Back to the lesson plan builder
Lesson length30 min45 min60 min

Print the plan for yourself; the student sheet prints on its own page after it.

Science lesson plan · 9th grade (Year 10 in England) · 60 minutes

How Earth's atmosphere changed over time

Earth and rocks

CCSS NGSS.HS-ESS2-7CCSS NGSS.HS-ESS1-6England: GCSE Combined Science: Chemistry of the atmosphere

Objective and success criteria

Students will: How Earth's atmosphere changed over time.

  • I can answer questions on today's skill on my own, without help.
  • I can explain each step and say why it works.
  • I can check my answer and spot a mistake.

Before and after

Needs first: The Earth's atmosphere; Earth's 4.6-billion-year history on a timeline

Leads to: the next skill in this area.

Materials: Rock samples, Hand lenses, Mini whiteboards, A diagram or short video clip of the idea, Printed student sheet (below).

Warm-up · 6 min

  • Quick retrieval from earlier learning (The Earth's atmosphere; Earth's 4.6-billion-year history on a timeline). Students answer on mini whiteboards.
  • Show answers together and note who needs support in the main task.
  1. Where did most of the oxygen in today's atmosphere come from? (volcanoes / the oceans boiling / photosynthesis by algae and plants over billions of years / the Sun) → photosynthesis by algae and plants over billions of yearsPrompt: Early Earth had almost no oxygen.
  2. What happened to much of the carbon dioxide in the early atmosphere? (It dissolved in oceans and was locked up in rocks and fossil fuels / It turned into nitrogen / It escaped to the Moon / It is all still in the air) → It dissolved in oceans and was locked up in rocks and fossil fuelsPrompt: Think of limestone, coal and oil.
  3. Early Earth's atmosphere was mostly… (helium / oxygen / carbon dioxide, with water vapour, released by volcanoes / argon) → carbon dioxide, with water vapour, released by volcanoesPrompt: Volcanic activity was intense.

Hook · 6 min

  • Pass round different rocks and ask how each one might have formed.
  • Share the objective: How Earth's atmosphere changed over time. Read the success criteria together.

I do: model it · 12 min

  • Work through the example out loud, saying why you do each step, not just what you do.
  • Example: Today's dry air is about 78 % nitrogen and 21 % oxygen. What percentage is made up of all the other gases together?
  • Step 1: 100 − 78 − 21 = 1
  • Step 2: So the answer is: 1 %
  • Answer: 1 %
  • Pause after each step and ask a student to say what comes next.

We do: guided practice · 12 min

  • Do these together. Students try each step on whiteboards before you reveal it.
  • Use the hints as prompts rather than giving the answer.
  1. Dry air is about 78 % nitrogen. In 250 cm³ of air, roughly what volume is nitrogen, in cm³? → 195 cm³Prompt: To find a percentage of an amount, multiply and divide by 100.
  2. Where did most of the oxygen in today's atmosphere come from? (melting ice / photosynthesis by algae and plants over billions of years / volcanic eruptions / meteorites) → photosynthesis by algae and plants over billions of yearsPrompt: Early volcanic gases contained little or no oxygen.

You do: independent practice · 17 min

  • Students work on the student sheet. Circulate and check the first two answers of every student early.
  • Students who finish: write a question of their own for a partner, with the answer.

The 8 questions are on the student sheet below, with answers in the key.

Exit ticket · 7 min

  • Two questions on their own. Sort answers into got it / nearly / not yet to plan the next lesson.
  1. Today's dry air is about 78 % nitrogen and 21 % oxygen. What percentage is made up of all the other gases together? → 1 %Prompt: Percentages of all the gases add up to 100.
  2. Scientists think the early atmosphere was mostly carbon dioxide, like Venus and Mars today. Why are they not certain? (There is limited direct evidence from billions of years ago / The atmosphere has never changed / Nobody has studied rocks / Venus has no atmosphere) → There is limited direct evidence from billions of years agoPrompt: Think about how old the evidence would have to be.

Watch out for

  • Everyday meanings of words getting in the way of the science meaning: define key words explicitly.
  • Remembering facts without the reason: ask "why?" and "what is the evidence?"

Support and stretch

Support

  • Review first: The Earth's atmosphere.
  • Use concrete materials: rock samples.
  • Give the first step of each question, or a partly worked example to finish.
  • Pair with a confident partner for the guided practice.

Stretch

  • Explain a common mistake in writing and how to fix it.
  • Write a word problem that uses today's skill, then solve a partner's.

Homework and more practice

Free online practice with hints and printable worksheets for this skill: eurekami.com/science/grade-9.

Free lesson plan from eurekami.com/lesson-plan-builder

eurekami

How Earth's atmosphere changed over time

Name

Date

Score/ 8

  1. Question 1

    Why did the amount of carbon dioxide in the early atmosphere decrease?

    • A. Volcanoes absorbed it
    • B. It dissolved in oceans, was used in photosynthesis and was locked in rocks and fossil fuels
    • C. It escaped into space
    • D. It turned into nitrogen
  2. Question 2

    Today's dry air is about 78 % nitrogen and 21 % oxygen. What percentage is made up of all the other gases together?

    Answer%

  3. Question 3

    Where did most of the oxygen in today's atmosphere come from?

    • A. meteorites
    • B. photosynthesis by algae and plants over billions of years
    • C. volcanic eruptions
    • D. melting ice
  4. Question 4

    Which gas makes up most of today's atmosphere?

    • A. carbon dioxide
    • B. nitrogen
    • C. oxygen
    • D. argon
  5. Question 5

    Dry air is about 21 % oxygen. In 1000 cm³ of air, roughly what volume is oxygen, in cm³?

    Answercm³

  6. Question 6

    Scientists think the early atmosphere was mostly carbon dioxide, like Venus and Mars today. Why are they not certain?

    • A. Venus has no atmosphere
    • B. There is limited direct evidence from billions of years ago
    • C. The atmosphere has never changed
    • D. Nobody has studied rocks
  7. Question 7

    Dry air is about 78 % nitrogen. In 400 cm³ of air, roughly what volume is nitrogen, in cm³?

    Answercm³

  8. Question 8

    Dry air is about 21 % oxygen. In 400 cm³ of air, roughly what volume is oxygen, in cm³?

    Answercm³

Free from eurekami.com

for the adult only

Answer key: How Earth's atmosphere changed over time

  1. 1. B. It dissolved in oceans, was used in photosynthesis and was locked in rocks and fossil fuels

  2. 2. 1 %

  3. 3. B. photosynthesis by algae and plants over billions of years

  4. 4. B. nitrogen

  5. 5. 210 cm³

  6. 6. B. There is limited direct evidence from billions of years ago

  7. 7. 312 cm³

  8. 8. 84 cm³