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Plate tectonics

Date post: 19-Jan-2016
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Plate tectonics. Mountain building and Volcanoes. Mountain building. A major force shaping the land is uplift Moving plates uplift land, forming mountains Three types of mountains are: Folded mountains Fault-block mountains Volcanic Mountains . - PowerPoint PPT Presentation
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Mountain building and Volcanoes PLATE TECTONICS
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Page 1: Plate tectonics

Mountain building and Volcanoes

PLATE TECTONICS

Page 2: Plate tectonics

A major force shaping the land is uplift

Moving plates uplift land, forming mountains

Three types of mountains are:Folded mountainsFault-block mountainsVolcanic Mountains.Each forms by a different type of plate movement.

MOUNTAIN BUILDING

Page 3: Plate tectonics

Formed when plates collide resulting in a formation of a fold or bulge, which becomes a mountain range.

Try thisPlace a sheet of paper flat on your desk. Place a hand on one edge of the paper. Push your other hand against the free edge of the paper. What happens?

Folded mountains

Page 4: Plate tectonics

Examples of folded mountains IncludeThe Rocky Mountains of North America

The Andes of South AmericaThe Alps of Central EuropeThe Himalayas of Asia

FOLDED MOUNTAINS

Page 5: Plate tectonics

HIMALAYAS

Page 6: Plate tectonics

Formed when blocks of Earth’s crust on either side of a fault are dropped below or pushed above the surrounding land

This happens where sections of crust are pulling apart or together

Fault-block mountains

Page 7: Plate tectonics

Examples of Fault-block mountains include:The Sierra Nevadas of California

Wasatch Range of UtahTeton Range of Wyoming

FAULT-BLOCK MOUNTAINS

Page 8: Plate tectonics

SIERRA NEVADAS

Page 9: Plate tectonics

Formed when material from inside Earth reaches the surface

They are most common at plates boundaries (convergent and divergent)

They are classified into three types based on how they formCinder cone volcanoesShield volcanoesComposite volcanoes (Stratovolcanoes)

VOLCANIC MOUNTAINS

(VOLCANOES)

Page 10: Plate tectonics

Cone-shaped moundFormed from cinders, ash, dust

Sudden, violent eruptionExamples:Mount Paracutin, Mexico, Isalco, and El Salvador

Cinder cone volcanoes

Page 11: Plate tectonics

CINDER CONE VOLCANOES

Page 12: Plate tectonics

CINDER CONE VOLCANO ERUPTION

Page 13: Plate tectonics

Low, gently-sloped sidesFormed from layers of cooled lava

Slow, gentle eruptionExamples:Mauna Loa, and Kea

Shield volcanoes

Page 14: Plate tectonics

SHIELD VOLCANO (ERTA ALE)

Page 15: Plate tectonics

ERTA ALE ERUPTION

Page 16: Plate tectonics

Cone-shaped mound, steep sides

Formed from alternating layers of ash and lava

Both violent and gentle eruptions

Examples:Mount St Helens, Egmont, and New Zealand

STRATOVOLCANOES

Page 17: Plate tectonics

STRATOVOLCANO

Page 18: Plate tectonics

STRATOVOLCANO ERUPTION


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