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Udurchukan Formation

Udurchukan 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 Udurchukan Formation rather than just read about it. In short: The Udurchukan Formation is a geological formation located in Amur Region, Far East Russia. Based on palynomorphs such as Wodehouseia spinata, the Udurchukan is considered of Maastrichtian age of the Late Cretaceous, during the Cretaceous Period.

Udurchukan Formation — main illustration
Udurchukan Formation — illustration

Key takeaways

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

Reference excerpt

The Udurchukan Formation is a geological formation located in Amur Region, Far East Russia. Based on palynomorphs such as Wodehouseia spinata, the Udurchukan is considered of Maastrichtian age of the Late Cretaceous, during the Cretaceous Period.

Fossil contnt

Since Wodehouseia spinata and Aquillapollenites subtilis are known in the Americas only from the Late Maastrichtian, the presence of these palynomorphs in the Udurchukan caused Godefroit to consider the unit and its lambeosaurine dominated fauna to be coeval with the Lance Formation and Hell Creek Formation. However, research in the Songliao Basin indicates Wodehouseia spinata is also known from the early (albeit not basal) and middle Maastrichtian of Asia.

Dinosaurs

Ornithischians

Ankylosaurs

Hadrosaurs

Sauropods

Theropods

Reptiles

Mammals

Insects

Flora

See also Geology of Russia Fossils of Russia

References

Bibliography Y. A. Popov. 1971. Historical development of the infraorder Nepomorpha (Heteroptera). Akademiya Nauk SSSR, Trudy Paleontologicheskogo Instituta 129:1-228

Illustrations

Udurchukan Formation illustration
Udurchukan Formation illustration
Udurchukan Formation illustration
Udurchukan Formation illustration
Udurchukan Formation illustration

Worked examples

Example 1 — a first encounter with Udurchukan Formation

Start with the simplest possible case. Write down what Udurchukan 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 Udurchukan 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 Udurchukan 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 Udurchukan Formation

In research
Udurchukan 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 Udurchukan 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
Udurchukan Formation is common in secondary-school and first-year university syllabi. It links to neighbouring topics Conglomerate formations, Cretaceous Russia, Fluvial deposits, so understanding it makes those chapters shorter.
In everyday life
Look for Udurchukan 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 Udurchukan Formation in 20 minutes

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

Frequently asked questions

What is Udurchukan Formation in simple terms?

The Udurchukan Formation is a geological formation located in Amur Region, Far East Russia. Based on palynomorphs such as Wodehouseia spinata, the Udurchukan is considered of Maastrichtian age of the Late Cretaceous, during the Cretaceous Period.

Why does Udurchukan 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 Udurchukan 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 Udurchukan Formation.

Tags

  • Conglomerate formations
  • Cretaceous Russia
  • Fluvial deposits
  • Geography of Amur Oblast
  • Geologic formations of Russia
  • Geology of the Russian Far East
  • Maastrichtian Stage
  • Mudstone formations
  • Paleontology in Russia
  • Sandstone formations
  • Upper Cretaceous Series of Asia

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