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GERAKAN LEMPENG TEKTONIK GERAKAN LEMPENG TEKTONIK
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Gerakan-Lempeng-Tektonik

Nov 08, 2014

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Gerakan-Lempeng-Tektonik
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Page 1: Gerakan-Lempeng-Tektonik

GERAKAN LEMPENG TEKTONIKGERAKAN LEMPENG TEKTONIKGERAKAN LEMPENG TEKTONIKGERAKAN LEMPENG TEKTONIK

Page 2: Gerakan-Lempeng-Tektonik
Page 3: Gerakan-Lempeng-Tektonik

earthquakes and plate tectonicsearthquakes and plate tectonicsearthquakes and plate tectonicsearthquakes and plate tectonics

Page 4: Gerakan-Lempeng-Tektonik

Global Earthquake PatternsGlobal Earthquake PatternsGlobal Earthquake PatternsGlobal Earthquake Patterns

Page 5: Gerakan-Lempeng-Tektonik

Where Earthquakes Occur

Page 6: Gerakan-Lempeng-Tektonik
Page 7: Gerakan-Lempeng-Tektonik

C

Transform

B

Convergent

A

Divergent

•plates are moving apart

•new crust is created

•Magma is coming to the surface

•plates are coming together

•crust is returning to the mantle

•plates are slipping past each other

•crust is not created or destroyed

Page 8: Gerakan-Lempeng-Tektonik

Plates move against each other

Stress builds up

Stress is released

earthquake

2 continental plates mountain range

Continental crust

rift valley

Oceanic crust mid-ocean ridge

C

Transform

B

Convergent

A

Divergent

2 oceanic plates oroceanic + continental subduction

Page 9: Gerakan-Lempeng-Tektonik
Page 10: Gerakan-Lempeng-Tektonik

GRABEN

HORST

NORMAL

REVERSED

Page 11: Gerakan-Lempeng-Tektonik