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Upper Bedoulian Formation

Upper Bedoulian Formation 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 Upper Bedoulian Formation rather than just read about it. In short: The Upper Bedoulian Formation is a geological formation in the Murcia Region, Spain whose strata date back to the Early Cretaceous (late Barremian to early Aptian stage). The marls were deposited in an open marine environment.

Upper Bedoulian Formation — main illustration
Upper Bedoulian Formation — illustration

Key takeaways

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

Reference excerpt

The Upper Bedoulian Formation is a geological formation in the Murcia Region, Spain whose strata date back to the Early Cretaceous (late Barremian to early Aptian stage). The marls were deposited in an open marine environment. The lower unit (30 metres (98 ft) thick) is marly with iron concretions and septaria. The formation was deposited in the Pre-Betic Basin in southeastern Spain. During deposition, Iberia was an island, separated by seas from North Africa and France. The Upper Bedoulian Formation has provided very few fossils; the ammonite Dufrenoyia dufrenoyi and the coral Montlivaltia multiformis.

Correlation

See also La Huérguina Formation, Barremian-Aptian Lagerstätte of the South Iberian Basin Arcillas de Morella Formation, Barremian-Aptian formation of the Morella Basin Xert Formation, Barremian-Aptian formation of the Maestrazgo Basin

References

Bibliography Morycowa, E.; Masse, J.P.; Arias, C.; Vilas, L. (2001), "Montlivaltia multiformis Toula (Scleractinia) from the Aptian of the Prebetic Domain (SE Spain)" (PDF), Revista Espanola de Paleontologia, 16: 131–144, retrieved 2019-10-10

Illustrations

Upper Bedoulian Formation illustration
Upper Bedoulian Formation illustration

Worked examples

Example 1 — a first encounter with Upper Bedoulian Formation

Start with the simplest possible case. Write down what Upper Bedoulian Formation 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 Upper Bedoulian Formation 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 Upper Bedoulian Formation 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 Upper Bedoulian Formation

In research
Upper Bedoulian Formation 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 Upper Bedoulian Formation 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
Upper Bedoulian Formation is common in secondary-school and first-year university syllabi. It links to neighbouring topics Aptian Stage, Barremian Stage, Cretaceous Spain, so understanding it makes those chapters shorter.
In everyday life
Look for Upper Bedoulian Formation 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 Upper Bedoulian Formation in 20 minutes

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

Frequently asked questions

What is Upper Bedoulian Formation in simple terms?

The Upper Bedoulian Formation is a geological formation in the Murcia Region, Spain whose strata date back to the Early Cretaceous (late Barremian to early Aptian stage). The marls were deposited in an open marine environment.

Why does Upper Bedoulian Formation 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 Upper Bedoulian Formation?

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 Upper Bedoulian Formation.

Tags

  • Aptian Stage
  • Barremian Stage
  • Cretaceous Spain
  • Geography of the Region of Murcia
  • Geologic formations of Spain
  • Lower Cretaceous Series of Europe
  • Marl formations
  • Open marine deposits
  • Paleontology in Spain

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