Chapter 32: The Physical Geography of Australia, Oceania, and Antarctica
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Transcript of Chapter 32: The Physical Geography of Australia, Oceania, and Antarctica
WHY ITrsquoS IMPORTANTmdash
Vast and sparsely populated the region
of Australia Oceania and Antarctica is
perhaps the most diverse of the worldrsquos
regions Parts of the regionmdashAustralia
and Oceaniamdashare developing close eco-
nomic ties to other countries in the
Pacific Rim the area bordering the
Pacific Ocean Such ties to prosperous
Pacific Rim nations will influence global
trade and trading networks for decades
to come Cold icy Antarctica lacks a
permanent human population but the
data gathered there by scientists will
broaden your understanding of the
worldrsquos climates and resources in the
years ahead
To learn more about Australia Oceania
and Antarctica and their impact on your
world view the World Regions video
ldquoAustralia Oceania and Antarcticardquo
Australia Oceania and AntarcticaAustralia Oceania and Antarctica
World Regions Video
U N I T1111
778 U n i t 1 1
GWG-778
null
52924355
Penguins in Antarctica
NGS ONLINEwwwnationalgeographiccomeducation
4What Makes Australia Oceania andAntarctica a Region
1 Shouldering the dayrsquos catcha spear fisher in the CookIslands watches his companiontake aim The Cook Islandsspread across 850000 squaremiles (22 million sq km) ofocean Like people through-out Oceania Cook Islandersdepend on the sea for food
3
2
Both palm trees and polar ice lie within this diverse region that includes two continentsmdashAustralia and Antarcticamdashandsome 25000 islands scattered across vast expanses of the Pacific Ocean
Australia is ancient and arid Low mountains curve down its easterncoast blocking rainfall to the flat interior where scrubland and deserts
form what Australians call the ldquooutbackrdquoAcross theTasman Sea lies New Zealandmdashlush green and moun-tainous North of New Zealandrsquos rugged shores liesthe rest of Oceania where groups of tropical islandsdot the blue ocean waters like tiny jewels
A different sort of jewel lies far to the south ofNew ZealandmdashAntarctica a glittering kingdom of iceand snow that sits astride the bottom of the world
1
U N I TREGIONAL ATLAS11
780 U n i t 1 1
GWG-780
null
56686073
A loaf-shaped mass of sand-stone Uluru (also known asAyers Rock) looms over the flatlandscape of central AustraliaUluru is sacred to Aboriginesthe countryrsquos native inhabi-tants Aborigines share theirhomeland with Australiarsquos othernativesmdashkangaroos and otheranimals found nowhere else onEarth
A sea of sheep parts for twobicyclists on New ZealandrsquosSouth Island Sheep greatlyoutnumber people in NewZealand where pastures thrivein a climate that is mild year-round The nation ranks as one of the worldrsquos leading producers of lamb mutton and wool
Fringed with coral reefs thethickly forested islands of Palauseem to float on the surface ofblue Pacific waters Palau is achain of about 200 islands afew hundred miles east of thePhilippines Its coral reefs areamong the worldrsquos most bio-logically diverse
2 3 4
4
U n i t 1 1 781
Lands Down Under
Europeans were latecomers to this region much ofwhich lies ldquodown underrdquo the Equator Australiarsquos origi-nal settlers were Aborigines the first settlers of NewZealand were the Maori During the 1800s the Britishcolonized both landsTodayAustralia and the islands
of Oceania are a blend ofEuropean traditional Pacific andAsian culturesAntarctica has nopermanent human inhabitants
Although huge livestock ranchesspread across Australia and NewZealand life in these two countriesis largely urban with most peopleliving in coastal cities For manyPacific Islanders life is more tradi-tional and people support them-selves mainly through fishing andsubsistence farming
A blend of cultures is reflectedby an Aborigine wearing west-ern-style clothing Aboriginesare thought to have arrived inAustralia from Asia at least40000 years ago Today manyAborigines are striving to pre-serve their ancient traditionswhile living in a modern world
1
1 2
3
U N I TREGIONAL ATLAS11
782 U n i t 1 1
GWG-782
null
47595253
Mirrored in the waters ofSydney Harbor the SydneyOpera House glows as eveningfalls The white shells that formthe buildingrsquos roof resemble bil-lowing sailsmdasha fitting tribute tothe city that is Australiarsquosbusiest seaport
Thatched houses called fale sit beneath palm trees on anisland in Samoa Open sidesallow cool ocean breezes toblow through the housesBlinds made of palm leavescan be let down to keep outrain or glaring sun
Bundled against the coldscientists in Antarctica loadequipment into a waiting heli-copter Antarctica is a continentreserved almost entirely for scientific research and explora-tion The United States is one of many countries operatingresearch stations here
2 3 4
4
U n i t 1 1 783
U N I TREGIONAL ATLAS11 Australia Oceania and Antarctica
PHYSICAL
140degE120degE
30degN
20degN
10degN
0deg
10degS
20degS
30degS
40degS
50degS
60degS
70degS
160degE 160degW 140degW 120degW180deg
TROPIC OF CANCER
TROPIC OF CAPRICORN
EQUATOR
P a c i f i c O c e a n
I n d i a n
O c e a n
Coral
Sea
TasmanSea
Arafura
Sea
Timor Sea Ba
rrierR
eef
Grea
t
LakeEyre
MurrayR
Dar
ling
R
SouthIsland
NorthIsland
Great SandyDesert
GreatVictoriaDesert
MacdonnellRanges
Tasmania
GREAT
DIVI
DING
RANGE
GibsonDesert
NullarborPlain
ArnhemLand
GreatArtesian
Basin
SouthernAlps
CapeYork
Peninsula
NewGuinea
NewBritain
Guam
Bougainville
Hawaiian Is
Fiji Is
Phoenix Is
Gilbert Is
Samoa Is
Tahiti
SolomonIslands
NewCaledonia
M I C R O N E S I AM E L A N E S I A P O L Y NE
SI
A
Caroline Is
LineIslands
Tuamotu Arch
Pitcairn I
NEW
ZEALAND
AUSTRALIA
CHINA
Mt Cook12316 ft
(3754 m)
INT
ER
NA
TIO
NA
L D
AT
E L
INE
N
Miller Cylindrical projection1500
15000
0
mi
km
Elevation Profile
2000 m
4000 m
6000 m
8000 m
6562 ft
13123 ft
19685 ft
26247 ft
Sea level
0 mi
0 km 500
500
GREATARTESIANBASIN
GIBSONDESERT
MACDONNELLRANGES CORAL
SEA
INDIANOCEAN
60degW
40degW
20degW 20degE
40degE
60degE
80degE
80degS
70degS
60degS
0deg
80degW
100degW
120degW
160degE
140degE
120degE
100degE
180deg
160deg
W140deg
W
ANTARC
TIC
CIR
CLE
EASTANTARCTICA
WESTANTARCTICA
ROSS ICESHELF
RONNE ICESHELF
ANTARCTICPENINSULA
EnderbyLand
ELLSWORTHLAND
QUEEN MAUD LAND
LAND
MARIE BYRD
TRANSANTARCTIC
MOUN
TAINS
WI L
KE
S
LA
ND
WeddellSea
Ross Sea
SouthPole
1000
10000
0
mi
kmLambert Azimuthal Equal-Area projection784
U n i t 1 1 785U n i t 1 1 785
POLITICAL
140degE120degE
30degN
20degN
10degN
0deg
10degS
20degS
30degS
40degS
50degS
60degS
160degE 160degW 140degW180deg
INT
ER
NA
TIO
NA
L D
AT
E L
INE
TROPIC OF CANCER
TROPIC OF CAPRICORN
EQUATOR
P a c i f i c O c e a n
I n d i a n
O c e a n
Coral
Sea
ArafuraSeaTimor
Sea
TasmanSea
US
US
NZ
NZ
NZ
Fr
FrFr
US
US
UK
SouthIsland
NorthIsland
Great SandyDesert
Tasmania
GreatD
ividin
gR
ange
HAWAII
GUAM
COOKISLANDS
FRENCHPOLYNESIA
PITCAIRN I
NEWCALEDONIA
NIUE
WALLIS ampFUTUNA
AMERICAN SAMOA
NORTHERNMARIANA IS
TOKELAU
Koror
PortMoresby
PalikirMajuro
Tarawa
Yaren
Honiara
Funafuti
Port-Vila Suva
Apia
Wellington
Christchurch
AucklandMelbourne
SydneyPerth
Brisbane
Canberra
Nuku alofa
rsquo
NEW
ZEALAND
A U S T R A L I A
PAPUA
NEW GUINEA
FEDERATED STATES
OF MICRONESIA
MARSHALL
ISLANDS
PHILIPPINES
CHINA
K I R I B A T I
I N D O N E S I A
TUVALU
NAURUSAMOA
VANUATU
TONGAFIJI
ISLANDS
SOLOMONISLANDS
PALAU
N
Miller Cylindrical projection1500
15000
0
mi
km
1 Which rivers drain the eastern partof Australia
2 Which countries claim parts ofAntarctica
StudyMAP
National capitalMajor city
60degW
40degW
20degW 20degE
40degE
80degE
60degE
0deg
80degW
100degW
120degW
140deg
W
160deg
W
160degE
140degE
120degE
100degE
180deg
70degS
80degS
ANTAR
CTICCIR
CLE
Atlantic
OCeaN
Indian
OCEaN
Pacific
OCEaN
SouthPole
A N T A R C T I C A
BRIT
ISH
CLAIM
ARGENTINE
CLA
IM
NEW ZEALAND CLAIM
NORWEGIAN CLAIM
AU
STR
ALIA
NC
LAIM
AUSTRALIANCLAIM
FRENCHCLAIM
Unclaimed
CHILEANCLAIM
Azimuthal Equal-Area projection500
5000
0
mi
km
U N I TREGIONAL ATLAS11 Australia Oceania and Antarctica
POPULATION DENSITY
N
Wellington
Christchurch
AucklandMelbourne
AdelaideSydney
Canberra
Perth
Brisbane
Darwin
PortMoresby
Suva
Noumacuteea
Hobart
140degE120degE
30degN
20degN
10degN
0deg
10degS
20degS
30degS
40degS
50degS
60degS
160degE 180deg
INT
ER
NA
TIO
NA
L
DA
TE
LIN
E
TROPIC OF CANCER
ANTARCTIC CIRCLE
TROPIC OF CAPRICORN
EQUATOR
P a c i f i c
O c e a n
I n d i a n
O c e a n
SOUTHEAST
ASIA
EAST
ASIA
A N T A R C T I C A
TimorSea
ArafuraSea
Tasman
Sea
Coral
Sea
