←Topic 12 · Geological Time
Practical 12 Oceanography CAPS block 8 · Term 1 · 1 hour

Geological Time

There is nothing to measure in this practical and nothing to mix. Every task does the same job: it takes 4.6 billion years — a number nobody has any feel for — and turns it into something your body already understands. A distance you can walk. A day you have already lived. That is not a gimmick; it is the outcome CAPS actually sets for this block.

What CAPS asks for

Investigations column, block 8, in full: "Develop a timeline in table form" · "See videos illustrating 'Toilet Roll' — unrolled down a passage, with humans arriving only in the last square of the roll" · "Compare geological time on a timeline" · "Compare the earth's history to a 24-hour day, in which humans exist only as of 1 minute before midnight". Resources column: "Timeline printed as a wall chart for the back of the classroom."

That is Investigations 1 to 4, and the wall chart is part of Investigation 1. The Depth column then says the point is "for learners to conceptually understand the age of the planet and relate this to evolution and other paleo-references" — understand, not recite. Investigation 5 is not a CAPS investigation. It is the half-life graph work that your Term 2 paper actually asked for, and it belongs on this sheet even though CAPS does not list it here.

What you need

No roll, or nowhere to unroll it? Every investigation still works.

Investigation 2 ships with a supplied roll — the sheet count and sheet length are given, so every calculation, every position and every analysis question can be done on paper at a desk. A ball of string and a passage does the same job if you would rather not use a roll. And Investigations 1, 3, 4 and 5 need nothing but a pencil and a calculator in the first place. Nothing on this sheet is gated on owning anything.

1 Develop a Timeline in Table Form CAPS Investigation, verbatim · + the Resources-column wall chart

Aim

To build the geologic time scale yourself, from the top down — eons, then eras, then periods — as a table, and then as a wall chart you will actually see every day.

Method

  1. Close the topic page. Fill in as much as you can from memory first, in pencil. Then open it and correct yourself in a different colour. The corrections are the useful part — they are your revision list.
  2. Work top-down: four eons, then the three eras inside the last eon, then the twelve periods inside those eras. Getting the nesting right matters as much as getting the names right.
  3. Fill in the dates from your booklet, and calculate each duration yourself rather than copying it.
  4. Then build the wall chart (CAPS Resources column) and put it somewhere you pass daily. Requirements are in Q6.

Results — Table 1.1 · the four eons

Table 1.1 — the four eons, oldest first
EonFrom (mya)To (mya)Duration (my)One defining feature

Results — Table 1.2 · the three eras of the Phanerozoic

Table 1.2 — the eras, oldest first
EraDates (mya)Its name means…"The age of…"How it ended

Results — Table 1.3 · the twelve periods

Table 1.3 — every period, oldest first, grouped under its era
EraPeriodDates (mya)One thing the rock record shows

Analysis

  1. Complete Table 1.1. Two marks per eon: the name with correct dates, and a defining feature. 8
  2. Complete Table 1.2. Three marks per era: dates, what the name means, and how it ended. 9
  3. Complete Table 1.3. One mark per period correctly named, in the right order, under the right era. 12
  4. Which three eons together make up the Precambrian, and why is the fourth left out of that grouping? 4
  5. Calculate the duration of each eon. Which is the longest, and roughly what fraction of Earth's whole history does the Phanerozoic — the eon containing almost every fossil you will ever see — actually occupy? 5
  6. Build the wall chart. It must show: all four eons drawn to scale along a strip, the three eras expanded out of the Phanerozoic, every period named, and a title. Mark it 2 for scale, 2 for completeness, 2 for legibility from across the room. 6
  7. CAPS asks you to develop a timeline rather than read one. Explain what you learned from building the table that you would not have got from looking at a finished one. 3
2 The Toilet Roll Walk CAPS Investigation, verbatim

Aim

To lay out the whole of Earth's history as a distance you can walk, and find out where on that walk everything you have ever heard of actually happens.

