Plate Tectonics Review

Upper mantle and crust

Outer core and inner core

Asthenosphere and mantle

Crust and core

It shows the convection currents in the mantle.

It shows the convection currents in the outer core.

It shows the radiation of heat through the mantle.

It shows the conduction of heat in the mantle.

They cool the plates down

They move the plates as the core heats the asthenosphere

They create earthquakes

They form mountains

Divergent

Convergent

Transform

Atlantis

located where the plates collide

located at the place where rocks are furthest from the rift valley

Located at the center of the ridge, where oceanic crust is formed

none of the above; all the rocks would be the same age

Rift valleys form where two continental plates diverge, or move away from each other

Rift valleys form where two continental plates converge, or move toward each other

Rift valleys form where one oceanic plate subducts beneath another continental plate

Rift valleys form at transform boundaries

A place to get free wifi

A column of mantle that is hotter than the surrounding material

A tectonic plate boundary

A type of earthquake

Hawaii

Yellowstone Park

Mount St. Helens

Kilauea

The denser oceanic plate slides on top of the less dense continental plate.

The denser oceanic plate slides under the less dense continental plate.

The less dense oceanic plate slides past the denser continental plate.

The less dense oceanic plate slides under the denser continental plate.

The oceanic crust is moved upward by the radiation of heat

The oceanic crust will melt as it moves deeper in the earth.

The continental crust will form a mountain range.

The two crusts will form an ocean basin

They are formed by a plate melting at a subduction zone

They are always found in the ocean

They are only found in tropical warm regions of the planet

They form due to pressure from the atmosphere

The older plate slides under the younger plate

The younger plate slides under the older plate

Both plates move apart

Both plates remain stationary

They are the highest mountains in the world

They are located in the USA

They are formed by volcanic activity

They are primarily made of sandstone

Earthquakes

Volcanoes

Mountain Ranges

Tsunamis