Miller Cylindrical projection1500
15000
0
mi
km
Per sq miPer sq kmOver 100
50ndash100
25ndash50
1ndash25
Under 1
Uninhabited
Over 250
125ndash250
60ndash125
2ndash60
Under 2
Uninhabited
Cities(Statistics reflect metropolitan areas)
Over 5000000
2000000ndash5000000
1000000ndash2000000
250000ndash1000000
Under 250000
0deg
70degS
80degS
40degW 20degW 20degE 40degE
80degE
60degE
100degE
120degE
140degE160degE180deg160degW
140degW
120degW
100degW
80degW
60degW
ANTAR
CTIC
CIR
CLE
SouthPole
WeddellSea
RossSea
Atlantic
OCeaN
Indian
OCEaN
Pacific
OCEaN
A N T A R C T I C A
Lambert Azimuthal Equal-Area projection500
5000
0
mi
km786 U n i t 1 1
U n i t 1 1 787
ECONOMIC ACTIVITY
Adelaide
Melbourne
Perth
SydneyNewcastle
Brisbane
Dunedin
Christchurch
Auckland
Wellington
Canberra
Coral
Sea
TasmanSea
P a c i f i c
O c e a n
140degE120degE
30degN
20degN
10degN
0deg
10degS
20degS
30degS
40degS
50degS
60degS
160degE
160degW
160degW
140degW
180deg
INT
ER
NA
TIO
NA
L D
AT
E L
INE
TROPIC OF CANCER
TROPIC OF CAPRICORN
ANTARCTIC CIRCLE
EQUATOR
HAWAII
GUAM
COOKISLANDS
FRENCHPOLYNESIA
PITCAIRN I
NEWCALEDONIA
NIUE
WALLIS ampFUTUNA IS
AMERICAN SAMOA
NORTHERNMARIANA IS
TOKELAU
NEW
ZEALAND
A U S T R A L I A
PAPUA
NEW GUINEA
FEDERATED STATES
OF MICRONESIA
MARSHALL
ISLANDS
PHILIPPINES
CHINA
K I R I B A T I
I N D O N E S I A
TUVALU
NAURUSAMOA
VANUATU
TONGAFIJI
ISLANDS
SOLOMON
ISLANDS
PALAU
Coconuts
Coconuts
Coconuts
CoconutsCoconuts
Coconuts
Coconuts
SugarcaneSugarcane
Fruit
Fruit
Sheep
Sheep
SheepSheep
Sheep
Cattle
Cattle
WheatWheat
N
N
N
Miller Cylindrical projection
1500
15000
0
mi
km
1 What is the primary agricultural productof the Pacific islands
2 Describe the overall population densityof the region
StudyMAP
Resources
Petroleum
Uranium
Coal
Iron ore
Lead
Manganese
Nickel
Zinc
Gold
Silver
N
0deg
70degS
80degS
40degW20degW 20degE 40degE
80degE
60degE
100degE
120degE
140degE160degE180deg160degW
140degW
120degW
100degW
80degW
60degW
ANTAR
CTICCIR
CLE
SouthPole
WeddellSea
RossSea
Atlantic
OCeaN
Indian
OCEaN
Pacific
OCEaN
A N T A R C T I C A
Lambert Azimuthal Equal-Area projection500
5000
0
mi
km
Land UseCommercial farming
Subsistence farming
Livestock raising
Hunting and gathering
Forests
Manufacturing and trade
Commercial fishing
Little or no activity
Australian Dollar
USDollar
USDollar
FijiDollar
Australian Dollar
Australian Dollar
NewZealandDollar
Parliamentary Democracy
Parliamentary Democracy
Republic
Republic
Republic
Republic
Republic
199000007 per sq mi3 per sq km
2988888 sq mi7741220 sq km
100000426 per sq mi164 per sq km
900000123 per sq mi47 per sq km
100000348 per sq mi134 per sq km
100000791 per sq mi305 per sq km
100001412 per sq mi545 per sq km
400000038 per sq mi15 per sq km
270 sq mi699 sq km
7054 sq mi18270 sq km
282 sq mi730 sq km
69 sq mi179 sq km
9 sq mi23 sq km
104452 sq mi270531 sq km
English
English Local Languages
English FijianHindi
English Gilbertese
English Local Languages
Nauruan English
English
Sugar
Canberra
AUSTRALIA
Palikir
FEDERATED STATES OF MICRONESIA
Suva
KIRIBATI
Tarawa
MARSHALLISLANDS
Majuro
NAURU
Yaren
Wellington
Coal
Phosphates
FIJI
CoconutProducts
NEW ZEALAND
Foods
Machinery
Machinery
Foods
Foods
Foods
Machinery
Fish
CoconutProducts
USDollar
Kina
Tala
Parliamentary Democracy
Republic
ConstitutionalMonarchy
550000031 per sq mi12 per sq km
178703 sq mi462841 sq km
EnglishLocal Languages Gold
200000157 per sq mi61 per sq km
1097 sq mi2841 sq kmSamoan English
20000113 per sq mi44 per sq km
178 sq mi461 sq kmEnglish Palauan
PALAU
Koror
Port Moresby
SAMOA
Apia
PAPUA NEW GUINEA
CoconutProducts
Machinery
Foods
Fish Machinery
Wool
COUNTRY
AND CAPITAL
FLAG AND
LANGUAGE
POPULATION
AND DENSITYLANDMASS
MAJOR
EXPORT
MAJOR
IMPORTCURRENCY GOVERNMENT
COUNTRY PROFILES
COUNTRIES AND FLAGS NOT DRAWN TO SCALE POPULATIONS ARE ROUNDED SOURCE 2003 WORLD POPULATION DATA SHEET
FOR AN ONLINE UPDATE OF THIS INFORMATION VISIT GEOGRAPHYGLENCOECOM AND CLICK ON ldquoTEXTBOOK UPDATESrdquo
U N I TREGIONAL ATLAS11 Australia Oceania and Antarctica
788 U n i t 1 1
Solomon Islands
Dollar
Parsquoanga
AustralianDollar
Vatu
ParliamentaryDemocracy
ParliamentaryDemocracy
ConstitutionalMonarchy
Republic
100001000 per sq mi385 per sq km
10 sq mi26 sq km
20000045 per sq mi17 per sq km
4707 sq mi12191 sq km
Tuvaluan English
Bislama EnglishFrench
50000044 per sq mi17 per sq km
100000370 per sq mi143 per sq km
11158 sq mi28899 sq km
EnglishLocal Languages
Tongan English Squash290 sq mi751 sq km
Honiara
TONGA
TUVALU
Funafuti
Port-Vila
Nuku alofa
Cocoa
SOLOMON ISLANDS
VANUATU
Machinery
Foods
Foods
CoconutProducts
CoconutProducts Machinery
COUNTRY
AND CAPITAL
FLAG AND
LANGUAGE
POPULATION
AND DENSITYLANDMASS
MAJOR
EXPORT
MAJOR
IMPORTCURRENCY GOVERNMENT
POPULATIONS ARE ROUNDED SOURCE 2003 WORLD POPULATION DATA SHEETCOUNTRIES AND FLAGS NOT DRAWN TO SCALE
Aerial view of harbor and city Papeete Tahiti
U n i t 1 1 789
With their big noses round faces and cuddly teddy-bear appearance koalas areamong Australiarsquos most famous native animals If you wanted to see a koala in thewild the best place to look would be in a eucalyptus tree Koalas live in eucalyptustrees and eat almost nothing but eucalyptus leavesmdashabout three pounds (14 kg)
of leaves per dayLike the koala eucalyptus trees are native to
Australia More than 500 different kinds growthere And for hundreds of years theyrsquove beenimportant not only to koalas but to Australiarsquos people as well
Long before Europeans arrived in AustraliaAborigines used many different native plants tomake medicinesThey discovered that eucalyptusleaves contain a strong-smelling oilmdasheucalyptusoilmdashthat has powerful antiseptic or germ-fightingpropertiesThe Aborigines used the leaves to treatseveral common ailments including infectionsfevers coughs colds and fluThey prepared theleaves in various ways so that the oil could berubbed onto the skin inhaled or mixed with a liquid and swallowed
When European colonists arrived in Australiasome were quick to recognize the value ofAboriginal remedies especially those made fromparts of eucalyptus trees Eucalyptus preparations
GLOBALCONNECTION
AUSTRALIA AND THE UNITED STATES
EUCALYPTUS
Koala nibbling eucalyptus leaf
U N I TREGIONAL ATLAS11
790 U n i t 1 1
GWG-790
null
9383093
became so popular that colonists tried themfor just about every imaginable ailmentfrom headaches and rheumatism to hair lossand stomach ailments
The popularity of eucalyptus quicklyspread beyond Australiarsquos shores Eucalyptusoil was one of the first products to beexported from the young colony By thenineteenth century millions of the treesthemselves were being shipped to the farcorners of the worldYou can find eucalyptus trees growing in southernCalifornia Florida and other parts of the southern United States
Today eucalyptus oil is an important ingredient in many common medicines especially cough and cold remediesThe next time you pop a cough drop into your mouth or use a ldquovapor rubrdquo to clear a stuffy nosecheck the label Chances are good the product contains eucalyptus oil
Eucalyptus tree in the Australian outback
American cold sufferer whomight benefit from eucalyptus oil
GWG-791
null
49162636
GeoJournalAs you read this chapter imagine that youare visiting interesting and beautiful loca-tions in Australia Oceania and AntarcticaWrite journal entries using vivid details to explain why these places are appealing
Chapter Overview Visit the Glencoe WorldGeography Web site at geographyglencoecomand click on Chapter OverviewsmdashChapter 32 to preview information about the physicalgeography of the region
GWG-792
null
65828657
The Land
A Geographic ViewAustralian LandscapeThe land breathes magic Not colored scarves and playing cardsbut real magic Weepy eucalyptustrees with [curving sword]-shapedleaves Dazzling-white ghostgums Termite mounds some redand bulbous as a Henry Mooresculpture others black and delicate as the spires of a Gothiccathedral A glory of birdsmdashsulfur-crested cockatoos thatlift from trees in clouds tinybee-eaters iridescent as opals
mdashCathy Newman ldquoThe UneasyMagic of Australiarsquos Cape YorkPeninsulardquo National Geographic June 1996
On Australiarsquos northeastern coast the Cape YorkPeninsula displays a landscape of great contrasts Rain forestssavannas and wetlands form an exotic patchwork in this areaAustralia Oceania and Antarctica together form the equallydiverse South Pacific region one that covers a huge portion of theglobe In this section you will explore the regionrsquos varied physicalgeography including coastal lowlands bordering mountains andplateaus islands rising from the sea and a vast ice cap spanning acontinent