Method

  1. Count the sheets on your roll — the packet usually says. Measure the length of one sheet in centimetres.
  2. Calculate the total length, and then the scale: how many million years does one sheet represent? Show this working; it is Q8.
  3. Unroll the whole roll down a passage, a driveway or a garden path. Keep it straight. Do not do this in a street — you will be walking backwards along it with your eyes on the paper.
  4. Starting from the free end as 4 600 million years ago, count sheets and use a sticky note to flag each event in Table 2.1.
  5. Now walk the roll from the start to the end, slowly. Notice how far you get before anything you recognise happens.
  6. Roll it back up. It is still perfectly usable.
Supplied — a measured roll, if you cannot unroll one

Use these figures exactly as if you had measured them yourself. Every question below can be answered from them.

Data set 2.1 — the supplied roll
MeasurementValue
Sheets on the roll240
Length of one sheet11.0 cm
Total unrolled length26.4 m
Age of Earth being modelled4 600 million years

If your own roll is different, use your own numbers. The answers will differ and that is correct — the proportions are what the investigation is about, and those come out the same on any roll.

Results — Table 2.1 · where each event falls

Sheet number counted from the free end, which is the moment Earth formed. Five of these are South African. SA

Table 2.1 — events on the roll
EventAge (mya)Sheet numberDistance from the start
Earth forms4 600
Oldest surviving crust (Hudson Bay)4 300
Archean eon begins4 000
Barberton stromatolites SA · Mpumalanga3 500
Proterozoic eon begins2 500
Great Oxygenation Event2 400
Vredefort meteorite impact SA · Free State2 020
Cambrian explosion — Phanerozoic begins541
Table Mountain sandstone laid down SA · Chapman's Peak510
Permian–Triassic extinction SA · Karoo251
Pangaea breaks up200
Cretaceous–Tertiary extinction65
Australopithecines SA · Cradle of Humankind~3.2
Homo sapiens appears~0.3
All of recorded human history~0.005

Analysis

  1. Calculate the scale of your roll: how many million years does one sheet represent? Show the working. 3
  2. Complete Table 2.1 — sheet number and distance for every event. 12
  3. How many sheets — and what percentage of the roll — are taken up by the Precambrian alone, before a single shelled animal exists? 4
  4. CAPS says humans arrive "only in the last square of the roll". Using your table, say whether that is true, and how far along that final sheet Homo sapiens actually appears. 4
  5. Calculate the length, in millimetres, of the strip representing all of recorded human history — every pyramid, every empire, every book ever written. Compare it to the width of the pencil line you would use to mark it. 5
  6. Five events on the roll are South African. Name the oldest of them, give its sheet number, and explain what it tells us about how long life has existed on Earth. 4
  7. You were told to walk the roll rather than just look at the numbers. Explain what walking it shows you that Table 2.1 does not. 3
  8. Every model gets something wrong. Give two things this one misrepresents about geological time. 4
3 Compare Geological Time on a Timeline CAPS Investigation, verbatim

Aim

To draw Earth's history to scale on a single line — and to run head-first into the problem that makes every real geological time chart look the way it does.

Method

  1. The strip below is 20 cm long. The left edge is 4 600 mya; the right edge is today.
  2. Work out the scale in million years per centimetre, then mark and label all four eons as bands.
  3. Now try to mark, on the same strip: the Cambrian explosion, the Permian–Triassic extinction, the K–T extinction, and the arrival of Homo sapiens.
  4. You will not be able to. That is the intended result. Do not fudge it — record what goes wrong, then fix it in Q17.
Before you draw A 20 cm strip for 4 600 million years gives 4600 ÷ 20 = 230 million years per centimetre, so 1 mm = 23 million years. Keep that number in front of you — most of this investigation is about what it does to everything you want to label.

