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John Verhoogen

John Verhoogen 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 John Verhoogen rather than just read about it. In short: John Verhoogen (born Jean Verhoogen, 1 February 1912, Brussels – 8 November 1993) was a Belgian-American geologist and geophysicist. Verhoogen became ill at age 17 from poliomyelitis, which caused him problems throughout the rest of his life.

Key takeaways

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

Reference excerpt

John Verhoogen (born Jean Verhoogen, 1 February 1912, Brussels – 8 November 1993) was a Belgian-American geologist and geophysicist. Verhoogen became ill at age 17 from poliomyelitis, which caused him problems throughout the rest of his life. Nevertheless, he studied mining at the University of Brussels (Ingénieur des Mines, degree 1933) and engineering geology at the University of Liège (Ingénieur-Géologue, degree 1934). He then went to the US, where he studied at the University of California, Berkeley under Howel Williams. In 1936 he received his doctorate in geology (with thesis Geology of Mt. St. Helens, Washington) from Stanford University, although most of the doctoral work was supervised by Williams at Berkeley. Verhoogen was then at the University of Brussels from 1936 to 1939. During the late 1930s and World War II, he was in the Belgian Congo, where he studied the volcano Nyamuragira and worked on the procurement of strategic mineral resources. From 1947 he was at the University of California, Berkeley, where he became a professor and remained until his retirement in 1976. He was an early advocate of plate tectonics (according to his own words, because at Brussels his professor Paul Fourmarier was a vehement opponent of plate tectonics). In the 1950s, Verhoogen at Berkeley was responsible for the expansion of research in geochronology with isotopes and paleomagnetism. He was the coauthor of an influential textbook on petrology. He is known for the development of a theory of thermodynamics of the formation of rocks and application of thermodynamics on processes in the Earth's mantle and crust, establishing convection as the dominant mode of heat transfer.

In 1961 he calculated the latent heat release associated with inner-core solidification and concluded it would indeed drive thermal convection in the outer core and, furthermore, could be a source of energy for generating Earth's magnetic field through dynamo action in the electrically conducting fluid outer core. Verhoogen was elected in 1956 a member of the National Academy of Sciences. He was a fellow of the American Academy of Arts and Sciences (elected 1970), the Royal Astronomical Society (elected 1950), the American Geophysical Union, and the Geological Society of America. In 1978 he received the Arthur L. Day Prize and Lectureship and in 1958 he received the Arthur L. Day Medal. He was twice a Guggenheim Fellow (academic years 1953-1954 and 1960–1961) and received the André Dumont Medal of the Belgian Geological Society. From 1951 to 1954 he was Vice President of the International Association of Volcanology and Chemistry of the Earth's Interior. He was married to Ilse Goldschmidt, a native of Austria. He was predeceased by his wife and was survived by two sons, two daughters, and seven grandchildren. His doctoral students include Allan V. Cox and Richard Doell.

Selected publications with Francis John Turner, Lionel E. Weiss, Clyde Wahrhaftig, and William S. Fyfe: The Earth: An Introduction to Physical Geology. Holt, Rinehart and Winston, 1970. with Francis John Turner: Igneous and Metamorphic Petrology. McGraw Hill 1951. revised edition with Ian S. E. Carmichael and F. T. Turner: Igneous Petrology. 1974. Energetics of the Earth. Arthur L. Day Lecture, National Academy of Sciences Press 1980.

References

External links Oral history interview transcript with John Verhoogen on 6 November 1990, American Institute of Physics, Niels Bohr Library & Archives "Finding Aid to the John Verhoogen Papers, 1935–1985". Online Archive of California.

Worked examples

Example 1 — a first encounter with John Verhoogen

Start with the simplest possible case. Write down what John Verhoogen 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 John Verhoogen 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 John Verhoogen 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 John Verhoogen

In research
John Verhoogen 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 John Verhoogen 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
John Verhoogen is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1912 births, 1993 deaths, 20th-century American geologists, so understanding it makes those chapters shorter.
In everyday life
Look for John Verhoogen 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 John Verhoogen in 20 minutes

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

Frequently asked questions

What is John Verhoogen in simple terms?

John Verhoogen (born Jean Verhoogen, 1 February 1912, Brussels – 8 November 1993) was a Belgian-American geologist and geophysicist. Verhoogen became ill at age 17 from poliomyelitis, which caused him problems throughout the rest of his life.

Why does John Verhoogen 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 John Verhoogen?

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 John Verhoogen.

Tags

  • 1912 births
  • 1993 deaths
  • 20th-century American geologists
  • 20th-century American physicists
  • American geophysicists
  • Belgian emigrants to the United States
  • Belgian geologists
  • Fellows of the American Academy of Arts and Sciences
  • Fellows of the American Geophysical Union
  • Fellows of the Geological Society of America
  • Fellows of the Royal Astronomical Society
  • Members of the United States National Academy of Sciences

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