Australia A Continent and a CountryAs the only place on the earth that is both a continent and a coun-
try Australia is unique Although water surrounds Australia in thesame way as an island geographers classify it as a continent becauseof its tremendous size Located in the Southern Hemisphere its namecomes from the Latin word australis meaning ldquosouthernrdquo
Guide to ReadingConsider What You KnowYou may have seen photographs ormovies showing the dry Australian out-back or Antarcticarsquos mountainous icecap What animals do you associatewith these areas
Reading StrategyCategorizing Complete a graphicorganizer similar to the one below bydescribing the three types of islandsin Oceania
Read to Find Outbull How do mountains plateaus and
lowlands differ in Australia andNew Zealand
bull How have volcanoes and conti-nental shelves formed the islandsof Oceania
bull Why does the physical geographyof Antarctica attract scientists
Terms to Knowbull artesian well bull lagoon
bull coral bull krill
bull atoll
Places to Locatebull Australia bull Melanesia
bull Great Dividing bull Micronesia
Range bull Polynesia
bull Nullarbor Plain bull New Zealand
bull Murray River bull North Island
bull Darling River bull South Island
bull Oceania bull Antarctica
C h a p t e r 3 2 793Evening in Antarctica
Termite mound Australia
Island Description
Low Island
High Island
Continental Island
GWG-793
null
10422713
794 U n i t 1 1
Central LowlandsThe Great Dividing Range and Western Plateau
are separated by the Central Lowlands This aridexpanse of grassland and desert stretches acrossthe east central part of Australia After heavy rain-fall rivers and lakes throughout the area fill withwater but because rains are infrequent most riversand lakes remain dry much of the year In thesoutheast however the Murray River and theDarling River supply water that supports farmingA vast treasure of pressurized underground waterknown as the Great Artesian Basin lies underneaththe lowlands Although the water that gushes fromartesian wells or wells from which pressurizedwater flows to the surface is too salty for humansor crops ranchers use it to water livestock
Great Barrier ReefAlong Australiarsquos northeastern coast lies the
Great Barrier Reef This famous natural wonder isthe worldrsquos largest coral reef home to brilliantly
The region of AustraliaOceania and Antarcticais about two and a halftimes the size of the continental United States
Australian Outback The rugged Australian outback is sparsely populated
Human-Environment Interaction Why do sofew people live in the Western Plateau area
Mountains and PlateausA chain of hills and mountains known as the
Great Dividing Range interrupts Australiarsquos other-wise level landscape The peaks stretch alongAustraliarsquos eastern coast from the Cape York Penin-sula to the island of Tasmania separated from themainland long ago by the sea Most of Australiarsquosrivers begin in the range and they water the mostfertile land in the country
The Western Plateau a low expanse of flat landin central and western Australia covers almosttwo-thirds of the continent Australians call thisarea where few people live the ldquooutbackrdquo Acrossthe plateau spread the hot sands of the GreatSandy Great Victoria and Gibson Deserts Nearthe edges of the deserts a few low mountainranges and huge rock formations thrust up fromthe earth When explorer Jean-Michel Cousteauvisited the arid Western Plateau he spoke of thelandrsquos effect on those few who inhabit it
ldquo For human or nonhuman life in thevast dry sea as we were soon to witnessdemands extraordinary survival strate-gies and those who endure do so withearthy ingenuity and tenacityrdquoJean-Michel Cousteau
Cousteaursquos Australia Journey 1993
South of the Great Victoria Desert lies theNullarbor Plain The name comes from the Latinnullus arbor meaning ldquono treerdquo This dry virtuallytreeless land ends abruptly in giant cliffs Hundredsof feet below the cliffs lies the churning GreatAustralian Bight a part of the Indian Ocean
GWG-794
null
15542812
Tasman
Sea
GreatAustralian
Bight
Pacific Ocean
A U S T R A L I A
PAPUANEW GUINEA
FEDERATED STATESOF MICRONESIA
MARSHALLISLANDS
K I R I B A T I
TUVALU
NAURU
SAMOA
VANUATU
TONGAFIJI
ISLANDS
SOLOMONISLANDS
PALAU
NEWZEALAND
NorthIsland
NewGuinea
Tasmania
SouthIsland
M E L A N E S I A
M I C R ON
E
SI A
P
OL Y
NE S I A
Hawaii
Midway
WakeIsland
GUAM
COOK ISLANDS
FRENCHPOLYNESIA
Tahiti
SocietyIslands
PITCAIRN I
NewCaledonia
NIUE
WALLIS AND FUTUNA
AMERICAN SAMOA
NORTHERNMARIANA IS
Tokelau
Nullarbor Plain
G r e a tD
i vid
ing
Range
0deg
10degN
20degN
10degS
20degS
30degS
40degS
50degS
120degE 140degE 160degE 180deg 160degW
60degS
140degW
TROPIC OF CANCER
TROPIC OF CAPRICORN
EQUATOR
INT
ERN
AT
ION
AL
DA
TE
LIN
E
Miller Cylindrical projection
1500
15000 mi
0 km
N
MAP STUDY
Australia Oceania and Antarctica Physical-Political
1 Interpreting Maps Which of New Zealandrsquostwo islands has higher elevations
Find NGS online map resources wwwnationalgeographiccommaps
2 Applying Geography Skills In what part ofAustralia are most rivers found How might theirlocation affect population patterns
60degW 60degE
0deg
120degW120
degE
180deg
70degS
80degS
ANTARCT
ICC
IRC
LE
AtlanticOCeaN
IndianOCEaN
PacificOCEaN
SouthPole
Mt Erebus12448 ft(3794 m)
Vinson Massif16067 ft(4897 m)
AntarcticPen
A N T A R C T I C A
Lambert Azimuthal Equal-Area projection1000
10000 mi
0 km
National boundaryMountain peak
Feet10000500020001000
0
MetersElevations
30001500
600300
0
C h a p t e r 3 2 795
colored tropical fish and underwater creaturesBecause of its unique beauty and the habitat it provides for multitudes of creatures Australia hasdesignated the reef a national park and the UnitedNations has named it a World Heritage SiteAlthough its name suggests a single reef the GreatBarrier Reef is actually a string of more than 2500small reefs Formed from coral the limestone skele-tons of a tiny sea animal it extends 1250 miles
(2012 km) This span equals the length of the coast-line from New York City to Miami Florida
Economics
Natural ResourcesAlthough only 10 percent of Australiarsquos land
can be farmed agriculture is important to thecountry Australian farmers make effective use oftheir land and water to grow wheat barley fruit
GWG-795
null
59716347
and sugarcane In arid areas ranchers raise cattlesheep and chickens
Australia also yields rich mineral resourcesincluding one-fourth of the worldrsquos bauxitemdashtheraw material for aluminum productionmdashand mostof the worldrsquos high-quality opals Deposits of coaliron ore lead zinc gold nickel and petroleumalso make the country one of the worldrsquos majormining areas
Oceania Island LandsThousands of islands differing in size and extend-
ing across millions of square miles of the PacificOcean form the region called Oceania (OHbullsheebullAbullneebulluh) Created by colliding tectonic plates mil-lions of years ago the islands are part of the Ring ofFire named for its volcanic and earthquake activity
Island ClustersOceaniarsquos islands are classified into three clus-
ters based on location how the islands formedand the inhabitantsrsquo cultures Melanesia meaning
ldquoblack islandsrdquo lies north and east of AustraliaThe ldquolittle islandsrdquo of Micronesia extend north ofMelanesia Polynesia or ldquomany islandsrdquo spans anarea larger than either Melanesia or Micronesiaranging from Midway Island in the north to NewZealand in the south
Island TypesEarthquakes and volcanic eruptions still occur on
many high islands one of three island types inOceania The landscapes of high islands such asTahiti and many of the islands of Fiji featuremountain ranges split by valleys that fan out intocoastal plains Bodies of freshwater dot the landand the volcanic soil on high islands supportssome agriculture
Volcanoes shaped Oceaniarsquos many low islandsdifferently than they shaped the high islands Lowislands such as many of the Marshall Islands inMicronesia are ring-shaped islands known asatolls formed by the buildup of coral reefs onthe rim of submerged volcanoes Atolls encirclelagoons shallow pools of clear water and usually
796 U n i t 1 1
PacificIslands Volcanic peaks are found on high islands suchas Tahiti (left) while low islands are known as atolls (right)
Region What is the third type of island found in the region
GWG-796
null
12893768