Results — the scaled timeline

Results — your solution to the scale problem

Analysis

  1. Draw the four eons to scale on the first strip, correctly labelled with their dates. 8
  2. Calculate, in millimetres, the width of the strip occupied by: (a) the Phanerozoic eon, (b) the Cenozoic era, (c) the whole of the Quaternary period. 6
  3. Which events could you not mark separately, and why? Answer with a number, not just "they were too close together". 4
  4. Real geological time charts all solve this problem the same way. Redraw your timeline using that fix, and name the technique. 6
  5. Look back at the eon ribbon on the topic page. Identify exactly where it does the same thing, and why it has to. 3
  6. A classmate says a to-scale timeline is more honest than one with a blown-up section. Argue against them — what does the to-scale version hide? 4
4 Earth's History as a 24-Hour Day CAPS Investigation, verbatim

Aim

To compress 4 600 million years into a single day, convert every event to a clock time, and then test CAPS's own claim about when humans turn up.

Method

  1. Earth forms at 00:00:00. Right now is 24:00:00.
  2. Work out the scale in million years per hour, per minute and per second. That is Q21.
  3. Convert every event in Table 4.1 using clock time = 24 × (4600 − age) ÷ 4600 hours, then convert the decimal into hours, minutes and seconds.
  4. Give your last three answers to the nearest second. The whole point of the investigation lives in those seconds.
Worked example, so you can check your method The Great Oxygenation Event, 2 400 mya: 24 × (4600 − 2400) ÷ 4600 = 24 × 2200 ÷ 4600 = 11.478 h.
0.478 h × 60 = 28.7 min, and 0.7 min × 60 ≈ 42 s. So it happens at 11:28:42 — Earth was more than half a day old before the air became breathable.

Results — Table 4.1 · the day

Table 4.1 — Earth's history as one 24-hour day
EventAge (mya)Clock time
Earth forms4 60000:00:00
Oldest surviving crust4 300
Archean eon begins4 000
Barberton stromatolites — life is already here SA3 500
Proterozoic eon begins2 500
Great Oxygenation Event2 40011:28:42
Vredefort impact SA2 020
Cambrian explosion541
Permian–Triassic extinction SA · Karoo251
Pangaea breaks up200
K–T extinction — dinosaurs gone65
Australopithecines SA · Cradle of Humankind~3.2
Genus Homo appears~2.8
Homo sapiens appears~0.3
All of recorded human history~0.005

Analysis

  1. On this scale, how many million years is one hour? One minute? And how many years is one second? 4
  2. Complete Table 4.1. 12
  3. At what time does the first evidence of life appear, and what fraction of the day had already passed? Comment on the answer. 4
  4. 🔴 The important one. CAPS states that humans exist "only as of 1 minute before midnight". Your calculation puts Homo sapiens at about six seconds before midnight — ten times later. Neither figure is a mistake. Explain what CAPS must mean by "humans" for its number to be right, name the group, and state which South African World Heritage Site is famous for their fossils. 6
  5. How long does all of recorded human history last on this clock? Give the answer in seconds. 3
  6. Compare the two models you have now built — the roll and the day. Give one thing each does better than the other. 4
  7. A news article says humans have been on Earth "for ages". Using one figure from this investigation, write a single sentence that puts that claim in proportion. 3
5 Read an Age Off a Decay Curve Not a CAPS investigation — added, because the exam does this
Why this is here when CAPS does not ask for it

Block 8's Investigations column is entirely about scale. But CAPS key concept 2 is half-life and radiometric dating, and Question 2.1 of your Term 2 Paper 1 was a decay graph you had to read an age off. An investigation column that does not rehearse the block's own assessed skill is a gap, so this drill fills it. Do not quote it as a CAPS investigation.

Aim

To plot a decay curve from your booklet's own Cobalt-60 example, and then use it backwards — the direction an exam asks for.

Method

  1. Complete Table 5.1. Cobalt-60 has a half-life of 5.26 years and the sample starts at 8.00 g.
  2. Plot mass remaining (y) against time in years (x) on the grid. Join the points with a smooth curve, not straight segments.
  3. Label both axes with quantity and unit, and give the graph a title. Those are marks.
  4. Then answer the questions by reading off your own curve, not by calculating.

