Layers of the Earth
Minerals
Rocks
The Rock Cycle
Uses of Rocks and Minerals
100

This is the thinnest and least dense layer of the Earth.

crust

100

Minerals usually have this type of shape.

geometric shape or crystal shape

100

Rocks are made of one or more of these.

minerals

100

This cycle describes how rocks change from one type to another.

rock cycle

100

Granite and marble are often used as these materials.

building materials

200

This layer is between the crust and the core.

mantle

200

This property measures how resistant a mineral is to scratching.

Hardness

200

Rocks are classified according to their composition and this.

texture

200

Cooling magma forms this type of rock.

igneous rocks

200

Coal is used as a source of this.

energy

300

The deepest layer of the Earth.

the core

300

Quartz can scratch orthoclase because quartz is this.

harder

300

Igneous rocks form when this cools and solidifies.

magma

300

Weathering and erosion create these small rock particles.

sediments

300

Minerals such as quartz are used in this type of technology.

electronics or technology

400

The continental crust can be between this many kilometers thick.

10–70 km

400

This scale is used to measure the hardness of minerals.

Mohs scale

400

Sedimentary rocks are formed by the accumulation of these materials.

sediments

400

Sediments become sedimentary rock through compaction and this process.

cementation

400

Places where rocks are extracted are called these.

quarries

500

This type of rock is commonly found in the oceanic crust.

basalt

500

A mineral that is attracted to a magnet has this property.

Magnetism

500

Heat and pressure transform rocks into this type of rock.

metamorphic rocks

500

Metamorphic rocks can melt and become this substance again.

magma

500

Extracting rocks and minerals can negatively affect this.

environment

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