Canterbury Plains In additionto producing grain New ZealandrsquosCanterbury Plains are economicallyimportant for the livestock they supportPlace How does the eastern coast of South Island differ from the westerncoast
rise only a few feet above sea level Low islandshave little soil and few natural resources
Continental islands are the third type formed bythe rising and folding of ancient rock from theocean floor Most of Oceaniarsquos large islands suchas New Guinea and New Caledonia fall into thiscategory Although volcanoes did not create theseislands many do have active volcanoes Coastalareas consist of plains swamps and riversBeyond the coastal areas the land rises intorugged interior mountains plateaus and steepvalleys Because of the variety of their rocks andsoil continental islands have most of Oceaniarsquosmineral deposits Their mining industries produceoil gold nickel and copper Some larger forestedislands support timber processing
New Zealand A Rugged Landscape
Located 1200 miles (1931 km) southeast of Aus-tralia New Zealandrsquos two largest islands make up99 percent of the countryrsquos landmass Both NorthIsland and South Island display sandy beachesemerald hillsides and snow-tipped mountains
North Islandrsquos northern region includes goldenbeaches ancient forests and rich soil that supportscitrus orchards A broad central plateau of volcanicstone features hot springs and several active vol-canoes Chief among them is Mount Ruapehu(ROObulluhbullPAYbullhoo) North Islandrsquos highest pointMount Ruapehu often spews molten rock Shiningfreshwater lakesmdashincluding Lake Taupo NewZealandrsquos largest lakemdashappear throughout theplateau East of the plateau a band of hills runsnorth and south Here ranchers graze sheep anddairy cattle
The towering snowy peaks of the Southern Alpsrun along South Islandrsquos western edge NewZealandrsquos earliest inhabitants the Maori named the highest peak on South Island Aorangi(owbullRAHNGbullee) which means ldquocloud piercerrdquoToday Aorangi is known as Mount Cook and risesto 12316 feet (3754 m) This high country also fea-tures sparkling lakes carved by glaciers and tum-bling rivers Lowlands called the Canterbury Plainslie on the eastern coast This land is New Zealandrsquosflattest and most fertile area Along the westerncoast pounding surf meets rugged cliffs deepfjords and coastal caves
GWG-797
null
15077786
798 U n i t 1 1
Natural ResourcesNew Zealandrsquos fertile soil perhaps its most
important resource greatly benefits the countryrsquoseconomy About 55 percent of the land supportscrops and livestock New Zealandrsquos sheep andwool products dominate exports and its forestsyield valuable timber The countryrsquos rivers anddams produce abundant hydroelectric power ful-filling about 75 percent of the countryrsquos needsNew Zealand also uses less typical means to gen-erate power geothermal energy is provided bywater heated underground by volcanoes
Warm and cold ocean currents meet in thewaters off the New Zealand coasts providing thecountry with a wide variety of fish Tuna marlinand sharks are abundant in the warmer tropicalcurrents while cod and hake a cod-like fishthrive in the cold Antarctic currents
Antarctica A White PlateauAntarctica almost twice the size of Australia
lies at the southern extreme of the earth beneath amassive ice cap Antarcticarsquos ice cap covers about98 percent of the continentrsquos landmass The ice isas much as 2 miles (32 km) thick in places andholds 70 percent of the worldrsquos freshwater
Like a jagged backbone the TransantarcticMountains extend northward across Antarcticaand the Antarctic Peninsula to within 600 miles
Student Web Activity Visit the Glencoe World GeographyWeb site at geographyglencoecom and click on Student WebActivitiesmdashChapter 32 for an activity about the Ring of Fire
(966 km) of South Americarsquos Cape Horn Themountains and the peninsula divide the continentinto two areas East of these mountains lies a highice-covered plateau Coastal mountains and val-leys near the plateaursquos edge form pathways forglaciers To the west the landmass is largely belowsea level including underwater volcanoes
Research StationsAlthough Antarctica contains mineral resources
international agreements limit activity on Antarcticato scientific research In year-round research sta-tions scientists from many countries gather fasci-nating information in this cold and barren landThey investigate weather patterns measure envi-ronmental changes and observe the sun and starsthrough an unpolluted atmosphere The coastal seaalso holds valuable resources Fishing boats fromseveral countries harvest krill a shrimplike animaleaten by some whales This plentiful protein-richfood may someday help lessen world hunger
Checking for Understanding1 Define artesian well coral atoll
lagoon krill
2 Main Ideas Create a graphic orga-nizer like the one below List thefeatures and resources for eachregion Then choose two of theregions and write a paragraphexplaining how they differ
Critical Thinking3 Predicting Consequences What
group of people would be mostaffected if Australiarsquos artesianwells dried up Why
4 Comparing and Contrasting Iden-tify similarities and differencesbetween New Zealandrsquos two mainislands and a high island such asTahiti
5 Decision Making Of the threetypes of islands found in Oceaniawhich type would you choose fora home Explain why
Analyzing Maps6 Location Study the physical-political
map on page 795 To which islandregion does Papua New Guineabelong
Australiabullbullbull
Oceaniabullbullbull
Antarcticabullbullbull
7 Effects of Location Considerthe location of Oceaniarsquosislands in relation to otherparts of the world Write a paragraph explaininghow this location mightaffect the development ofnatural resources
Applying Geography
GWG-798
null
15239761
Guide to ReadingConsider What You KnowScientists who live and work atresearch stations in Antarcticarsquosharsh climate make exciting discoveries about the earth Whymight this bleak and icy land be agood location for studying ecologybiology climatology or astronomy
Reading StrategyOrganizing As you read about theclimate and vegetation of AustraliaOceania and Antarctica complete agraphic organizer similar to the onebelow by describing each region
Read to Find Outbull How do variations in rainfall
affect Australiarsquos climate and vegetation
bull How does elevation affect climatepatterns in New Zealand
bull What vegetation survives in thecold dry Antarctic climate
Terms to Knowbull wattle
bull doldrums
bull typhoon
bull manuka
bull lichen
bull crevasse
Places to Locatebull Papua New Guinea
bull Antarctic Peninsula
Climate andVegetation
A Geographic ViewA Frozen FrontierI have grown to love this coldstrange place Such a reactionmay seem odd to those who havenever heard the sigh of ice floesjostling on the swells Alightinghere briefly like a bird of passageI have come to see this transientfrontier not as a harsh place butas a living creature that nurturesa multitude of other lives We canrsquot conquer it settle iteven own it The winter icebelongs only to itself
mdashJane Ellen Stevens ldquoExploring Antarctic Icerdquo National Geographic May 1996
Just as there is a surprising variety of life in anarea that appears to be a frozen desert there are other startling geo-graphic contrasts throughout Australia Oceania and Antarctica Inthis section you will learn about the climates and vegetation of oneof the worldrsquos most geographically diverse regions
AustraliaIn Australia climate and vegetation vary greatly from area to area
The countryrsquos climate and vegetation regions include tropical rainforests in the northeast dry desert expanses in the interior and tem-perate areas of grasslands scrub and mixed forests along the easternsouthern and southwestern coasts Differences in rainfall cause thesesignificant changes in climate and vegetation throughout Australia
Subtropical high-pressure air masses block moisture-laden PacificOcean winds from reaching the Western Plateau Australiarsquos large
C h a p t e r 3 2 799
Ice shelf Antarctica
Region Climate Vegetation
Australia
Oceania
New Zealand
Antarctica
GWG-799
null
10631681
800 U n i t 1 1
interior desert area The sun scorches the land butnight temperatures drop dramatically One trav-eler writes of the arid Western Plateau as seenfrom a railroad car
ldquo At twilight the shrieking dieselhorn scatters flights of long-beaked birdsnesting in a sparse underbrush of burrs
140degE120degE20degN
10degN
0deg
10degS
20degS
30degS
40degS
50degS
60degS
160degE
160degW
140degW180deg
TROPIC OF CAPRICORN
