click below
click below
Normal Size Small Size show me how
Chapter Seven
Plate Tectonics
| Term | Definition |
|---|---|
| Pangaea | Alfred Wegenger proposed that all the continents were once part of a super continent. |
| Continental drift | Continents are in constant motion on the surface of the earth. |
| Mid ocean ridges | The mountain ranges in the middle of the ocean |
| Seafloor spreading | New oceanic crusts forms along a mid ocean range and older oceanic crusts moves away from the ridge |
| Normal polarity | magnetized objects such as compass needles, will orient themselves to point north. |
| magnetic reversal | magnetized field reverses direction |
| reversed polarity | magnetized objects would reverse direction and orient themselves to point south. |
| Plate tectonics | Earths surface is made up of rigid slabs of rock , or plates that move with respect to each other |
| lithosphere | The cold and rigid outermost rock layer |
| divergent plate boundary | forms where two plates separate |
| transform plate boundary | forms where two plates slide past each other |
| convergent plate boundary | where two plates collide. |
| subduction | the denser the plate sinks the more buoyant plate in a processs |
| convection | The circulation of material caused by difference in temperature and density. |
| ridge push | Rising mantle material at mid ocean ridges creates the potential for plates to move away from the ridge with a force |
| slab pull | as a slab sinks, it pulls the rest of the plate with a force. |