Sedimentary rocks
Igneous rocks
Metamorphic rocks
Minerals
Properties
100

These are the preserved remains or prints of ancient plants and animals, which are almost always found inside sedimentary rocks.

fossils

100

This liquid, molten rock is found inside the Earth before it erupts or leaks out onto the surface.

magma

100

These are the two intense forces deep underground that work together to bake and squeeze older rocks into metamorphic ones.

heat and pressure

100

This is the hardest mineral on Earth.

diamond

100

This property is the easiest to see first, but it is often unreliable because minerals like quartz can come in purple, pink, or clear varieties.

color

200

This specific type of sedimentary rock is made when tiny grains of sand get squeezed and glued together over millions of years.

sandstone

200

This is the name for molten rock once it breaks through the Earth's crust and flows out of a volcano.

lava

200

This beautiful metamorphic rock is formed when limestone is baked underground and is often used by sculptors or for fancy kitchen counters.

marble

200

This property describes how shiny a mineral is, or how it reflects light, like looking metallic or glassy.


luster

200

This property measures how much mass is packed into a specific volume, or how heavy a rock feels for its size.


density

300

This word describes the bits of broken rock, sand, mud, and shells that get moved by wind or water and settle at the bottom of lakes and oceans.

sediment

300

This glassy, dark igneous rock cools so quickly on the surface that no visible crystals have time to grow.

obsidian

300

This word describes the wavy bands or striped lines seen in some metamorphic rocks when intense pressure flattens their minerals.

bands

300

To test this property, you scratch a mineral against a white plate to see the color of its powder.

streak

300

Some minerals, like magnetite, have this special invisible property that allows them to attract metal paperclips

magnetism

400

Sedimentary rocks are famous for forming in these flat, horizontal bands that look like stripes or layers.

layers

400

This common intrusive rock cools slowly underground, creating large mineral crystals often seen on kitchen countertops.

granite

400

This smooth, flat metamorphic rock starts out as soft shale mudstone before being squished, and is used to make traditional chalkboards.

slate

400

Named after a scientist, this 1-to-10 scale measures how easy or hard it is to scratch a mineral

mohs scale

400

This property simply describes how a mineral splits smoothly along flat, even surfaces like sheets of paper.

cleavge

500

This is the final step in making a sedimentary rock, where minerals in groundwater act like a natural glue to lock the grains into solid stone.

cementation

500

This dark, heavy igneous rock makes up most of the oceanic crust under the ocean floor and cools quickly from lava.

basalt

500

This high-grade metamorphic rock develops thick, alternating light and dark mineral bands, and its name starts with a silent letter g.

gneiss

500

This mineral is so strong that it can only be scratched by another diamond.


dimond

500

This is the physical property that tells you how heavy or light a rock feels for its size

density

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