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Geological Evidences of the Antiquity of Man

Geological Evidences of the Antiquity of Man 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 Geological Evidences of the Antiquity of Man rather than just read about it. In short: Geological Evidences of the Antiquity of Man is a book written by British geologist, Charles Lyell in 1863. The first three editions appeared in February, April, and November 1863, respectively.

Geological Evidences of the Antiquity of Man — main illustration
Geological Evidences of the Antiquity of Man — illustration

Key takeaways

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

Reference excerpt

Geological Evidences of the Antiquity of Man is a book written by British geologist, Charles Lyell in 1863. The first three editions appeared in February, April, and November 1863, respectively. A much-revised fourth edition appeared in 1873. Antiquity of Man, as it was known to contemporary readers, dealt with three scientific issues that had become prominent in the preceding decade: the age of the human race, the existence of ice ages, and Charles Darwin's theory of evolution by natural selection. Lyell used the book to reverse or modify his own long-held positions on all three issues. The book drew sharp criticism from two of Lyell's younger colleagues – paleontologist Hugh Falconer and archaeologist John Lubbock – who felt that Lyell had used their work too freely and acknowledged it too sparingly. It sold well, however, and (along with Lubbock's 1865 book Prehistoric Times) helped to establish the new science of prehistoric archaeology in Great Britain.

Background Lyell had been consistently skeptical of evidence for high human antiquity since the early 1830s, and distanced himself from the theory of ice ages after a brief flirtation with it in the early 1840s. He attacked the evolutionary ideas of Lamarck in detail in his book Principles of Geology. New developments in all three areas forced him to reconsider these positions in the late 1850s and early 1860s, and became the subject matter for Antiquity of Man.

Content The section about man summed up the evidence for human antiquity that had been brought to light by British geologists in 1858-59, and integrated it with archaeological evidence from the Paleolithic, Neolithic, and Bronze Age. The section about glaciation integrated continental ice ages into the larger picture of the Quaternary Period that Lyell had built up in his earlier works. The section about evolution recapitulated Darwin's arguments and endorsed them, though not enthusiastically. It acknowledged that human bodies might have evolved, but left open the possibility of divine intervention in the origins of human intellect and moral sense.

Controversy Hugh Falconer, a key player in the establishment of human antiquity, charged that Lyell – a minor player in the process – had misleadingly cast himself in the lead while ignoring the contributions of others. He raised his charges in the pages of the weekly journal The Athenaeum, and pressed them with a vehemence that some of his colleagues found distasteful. John Lubbock, a young but rising scientific star and a member of Darwin's inner circle, charged that Lyell had incorporated large amounts of material that Lubbock had published in articles and was then reworked into a book of his own. His criticism was largely private, but well known in the scientific circles in which both moved. Lyell gradually changed the text of Antiquity of Man to blunt some of their criticisms, but throughout the process held that he had been wrongly accused. Lyell's response is recorded in his archive, held at the University of Edinburgh's Heritage Collections, who have also created a dedicated website to Lyell's work.

Impact Antiquity of Man had its greatest impact in the years immediately after its publication. Lyell's presentation and endorsement of the new evidence for human antiquity firmly established the theory as scientific orthodoxy. His integration of both ice ages and a very old human race into the (geologically) recent history of the Earth was novel for its time, as was his presentation of archaeological data that from continental Europe. Until the early 1860s, "archaeology" had been synonymous, in England, with the study of antiquity and the Middle Ages through artifacts. Antiquity of Man expanded it to include the study of prehistory. The book's three-part structure meant, however, that it was quickly supplanted by more detailed works that followed in its wake. Lubbock's Prehistoric Times (1865), Darwin's The Descent of Man (1871), James Archibald Geike's The Great Ice Age (1874) and William Boyd Dawkins' Early Man in Britain (1880) became the standard works on the fields to which Lyell had introduced a generation of mid-Victorian readers.

See also Comparison with Huxley's Man's Place in Nature

References

External links The full text of Geological Evidences of the Antiquity of Man at Wikisource

4th edition of Antiquity of man at Google books

The Antiquity of Man at Project Gutenberg Special Publication of the Geological Society of London by Claudine Cohen that discusses the development and impact of The Antiquity of Man.

Illustrations

Geological Evidences of the Antiquity of Man illustration

Worked examples

Example 1 — a first encounter with Geological Evidences of the Antiquity of Man

Start with the simplest possible case. Write down what Geological Evidences of the Antiquity of Man 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 Geological Evidences of the Antiquity of Man 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 Geological Evidences of the Antiquity of Man 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 Geological Evidences of the Antiquity of Man

In research
Geological Evidences of the Antiquity of Man 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 Geological Evidences of the Antiquity of Man 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
Geological Evidences of the Antiquity of Man is common in secondary-school and first-year university syllabi. It links to neighbouring topics 1860s in science, 1863 non-fiction books, Archaeology books, so understanding it makes those chapters shorter.
In everyday life
Look for Geological Evidences of the Antiquity of Man 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 Geological Evidences of the Antiquity of Man in 20 minutes

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

Frequently asked questions

What is Geological Evidences of the Antiquity of Man in simple terms?

Geological Evidences of the Antiquity of Man is a book written by British geologist, Charles Lyell in 1863. The first three editions appeared in February, April, and November 1863, respectively.

Why does Geological Evidences of the Antiquity of Man 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 Geological Evidences of the Antiquity of Man?

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 Geological Evidences of the Antiquity of Man.

Tags

  • 1860s in science
  • 1863 non-fiction books
  • Archaeology books
  • British non-fiction literature
  • Geology books
  • Human evolution books

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