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GERAKAN LEMPENG TEKTONIK GERAKAN LEMPENG TEKTONIK

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

A

Divergent

B

Convergent

C

Transform

•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

A

Divergent

B

Convergent

C

TransformContinental crust

rift valley

Oceanic crust mid-ocean ridge

2 continental plates mountain range

Plates move against each other

Stress builds up

Stress is released

earthquake2 oceanic plates oroceanic + continental subduction

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

GRABEN

HORST

NORMAL

REVERSED

Page 11: Gerakan Lempeng Tektonik