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Did You Know?

A History of the Warfare of Science with Theology in Christendom (e.g.

Basin and Range (1981).Stephen Toulmin and June Goodfield (1965), The Ancestry of Science: The Discovery of Time, p.

As a young naturalist and geological theorist, Darwin studied the successive volumes of Lyell's book exhaustively during the Beagle survey voyage in the 1830s, before beginning to theorise about evolution.Physicist Gregory Benford addresses the concept, in Deep Time: How Humanity Communicates Across Millennia, as does paleontologist and Nature editor Henry Gee in In Search of Deep Time. Stephen Jay Gould's Time's Arrow, Time's Cycle (1987) also deals in large part with the concept.One of the first uses of "deep time" in a general interest publication may have been by John McPhee in his 1981 book, Basin and Range, parts of which originally appeared in The New Yorker magazine. One of the metaphors McPhee used in explaining the concept of deep time was cited in Time's Arrow, Time's Cycle by Gould: Consider the earth's history as the old measure of the English yard, the distance from the King's nose to the tip of his outstretched hand.

The Man Who Found Time: James Hutton and the Discovery of the Earth's Antiquity (e.g.

In 1788 the sight of Hutton's Unconformity at Siccar Point convinced Playfair and Hall of this extremely slow cycle, and in that same year Hutton memorably wrote "we find no vestige of a beginning, no prospect of an end".Other scientists such as Georges Cuvier put forward ideas of past ages, and Werner's ideas were incorporated into concepts of catastrophism by geologists such as Adam Sedgwick who inspired his university student Charles Darwin to exclaim "What a capital hand is Sedgewick for drawing large cheques upon the Bank of Time!". In a competing theory, Hutton's comprehension of endless deep time as a crucial scientific concept was developed into uniformitarianism by Charles Lyell in his Principles of Geology (1830-33).

Hutton's innovative 1785 theory based on Plutonism visualised an endless process of rocks forming under the sea, being uplifted and tilted, then eroded to form new strata under the sea.