It is a place where tectonic plates meet.

A single large continent that means all earth in Greek.

The theory that Earth's lithosphere is divided into tectonic plates.

The central part of Earth below the mantle.

The process by which new oceanic lithosphere forms as magma rises to Earth's surface.

The boundary at which two tectonic plates collide.

The idea that states that the continents once formed a single land mass that then broke up, and drifted to their present location.

Oceanic crust.

The thin and solid outermost layer of Earth above the mantle.

Below the Asthensosphere.

The boundary at which two tectonic plates separate.

The two continents that split away from the one super continent.

Pieces of lithosphere moving around on the top of the Asthenosphere.

The layer of rock between Earth's crust and core.

It is thicker than oceanic crust.

A series of volcanic Islands.

Fossils of organisms were found on different continents this is evidence for this theory.

They move between 2.5 cm per year and 15 cm per year.

The solid outer layer of Earth that consists of crust and rigid upper part of the middle.

At which two tectonic plates slide past one another.

A plate of oceanic lithosphere may collide with a plate of continental lithosphere. The denser oceanic oceanic crust sinks, beneath the less dense continental crust.

Alfred Wegener.

They are the North American, Pacific, Nazca, South American, African, Antarctic, Indian, Eurasian, And Australian plates.

The soft layer of the mantle on which the tectonic plates move.

It measures the time seismic waves take to travel various distances.