Earth’s Landmasses
Islands – small landmasses completely surrounded by water Four Major landmasses on Earth - Eurasia and Africa, North and South America, Antarctica (2x the size of the US; first known exploration occurred in 1901) , Australia (only continent that is single country; sometimes referred to as the island continent)
Continent – landmass that measures millions of square km and rises a considerable distance above sea level; each has at least one large area of very old rock exposed at its surface (this area is called a shield) Seven continents on the Earth – Asia, Africa, Europe, Australia, N and S America, and Antarctica
Topography Scientists refer to the shape of the Earth’s surface as its topography The Earth’s topography is made up of different kinds of landscapes A landscape is the physical features of the Earth’s Surface found in an area
Each type of landscape has different characteristics Elevation – height above sea level (high or low)  Relief – difference in region’s elevation
Three Main Types of Landscape Regions Mountains – natural landforms that reach high elevations  Have narrow summits or tops, and steep slopes, or sides These landscapes have very high relief All mountains did not form at the same time
Mountain Formation Fault-block Mountain – result from the folding and breaking of the Earth’s surface Volcanic Mountain – created when hot magma from the Earth’s interior breaks through the Earth’s surface Mountain Range – roughly parallel series of mountains that have the same general shape and structure
Mountain System – a group of mountain ranges in one area Mountain Belt – a larger group of mountains composed of mountain ranges and systems
Folded Mountains Formed when rock layers are squeezed from opposite sides and rock layers buckle and fold Example: The Appalachian Mountains
Unwarped Mountains Formed when rocks are pushed up by forces inside earth
Fault-Block Mountains Made of huge tilted blocks of rocks that are separated from surrounding rock by faults. Example: Sierra Nevada Mountains in California
Volcanic Mountains Begin when molten material reaches the surface through a weak area of the crust. The materials pile up, one layer on top of another, until one cone-shaped structure forms. Example: The Hawaiian Islands
Some of the World’s Famous Mountains
Aconcagua, Andes Argentina 6569 m, Highest Mountain in Western Hemisphere
Cotopaxi, Andes in Ecuador 5897 m, Highest active volcano in the world
Elbert, Colorado 4399 m, Highest mountain in Rockies
Everest, Himalayas (Nepal-Tibet border) 8848 m, Highest mountain in the world
K2, Kashmir 8611 m, 2nd highest mountain in the world
Kanchenjunga, Himalayas (Nepal-India border) 8598 m, 3 rd  highest mountain in the world
Logan, Yukon 5950 m, Highest mountain in Canada
Mauna Kea, Volcanic Island in Hawaii 4205 m, Highest Island Mountain in the world
Mauna Loa, Volcanic Island in Hawaii 4169 m
McKinley, Alaska 6194 m, Highest mountain in North America
Mitchell, North Carolina 2037 m, Highest mountain in the Appalachians
Mont Blanc, France 4807 m, Highest mountain in the Alps
Mt. St. Helens, Cascades in Washington 2549 m, Recent active volcano in the US
Pikes Peak, Colorado 4301 m, most famous in the Rocky Mountains
Rainier, Cascades in Washington 4392 m, Highest mountain in Washington
Vesuvius, Italy 1277 m, only active volcano on the mainland of Europe
Whitney, Sierra Nevada in California 4418 m, Highest mountain in California
Plains Flat land areas that do not rise far above sea level They are areas of low relief Characterized by broad rivers and streams
Coastal Plains – Low flat areas along the coasts Coast – a place where the land meets the ocean Interior Plains – low, flat areas found inland on a continent
Plateaus Broad, flat areas of land that rise more than 600 m above sea level They are not considered mountains because their surfaces are fairly flat Many plateaus of the world are dry, nearly desert areas Often used for grazing

Earth’s landmasses

  • 1.
  • 2.
    Islands – smalllandmasses completely surrounded by water Four Major landmasses on Earth - Eurasia and Africa, North and South America, Antarctica (2x the size of the US; first known exploration occurred in 1901) , Australia (only continent that is single country; sometimes referred to as the island continent)
  • 3.