EQUATOR
ANTARCTIC CIRCLE
INT
ERN
AT
ION
AL
DA
TE
LIN
E
Pacific Ocean
Indian Ocean
Coral
Sea
TasmanSea
Wellington
Christchurch
Melbourne
Adelaide SydneyPerth
Brisbane
Darwin
Canberra
Port Moresby
Suva
N
Miller Cylindrical projection
1000
10000
0
mi
km
MAP STUDY
Australia Oceania and Antarctica Climate Regions
and thistles Dawn purples a line ofmesa-type flat-topped hills outlinedagainst a cloudless blue skyrdquoHugh A Mulligan ldquoThe Ghan Australiarsquos
Notoriously Lethargic Train to the OutbackrdquoThe Columbian November 11 1999
With less than 10 inches (25 cm) of rain annuallythere is not even enough vegetation for grazing
Tropical rain forestTropical savanna
SteppeDesert
Marine west coastMediterraneanHumid subtropical
TundraIce cap
Highlands(climate varieswith elevation)
Tropical Dry
Mid-Latitude High Latitude
1 Interpreting Maps What types of climatecharacterize the eastern coast of Australia
Find NGS online map resources wwwnationalgeographiccommaps
2 Applying Geography Skills Why does PortMoresby have a warmer climate than Wellington
60degW
40degW
20degW
20degE
40degE
80degE
60degE
0deg
80degW
100degW
120degW 140deg
W
160degW
160degE
140degE
120degE
100degE
180deg
70degS
80degS
ANTARCTICCIRC
LE
PaCIFIC
OCeaN
ATLaNTIC
OCEaN
INDIaN
OCEaN
SouthPole
A N T A R C T I C A
Lambert Azimuthal Equal-Area projection1000
10000
0
mi
km
GWG-800
null
52401894
C h a p t e r 3 2 801
An area of milder steppe climate encirclesAustraliarsquos desert region Here more regular rainfallbrings vegetation such as eucalyptus and acaciatrees and small shrubs to life Saplings of the aca-cia tree were used by early settlers to make wattlea strong interwoven wooden framework used forbuilding homes Rains fall only during the wetseason however and the amount can vary greatlyfrom year to year Annual rainfall ranges from 10
to 20 inches (25 to 51 cm) Short grasses ideal forgrazing also grow here as do irrigated crops
Australiarsquos coastal areas have a variety of moisterclimates The humid subtropical northeastern coastaverages more than 20 inches (51 cm) of rainyearly Less rain falls in the Mediterranean climateof the southern coasts and in the marine west coastclimate along the southeastern coast Coastal areassupport most of Australiarsquos agriculture
Perth
Sydney
Brisbane
Christchurch
Wellington
Canberra
PortMoresby
Darwin
Adelaide
Melbourne
Suva
140degE120degE20degN
10degN
0deg
10degS
20degS
30degS
40degS
50degS
60degS
160degE 160degW 140degW180deg
TROPIC OF CAPRICORN
ANTARCTIC CIRCLE
EQUATOR
INT
ERN
AT
ION
AL
DA
TE
LIN
E
Pacific Ocean
Indian Ocean
Coral
Sea
TasmanSea
N
Miller Cylindrical projection
1500
15000
0
mi
km
MAP STUDY
Australia Oceania and Antarctica Natural Vegetation
1 Interpreting Maps What type of vegetation isfound in western Australia
Find NGS online map resources wwwnationalgeographiccommaps
2 Applying Geography Skills What physicalprocesses might affect patterns of economicconditions in southeastern Australia
60degW
40degW
20degW
20degE
40degE
60degE
80degE
0deg
80degW
100degW
120degW 140deg
W
160degW
160degE
140degE
120degE
100degE
180deg
70degS
80degS
ANTARCTICCIRC
LE
PaCIFIC
OCeaN
ATLaNTIC
OCEaN
INDIaN
OCEaN
SouthPole
A N T A R C T I C A
Lambert Azimuthal Equal-Area projection1000
10000
0
mi
km
Tropical forest
Chaparral
Deciduous and mixeddeciduous-coniferous forest
Tropical grassland
Temperate grassland
Desert scrub and desert waste
Tundra
Ice cap
GWG-801
null
603433
802 U n i t 1 1
OceaniaBecause much of Oceania lies between the Equa-
tor and the Tropic of Capricorn most islands havea tropical rain forest climate Most days are warmthroughout the year ranging from 70degF (21degC) to80degF (27degC) though Pacific ocean winds cool atollsand the windward sides of higher islands Somemountainous areas of Papua New Guinea evenremain snow-covered year-round
Seasons throughout most of Oceania alternatebetween wet and dry The dry season features thecloudless blue skies often seen in travel advertise-ments but the wet season brings constant rain andhigh humidity The amount of rainfall varies fromisland to island Low islands get little rainfall butthe larger landmasses of high islands give offwarm moisture-laden air When this air rises andmixes with cool ocean breezes heavy rains fallSome high islands receive as much as 150 inches(381 cm) annually
Only shrubs and grasses grow on dry lowislands but coconut palms and other trees appear
on islands with more rain-fall Hot steamy rain foreststhrive where heavy rainsdrench island interiors A gen-erally windless area called thedoldrums occupies a narrow
band near the Equator where opposing ocean cur-rents meet The eerie calm within the doldrumscan change to violent storms called typhoonsTheir forceful winds and heavy rain devastateland and vegetation and threaten lives
New ZealandA marine west coast climate is found in most of
New Zealand Ocean winds warm the land in win-ter and cool it in summer preventing temperatureextremes Temperatures hover between 65degF (18degC)and 85degF (29degC) in summer and between 35degF(2degC) and 55degF (13degC) in winter Abundant sun-shine graces New Zealandrsquos beaches and inlandlandscape but clashing air masses may bring sud-den clouds and rain
Geographic differences also cause climaticvariations North Islandrsquos central plateau iswarm and sunny during summer but mountain-tops may have snow year-round Fierce winds orblizzards may strike these mountains at any time
A Diverse Region A ranchingstation in the Australian steppe (left) a tropical forest and island beach inPolynesia (middle) and a farm in the marine west coast climate of NewZealand (right) are just a sampling of the diverse landscapes of the region
Place What kind of climate is found in most of New Zealand
GWG-802
null
1458141
Checking for Understanding1 Define wattle doldrums typhoon
manuka lichen crevasse
2 Main Ideas Create a Venn diagramlike the one below Fill in the climate factors for each locationputting those factors that bothplaces have in common in the area where the circles overlap
Critical Thinking3 Making Inferences What type
of climate does most of NewZealand have Why might it appeal to settlers
4 Problem Solving What problemsmight researchers encounter inAntarctica and how could theseconditions be overcome
5 Identifying Cause and Effect Howdo Pacific ocean currents andwinds affect the climate of Ocea-nia How do they affect vegetation
Analyzing Maps6 Human-Environment Interaction
Study the vegetation map on page801 What type of vegetation issuitable for raising livestock andwhere in Australia is it found
7 Understanding ClimateMaps Note the climateregions on the map onpage 800 Write a para-graph explaining how cli-mate relates to the wayfarmers operate in NewZealand and Australia
Applying Geography
of year Mountainous areas exposed to westernwinds generally have more rainfall than do otherareas Although the country as a whole averages25 to 60 inches (64 to 152 cm) of rain annually theSouthern Alps on South Island have an averageannual rainfall of 315 inches (800 cm) Humiditylevels in inland areas are about 10 percent lowerthan coastal areas Maurice Shadbolt a populartravel writer describes New Zealand as a ldquolonglean land fated to fickle weatherrdquo In fact he saysldquoAt its most temperamental New Zealand canoffer the traveller all four seasons in one dayrdquo
New Zealandrsquos geographic isolation gives riseto unique plant life Almost 90 percent of thecountryrsquos indigenous plants are native onlyto New Zealand Manuka a small shrub carpetsland where prehistoric volcanic eruptionsdestroyed ancient forests Early settlers fromGreat Britain cut down almost all of the pinelikekauri trees but some still grow among thrivingevergreen forests In an effort to repair severe ero-sion damage in deforested areas New Zealandrsquosforest service has imported several tree speciesfrom Europe and North America A species ofpine tree native to California in the United Statesfor example now grows in large areas of the vol-canic plateau of North Island Willows andpoplars from Europe also help keep soil on hill-sides from eroding
AntarcticaAntarctica is the earthrsquos highest driest windiest
and coldest continent Though very cold year-round Antarcticarsquos climate exhibits some variationAir loses moisture as it rises over Antarcticarsquosplateau making the plateau drier than Australiarsquosdeserts but much colder Temperatures may plungeas low as ndash129degF (ndash89degC) in winter The AntarcticPlateau descends to coastal areas that have a mildermoister climate Annual snowfall averages no morethan 2 inches (5 cm) inland but along the coast itoften measures 24 inches (61 cm)
