C2.3

Sedimentary rocks

Indicative relationship: Activate 1 · Chemistry contextual consolidation
KS3 science lesson

Sedimentary rocks

Lesson focus: How can loose sand become rock?

Learning objective

Sequence , , , and .

Build on earlier learning

Mixtures

Consider the properties of different particles in a mixture.

Practical

Modelling sedimentary rock

  1. Shake sand, gravel and soil in a jar of water and let it settle.
  2. Observe the layers: larger, denser grains settle first.
  3. Relate the layers to compaction and cementation over time.

Record: A labelled drawing of the layers with grain sizes.

You will be successful when you can…

  • Distinguish weathering from erosion.
  • Sequence a clastic pathway.
  • Explain compaction and cementation.
  • Recognise other sedimentary routes.
KEY VOCABULARY

Words that carry the science

weathering
Breakdown of rock in place.
erosion
Removal and transport of weathered material.
deposition
Settling of transported sediment.
compaction
Grains pressed closer together during burial.
cementation
Minerals deposited between grains bind them together.
BUILD YOUR UNDERSTANDING

Keep weathering, transport and rock formation as distinct processes

01Break down before moving

Physical, chemical or biological acts on rock in place. then removes and transports material by water, wind, ice or gravity.

02Flow controls deposition

When a transporting fluid loses energy, larger or denser particles often settle sooner, while fine particles may remain suspended longer.

03Burial turns sediment into rock

Overlying layers compact sediment and minerals precipitated in pore spaces cement grains. This describes clastic rocks; chemical precipitation and biological material form others.

A cross-section follows rock from a cliff to the sea. 1: weathering breaks up exposed rock. 2: a river erodes and transports the fragments downhill. 3: sediment is deposited in layers on the sea floor. 4: newer layers bury older ones and compact them, squeezing out water. 5: dissolved minerals cement the grains into sedimentary rock.1 weathering2 erosion and transportsea3 deposition in layersnew loose sediment4 burial and compaction5 cementation → sedimentary rock
Figure · This is a clastic-rock pathway, not a rule for every sedimentary rock. Some sedimentary rocks form through chemical precipitation or biological material, such as parts of limestone and chalk.
Animation

Sedimentary rock forming

Rivers carry broken bits of rock into lakes and seas. The bits settle in layers: big, heavy grains sink fastest, fine clay last. Layers build up; their weight compacts the lower layers and minerals cement them into rock.

Deposition

Brown: sand and pebbles (sink fastest). Tan: silt. Grey: clay (sinks slowest).

Controls

Layers deposited0 of 5
StageDeposition: grains settle, biggest first
Oldest layerAt the bottom (law of superposition)

Speeds are illustrative; real layers take thousands to millions of years. Fossils are found in sedimentary rocks such as sandstone, limestone and mudstone.

WORKED EXAMPLE

Explain graded sediment

A flood layer has coarse grains at the bottom and finer grains above.

  1. Fast water can carry a wide range of grain sizes.
  2. As flow loses energy, larger grains settle first.
  3. Finer particles stay suspended longer.
  4. Continued slowing deposits finer grains above the coarse layer.

How to make the reasoning visible: The vertical grain-size pattern can preserve evidence of changing flow energy.

LEARN BY DOING

Process and evidence sequence

Connect each process to an observable consequence.

ProcessLocation/actionEvidenceCommon confusion
WeatheringRock breaks in placeCracks/fragmentsNot transport
ErosionMaterial removed/movedRounded grains/pathwayNot deposition
DepositionSediment settlesLayers/graded bedsNot cementation
CompactionBurial pressureReduced pore spaceDoes not melt
CementationMinerals bind grainsCement between grainsNot simple drying
  1. How can several layers record several events?

  2. Why may coarse grains lie below fine grains?

  3. Use the table. What is the difference between weathering and erosion?

RETRIEVE · APPLY · CHECK

Check your understanding

Answer from memory, then check against the suggested answer.

What is weathering?

What is erosion?

What is deposition?

What is compaction?

Give an example of a sedimentary rock.

Apply the idea

Describe how loose sand becomes sandstone.

Stretch and challenge

Why is chalk a warning against treating the clastic sequence as universal?

Why are fossils usually found in sedimentary rocks and not igneous rocks?

Exam Question Practice

C2.3Describe4 marks

Exam Question Practice

Mark points shown after marking

Describe how loose sediment becomes sedimentary rock.

(4)

Total for this question: 4 marks

Command word: Give the stages in causal order and do not include melting.

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