Results — Table 5.1 · the decay of 8 g of Cobalt-60

Table 5.1 — complete the columns
Half-lives elapsedTime (years)Mass of ⁶⁰Co remaining (g)% of original
008.00100
15.264.0050
2
3
4
5
6

Results — the decay curve

Analysis

  1. Complete Table 5.1 — time, mass and percentage for half-lives 2 to 6. 8
  2. Plot the curve. Marks: axes labelled with units (2), sensible scale (2), points correct (2), smooth curve and a title (2). 8
  3. A sample of the same material contains 0.50 g of ⁶⁰Co and is known to have started at 8.00 g. Use the graph to find its age, then check it by counting half-lives. 4
  4. Another sample has 3.0 g remaining. Read its age off your curve. Explain why you could not have got this one by counting half-lives. 4
  5. The curve never actually reaches zero. Explain what that means physically, and why it matters for dating very old rock. 4
  6. Explain why Carbon-14 would be useless for dating the 200-million-year-old rock from Investigation 2, and name an isotope from the topic page that would work. 4
  7. Your booklet gives the half-life of Potassium-40 as 4.468 billion years, and the topic page says the true value is 1.25 billion years. State which number you would use in an exam and why, and explain what the booklet has confused it with. 4
Memo — worked answers and mark allocation (does not print)

Total: 189 marks — Investigation 1: 47 · Investigation 2: 39 · Investigation 3: 31 · Investigation 4: 36 · Investigation 5: 36.

Note on the supplied roll. All Investigation 2 answers below assume the supplied roll: 240 sheets × 11.0 cm = 26.4 m, so 1 sheet = 4600 ÷ 240 = 19.17 million years. If the learner measured their own roll, mark for correct method and internal consistency, not against these numbers.

Investigation 1 — the table and the wall chart

  • Q1 (8): Hadean 4600–4000, 600 my, Earth molten, no solid surface · Archean 4000–2500, 1500 my, crust cools, oceans form, first life · Proterozoic 2500–541, 1959 my, oxygen appears, first complex and multicellular life · Phanerozoic 541–today, 541 my, abundant life with hard parts. (2 each.)
  • Q2 (9): Palaeozoic 541–251, "ancient life", ends with the Permian–Triassic extinction · Mesozoic 251–65, "intermediate life", ends with the Cretaceous–Tertiary extinction · Cenozoic 65–today, "recent life", ongoing. (3 each.)
  • Q3 (12): Palaeozoic: Cambrian 541–488 · Ordovician 488–443 · Silurian 443–416 · Devonian 416–359 · Carboniferous 359–299 · Permian 299–251. Mesozoic: Triassic 251–199 · Jurassic 199–145 · Cretaceous 145–65. Cenozoic: Palaeogene 65–23 · Neogene 23–2 · Quaternary ~2–today. One mark each, awarded only if the order and the parent era are both right.
  • Q4 (4): Hadean, Archean and Proterozoic (3). The Phanerozoic is excluded because the grouping is defined by what came before the Cambrian — before animals had hard parts, so before the fossil record properly begins (1).
  • Q5 (5): Durations 600 / 1500 / 1959 / 541 my (2). Proterozoic is longest (1). Phanerozoic = 541 ÷ 4600 = 11.8%, so roughly one-ninth of Earth's history holds almost the entire fossil record (2). Accept "about 12%".
  • Q6 (6): Marked as stated. The commonest failure is drawing the four eons as four equal blocks — check the Phanerozoic band really is about a ninth of the strip.
  • Q7 (3): Any defensible answer, e.g. the nesting only becomes obvious when you have to decide which column a name goes in (1); the gaps show you what you did not know (1); calculating the durations shows how uneven they are, which reading a finished chart hides (1).