Despite the severe climate some species ofmosses and algae have adapted well to life onAntarctica In rocky areas along the coasts tinysturdy plants called lichens thrive Of the approxi-mately 800 plant species in Antarctica about 350 arelichens These plants survive by remaining dormantfor long periods and almost instantly beginning tophotosynthesize during brief periods of milderweather The continentrsquos only two flowering plantsgrow in a small area on the Antarctic Peninsulathat lies in a tundra climate zone Summer temper-atures there may reach almost 60degF (16degC)
Although frozen Antarcticarsquos ice is not motion-less The caprsquos tremendous weight causes the frozenmass to spread toward the coasts As it moves theice breaks into pieces causing huge crevasses orcracks as much as 100 feet (30 m) wide
C h a p t e r 3 2 803
Australia Both New Zealand
Comparing Climates
GWG-803
null
18792761
Learning the SkillWhen you hear about a coun-
try or an event in news reports orread about it in magazines andbooks you may still have ques-tions afterward Most sources donot contain all the informationon a subject but they may offerenough information for you toinfer or figure out the answersto your questions
Different sources presentinformation in different formsStatistical charts for exampleoften compare informationfrom which you might infer dif-ferences similarities or trendsover time These steps will helpyou make inferences from achart
bull Read the title and otherlabels to know what infor-mation the chart presents
bull Determine whether the chartprovides detailed informa-tion about one topic com-pares two or more topics or shows changes over time Some charts may giveseveral different types ofinformation
bull Make a list of the informationthat is not given in the chartor the questions that arisefrom it
bull Infer answers to your ques-tions Make logical inferencesbased on the facts given
Practicing the SkillA tourist traveling to the
Solomon Islands might use achart to learn about the countryAnswer the following questionsby making inferences about theSolomon Islands from the infor-mation in the chart above
1 Given the information in thischart is it more likely thatthe form of government inthe Solomon Islands is a par-liamentary democracy or acommunist state Explain
2 What can you infer about thehealth of the people in theSolomon Islands Explain
3 What can you infer aboutthe animal life on theSolomon Islands Explain
4 What sorts of activities might a tourist enjoy in theSolomon Islands Explain
Making InferencesYou see a police car stopped behind another car by the road-
side The emergency lights are flashing on the police car Youinfer or conclude that the driver was speeding based on the in-formation you already have from similar circumstances Makingan inference means using information to draw a conclusion
804 U n i t 1 1
Locate a chart with informationabout another country in thisregion from a newspaper maga-zine or Web site Use the steps tomake inferences from the facts pre-sented Draft several questionsbased on your inferences Exchangecharts with another student andcomplete each otherrsquos questions
The Glencoe Skillbuilder Interactive Workbook
Level 2 provides instruction andpractice in key social studies skills
Solomon Islands
Population 500000
Government Under British rule from 1893 to 1978 when it gainedindependence member of the Commonwealth of Nations
Capital Honiara
Languages 120 indigenous languages English
Land About 900 islands scattered over approximately 11000square miles (28900 sq km) of ocean
Geography Mountainous volcanic islands and small atolls coral reefs
Climate Tropical
Rainfall Ranges from 120 to 140 inches (305 to 356 cm) annually
Temperature Ranges from 70deg to 90degF (21deg to 32degC)
Vegetation Tropical forests on main islands
Exports Fish timber cocoa
Life Expectancy 67 years
Sources National Geographic Atlas of the World 7th edition 2001 World Population Data Sheet
GWG-804
null
13562537
C h a p t e r 3 2 805
Key Pointsbull Australia both a country and a continent
encompasses mountains central lowlands andexpansive deserts Rich mineral deposits andproductive farms and ranches contribute to theAustralian economy
bull Oceaniarsquos thousands of islands extend across thesouthern Pacific Ocean The islands of Oceaniawere formed either directly or indirectly by volcanic activity
bull New Zealandrsquos main features are two largeislands with mountain ranges rivers and lakesThe country boasts rich soil and timberland
bull Antarctica is an ice-covered continent WhileAntarctica may have important mineralresources its key resource is the information it offers to scientists
Organizing Your NotesUse a chart like the one belowto help you organize informa-tion about the physical featuresand resources of Australia Oceania and Antarctica
Terms to Knowbull wattlebull doldrumsbull typhoonbull manukabull lichenbull crevasse
Key Pointsbull Australia generally has a hot dry climate Along
the edges of the vast interior desert the steppereceives sufficient rainfall for raising livestockOnly the coastal climates provide enough rainfallfor growing crops without irrigation
bull Oceania enjoys a warm moist tropical climateMost islands have wet and dry seasons Theamount of rain during the wet season deter-mines whether shrubs and grasses or dense rain forests will grow
bull New Zealandrsquos marine west coast climate pro-vides year-round rainfall with temperaturesthat vary without being extreme
bull Antarcticarsquos extremely cold and windy climatesupports primarily lichens and mosses
Organizing Your NotesUse an outline like the onebelow to help you organize theinformation in this section aboutclimate and vegetation
Terms to Knowbull artesian wellbull coralbull atollbull lagoonbull krill
SECTION 1 The Land (pp 793ndash798)
SECTION 2 Climate and Vegetation (pp 799ndash803)
SUMMARY amp STUDY GUIDE
Geographic Natural Features Resources
AustraliaOceaniaNew ZealandAntarctica
I AustraliaA Mountains and PlateausB Central Lowlands
II Oceania
Climate and Vegetation
Critical Thinking1 Making Inferences Based on the infor-
mation in Section 1 would you infer thatAustralia does or does not have an even dis-tribution of population across the continent
2 Comparing and Contrasting How areOceaniarsquos islands similar Different
3 Identifying Cause and Effect Create achart like the one below and fill in the effectsof different climates on vegetation Thenchoose one effect and write a paragraphdescribing its possible economic impact
ASSESSMENT amp ACTIVITIES
806 U n i t 1 1
New Australia Oceania Zealand Antarctica
ClimateVegetation
Reviewing Key TermsWrite the letter of the key term that best matcheseach definition below
a artesian well f doldrums
b coral g typhoon
c atoll h manuka
d lagoon i lichen
e krill j crevasse
1 limestone skeletons of a tiny sea animal
2 windless area near the Equator
3 shrimplike animal
4 small sturdy plants
5 well from which pressurizedwater flows to the surface
6 huge crack in an ice cap
7 small shrub that grows in NewZealand
8 pool of water inside an atoll
9 violent Pacific Ocean storm
10 low ring-shaped island
Reviewing FactsSECTION 1
1 What formation lies just off Australiarsquos northeastern coast
2 Name the three types of islandsthat are found in Oceania
3 What is New Zealandrsquos mainnatural resource
4 List the local resources thathelp to meet New Zealandrsquosenergy needs
SECTION 25 What climate supports most of
Australiarsquos agricultural lands
6 Describe the factor that pre-vents temperature extremes inNew Zealand
7 What causes the motion of theAntarctic ice cap
Locating PlacesAustralia and New ZealandPhysical-Political Geography
Match the letters on the map with the places and physical features of
Australia and New Zealand Write your answers on a sheet of paper
1 Great Barrier Reef2 Great Victoria
Desert 3 Great Dividing Range
4 Tasmania 5 Cape York Peninsula 6 Great Australian
Bight
7 Coral Sea8 Lake Eyre 9 North Island
10 South Island
140degE 150degE120degE 130degE
0deg
10degS
20degS
30degS
40degS
160degE 170degE
TROPIC OF CAPRICORN
EQUATOR
A
C
EF
GJ
H
I
D
B
N
Miller Cylindrical projection1500
15000
0
mi
km
C h a p t e r X 807
Read the chart and become familiar with the information it contains beforeyou answer the questions Do not how-
