ArticleslgStudy

earth science

Pebidian Supergroup

Pebidian Supergroup 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 Pebidian Supergroup rather than just read about it. In short: The Pebidian Supergroup is an Ediacaran (i.e. late Precambrian) lithostratigraphic supergroup (a sequence of rock strata) in Pembrokeshire, west Wales. The term 'Pebidian' (along with Dimetian) was coined by geologist Henry Hicks in 1876 and published in a scientific paper in the Quarterly Journal of the Geological Society in the following year.

Key takeaways

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

Reference excerpt

The Pebidian Supergroup is an Ediacaran (i.e. late Precambrian) lithostratigraphic supergroup (a sequence of rock strata) in Pembrokeshire, west Wales. The term 'Pebidian' (along with Dimetian) was coined by geologist Henry Hicks in 1876 and published in a scientific paper in the Quarterly Journal of the Geological Society in the following year. It was named for Pebidiauc, an ancient local name for the St Davids area.

Outcrops These rocks are exposed in the St David's peninsula in northwestern Pembrokeshire. One outcrop stretches east from Treginnis, wrapping around the north of St David's to Treglemais. Another underlies Hayscastle Cross with scattered outcrops elsewhere in the area.

Lithology and stratigraphy The supergroup comprises at its base the Treginnis, Treglemais and Penrhiw 'Groups' of the Lower Pebidian which include trachytic and andesitic tuffs and halleflinta. Overlying these are the tuffs, lavas and conglomerates of the Caerbwdy Group, Ramsey Sound Group and the Rhosson Group. Uppermost i.e. youngest is the Ogofgolchfa Group which includes slates and tuffs. This whole assemblage has also been referred to as the Pebidian Volcanic Complex or Pebidian Volcanic Series.

References

Worked examples

Example 1 — a first encounter with Pebidian Supergroup

Start with the simplest possible case. Write down what Pebidian Supergroup 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 Pebidian Supergroup 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 Pebidian Supergroup 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 Pebidian Supergroup

In research
Pebidian Supergroup 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 Pebidian Supergroup 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
Pebidian Supergroup is common in secondary-school and first-year university syllabi. It links to neighbouring topics Conglomerate groups, Ediacaran Europe, Ediacaran geology, so understanding it makes those chapters shorter.
In everyday life
Look for Pebidian Supergroup 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.
Ask Teacher Smith questions about this articleOpens your AI tutor with a question about “Pebidian Supergroup” →

Affiliate

Preply — study more efficiently by working with a personal tutor. 50% off.

How to study Pebidian Supergroup in 20 minutes

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

Frequently asked questions

What is Pebidian Supergroup in simple terms?

The Pebidian Supergroup is an Ediacaran (i.e. late Precambrian) lithostratigraphic supergroup (a sequence of rock strata) in Pembrokeshire, west Wales. The term 'Pebidian' (along with Dimetian) was coined by geologist Henry Hicks in 1876 and published in a scientific paper in the Quarterly Journal…

Why does Pebidian Supergroup 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 Pebidian Supergroup?

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 Pebidian Supergroup.

Tags

  • Conglomerate groups
  • Ediacaran Europe
  • Ediacaran geology
  • Geologic supergroups of the United Kingdom
  • Geology of Wales
  • Trachyte formations
  • Tuff formations of the United Kingdom

Keep exploring