Investigation 2 — the toilet roll

  • Q8 (3): 4600 my ÷ 240 sheets = 19.17 million years per sheet (2), working shown (1). Equivalently 174 my per metre, or 1.74 my per centimetre.
  • Q9 (12): Sheet = (4600 − age) ÷ 19.17; distance = sheet × 11 cm. Earth forms 0 · oldest crust 15.7 (1.72 m) · Archean 31.3 (3.44 m) · Barberton 57.4 (6.31 m) · Proterozoic 109.6 (12.05 m) · Great Oxygenation 114.8 (12.63 m) · Vredefort 134.6 (14.81 m) · Cambrian explosion 211.8 (23.30 m) · Table Mountain sandstone 213.4 (23.47 m) · Permian–Triassic 226.9 (24.96 m) · Pangaea breaks up 229.6 (25.25 m) · K–T 236.6 (26.03 m) · australopithecines 239.8 · H. sapiens 239.98 · recorded history 240.0. Allow ±0.5 of a sheet.
  • Q10 (4): The Precambrian ends at sheet 211.8, so it occupies 211.8 of 240 sheets ≈ 88% (3) — about 23.3 m of the 26.4 m roll (1). The topic page quotes 87%, which comes from rounding the Phanerozoic to 600 my. Accept 87% or 88%; do not penalise either.
  • Q11 (4): True (1). Sheet 240 covers 19.17 mya to today, and H. sapiens at 0.3 mya falls at (19.17 − 0.3) ÷ 19.17 = 98.4% of the way along the final sheet (2) — about 1.7 mm from the end of the roll (1).
  • Q12 (5): 0.005 my ÷ 19.17 my per sheet = 0.000261 sheets; × 110 mm = 0.029 mm, i.e. about three hundredths of a millimetre (3). A pencil line is roughly 0.5 mm wide, so the line you draw to mark recorded history is about 17 times thicker than the thing it marks (2). This is the single best number on the sheet — the act of recording it destroys the scale.
  • Q13 (4): Barberton (1), sheet 57.4 (1). It carries 3.5-billion-year-old stromatolite fossils, so life already existed less than a quarter of the way along the roll (1) — life is not a late addition to Earth's history but an early one, and it was marine (1).
  • Q14 (3): Walking makes the duration physical: you cover more than 20 m of empty Precambrian before anything with a shell appears (2), and the entire part of the story you have ever been taught happens in the last two paces (1).
  • Q15 (4): Any two, 2 each: the roll is uniform so it implies a constant rate of change, when the pace of geological and biological change is wildly uneven; it is linear, so everything recent is unreadable; it has a hard start, but Earth's formation took tens of millions of years and was not an instant; the dates themselves carry uncertainty that a sheet boundary hides.

Investigation 3 — the scaled timeline

  • Q16 (8): 230 my/cm. Hadean 0–2.6 cm · Archean 2.6–9.1 cm · Proterozoic 9.1–17.6 cm · Phanerozoic 17.6–20 cm. Marks: correct scale (2), four bands correctly proportioned (4), labelled with dates (2).
  • Q17 (6): (a) Phanerozoic 541 ÷ 230 = 2.35 cm = 23.5 mm (2) · (b) Cenozoic 65 ÷ 230 = 0.283 cm = 2.8 mm (2) · (c) Quaternary 2 ÷ 230 = 0.0087 cm = 0.087 mm (2), which is under a tenth of a millimetre.
  • Q18 (4): The K–T extinction (65 mya) and the arrival of H. sapiens (0.3 mya) are 2.8 mm and 0.013 mm from the right-hand edge respectively (2), so they fall within one pencil line of each other and of the end of the timeline (2). The answer must contain a number.
  • Q19 (6): The technique is an inset, blow-up or expanded section — accept "log scale" as an alternative with reasoning (2). Redrawn timeline with a to-scale main strip plus an expanded Phanerozoic beneath it, clearly linked (4).
  • Q20 (3): The topic page's eon ribbon draws the four eons to scale, so the Phanerozoic is a thin strip at the right — and then expands its three eras into separate cards below (2). It has to, because at true scale the eras are a few pixels wide and could not be labelled or tapped (1).
  • Q21 (4): The to-scale version is honest about proportion but hides content (1): almost everything with a name — every period, every extinction, every fossil group — is compressed into the last centimetre and becomes invisible (2). A chart nobody can read is not more honest, it is just unusable; the blow-up is a labelled exception rather than a distortion, which is why real charts say so on the diagram (1).

