Earth Science Unit 6 Plate Tectonics

Evidence for Continental Drift based on traces of very cold climate in today's warm regions.

A cause of hot spots that may not move as the plates do.

Waves that travel transverse waves they cause the some damage and middle speed.

Evidence of Sea Floor Spreading base on seismograph data

Waves that can travel through the interior of the earth

A plate boundary were the two plates are colliding

A cause of plate motion caused by the formation of new crust at divergent plate boundaries.

Small quakes that precede or follow a major quake that concentrate or release energy.

The tool that scientists use to study earthquakes

The scientist that proposed Continental Drift

The name of the super continent that existed 200 million years ago

Evidence for Continental Drift based on remains of plants and animals in separated continents.

A vibration of the lithosphere caused by the release of energy at plate boundaries.

The way the energy from the earthquake moves away from the point of origin.

A plate boundary were the two plates are sliding past one another

Evidence for Continental Drift based on mountain ranges the same age on separated continents.

The thin rocky outer layer of the earth

A feature that is formed at a divergent boundary between two oceanic plates.

A cause of plate motion related to gravity acting on the plates at subduction zones.

When the friction that is resisting the plate motion is overcome the earthquake starts.

A feature that is formed at a convergent boundary between oceanic and continental plates.

A part of the crust that is thinner, but composed of heavier minerals and is more dense.

Evidence of Sea Floor Spreading base on old rocks near continents and young rocks near ridges

A part of the crust that is thicker, but composed of lighter minerals and is less dense.

A plate boundary were the two plates are separating

A plate boundary where new crust is being created

A plate boundary also known as a spreading center.

The central part of the interior, made molten and solid nickel and iron.

A cause of plate motion related to the motion of heated material in the mantle

The point on the earth's surface above the point where the earthquake starts

The point within the earth where the earthquake starts

A plate boundary where crust is not created or destroyed

A plate boundary were old crust is being destroyed.

A layer of the earth that includes the crust and part of the upper mantle.

A feature that is formed at a convergent boundary between two continental plates.

A plate boundary where Earthquakes occur

Waves that travel the fastest as longitudinal waves they cause the least damage.

Evidence of Sea Floor Spreading from changes in the magnetic field of the earth over time.

A feature that is formed at a convergent boundary between two oceanic plates.

The scientist that proposed Seafloor Spreading

Once the friction is released the rocks snap back into their relaxed shape

The scientist that proposed Plate Tectonics

Waves that travel along the surface of the earth, they are the slowest but most damaging waves

Long curved valleys found along the edges of continents on the ocean floor.

The thickest part of the interior, made of rocks that are plastic because of heat and pressure

A system of mountains found in the oceans that extends for 70000 km

Evidence for Continental Drift found in the matching the shore lines of the continents.

A part of the upper mantel that is very flexible, is allows the plates of crust to side around.

A plate boundary also known a strike/slip fault

Before an earthquake the movement of the plates stores energy by