ever study the chart in depth The quickest way toanswer both question 1 and question 2 is to readthrough each answer choice and use the process ofelimination to get rid of those that you think are wrong
Using the Regional AtlasRefer to the Regional Atlas on pages 784ndash787
1 Location Which Australian city is locatedon the coast just south of the Great BarrierReef
2 Location In which part of Australia aremost of the coal deposits found
Thinking Like a GeographerThink about the activities of explorers scientistsand tourists in Antarctica What changes toAntarcticarsquos physical geography might happen asa result As a geographer what safeguardswould you suggest to preserve this unspoiledenvironment
Problem-Solving ActivityContemporary Issues Case Study Use printand nonprint resources to learn more aboutkrill Investigate how these tiny crustaceans fitinto the food chain in the waters surroundingAntarctica Find out about issues related to har-vesting krill commercially as well as its potentialfor reducing world hunger Write a brief reportof your findings and give recommendations forusing krill responsibly
GeoJournalTravel Brochure Imagine that you are a travelwriter and draft a brochure about one locationyou wrote about in your GeoJournal Includevivid details and information about the land-forms climate and vegetation of the locationyou choose Use your textbook and the Internetto make the brochure lively and interesting
Technology ActivityUsing the Internet for Research
Search the Internet for photographs and infor-mation about plants mentioned in Section 2such as acacia and manuka Look for detailsabout their habitats and their uses Create a dis-play of the information and images and sharethe finished product with your class
Standardized Test Practice
Use the chart below to choose the best answerfor each of the following multiple-choice questions If you have trouble answering thequestions use the process of elimination tonarrow your choices
1 If tourists were traveling to Australia inJanuary and wanted to avoid both exces-sive heat and heavy rainfall to whichcity should they travel
A Melbourne C DarwinB Brisbane D Sydney
2 What information in the chart shows thatthe Australian cities are in the SouthernHemisphere
F Julyrsquos temperatures are higher than Januaryrsquos
G Januaryrsquos temperatures are higher thanJulyrsquos
H The cities have abundant rainJ The cities have a dry season
C h a p t e r 3 2 807
0
5
10
15
20
25
30
Average Yearly AveragePrecipitation Temperature Range
Australian City (inches) January (degF) July (degF)
Alice Springs 10ndash20 75degndash85deg 45degndash55degBrisbane over 30 75degndash85deg 55degndash65degDarwin over 30 75degndash85deg over 75deg
Melbourne 20ndash30 65degndash75deg 45degndash55degPerth over 30 75degndash85deg 45degndash55deg
Sydney over 30 65degndash75deg 45degndash55deg
Self-Check Quiz Visit the Glencoe WorldGeography Web site at geographyglencoecomand click on Self-Check QuizzesmdashChapter 32 toprepare for the Chapter Test
Air in Motion
Winds are hori-zontal air
movements caused bytemperature differencesamong air massesSurface winds are usu-ally strongest duringthe day when the sunheats the ground Theincreased ground tem-perature causes the airto spread out becomelighter and rise Asthin air rises cold airmoves down to takeits place This move-ment of air is the windblowing Winds usually
but not always become gentler at night Wind pat-terns have a significant impact on an arearsquos climateand they are often themselves affected by localweather patterns and conditions People generallyidentify winds based on the direction from whichthey blow
Tropical storms are created when an area of lowatmospheric pressure is surrounded by circulatingwinds Twenty to twenty-five typhoons blast acrossthe Pacific Ocean each year The word typhooncomes from the Chinese word tai-fung whichmeans ldquogreat windrdquo These storms which are calledtropical cyclones or hurricanes in other parts of theworld have spiraling winds that reach 100 to 150miles per hour (161 to 241 km per hour)
Materialsbull Drinking strawbull Scissorsbull Thin stiff plastic for the arrowhead and tail
5 78 in times 5 78 in (15 cm times 15 cm)bull Clear tapebull Straight pinbull Wood block 2 in times 2 in times 17 34 in
(5 cm times 5 cm times 45 cm)bull Hammerbull Metal washerbull Photocopy of Figure 1mdashCompassbull Photocopy of Figure 2mdashData chart
ProceduresIn this activity you will build and use a windvane to see how local changes in wind direc-tion are related to local weather changes
1 To construct the arrow make two small slitsin each end of the drinking straw The slits at the arrow end should be 1 18inches (3 cm)long The slits at the tail end should be2 inches (5 cm) long Make sure the slitsalign with each other
2 Cut a small arrowhead and a large tail out of the plastic Insert the arrowhead and thetail into the strawrsquos slits and secure themwith a small amount of tape
3 Balance the straw on your finger NOTE The balancing point may not be inthe center of the straw When you find thispoint poke the straight pin through thestraw Enlarge the hole slightly
808 U n i t 1 1
Large tropical storms canbe seen from space
C h a p t e r 3 2 809
Figure 1
Meteorologists use technology tomonitor tropical storms and issue warnings thatcan save lives and property Specialists scansatellite photographs for thunderstorm clustersThey reexamine cluster images hourly for signsof rotating winds If these conditions developtropical storm warnings go out to people onships on aircraft and along coastlines
4 Photocopy Figure 1 (the compass)and tape it to the top of the woodblock Using the hammer gentlydrive the pin through the metalwasher and into the center of thecompass
5 Take the wind vane outside to anopen area
6 Hold the wind vane so that the Non the block points north The windvanersquos arrow will point into the windUse the compass to determine thedirection from which the wind is blowing This is the wind direction
7 Photocopy or draw Figure 2 (the datachart) and record the wind directionthree times a day for five days
1 Why do you think the arrow of a wind
vane points into the wind
2 In which direction did your arrow point
most often
3 According to your results how often does
the wind direction change in your area
4 Drawing Conclusions Weather stations
take wind direction readings from the
tops of tall buildings or high poles Why
do you think this is so
Lab Report
Find Out MoreIn addition to measuring wind direction youcan measure wind speed Use nylon thread toattach a table tennis ball to the center of thestraight edge on a protractor In the windiestarea of the school grounds hold the protractorwith the straight edge up and level Now facethe wind The angle made by the nylon line onthe protractor will be the wind speed in degreesThe degree of wind speed converts to the fol-lowing wind speeds
10 degrees = 8 mph (13 kmh)20 degrees = 12 mph (192 kmh)30 degrees = 15 mph (24 kmh)40 degrees = 179 mph (288 kmh)50 degrees = 209 mph (336 kmh)60 degrees = 258 mph (416 kmh)70 degrees = 328 mph (528 kmh)
Figure 2
N
NW NE
W E
SW SE
S
Date Time Wind Direction123123123123123
- Glencoe World Geography
-
- Table of Contents
-
- Geography Skills for Life
- Reading for Information
- National Geographic Reference Atlas
-
- World Physical
- World Political
- United States Physical
- United States Political
- Canada PhysicalPolitical
- Middle America PhysicalPolitical
- North America Physical
- North America Political
- South America Physical
- South America Political
- Africa Physical
- Africa Political
- Europe Physical
- Europe Political
- Asia Physical
- Asia Political
- Oceania PhysicalPolitical
- Pacific Rim PhysicalPolitical
- Ocean Floor
- World Land Use
- World Gross Domestic Product Cartogram
- World Population Cartogram
- Arctic Ocean Physical
- Antarctica Physical
-
- National Geographic Geography Skills Handbook
-
- Thinking Like a Geographer
- From Globes to Maps
- Common Map Projections
- Reading a Map
- Types of Maps
- Graphs Charts and Diagrams
- Geographic Dictionary
-
- Unit 1 The World
-
- Chapter 1 How Geographers Look at the World
-
- Section 1 Exploring Geography
- Section 2 The Geographers Craft
- Chapter 1 Summary amp Study Guide
- Chapter 1 Assessment amp Activities
-
- Chapter 2 The Earth
-
- Section 1 Planet Earth
- Section 2 Forces of Change
- National Geographic Viewpoint A Global Concern Invasive Species
- Section 3 Earths Water
- Chapter 2 Summary amp Study Guide
- Chapter 2 Assessment amp Activities
-
- Chapter 3 Climates of the Earth
-
