---
title: "Discovery of human antiquity"
chunk: 3/4
source: "https://en.wikipedia.org/wiki/Discovery_of_human_antiquity"
category: "reference"
tags: "science, encyclopedia"
date_saved: "2026-05-05T03:38:57.794617+00:00"
instance: "kb-cron"
---

The three-age system was in place from about 1820, in the form given to it by Christian Jürgensen Thomsen in his work on the collections that became the National Museum of Denmark. He published his ideas in 1836. Postulating cultural change, in itself and without explaining a rate of change, did not generate reasons to revise traditional chronology. But the concept of Stone Age artifacts became current. Thomsen's book in Danish, Ledetraad til Nordisk Oldkyndighed, was translated into German (Leitfaden zur Nordischen Alterthumskunde, 1837), and English (Guide to Northern Archæology, 1848).
John Frere's 1797 discovery of the Hoxne handaxe helped to initiate the 19th century debate, but it started in earnest around 1810. There were then a number of false starts relating to different European sites. William Buckland misjudged what he had found in 1823 with the misnamed Red Lady of Paviland, and explained away the mammoth remains with the find. He also was dismissive of the Kent's Cavern findings of John MacEnery in the later 1820s. In 1829 Philippe-Charles Schmerling discovered a Neanderthal fossil skull (at Engis). At that point, however, its significance was not recognised, and Rudolf Virchow consistently opposed the theory that it was very old. The 1847 book Antiquités Celtiques et Antediluviennes by Boucher de Perthes about Saint-Acheul was found unconvincing in its presentation, until it was reconsidered about a decade later.

The debate moved on only in the context of

further stone tools that were admitted to be made by Stone Age man, found
on sites where the stratigraphy could be argued to be clear and undisturbed, with
remains of animals that were (in the consensus of palaeontologists) now extinct.
It was this combination, "extinct faunal remains" + "human artifacts", that provided the evidence that came to be seen as crucial. A sudden acceleration of research was seen from mid-1858, when the Geological Society set up a "cave committee". Besides Hugh Falconer who had pressed for it, the committee comprised Charles Lyell, Richard Owen, William Pengelly, Joseph Prestwich, and Andrew Ramsay.

=== Debate on uniformity and change ===

On the one hand, lack of uniformity in prehistory is what gave science traction on the question of the antiquity of man; and, on the other hand, there were at the time theories that tended to rule out certain types of lack of regularity. John Lubbock outlined in 1890 the way the antiquity of man had in his time been established as derived from change in prehistory: in fauna, geography and climate. The hypotheses required to establish that these changes were facts of prehistory were themselves in tension with the uniformitarianism that was held to by some scientists; therefore the protean concept "uniformitarianism" was adjusted to accommodate the past changes that could be established.
Zoological uniformity on earth was debated already in the early eighteenth century. 
George Berkeley argued in Alciphron that the lack of human artifacts in deeper excavations suggested a recent origin of man. Evidence of absence was, of course, seen as problematic to establish. Gottfried Leibniz in his Protogaea produced arguments against identification of a species via morphology, without evidence of descent (having in mind a characterisation of humans by possession of reason); and against the discreteness of species and their extinction.
Uniformitarianism held the field against the competitor theories of Neptunism and catastrophism, which partook of Romantic science and theological cosmogony; it established itself as the successor of Plutonism, and became the foundation of modern geology. Its tenets were correspondingly firmly held. Charles Lyell put forward at one point views on what were called "uniformity of kind" and "uniformity of degree" that were incompatible with what was argued later. Lyell's theory, in fact, was of a "steady state" geology, which he deduced from his principles. This went too far in restricting actual geological processes, to a predictable closed system, if it ruled out ice ages (see ice ages#Causes of ice ages), as became clearer not long after Lyell's Principles of Geology appeared (1830–3). Of Lubbock's three types of change, the geographical included the theory of migration over land bridges in biogeography, which in general acted as an explanatory stopgap, rather than in most cases being one supported by science. Sea level changes were easier to justify.

=== Glacial conditions ===

The identification of ice ages was important context for the antiquity of man because it was accepted that certain mammals had died out with the last of the ice ages which were clearly marked in the geological record. Georges Cuvier's Recherches sur les ossements fossiles de quadrupèdes (1812) had accepted facts of the extinctions of mammals that were to be relevant to human antiquity. The concept of an ice age was proposed in 1837 by Louis Agassiz, and it opened the way to the study of glacial history of the Quaternary. William Buckland came to see evidence of glaciers in what he had taken to be remains of the biblical Flood. It seemed adequately proved that the woolly mammoth and woolly rhinoceros were mammals of the ice ages, and had ceased to exist with the ice ages: they inhabited Europe when it was tundra, and not afterwards. In fact such extinct mammals were typically found in diluvium as it was then called (distinctive gravel or boulder clay).

Given that the animals were associated with these strata, establishing the date of the strata could be by geological arguments, based on uniformity of stratigraphy; and so the animals' extinction was dated. An extinction can still strictly only be dated on assumptions, as evidence of absence; for a particular site, however, the argument can be from local extinction.
Neither Agassiz nor Buckland adopted the new views on the antiquity of man.