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Geophysical global cooling

Geophysical global cooling is a physics 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 Geophysical global cooling rather than just read about it. In short: Before the concept of plate tectonics, global cooling was a geophysical theory by James Dwight Dana, also referred to as the contracting earth theory. It suggested that the Earth had been in a molten state, and features such as mountains formed as it cooled and shrank.

Geophysical global cooling — main illustration
Geophysical global cooling — illustration

Key takeaways

  • Geophysical global cooling belongs to physics; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Geophysical global cooling to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Geophysical global cooling from memory before moving on to harder problems.

Reference excerpt

Before the concept of plate tectonics, global cooling was a geophysical theory by James Dwight Dana, also referred to as the contracting earth theory. It suggested that the Earth had been in a molten state, and features such as mountains formed as it cooled and shrank. As the interior of the Earth cooled and shrank, the rigid crust would have to shrink and crumple. The crumpling could produce features such as mountain ranges.

Application The Earth was compared to a cooling ball of iron, or a steam boiler with shifting boiler plates. By the early 1900s, it was known that temperature increased with increasing depth. With the thickness of the crust, the "boiler plates", being estimated at ten to fifty miles, the downward pressure would be hundreds of thousands of pounds per square inch. Although groundwater was expected to turn to steam at a great depth, usually the downward pressure would contain any steam. Steam's effect upon molten rock was suspected of being a cause of volcanoes and earthquakes, as it had been noticed that most volcanoes are near water. It was not clear whether the molten rock from volcanoes had its origin in the molten rock under the crust, or if increased heat due to pressure under mountains caused the rock to melt. One of the reasons for volcanoes was as a way in which "the contracting earth disposes of the matter it can no longer contain." A relationship between earthquakes and volcanoes had been noted, although the causes were not known. Fault lines and earthquakes tended to happen along the boundaries of the shifting "boiler plates", but the folding of mountains indicated that sometimes the plates buckled. In the early 1900s, Professor Eduard Suess used the theory to explain the 1908 Messina earthquake, being of the opinion that the Earth's crust was gradually shrinking everywhere. He also predicted that eruptions would follow the earthquake and tsunami in Southern Italy. He attributed the earthquake to the sinking of the Earth's crust, in the zone of which the Aeolian Islands are the center. He declared that as the process of sinking went on, the Calabrian and Sicilian highlands on either side of the Straits of Messina would be submerged, only the highest peaks remaining above the sea. The strait, he said, would thereby be greatly widened. Similarly, Professor Robert T. Hill explained at that time that "the rocks are being folded, fractured and otherwise broken or deformed by the great shrinking and settling of the earth's crust as a whole. The contraction of the earth's sphere is the physical shrinkage of age that is measured in aeons instead of years. The prehistoric convulsions of the earth before man inhabited this planet were terrific, almost inconceivable." There "was no doubt that earthquakes are diminishing." The displacement of the 1906 San Francisco earthquake was only a few feet, while prehistoric earthquakes made fissures and slides of 20,000 feet.

The Pacific Ring of Fire had been noticed, as well as a second earthquake belt which went through:

the Philippines Panama the Caribbean Spain the Alps the Himalayas Asia to Japan A contracting Earth served as framework for Leopold Kober and Hans Stille who worked on geosyncline theory in the first half of the 20th century.

Objections Some of the objections include:

Some large-scale features of the Earth are the result of extension rather than shortening. After radioactive decay was discovered, it was realized it would release heat inside the planet. This undermines the cooling effect upon which the shrinking planet theory is based. Identical fossils have been found thousands of kilometres apart, showing the planet was once a single continent which broke apart because of plate tectonics.

Current status This theory is now disproven and considered obsolete. In contrast to Earth, however, global cooling remains the dominant explanation for scarp (cliff) features on the planet Mercury. After resumption of Lunar exploration in the 1990s, it was discovered there are scarps across the Moon's surface which are caused by contraction due to cooling.

See also Expanding Earth Timeline of the development of tectonophysics

References

Bibliography Şengör, Celâl (1982). "Classical theories of orogenesis". In Miyashiro, Akiho; Aki, Keiiti; Şengör, Celâl (eds.). Orogeny. John Wiley & Sons. ISBN 0-471-103764.

Worked examples

Example 1 — a first encounter with Geophysical global cooling

Start with the simplest possible case. Write down what Geophysical global cooling claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In physics, 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 Geophysical global cooling 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 Geophysical global cooling 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 Geophysical global cooling

In research
Geophysical global cooling appears in physics 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 Geophysical global cooling 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
Geophysical global cooling is common in secondary-school and first-year university syllabi. It links to neighbouring topics Geodynamics, Geophysics, Obsolete geology theories, so understanding it makes those chapters shorter.
In everyday life
Look for Geophysical global cooling 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 Geophysical global cooling in 20 minutes

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

Frequently asked questions

What is Geophysical global cooling in simple terms?

Before the concept of plate tectonics, global cooling was a geophysical theory by James Dwight Dana, also referred to as the contracting earth theory. It suggested that the Earth had been in a molten state, and features such as mountains formed as it cooled and shrank.

Why does Geophysical global cooling matter?

Because it connects several physics 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 Geophysical global cooling?

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 Geophysical global cooling.

Tags

  • Geodynamics
  • Geophysics
  • Obsolete geology theories

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