Layers of the Earth
The Mantle
A State of Matter
Differentiation
Am I Really That Dense?
Earth Rules
100

The only true liquid layer of the Earth

Outer Core

100

Although the mantle is considered a single layer of the Earth, it is broken into these three layers.

Lithosphere, Asthenosphere, and Mesosphere

100

The only layer in the Mantle that that is considered to have motion

Asthenosphere

100

Differentiation is the process where a new planet seporates in layers due to this.

Density

100

The least dense layer of the the Earth

The Crust 

100

Between oceanic and continental crust, this type is thinner, denser, and primarily made of basalt

Oceanic Crust 

200

This layer of the Earth is the largest layer and broken into 3 different layers 

The Mantle

200

This layer of the mantle carries it's best friend the crust, on it's shoulders

Lithosphere

200

The Lithosphere State of matter

Solid, Brittle Rock

200

4.5 BYA, rock dust and meteors stick together to form the early Earth know as this theory

Mudball Earth

200

The chemical composition of this crust layer my be thinner, but has greater density

Oceanic crust 

200

The inner core remains a solid state despite extreme temperatures because of this opposing physical force

Extreme Pressure 

300

The outer most layer of the Earth

The Crust
300

They say convection currents are the driving force of tectonic plates, so they must only occor in this layer

Asthenosphere 

300

Your are able to find these in the only liquid layer in the Earth

Convection Currents 

300

This is how Geologist calculate the Earths temperature through its layers

Geothermal Gradiant 

300

Considering convection currents, when ultramafic rock is at the top of the astenosphere it does this,

Cools, becomes more dense, and sinks

300

Due to the liquid outer core moving around the solid inner core, this invisable force field is genorated to keep us safe from solar winds. 

Eletromagnetic Field 

400

This layer of the Earth is under so much presure not a single element of Fe or Ni can move

Inner Core

400

Only this layer of the mantle is considered to be in motion 

Asthenosphere 

400

The inner Core's state of matter

Solid

400

In early Earth's history, pressure was not the only source of heat to melt material.  This thermal energy source unstable isotopes such as uranium-235

Radioactive Decay

400

This physical process caused heavier, dense molten metals like iron to sink toward Earth's center while lighter silicates rose to the surface.

Planetary Differentiation

400

These are the Earth's 6 layers in order from least dense to most dense. 

Crust, Lithosphere, Asthenosphere, Mesosphere, Outer Core, Inner Core 

500

 The two types of crust that make up the crust

Oceanaic and Continental Crust

500

Although the Mesosphere is its official name, it is oftern refered to as  one of these two names

Lower mantleand transition zone

500

Pressure keeps the Mesosphere in a solid state of matter even though it is this

Molten rock

500

During early Earth, volcanic eruptions relised this into the atmosphere

Carbon Dioxide 

500

A geological process where one tectonic plate slides beneath another plate and sinks into the Earth's mantle at a convergent boundary

Subduction

500

The Earths gravitational pull is due to it's 

Mass