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Fill In: Plate Tectonics Intro

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Intro to plate tectonics.

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Âge recommandé: 11 ans
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Benjamin D Morgan
Benjamin D Morgan
United States

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Fill In: Plate Tectonics Intro

Intro to plate tectonics.

Benjamin D Morgan
1

THEORY farther volcanoes LAW ConveyorBelt young boundary RIDGE boundaries CRACK opposite CANNOT lava FLAT SeafloorSpreading divergent convergent created StraightLine transform cracked ShapeOfTheContinentCoastlines plates old two bigger

A is an explanation based on a huge amount of experimental evidence . A is NOT an explanation , but a statement that describes a scientific phenomena , but does NOT explain why it happens . A theory become a law .

They have mapped out the ocean floor . What they found is that it is not . On the bottom of the ocean they found a system . A ridge is a in the Earth . The ridge shape is not a . The ridge shape follows the . Ridges are underwater . They are not just mountains . Ridges release when they erupt .

The ocean floor is considered to be geologically . The continents are compared to the ocean floor . Ridges are pulled apart by convection currents moving in the direction from one another . At ridges seafloor is .

The you travel from a ridge the older the seafloor becomes . This is because seafloor is created at the ridge and then gets pushed out like a by the convection currents underneath the lithosphere . This process is known as .

In the Theory of Plate Tectonics the Earth is . These sections are very large . They are than the size of the continents . These sections of the cracked Earth's lithosphere are called . These cracked sections move around the planet .

The spot where the two plates meet is a crack in the Earth . Where two plates meet it is called a . Two plates that pull away from one another are called boundaries . Two plates that collide are called boundaries . And , two plates that slide past one another are called fault boundaries . Ridges occur along divergent .

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