    Continent – landmassthat measures millions of square km and rises a considerable distance above sea level; each has at least one large area of very old rock exposed at its surface (this area is called a shield) Seven continents on the Earth – Asia, Africa, Europe, Australia, N and S America, and Antarctica
  • 4.
    Topography Scientists referto the shape of the Earth’s surface as its topography The Earth’s topography is made up of different kinds of landscapes A landscape is the physical features of the Earth’s Surface found in an area
  • 5.
    Each type oflandscape has different characteristics Elevation – height above sea level (high or low) Relief – difference in region’s elevation
  • 6.
    Three Main Typesof Landscape Regions Mountains – natural landforms that reach high elevations Have narrow summits or tops, and steep slopes, or sides These landscapes have very high relief All mountains did not form at the same time
  • 7.
    Mountain Formation Fault-blockMountain – result from the folding and breaking of the Earth’s surface Volcanic Mountain – created when hot magma from the Earth’s interior breaks through the Earth’s surface Mountain Range – roughly parallel series of mountains that have the same general shape and structure
  • 8.
    Mountain System –a group of mountain ranges in one area Mountain Belt – a larger group of mountains composed of mountain ranges and systems
  • 9.
    Folded Mountains Formedwhen rock layers are squeezed from opposite sides and rock layers buckle and fold Example: The Appalachian Mountains
  • 10.
    Unwarped Mountains Formedwhen rocks are pushed up by forces inside earth
  • 11.
    Fault-Block Mountains Madeof huge tilted blocks of rocks that are separated from surrounding rock by faults. Example: Sierra Nevada Mountains in California
  • 12.
    Volcanic Mountains Beginwhen molten material reaches the surface through a weak area of the crust. The materials pile up, one layer on top of another, until one cone-shaped structure forms. Example: The Hawaiian Islands
  • 13.
    Some of theWorld’s Famous Mountains
  • 14.
    Aconcagua, Andes Argentina6569 m, Highest Mountain in Western Hemisphere
  • 15.
    Cotopaxi, Andes inEcuador 5897 m, Highest active volcano in the world
  • 16.
    Elbert, Colorado 4399m, Highest mountain in Rockies
  • 17.
    Everest, Himalayas (Nepal-Tibetborder) 8848 m, Highest mountain in the world
  • 18.
    K2, Kashmir 8611m, 2nd highest mountain in the world
  • 19.
    Kanchenjunga, Himalayas (Nepal-Indiaborder) 8598 m, 3 rd highest mountain in the world
  • 20.
    Logan, Yukon 5950m, Highest mountain in Canada
  • 21.
    Mauna Kea, VolcanicIsland in Hawaii 4205 m, Highest Island Mountain in the world
  • 22.
    Mauna Loa, VolcanicIsland in Hawaii 4169 m
  • 23.
    McKinley, Alaska 6194m, Highest mountain in North America
  • 24.
    Mitchell, North Carolina2037 m, Highest mountain in the Appalachians
  • 25.
    Mont Blanc, France4807 m, Highest mountain in the Alps
  • 26.
    Mt. St. Helens,Cascades in Washington 2549 m, Recent active volcano in the US
  • 27.
    Pikes Peak, Colorado4301 m, most famous in the Rocky Mountains
  • 28.
    Rainier, Cascades inWashington 4392 m, Highest mountain in Washington
  • 29.
    Vesuvius, Italy 1277m, only active volcano on the mainland of Europe
  • 30.
    Whitney, Sierra Nevadain California 4418 m, Highest mountain in California
  • 31.
    Plains Flat landareas that do not rise far above sea level They are areas of low relief Characterized by broad rivers and streams
  • 32.
    Coastal Plains –Low flat areas along the coasts Coast – a place where the land meets the ocean Interior Plains – low, flat areas found inland on a continent
  • 33.
    Plateaus Broad, flatareas of land that rise more than 600 m above sea level They are not considered mountains because their surfaces are fairly flat Many plateaus of the world are dry, nearly desert areas Often used for grazing