Sediment
Sedimentation
Compaction
Cementation
Formation Sequence
100

What is sediment and where does it come from?

Small rock pieces from weathering and erosion.

100

What is sedimentation?

Sediment settling into layers.

100

What is compaction?

Pressure squeezes sediment layers.

100

What is cementation?

Minerals glue grains together.

100

What rock forms from sediment?

Sedimentary rock.

200

What are three examples of sediment?

Sand, silt, clay.

200

Why do layers form?

Heavy particles settle first.

200

Why does compaction force water out?

Pressure closes spaces.

200

Two minerals that act as cement?

Silica, calcite.

200

First step of formation?

Sedimentation

300

Why do different sediments have different sizes?

Different weathering processes.

300

What are sediment layers called?

Strata.

300

Why are deeper layers more compacted?

More weight above them.

300

Where do cementing minerals come from?

Dissolved minerals in water.

300

Second step of formation?

Compaction

400

Where does sediment naturally build up?

Rivers, lakes, beaches.

400

Why do layers have different colours?

Different materials or minerals.

400

How does compaction change sediment?

Makes it denser and tighter.

400

What must minerals do to cement grains?

Crystallise.

400

Third step of formation?

Cementation.

500

Why is sediment in fast water different from slow water?

Fast water carries larger particles.

500

How does sedimentation help preserve fossils?

Sediment quickly buries organisms.

500

What happens if sediment isn’t compacted?

It stays loose.

500

How do compaction and cementation work together?

Pressure packs grains; minerals glue them.

500

Explain the full sequence.

Sediment settles → squeezed → glued.

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