanks
Saltwater intrusion into aquifers near
shorelines
Leaks from waste disposal sites
Radon

Radon Another source of natural groundwater pollution is radon

gas, which is one of the leading causes of cancer in the United
States. Radon found in groundwater is one of the products of the
radioactive decay of uranium in rocks and sediment, and it usually
occurs in very low concentrations in all groundwater. However,
some rocks, especially granite and shale, contain more uranium
than others. Therefore the groundwater in areas where these rocks

are present contains higher levels of radon. Some radon can seep
into houses, and, because it is heavier than air, it can accumulate in
poorly ventilated basements. The United States Environmental
Protection Agency (EPA) advises homeowners in radon-prone
regions to have their homes tested regularly for radon gas.

Protecting Our Water Supply
There are a number of ways by which groundwater resources can be
protected and restored. First, major pollution sources, many of which
are listed in Table 10.2, need to be identified and eliminated.
Pollution plumes that already exist can be monitored with observation
wells and other techniques. Most pollution plumes spread slowly providing adequate time for alternate water supplies to be found. In some
cases, pollution plumes can be stopped by building impermeable
underground barriers around the polluted area. Sometimes, polluted
groundwater can be pumped out for chemical treatment on the
surface.
While these measures can have limited success, they alone cannot
save Earth’s water supply. Humans must be aware of how their activities impact the groundwater system so that they can protect the
water supply.

Section 10.3

Assessment

Section Summary

Understand Main Ideas

◗ Wells are drilled into the zone of
saturation to provide water.

1.

◗ Overpumping of shallow wells
produces cones of depression.

3. Illustrate the difference between an artesian well and an ordinary well.

◗ Artesian wells tap confined aquifers
in which water is under pressure.
◗ When groundwater withdrawal
exceeds recharge, it lowers the water
table
◗ The most common sources of
groundwater pollution include sewage, landfills, and other waste disposal sites.

268 Chapter 10 • Groundwater

MAIN Idea

Evaluate the problems associated with overpumping wells.

2. Explain why artesian wells contain water under pressure.
4. Differentiate between the effects of radon and the effects of salt dissolved in
groundwater.

Think Critically
5. Formulate an experiment which would test if there were impermeable barriers
around a polluted area.
6. Analyze how best to prevent groundwater pollution in a residential area.

Earth Science
7. Predict how the permeability of an aquifer can affect the spread of pollutants.

Self-Check Quiz glencoe.com


Watcher of the Water
Safe drinking water is something that many
people take for granted. Most of the water
that is used for human consumption comes
from groundwater. Who ensures that groundwater sources remain safe?
Hydrogeologists A groundwater scientist,
called a hydrogeologist, is responsible for
finding and monitoring groundwater sources
to ensure the water supply is free of contaminants and is not used faster than it is replaced.
What does a typical day in the life of a hydrogeologist look like? One day might be spent in
the field conducting tests on the water levels.
The next day might be spent evaluating the
data in the office. The day after that might
involve looking for trouble in the water-supply
line of a house.

Aquifer case study Suppose a farmer
wants to install an irrigation system, which
involves digging a new well. First, the water
level in the area’s aquifer must be checked to
ensure that a new well will not cause shortages for other users. The hydrogeologist finds
an active well nearby and hooks it up to a
pump that continuously draws water for

24 hours. Periodic checks of other wells in the
area determine the changes in the water level
and quality. From the data gathered, he or she
computes how much water the aquifer contains and determines the amount of water
available for a new well.
Suppose that, after the farm starts using the
irrigation system, a house down the road loses
its water supply. The hydrogeologist goes to
the house and checks for technical problems,
such as a hole in the well casing. If the cause is
not technical, he or she will reassess the irrigation system by rechecking the water supply in
the aquifer.

These hydrogeologists collect water from a well to determine whether
or not it has been contaminated.

Quality assurance Hydrogeologists are
also responsible for checking water quality.
If the water from a particular aquifer develops
a strange taste and odor, the residents would
want to ensure the water is safe to drink.
The hydrogeologist gathers samples and sends
them to a lab to test for various contaminants,
such as sewage, pesticides, dissolved metals,
or organic material. If a contaminant is found,
the hydrogeologist will advise the residents
not to drink the water until the source is
discovered and the problem is resolved. The
hydrogeologist will then begin investigating
the problem and searching for clues to find

and stop the contamination.

Earth Science
Journal Research more about what
a hydrogeologist does at glencoe.com.
Then, imagine you are accompanying a
groundwater scientist on a day on the job.
Describe what you saw, what you did,
and what you learned about aquifers.
Earth Science and the Environment

269

Kevin Fleming/CORBIS


MAPPING: TRACK GROUNDWATER POLLUTION
Background: You can use a topographic map to

U. S. Geological Survey topographic map of Forest City,
Florida
transparent paper
ruler
graph paper
calculator

6. Draw a small line at each place where a contour
line intersects the line from Lake Lotus to Lake
Lucien. Also note the elevation at each hash mark
and any rivers crossed.

