ArticleslgStudy

earth science

Jean-Baptiste Élie de Beaumont

Jean-Baptiste Élie de Beaumont 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 Jean-Baptiste Élie de Beaumont rather than just read about it. In short: Jean-Baptiste Armand Louis Léonce Élie de Beaumont (25 September 1798 – 21 September 1874) was a French geologist. Among his ideas was that mountains were created in a series of episodes over geological time due to the cooling and shrinking of the earth.

Jean-Baptiste Élie de Beaumont — main illustration
Jean-Baptiste Élie de Beaumont — illustration

Key takeaways

  • Jean-Baptiste Élie de Beaumont 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 Jean-Baptiste Élie de Beaumont to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Jean-Baptiste Élie de Beaumont from memory before moving on to harder problems.

Reference excerpt

Jean-Baptiste Armand Louis Léonce Élie de Beaumont (25 September 1798 – 21 September 1874) was a French geologist. Among his ideas was that mountains were created in a series of episodes over geological time due to the cooling and shrinking of the earth. He also suggested that there was a pattern in the orientation of the mountain systems of the world which followed a system of five circles meeting at points on the earth that marked the points of a polyhedron.

Biography Élie de Beaumont was born in a family castle in Canon, in Calvados. He was educated at the Lycee Henri IV where he took the first prize in mathematics and physics at the École polytechnique, where he stood first at the exit examination in 1819; and at the École des mines (1819–1822), where he began to show a decided preference for the science with which his name is associated. In 1823 he was selected along with Dufrénoy by Brochant de Villiers, the professor of geology in the École des Mines, to accompany him on a scientific tour to England and Scotland, in order to inspect the mining and metallurgical establishments of the country, and to study the principles on which George Bellas Greenough's geological map of England (1820) had been prepared, with a view to the construction of a similar map of France.

In 1832 he succeeded Georges Cuvier's chair of natural history at the Collège de France. In 1835 he was appointed professor of geology at the École des Mines, in succession to Brochant de Villiers, whose assistant he had been in the duties of the chair since 1827. He held the office of engineer-in-chief of mines in France from 1833 until 1847, when he was appointed inspector-general; and in 1861 he became vice-president of the Conseil-General des Mines and a grand officer of the Legion of Honour. His growing scientific reputation secured his election to the membership of the Academy of Berlin, of the French Academy of Sciences, of the Royal Society of Edinburgh (1845), of the Royal Society of London, as a foreign member of the Royal Swedish Academy of Sciences (1848), and as an international member of the American Philosophical Society (1860). By a decree of the president he was made a senator of France in 1852, and on the death of François Arago in 1853 he was chosen as perpetual secretary of the Academy of Sciences. Élie de Beaumont's name is widely known to geologists in connection with his theory of the origin of mountain ranges, first propounded in a paper read to the Academy of Sciences in 1829, and afterwards elaborated in his Notice sur le système des montagnes (3 volumes, 1852). According to his view, all mountain ranges parallel to the same great circle of the earth are of strictly contemporaneous origin, and between the great circles a relation of symmetry exists in the form of a pentagonal réseau. An elaborate statement and criticism of the theory was given in his anniversary address to the Geological Society of London in 1853 by William Hopkins. The theory did not find general acceptance, but it proved of great value to geological science, owing to the extensive additions to the knowledge of the structure of mountain ranges which its author made in endeavouring to find facts to support it. Mount Elie de Beaumont is in the Westland Tai Poutini National Park, on the west coast of New Zealand's the South Island and near the boundary with Aoraki / Mount Cook National Park. It is 3109m high. Probably the best service Élie de Beaumont rendered to science, however, was in connection with the geological map of France, in the preparation of which he had the leading share. During this period Élie de Beaumont published many important memoirs on the geology of the country. After his retirement from the École des Mines he continued to superintend the issue of the detailed maps almost until his death, which occurred at Canon. His academic lectures for 1843-1844 were published in 2 volumes, (1845–1849), under the title Leçons de Géologie pratique. The Beaumont crater on the Moon is named after him.

References

This article incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Élie de Beaumont, Jean Baptiste Armand Louis Léonce". Encyclopædia Britannica. Vol. 9 (11th ed.). Cambridge University Press. pp. 272–273. Catholic Encyclopedia article

Illustrations

Jean-Baptiste Élie de Beaumont illustration
Jean-Baptiste Élie de Beaumont: Élie de Beaumont's theory of pentagonal networks of mountain chains on the Earth
Élie de Beaumont's theory of pentagonal networks of mountain chains on the Earth

Worked examples

Example 1 — a first encounter with Jean-Baptiste Élie de Beaumont

Start with the simplest possible case. Write down what Jean-Baptiste Élie de Beaumont 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 Jean-Baptiste Élie de Beaumont 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 Jean-Baptiste Élie de Beaumont 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 Jean-Baptiste Élie de Beaumont

In research
Jean-Baptiste Élie de Beaumont 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 Jean-Baptiste Élie de Beaumont 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
Jean-Baptiste Élie de Beaumont is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1798 births, 1874 deaths, Corps des mines, so understanding it makes those chapters shorter.
In everyday life
Look for Jean-Baptiste Élie de Beaumont 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.
Ask Teacher Smith questions about this articleOpens your AI tutor with a question about “Jean-Baptiste Élie de Beaumont” →

Affiliate

Preply — study more efficiently by working with a personal tutor. 50% off.

How to study Jean-Baptiste Élie de Beaumont in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Jean-Baptiste Élie de Beaumont 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 Jean-Baptiste Élie de Beaumont out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Jean-Baptiste Élie de Beaumont in simple terms?

Jean-Baptiste Armand Louis Léonce Élie de Beaumont (25 September 1798 – 21 September 1874) was a French geologist. Among his ideas was that mountains were created in a series of episodes over geological time due to the cooling and shrinking of the earth.

Why does Jean-Baptiste Élie de Beaumont 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 Jean-Baptiste Élie de Beaumont?

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 Jean-Baptiste Élie de Beaumont.

Tags

  • 1798 births
  • 1874 deaths
  • Corps des mines
  • Fellows of the Royal Society of Edinburgh
  • Foreign members of the Royal Society
  • French fellows of the Royal Society
  • French geologists
  • French mining engineers
  • International members of the American Philosophical Society
  • International members of the National Academy of Sciences
  • Lycée Henri-IV alumni
  • Members of the French Academy of Sciences

Keep exploring