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The Earth Inside and Out
Main Ideas• The earth is the only
habitable planet in the sun’ssolar system.
• The drifting of the continentsshaped the world we live intoday.
Places & Termscontinent
solar system
core
mantle
magma
crust
atmosphere
lithosphere
hydrosphere
biosphere
continentaldrift
BA
SIC
S
A HUMAN PERSPECTIVE A quick look at a world map will convinceyou that the continents, landmasses above water on earth, fit togetherlike a huge jigsaw puzzle. South America and Africa are good examples.With imagination, you can see how other continents might fit togetheras well. The first person to suggest that the seven continents were onceall one supercontinent was Englishman Francis Bacon in 1620. Bacon’sidea received support in the early 1900s, when scientists found rocks in Africa that matched rocks in South America. Other evidence also supported the idea of a supercontinent millions of years ago.
The Solar SystemThe “home address” of the earth is the third planet in the solar systemof the sun, which is a medium-sized star on the edge of the Milky Waygalaxy. Its distance from the sun is 93 million miles. The solar systemconsists of the sun and nine known planets, as well as other celestialbodies that orbit the sun. The solar system also contains comets,spheres covered with ice and dust that leave trails of vapor as they racethrough space. Asteroids—large chunks of rocky material—are foundin space as well. As you can see in the diagram, our solar system has anasteroid belt between the orbits of Jupiter and Mars.
LOCATION This not-to-scaleillustration shows the nineplanets and other objectsin our solar system. What is the earth’s relativelocation in the solar system?
Mercury
VenusEarth
Mars
JupiterSaturn
Uranus
Neptune
Pluto
comet
Sunasteroid belt
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The Structure of the EarthThe earth is about 24,900 miles in circumference and about 7,900 milesin diameter. Although the earth seems like a solid ball, it is really morelike a series of shells that surround one another.
INSIDE THE EARTH The core is the center of the earth and is made upof iron and nickel. The outer core is liquid, but the inner core is solid.Surrounding the core is the mantle, which has several layers. The man-tle contains most of the earth’s mass. Magma, which is molten rock, canform in the mantle and rise through the crust, the thin layer of rock atthe earth’s surface. Study the diagram below to learn more about theearth’s interior.
ON AND ABOVE THE EARTH Surrounding the earth is a layer of gasescalled the atmosphere. It contains the oxygen we breathe, protects theearth from radiation and space debris, and provides the medium forweather and climate. The solid rock portion of the earth’s surface is thelithosphere, which includes the crust and uppermost mantle. Under theocean, the lithosphere forms the seafloor. The huge landmasses abovewater are called continents. There are seven continents: North America,South America, Europe, Asia, Africa, Australia, and Antarctica. Thehydrosphere is made up of the water elements on the earth, whichinclude oceans, seas, rivers, lakes, and water in the atmosphere.Together, the atmosphere, the lithosphere, and the hydrosphere formthe biosphere, the part of the earth where plants and animals live.
BackgroundPart of the upperportion of themantle is knownas the asthenos-phere. It is the hot,but still mostlysolid, rock belowthe cold, brittlerock of the lithosphere.
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Inner Core760 mile radius
Outer Core1,380 miles thick
Mantle1,800 miles thick
Crust19–37 miles thick
Lithosphere30–90 miles thick
Asthenosphere400 miles thick
Mantle
Ocean
Continent OceanicCrust
ContinentalCrust
CrustThe earth is made up of the core,the mantle, and the crust.
SKILLBUILDER: Interpreting GraphicsLOCATION Approximately how thick is the core of the earth?
LOCATION In what part of the earth would thelithosphere be found?
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The Earth Inside and Out 29
Places & TermsIdentify and explainwhere on the earththese terms would befound.
• continent
• mantle
• magma
• crust
• biosphere
MAKING COMPARISONS Study the diagrams of continental drift on this page. Write a description of the location of the continents in the past in comparison with their current location.
Taking Notes PLACE Review the notes you tookfor this section.
• What are the three basic parts ofthe earth’s interior?
• What are four basic spheresfound on or above the earth?
Main Ideas a. What makes up the
interior of the earth?
b. What makes up thebiosphere?
c. How can the presence of seven continents on the earth’s surface beexplained?
Geographic ThinkingMaking Inferences How dothe earth’s spheres influenceone another? Think about:
• the function of theatmosphere
• the makeup of thebiosphere
See SkillbuilderHandbook, page R4.
CONTINENTAL DRIFT In 1912,Alfred Wegener of Germany presented a new idea about continents—the continental drifthypothesis. It maintained that theearth was once a supercontinentthat divided and slowly driftedapart over millions of years.Wegener called the supercontinentPangaea (from a Greek word mean-ing “all earth”). An ocean calledPanthalassa surrounded it. Thesupercontinent split into manyplates that drifted, crashed intoeach other, and split apart severaltimes before they came to their cur-rent positions. This processoccurred over millions of years.
In the 1960s, scientists study-ing the sea floor discovered thatthe youngest rocks were in themiddle of the ocean, at longcracks in the crust. This suggestedthat the new sea floor was beingadded, pushing the continentsapart. Later in this chapter, youwill learn how the rocks of theearth’s surface are broken intogiant plates that move and con-tinue to shape the earth.
LivingPlanet
Earth
Inside & Out
PA
NG
AE
A
TethysSea
PANTHALASSAOCEAN
200 million y
NORTHAMERICA A S I A
AFRICASOUTH
AMERICA INDIA
AUSTRALIA
ANTARCTICA
65 m ll on years ago
AmericanPlate
PacificPlate
PacificPlate
EurasianPlate
AfricanPlate Indo-
AustralianPlate
Antarctic Plate
ANTA
ANTARCTICA
NORTHAMERICA A S I A
AFRICA
SOUTH AMERICA
AUSTRALIA
EUROPE
Today
200 million yearsago The super-continent wasnamed Pangaea.An ocean calledPanthalassasurrounded it.
65 million yearsago The super-continent split apartand began movingin different direc-tions. Notice thatIndia broke awayfrom Antarcticaand Australia anddrifted toward Asia.
Today The contin-ents continue todrift even today.
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