Sedimentary rocks are formed when sediments are pressed together over a long period of time.
Sediments include rock particles, such as mud, sand or pebbles, usually washed into rivers and eventually deposited on the riverbed or sea.
They can also come from remains of living things, such as plants and animals
Chemical sedimentary rocks form when water evaporates, leaving behind a solid substance.
Metamorphic rocks are formed when other types of rocks are changed by extreme heat and pressure inside the Earth.
When igneous, sedimentary or even metamorphic rocks are heated to extreme temperatures by magma, or when placed under pressure due to rocks above them, they can change into a different type of rock.
Metamorphic rocks are stronger than the original rocks as they are formed under great pressure and heat
Bands can also appear, which tell us that the crystals have been squeezed together under immense pressure.
The gradual breaking down of rocks is called weathering.
Rocks are gradually broken down and sculpted through both physical and chemical processes.
Rocks are slowly worn down into smaller pieces by weathering.
The causes are either chemical or physical
Physical weathering refers to the breakdown of rocks by non-living things.