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Schriebers Meadow Cone

Schriebers Meadow Cone 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 Schriebers Meadow Cone rather than just read about it. In short: Schriebers Meadow Cone is a small parasitic cone on the southeastern flank of Mount Baker in the U.S. state of Washington. It was formed about 9,800 years ago by the only known Holocene flank eruption of Mount Baker.

Schriebers Meadow Cone — main illustration
Schriebers Meadow Cone — illustration

Key takeaways

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

Reference excerpt

Schriebers Meadow Cone is a small parasitic cone on the southeastern flank of Mount Baker in the U.S. state of Washington. It was formed about 9,800 years ago by the only known Holocene flank eruption of Mount Baker. A basaltic lava flow traveled down the Sulphur Creek valley and across the Baker River valley; this is the most recent lava flow at Mount Baker. Future eruptions from Schriebers Meadow Cone are unlikely to occur as it is considered a short-lived feature. Schriebers Meadow Cone produced thick dark-reddish-brown to yellowish-red scoria that blankets the sides of the Sulphur Creek valley near and southeast of Schriebers Meadow. Near Schriebers Meadow the scoria deposit is thickest on the north valley wall and it decreases in grain size and thickness within short distances. Within 0.62 mi (1.00 km) of the cone the scoria fragments are as much as 9.8 in (25 cm) in diameter and the deposit is 20 to 39 in (51 to 99 cm) thick; 3.7 mi (6.0 km) to the northeast the fragments are of sand size and the deposit is no more than 1.2 in (3.0 cm) thick.

References

Illustrations

Schriebers Meadow Cone illustration

Worked examples

Example 1 — a first encounter with Schriebers Meadow Cone

Start with the simplest possible case. Write down what Schriebers Meadow Cone 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 Schriebers Meadow Cone 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 Schriebers Meadow Cone 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 Schriebers Meadow Cone

In research
Schriebers Meadow Cone 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 Schriebers Meadow Cone 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
Schriebers Meadow Cone is common in secondary-school and first-year university syllabi. It links to neighbouring topics Cascade Volcanoes, Cinder cones of the United States, Holocene cinder cones, so understanding it makes those chapters shorter.
In everyday life
Look for Schriebers Meadow Cone 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 Schriebers Meadow Cone in 20 minutes

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

Frequently asked questions

What is Schriebers Meadow Cone in simple terms?

Schriebers Meadow Cone is a small parasitic cone on the southeastern flank of Mount Baker in the U.S. state of Washington. It was formed about 9,800 years ago by the only known Holocene flank eruption of Mount Baker.

Why does Schriebers Meadow Cone 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 Schriebers Meadow Cone?

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 Schriebers Meadow Cone.

Tags

  • Cascade Volcanoes
  • Cinder cones of the United States
  • Holocene cinder cones
  • Mount Baker
  • Parasitic cones
  • Volcanoes of Washington (state)
  • Whatcom County, Washington, geography stubs

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