Plate Tectonics. The Earth’s outer layer or shell Crust Made mostly of oxygen and silicon.

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Transcript of Plate Tectonics. The Earth’s outer layer or shell Crust Made mostly of oxygen and silicon.

PlateTectonics

The Earth’s outer layer or shellCrust

Made mostly of

oxygen and silicon

Cycles created by hot materials rising, cooling off, and then sinking back

down

Convection Currents

the innermost layer of Earth, made mostly of the elements iron and nickel

Core

The outer core is molten. The inner core is solid.

the outer zone of Earth, made of the crust and upper mantle /makes up the

tectonic plates

Lithosphere

The slowly flowing, semi-solid layer of rock under the lithosphere

Asthenosphere

Tectonic plates “float” on the semi-solid asthenosphere.

the strong, lower part of the mantleMesophere

The mantle is made up of 3 sub layers.

The idea that Earth’s

continents were once

connected and have broken

apart and drifted to their

present location

Theory of Continental Drift

German geologist, Alfred Wegener, was the first to describe continental drift.

the theory that the outer part of Earth is divided into several distinct

segments, called plates which move

Plate Tectonics

A border where tectonic plates move towards one another

Convergent Boundary

Converge means to come together.

A border where tectonic plates move apart from each other

Divergent Boundary

Diverge means to divide.

A border where tectonic plates slide past each other

Transform Boundary