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Geography · Rocks and rock-cycle reasoning

Classifying a rock from formation evidence

You know the three rock types, yet a described specimen leaves you guessing.

To classify a rock, read the evidence first: crystals, layers or bands. Each points to a formation process, and the process gives the family.

This lesson is part of rocks and rock-cycle reasoning. When you can classify, move to tracing two possible pathways through the rock cycle.

What evidence points to which family?

Evidence in the description Process Family
Interlocking crystals, large Slow cooling of magma underground Igneous, intrusive
Interlocking crystals, tiny or glassy Fast cooling of lava at the surface Igneous, extrusive
Layers, fossils, rounded grains Deposition, compaction and cementation Sedimentary
Bands, aligned minerals, very hard Heat and pressure change an older rock Metamorphic

Use the table to match clues to families, not to memorise by rote.

Worked example: three invented specimens

Specimen A. Large, visible crystals of different minerals fit together like a jigsaw. No layers.

The evidence is crystal size, so the rock cooled slowly from magma. It is intrusive igneous.

Specimen B. Thin, flat layers of fine sand, with an impression of a shell.

Layers and a fossil show that sediment was laid down and buried, then compacted and cemented. It is sedimentary.

Specimen C. Hard, compact rock with wavy bands where dark and light minerals line up. The description says it was buried near a large mass of magma.

Heat and pressure changed an earlier rock and aligned its minerals. It is metamorphic.

The mistake that costs marks

The common slip is to write “it is sedimentary because it is a rock found on land”. That is not evidence, and it would fit any rock.

A stronger sentence quotes the clue and the process: “The rock has layers and a shell impression, which shows deposition and compaction of sediment, so it is sedimentary.” The answer names the clue, the process and the family in one sentence.

Check yourself

A rock has tiny crystals you cannot see without a hand lens and small holes where gas escaped. It was found beside an old volcano. Classify it and explain.

Answer

It is extrusive igneous rock. The tiny crystals show fast cooling, because lava at the surface loses heat quickly and crystals have no time to grow. The gas holes and the volcano location support a surface eruption.

What to study next

Go on to tracing two possible pathways through the rock cycle. Use the claim, evidence and explanation revision desk to rehearse the clue, process, family sentence.

If you want a teacher to give you fresh specimen descriptions, see online one-to-one Geography tuition.

Common questions

How can I tell igneous from sedimentary quickly?

Look for crystals that interlock and no layers for igneous, and look for layers, fossils or rounded grains for sedimentary. If both seem present, read the description again for the dominant texture.

What is the difference between intrusive and extrusive igneous rock?

Intrusive rock cools slowly underground and has large crystals. Extrusive rock cools fast at the surface and has small crystals or a glassy texture. Crystal size is the evidence for cooling speed.

What clue points to metamorphic rock?

Look for bands or aligned minerals, a harder and more compact texture, and a mention of heat or pressure. The rock formed from an earlier rock that was changed without fully melting.

Do I need to name a specific rock like granite?

Name the family first, then the example if the evidence fits it. Granite is coarse intrusive igneous rock, but the mark is usually for the family and the reason.

If you guess the rock type from the name instead of the clue, one-to-one Geography lessons let a teacher drill the clue-first habit on new specimens.

  • Online one-to-one lessons for your child with an experienced teacher.
  • Your first class is a one-hour trial, from RM50. The fee is agreed before you book.
  • Happy with the teacher? Continue with lessons of about 1.5 hours. If not, ask for another teacher.