Convection Currents

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Created by:

OLIVIADURRETT  on January 25, 2011

Subjects:

science

Description:

A, B, C, D, and Continental Drift

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Convection Currents

A
Getting hoter.
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A Getting hoter.
A to B The molecules expand because they are less dense because they are hot and the rise.
B The magma hits the hard lithosphere and turns.
B to C The magma is cooling down.
C The molecules are becoming more dense.
C to D The pull of gravity makes the molecules sink.
D The molecules hit the hard mantel and turn again.
D to A The molecules are getting hotter.
Evidence from Landforms Continents fit together.
Evidence from Climate There were once tropical swamps in places that are now in cold climates.
Evidence from Fossils Identical fossils from organisms that could not have crossed the ocean were found on seperate continents.
Evidence from Rocks Rocks of similar type and age were found on seperate continents.
Evidence from Mountains Mountain ranges match across continents.

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