7. Draw a table to use for your topographic profile,
using the width representing the distance between
Lake Lotus to Lake Lucien. For the y-axis, use the
elevations 60, 70, 80, 90, and 100 ft.
8. Now take your paper where you marked your lines
and place it along the base of the table.
9. Mark a corresponding dot on the table for each elevation, and mark the position of Jim’s gas station.
10. Connect the dots to create a topographic profile.
11. Note the elevations of the nearby bodies of water to
approximate the distance from the ground surface
to the water table. Use dots to indicate those distances on the topographic profile. Connect the dots
to draw the water table on the topographic profile.

Procedure

Analyze and Conclude

estimate the direction of groundwater flow. Groundwater pollution spreads out from its source and follows the flow of groundwater. The spread and
movement of the pollution resembles a plume that
stems from its source.

Question: How can you determine the movement of
a pollution plume?

Materials

Imagine that Jim’s Gas Station has discovered a major
gasoline leak from one of its underground tanks. As the
local hydrogeologist, you are asked to determine the
path that the gasoline will take through the groundwater, and to notify the residents of the areas that might be

affected by the contamination.
1. Read and complete the lab safety form.
2. Identify the lakes and swamps in the southwest corner of the map and list their names and elevations in
a data table. (Note: The elevations are given or can be
estimated from the contour lines. The elevation of the
water table in each area can be estimated from the elevations of nearby bodies of water).
3. Note the location of Jim’s gas station on Forest City
Rd., about 1400 feet north of the Seminole County
line (at the 96-foot elevation mark).
4. Take out a piece of paper to construct a cross section
of the surface topography and the water table. Lay
the paper on the map from Lake Lotus to Lake
Lucien (through Jim’s Gas Station).
5. On this piece of paper, mark the location of Jim’s gas
station.
270

GeoLab

1. Calculate the slope of the ground surface on either
side of Jim’s Gas Station.
2. Estimate the slope of the water table at Jim’s Gas
Station.
3. Infer the direction toward which the pollution
plume will move.
4. Identify the houses and bodies of water that are
threatened by this pollution plume.
5. Conclude Prepare a written statement to present to
the local community. Explain the path the plume is
predicted to take, and how this was determined.

APPLY YOUR SKILL
Design Using what you have learned in this lab and in
the chapter, develop a plan for stopping the pollution
plume. Make a map showing where your plan will be
implemented. Indicate the sites where water quality will
be monitored regularly.


GeoLab 271
USGS


Download quizzes, key
terms, and flash cards
from glencoe.com.

BIG Idea Precipitation and infiltration contribute to groundwater, which is stored
in underground reservoirs until it surfaces as a spring or is drawn from a well.
Vocabulary

Key Concepts

Section 10.1 Movement and Storage of Groundwater
• aquiclude (p. 255)
• aquifer (p. 255)
• geyser (p. 258)
• hot spring (p. 258)
• infiltration (p. 253)
• permeability (p. 255)

• spring (p. 256)
• water table (p. 254)
• zone of aeration (p. 254)
• zone of saturation (p. 254)

MAIN Idea

•
•
•
•

Groundwater reservoirs provide water to streams and wetlands
wherever the water table intersects the surface of the ground.
Some precipitation infiltrates the ground to become groundwater.
Groundwater is stored below the water table in pore spaces of rocks and
sediment.
Groundwater moves through permeable layers called aquifers and is
trapped by impermeable layers called aquicludes.
Groundwater emerges from the ground where the water table intersects
Earth’s surface.

Section 10.2 Groundwater Weathering and Deposition
• cave (p. 260)
• karst topography (p. 261)
• sinkhole (p. 261)
• stalactite (p. 261)
• stalagmite (p. 261)

MAIN Idea

•
•
•
•

Chemical weathering of limestone by water causes the characteristic topography of karst areas.
Groundwater dissolves limestone and forms underground caves.
Sinkholes form at Earth’s surface when bedrock is dissolved or when
caves collapse.
Irregular topography caused by groundwater dissolution is called karst
topography.
The precipitation of dissolved calcite forms stalactites and stalagmites in
caves.