Investigation 4 — the 24-hour day

  • Q22 (4): 1 hour = 4600 ÷ 24 = 191.7 my (1) · 1 minute = 3.19 my (1) · 1 second = 4600 ÷ 86 400 = 0.0532 my = about 53 000 years (2).
  • Q23 (12): Oldest crust 01:33:55 · Archean 03:07:50 · Barberton 05:44:21 · Proterozoic 10:57:23 · Vredefort 13:27:39 · Cambrian explosion 21:10:39 · Permian–Triassic 22:41:26 · Pangaea 22:57:23 · K–T 23:39:39 · australopithecines 23:59:00 · genus Homo 23:59:07 · H. sapiens 23:59:54 · recorded history 23:59:59.9. Allow ±2 s.
  • Q24 (4): Barberton stromatolites at 05:44:21 (2) — under a quarter of the day gone (1). The comment should note that life appears early, and that everything after it is not the arrival of life but its elaboration (1).
  • Q25 (6): CAPS must mean the hominin lineage, not our own species (2). One minute before midnight is 3.19 mya, which is the time of the australopithecines — Australopithecus (2). The site is the Cradle of Humankind in Gauteng, with Sterkfontein its best-known cave (2). Marking note: full marks require the learner to say that neither figure is wrong — the word "humans" is doing the work. This is the best question on the sheet, and it is a real disagreement in a real syllabus, not a trick.
  • Q26 (3): 0.005 my ÷ 0.0532 my per second = 0.094 seconds — under a tenth of a second (2), less time than it takes to blink (1).
  • Q27 (4): Any reasonable pair, 2 each. The roll is better at duration — you physically walk it, and boredom is part of the lesson; it also survives on a wall. The day is better at the very recent end, because seconds are a unit we have intuition for, where 1.7 mm of paper is not; it also needs no equipment at all.
  • Q28 (3): One sentence containing one figure, e.g. "On a clock where Earth forms at midnight and it is now midnight again, our species appears at 23:59:54 — we have been here for six seconds of a 24-hour day." (3)

Investigation 5 — the decay curve

  • Q29 (8): 2 half-lives → 10.52 y, 2.00 g, 25% · 3 → 15.78 y, 1.00 g, 12.5% · 4 → 21.04 y, 0.50 g, 6.25% · 5 → 26.30 y, 0.25 g, 3.125% · 6 → 31.56 y, 0.125 g, 1.5625%. (Roughly 1.5 per row; be generous on the recurring percentages.)
  • Q30 (8): As allocated. The commonest error is joining the points with straight lines — decay is exponential and the curve must be smooth and always falling, never reaching the axis.
  • Q31 (4): 0.50 g is 1/16 of 8.00 g = 2⁻⁴, so 4 half-lives = 4 × 5.26 = 21.04 years (3), and the graph should be read at the same point (1).
  • Q32 (4): Reading off gives roughly 7.4 years (2); accept 7–8 years. You cannot count half-lives because 3.0 g is not a simple fraction of 8.00 g — 3/8 is not a power of one-half, so the age falls between whole half-lives and only the curve can give it (2). This is precisely why the exam gives you a graph rather than a table.
  • Q33 (4): Each half-life removes half of what is left, so there is always something remaining — mathematically it approaches zero without arriving (2). For very old rock the surviving parent becomes so small that measurement error swamps it, which is what sets the practical upper limit of any isotope, and why different isotopes are used for different age ranges (2).
  • Q34 (4): Carbon-14's half-life is only 5 730 years, so after 200 million years — some 35 000 half-lives — no measurable ¹⁴C remains at all (2). Use Potassium-40 (1.25 by) or Uranium-238 (4.5 by) (2). Both also require igneous rock, which is the Investigation-2 link back to bracketing.
  • Q35 (4): Use the number the question gives you, because the marks are for the method — counting half-lives and reading the graph — not for the constant (2). The booklet has confused Potassium-40 with Uranium-238, whose half-life genuinely is 4.468 billion years and which is quoted correctly one line earlier in the same passage (2).

Marking note. Investigations 2, 3 and 4 all model the same 4 600 million years, and a learner who has done all three should be able to move between them. If the three sets of answers are internally inconsistent — a Cambrian explosion at 88% of the roll but at 15:00 on the clock — that is worth flagging even though no single question asks for it.