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Pongola glaciation

Pongola glaciation is a earth science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Pongola glaciation rather than just read about it. In short: The Pongola glaciation was a glacial period that occurred in the Mesoarchean, from around 2.985-2.837 billion years ago. It is the oldest known glaciation on Earth.

Key takeaways

  • Pongola glaciation belongs to earth science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Pongola glaciation to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Pongola glaciation from memory before moving on to harder problems.

Reference excerpt

The Pongola glaciation was a glacial period that occurred in the Mesoarchean, from around 2.985-2.837 billion years ago. It is the oldest known glaciation on Earth.

Geology The oldest known traces of glaciation date from the Mesoarchean. They correspond to the diamictite of the Pongola supergroup (more precisely to the Mozaan formation,) in KwaZulu-Natal and in Eswatini.

Climate Even if the climate of the Mesoarchean is not well known, the study of the oxygen isotopes in the cherts of the time seem to show that the climate of the Mesoarchean was warm or, at least, temperate, in particular due to high levels of methane and carbon dioxide in the atmosphere; a glaciation is therefore likely to have been caused by a drop in the rate of these greenhouse gases. The Pongola glaciation is also associated with changes in sulfur isotopes (δ34S), suggesting that this may also involve early and short-lived oxygenation of the Earth's atmosphere.

Extension The extension of the glaciation is not determined with certainty. Some authors argue that the glacial deposits were formed at low latitudes, below 30° N, therefore close to the tropics, which would imply extensive glaciation, while others argue that the area was located at mid-latitude or even high latitude, closer to the pole, where a polar glacier could have formed, like the current situation. Regarding its duration, the corresponding glacial deposits fall within the interval 2.985 ± 1 and 2.837 ± 5 Bya.

See also

Huronian glaciation

References

Bibliography Deconinck, J.F. "Variabilité climatique et cycles géodynamiques" (PDF) (in French). CNRS. "Pongola supergroup. The first record of ancient life". University of KwaZulu-Natal. Young, Grant M.; von Brunn, Victor; Gold, Digby J. C.; Minter, W. E. L. (1998). "Earth's Oldest Reported Glaciation: Physical and Chemical Evidence from the Archean Mozaan Group (~2.9 Ga) of South Africa". The Journal of Geology. 106 (5): 523-538. doi:10.1086/516039. S2CID 129717765. Kopp, Robert E.; Kirschvink, Joseph L.; Hilburn, Isaac A.; Nash, Cody Z. (9 August 2005). "The Paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesis". PNAS. 102 (32): 11131–11136. doi:10.1073/pnas.0504878102. PMC 1183582. PMID 16061801. Gold, D.J.C.; Johnson, M.R.; Anhaeusser, C.R.; Thomas, Bob (2006). "The Pongola Supergroup. The geology of South Africa". Geol. Soc. South Afr.: 135-148. Kasting, James F.; Ono, Shuhei (29 June 2006). "Palaeoclimates: the first two billion years". Philosophical Transactions B. 361 (1470): 917–929. doi:10.1098/rstb.2006.1839. PMC 1868609. PMID 16754607. Kasting, James F.; Howard, M. Tazewell (29 October 2006). "Atmospheric composition and climate on the early Earth". Philosophical Transactions B. 361 (1474): 1733–1742. doi:10.1098/rstb.2006.1902. PMC 1664689. PMID 17008214. Antarctica: A Keystone in a Changing World. National Academies Press. 2008. ISBN 9780309118545. Zalasiewicz, Jan; Williams, Mark (2012). The Goldilocks Planet: The 4 billion year story of Earth's climate. Oxford University Press. ISBN 978-0-19-959357-6. Alain R. Meunier (2014). La naissance de la Terre (in French). Dunod. p. 235. El Albani, Abderrazak; Macchiarelli, Roberto; Meunier, Alain R. (2016). Aux origines de la vie: Une nouvelle histoire de l'évolution (in French). Dunod. ISBN 9782100748259.

Worked examples

Example 1 — a first encounter with Pongola glaciation

Start with the simplest possible case. Write down what Pongola glaciation claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In earth science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Pongola glaciation before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Pongola glaciation ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Pongola glaciation

In research
Pongola glaciation appears in earth science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Pongola glaciation in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Pongola glaciation is common in secondary-school and first-year university syllabi. It links to neighbouring topics Geography of KwaZulu-Natal, Geology of Eswatini, Geology of South Africa, so understanding it makes those chapters shorter.
In everyday life
Look for Pongola glaciation outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Pongola glaciation in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Pongola glaciation means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Pongola glaciation out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Pongola glaciation in simple terms?

The Pongola glaciation was a glacial period that occurred in the Mesoarchean, from around 2.985-2.837 billion years ago. It is the oldest known glaciation on Earth.

Why does Pongola glaciation matter?

Because it connects several earth science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Pongola glaciation?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Pongola glaciation.

Tags

  • Geography of KwaZulu-Natal
  • Geology of Eswatini
  • Geology of South Africa
  • Ice ages

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