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Orosirian

Orosirian 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 Orosirian rather than just read about it. In short: The Orosirian ( ; Ancient Greek: ὀροσειρά, romanized: oroseirá, meaning "mountain range") is the third geologic period in the Paleoproterozoic Era. It spans 250 million years and lasted from 2050 to 1800 million years ago (Ma), following the Rhyacian Period and preceding the Statherian Period.

Orosirian — main illustration
Orosirian — illustration

Key takeaways

  • Orosirian 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 Orosirian to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Orosirian from memory before moving on to harder problems.

Reference excerpt

The Orosirian ( ; Ancient Greek: ὀροσειρά, romanized: oroseirá, meaning "mountain range") is the third geologic period in the Paleoproterozoic Era. It spans 250 million years and lasted from 2050 to 1800 million years ago (Ma), following the Rhyacian Period and preceding the Statherian Period. Instead of being based on stratigraphy, these dates are defined chronometrically.

History For the time period from about 2060 to 1780 Mya, an alternative period based on stratigraphy rather than chronometry, named the Columbian, was suggested in the geological timescale review 2012 edited by Gradstein et al., but as of February 2022, this has not yet been officially adopted by the IUGS.

Paleogeography

Two of the largest known impact events on Earth occurred during the Orosirian. Early in the period, 2023 Mya, a large asteroid collision created the Vredefort impact structure. The event that created the Sudbury Basin structure occurred near the end of the period, 1850 Mya. The later half of the period was an episode of intensive orogeny on virtually all continents. The supercontinent Columbia may have formed at the end of this period.

References

Further reading "Orosirian Period". GeoWhen Database. Retrieved July 8, 2011. James G. Ogg (2004). "Status on Divisions of the International Geologic Time Scale". Lethaia. 37 (2): 183–199. doi:10.1080/00241160410006492. David Huddart; Tim Stott (16 April 2013). Earth Environments: Past, Present and Future. John Wiley & Sons. pp. 1599–. ISBN 978-1-118-68812-0.

Illustrations

Orosirian illustration
Orosirian: Vredefort impact structure is believed to have formed in this period
Vredefort impact structure is believed to have formed in this period

Worked examples

Example 1 — a first encounter with Orosirian

Start with the simplest possible case. Write down what Orosirian 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 Orosirian 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 Orosirian 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 Orosirian

In research
Orosirian 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 Orosirian 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
Orosirian is common in secondary-school and first-year university syllabi. It links to neighbouring topics Geochronology stubs, Geological periods, Paleoproterozoic, so understanding it makes those chapters shorter.
In everyday life
Look for Orosirian 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 Orosirian in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Orosirian 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 Orosirian out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Orosirian in simple terms?

The Orosirian ( ; Ancient Greek: ὀροσειρά, romanized: oroseirá, meaning "mountain range") is the third geologic period in the Paleoproterozoic Era. It spans 250 million years and lasted from 2050 to 1800 million years ago (Ma), following the Rhyacian Period and preceding the Statherian Period.

Why does Orosirian 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 Orosirian?

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 Orosirian.

Tags

  • Geochronology stubs
  • Geological periods
  • Paleoproterozoic
  • Proterozoic geochronology

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