- Section 1 Earth-Sun Relationships
- Section 2 Factors Affecting Climate
- Section 3 World Climate Patterns
- Chapter 3 Summary amp Study Guide
- Chapter 3 Assessment amp Activities
-
- Chapter 4 The Human World
-
- Section 1 World Population
- Section 2 Global Cultures
- Section 3 Political and Economic Systems
- Section 4 Resources Trade and the Environment
- Chapter 4 Summary amp Study Guide
- Chapter 4 Assessment amp Activities
-
- Unit 2 The United States and Canada
-
- National Geographic Regional Atlas
-
- What Makes the United States and Canada a Region
- Country Profiles
- Global Connection Ice Hockey
-
- Chapter 5 The Physical Geography of the United States and Canada
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 5 Summary amp Study Guide
- Chapter 5 Assessment amp Activities
-
- Chapter 6 The Cultural Geography of the United States and Canada
-
- Section 1 Population Patterns
- National Geographic Geography and History Give-and-Take Across the Border
- Section 2 History and Government
- Section 3 Cultures and Lifestyles
- Chapter 6 Summary amp Study Guide
- Chapter 6 Assessment amp Activities
-
- Chapter 7 The United States and Canada Today
-
- Section 1 Living in the United States and Canada
- Section 2 People and Their Environment
- National Geographic Viewpoint United Statess Wetlands Under Siege
- Chapter 7 Summary amp Study Guide
- Chapter 7 Assessment amp Activities
-
- Unit 3 Latin America
-
- National Geographic Regional Atlas
-
- What Makes Latin America a Region
- Country Profiles
- Global Connection Food Crops
-
- Chapter 8 The Physical Geography of Latin America
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 8 Summary amp Study Guide
- Chapter 8 Assessment amp Activities
-
- Chapter 9 The Cultural Geography of Latin America
-
- Section 1 Population Patterns
- National Geographic Geography and History Passage Through Panama
- Section 2 History and Government
- Section 3 Cultures and Lifestyles
- Chapter 9 Summary amp Study Guide
- Chapter 9 Assessment amp Activities
-
- Chapter 10 Latin America Today
-
- Section 1 Living in Latin America
- Section 2 People and Their Environment
- National Geographic Viewpoint Brazils Rain Forests Biodiversity at Risk
- Chapter 10 Summary amp Study Guide
- Chapter 10 Assessment amp Activities
-
- Unit 4 Europe
-
- National Geographic Regional Atlas
-
- What Makes Europe a Region
- Country Profiles
- Global Connection Architecture
-
- Chapter 11 The Physical Geography of Europe
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 11 Summary amp Study Guide
- Chapter 11 Assessment amp Activities
-
- Chapter 12 The Cultural Geography of Europe
-
- Section 1 Population Patterns
- National Geographic Geography and History Yugoslavia Then and Now
- Section 2 History and Government
- Section 3 Cultures and Lifestyles
- Chapter 12 Summary amp Study Guide
- Chapter 12 Assessment amp Activities
-
- Chapter 13 Europe Today
-
- Section 1 Living in Europe
- Section 2 People and Their Environment
- National Geographic Viewpoint Germanys Forests In the Path of Acid Rain
- Chapter 13 Summary amp Study Guide
- Chapter 13 Assessment amp Activities
-
- Unit 5 Russia
-
- National Geographic Regional Atlas
-
- What Makes Russia a Region
- Country Profiles
- Global Connection Nutcracker
-
- Chapter 14 The Physical Geography of Russia
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 14 Summary amp Study Guide
- Chapter 14 Assessment amp Activities
-
- Chapter 15 The Cultural Geography of Russia
-
- Section 1 Population Patterns
- Section 2 History and Government
- National Geographic Geography and History Russias Iron Road
- Section 3 Cultures and Lifestyles
- Chapter 15 Summary amp Study Guide
- Chapter 15 Assessment amp Activities
-
- Chapter 16 Russia Today
-
- Section 1 Living in Russia
- National Geographic Viewpoint Russias Supertrawlers Factories at Sea
- Section 2 People and Their Environment
- Chapter 16 Summary amp Study Guide
- Chapter 16 Assessment amp Activities
-
- Unit 6 North Africa Southwest Asia and Central Asia
-
- National Geographic Regional Atlas
-
- What Makes North Africa Southwest Asia and Central Asia a Region
- Country Profiles
- Global Connection Religions
-
- Chapter 17 The Physical Geography of North Africa Southwest Asia and Central Asia
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 17 Summary amp Study Guide
- Chapter 17 Assessment amp Activities
-
- Chapter 18 The Cultural Geography of North Africa Southwest Asia and Central Asia
-
- Section 1 Population Patterns
- National Geographic Geography and History Black Gold in the Persian Gulf
- Section 2 History and Government
- Section 3 Cultures and Lifestyles
- Chapter 18 Summary amp Study Guide
- Chapter 18 Assessment amp Activities
-
- Chapter 19 North Africa Southwest Asia and Central Asia Today
-
- Section 1 Living in North Africa Southwest Asia and Central Asia
- Section 2 People and Their Environment
- National Geographic Viewpoint Turkeys Atatuumlrk Dam Diverting a Rivers Flow
- Chapter 19 Summary amp Study Guide
- Chapter 19 Assessment amp Activities
-
- Unit 7 Africa South of the Sahara
-
- National Geographic Regional Atlas
-
- What Makes Africa South of the Sahara a Region
- Country Profiles
- Global Connection Roots of Jazz
-
- Chapter 20 The Physical Geography of Africa South of the Sahara
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 20 Summary amp Study Guide
- Chapter 20 Assessment amp Activities
-
- Chapter 21 The Cultural Geography of Africa South of the Sahara
-
- Section 1 Population Patterns
- Section 2 History and Government
- Section 3 Cultures and Lifestyles
- National Geographic Geography and History Conflict in Central Africa Hutu versus Tutsi
- Chapter 21 Summary amp Study Guide
- Chapter 21 Assessment amp Activities
-
- Chapter 22 Africa South of the Sahara Today
-
- Section 1 Living in Africa South of the Sahara
- Section 2 People and Their Environment
- National Geographic Viewpoint Southern Africas Dilemma Renew the Ivory Trade
- Chapter 22 Summary amp Study Guide
- Chapter 22 Assessment amp Activities
-
- Unit 8 South Asia
-
- National Geographic Regional Atlas
-
- What Makes South Asia a Region
- Country Profiles
- Global Connection Textiles
-
- Chapter 23 The Physical Geography of South Asia
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 23 Summary amp Study Guide
- Chapter 23 Assessment amp Activities
-
- Chapter 24 The Cultural Geography of South Asia
-
- Section 1 Population Patterns
- Section 2 History and Government
- National Geographic Geography and History Mountain Madness Struggle for Kashmir
- Section 3 Cultures and Lifestyles
- Chapter 24 Summary amp Study Guide
- Chapter 24 Assessment amp Activities
-
- Chapter 25 South Asia Today
-
- Section 1 Living in South Asia
- Section 2 People and Their Environment
- National Geographic Viewpoint Indias Green Revolution Success or Failure
- Chapter 25 Summary amp Study Guide
- Chapter 25 Assessment amp Activities
-
- Unit 9 East Asia
-
- National Geographic Regional Atlas
-
- What Makes East Asia a Region
- Country Profiles
- Global Connection Electronics
-
- Chapter 26 The Physical Geography of East Asia
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 26 Summary amp Study Guide
- Chapter 26 Assessment amp Activities
-
- Chapter 27 The Cultural Geography of East Asia
-
- Section 1 Population Patterns
- National Geographic Geography and History A Tale of Two Chinas
- Section 2 History and Government
- Section 3 Cultures and Lifestyles
- Chapter 27 Summary amp Study Guide
- Chapter 27 Assessment amp Activities
-
- Chapter 28 East Asia Today
-
- Section 1 Living in East Asia
- Section 2 People and Their Environment
- National Geographic Viewpoint Chinas Three Gorges Before the Flood
- Chapter 28 Summary amp Study Guide
- Chapter 28 Assessment amp Activities
-
- Unit 10 Southeast Asia
-
- National Geographic Regional Atlas
-
- What Makes Southeast Asia a Region
- Country Profiles
- Global Connection Cuisine
-
- Chapter 29 The Physical Geography of Southeast Asia
-
- Section 1 The Land
- Section 2 Climate and Vegetation
- Chapter 29 Summary amp Study Guide
- Chapter 29 Assessment amp Activities
-
- Chapter 30 The Cultural Geography of Southeast Asia
-
- Section 1 Population Patterns
- Section 2 History and Government
- National Geographic Geography and History The Long War America in Vietnam
- Section 3 Cultures and Lifestyles
- Chapter 30 Summary amp Study Guide
- Chapter 30 Assessment amp Activities
-
- Chapter 31 Southeast Asia Today
-