Clues to Plate Movements



This is a drawing of the Earth's lithosphere.
Click on image for full size version (40K GIF)

Many kinds of surface features provide evidence of a sliding lithosphere.

When two plates move apart, rising material from the mantle pushes the lithosphere aside. Two types of features can form when this happens. At mid ocean ridges, the bottom of the sea comes apart to make way for new ocean crust formed from molten rock, or magma, rising from the mantle. Continental rifts form when a continent begins to split apart (the East African Rift is an example). If a continental rift continues to split a continent apart it can eventually form an ocean basin.

When two plates move towards each other, several features can form. Often, one of the plates is forced to go down into the hot asthenosphere at a subduction zone. Volcanoes may form when a subducted plate melts and the molten rock comes to the surface. If neither plate is subducted, the two crash into each other and can form huge mountains like the Himalayas.

If these features are found on a planet's surface, they provide evidence that the planet's surface is in motion. There are only a few other planets that have a surface in motion.


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Making Earthquakes... Indoors - streaming RealVideo (1 min. 6 sec.) from NSF


Clues to Plate Movements



This is a drawing of the Earth's lithosphere.
Click on image for full size version (40K GIF)

Many kinds of surface features are clues that our lithosphere is sliding.

Two types of features can form when plates move apart. At mid ocean ridges, the bottom of the sea splits apart and new crust is formed from molten rock, or magma, rising from the mantle. Continental rifts form when a continent begins to split apart. If a continental rift continues to split a continent apart it can eventually form an ocean basin.

When two plates move towards each other, several features can form. Often, one of the plates is forced to go down into the hot asthenosphere at a subduction zone. Volcanoes may form when a subducted plate melts and the molten rock comes to the surface. If neither plate is subducted, the two crash into each other forming huge mountains.

If these features are found on a planet's surface, they provide evidence that the planet's surface is in motion. The sliding lithosphere makes Earth special because there are only a few other planets that have a surface in motion.


Return to Plate Tectonics

Return to Earth's Surface & Interior

Making Earthquakes... Indoors - streaming RealVideo (1 min. 6 sec.) from NSF


Clues to Plate Movements



This is a drawing of the Earth's lithosphere.
Click on image for full size version (40K GIF)
Many kinds of surface features are clues to a sliding lithosphere.

Two types of features can form when plates move apart. At ocean ridges, the crust splits apart to make room for molten mantle rock. Continental rifts form when a continent begins to split apart.

When two plates move towards each other, sometimes one of the plates is forced to go down into Earth’s hot interior at a subduction zone and volcanoes form nearby. Or, if neither plate is subducted, the two will crash into each other forming huge mountains.

These features are special clues that prove our planet's surface is in motion. There are only a few other planets that have clues like these.


Return to Plate Tectonics

Return to Earth's Surface & Interior

Making Earthquakes... Indoors - streaming RealVideo (1 min. 6 sec.) from NSF



Last modified March 2, 2008 by Randy Russell.
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