Section 10.3 Groundwater Supply
• artesian well (p. 264)
• drawdown (p. 263)
• recharge (p. 263)
• well (p. 263)

MAIN Idea

•
•
•
•
•

272 Chapter 10

X ••Study
StudyGuide
Guide

Water is not always available in the quantities and in the locations where it is needed and might be compromised by pollution.
Wells are drilled into the zone of saturation to provide water.
Overpumping of shallow wells produces cones of depression.
Artesian wells tap confined aquifers in which water is under pressure.
When groundwater withdrawal exceeds recharge, it lowers the water
table.
The most common sources of groundwater pollution include sewage,
landfills, and other waste disposal sites.

Vocabulary
PuzzleMaker
glencoe.com
Vocabulary
PuzzleMaker
biologygmh.com


Vocabulary Review
Match each phrase with a vocabulary term from the
Study Guide.
1. the depth below Earth’s surface at which all pores
in layers of soil are filled with water
2. the vertical movement of water through ground
layers
3. all of the permeable layers at a location
4. the percentage of pore space in a material

Each of the following sentences is false. Make each
sentence true by replacing the italicized words with
a vocabulary term from the Study Guide.

12. What are distinct adjacent spaces within a cave
system called?
A. chambers and passages
B. holes and mounds
C. sinkholes and pools
D. dripstone and depositions
13. What is the name of a layer of sediment or rock
that does not allow water to pass through it?
A. a permeable layer
B. an aquiclude
C. an aquifer
D. a nonaqueous layer

Use the diagram below to answer Questions 14 and 15.

5. Drawdown is produced in limestone regions that
have sinkholes and sinking streams.
6. Stalagmites are icicle-shaped deposits hanging from
the ceiling of caves.

1

7. Collapsing caves or dissolution of bedrock at the
surface produce systems of caves.

2

3

Use what you know about the vocabulary terms found
on the Study Guide to answer the following questions.
8. What two features are most often associated with
the formation of springs?

4

9. What is the main difference between regular
springs and artesian springs?

Understand Key Concepts

14. Which sequence of terms correctly labels the features shown in the diagram?
A. 2: water table, 3: impermeable layer
B. 3: surface zone, 4: impermeable layers
C. 1: zone of aeration, 3: zone of saturation
D. 1: zone of saturation, 3: zone of aeration

11. Which single source of freshwater represents the
largest volume of freshwater worldwide readily
available for use by humans?
A. ice caps and glaciers
B. freshwater lakes
C. rivers and streams
D. groundwater deposits

15. In which layer do the pores contain mostly air,
although the materials are moist?

A. layer 1
B. layer 2
C. layer 3
D. layer 4

10. What are explosive hot springs that develop in
volcanic areas?

Chapter Test glencoe.com

Chapter 10 • Assessment 273


16. Which characteristics do most areas with karst
topography share?
A. they are dry areas; limestone bedrock
B. they are humid areas; granite bedrock
C. they are humid areas; limestone bedrock
D. they are dry areas; granite bedrock

Use the diagram below to answer Question 21.

Use the graph below from a single well in North
Carolina to answer Questions 17 and 18.
Groundwater Availability

Groundwater level
below surface (m)

43

49
55
60
67
1994

1996

Source: USGS

1998

2000

2002

2004

Year

17. Which statement is a logical conclusion that can be
drawn from information in the graph?
A. From 1993 through 2003, groundwater availability at this well has increased.
B. From 2002 through 2003, the water table has
fallen faster than from 1993 through 1994.
C. From 1993 through 1994, the water table has
fallen less than from 2002 through 2003.
D. From 1993 through 2003, groundwater availability at this well has declined.
18. What year was the groundwater level the highest?
A. 2004

C. 1996
B. 2003
D. 1993
19. What forms when calcium ions precipitate?
A. calcite
C. carbonic acid
B. acid rain
D. hydrogen ions
20. What characteristic must porous rocks have for
them to be permeable?
A. They must be above the water table.
B. Their pores must be large.
C. Their pores must be interconnected.
D. They must be below the water table.
274

Chapter 10 • Assessment

21. What conditions are required for the formation of
the spring?
A. defined areas of aeration, saturation, and an
impermeable layer
B. an aquiclude holding water above defined areas
of aeration and saturation
C. an aquiclude holding water above the main
water table, and recharged from above
D. an aquiclude defining a main water table, and
recharged from above

Constructed Response

22. Classify where the water table is located in a lake
or wetland as opposed to a region with no standing
water.
23. Identify the two features an aquifer must have to
be a source of artesian water.
24. Compare and contrast how the water table differs
between humid and arid regions.
25. Examine how the cement that binds the grains of
sedimentary rocks affects the porosity and permeability of the rock.
26. Predict how a small aquifer will be affected by
a multiyear drought.
27. Generalize whether caves are more likely to
develop in a region containing limestone bedrock
or sandstone bedrock. Justify your answer.
28. Explain why disposal of toxic waste into a
sinkhole can pose serious hazards for local drinking water.
Chapter Test glencoe.com