Charles Lyell

Charles Lyell

Charles Lyell (1797-1875) is widely regarded as one of history’s most notable and influential scientists. His work in historical geology helped cement our understand­ing of the earth’s formation. Yet, for all Lyell’s efforts to gain acceptance and recognition of geo­logical theory and the emerging science of histori­cal geology, it is his impact on Darwinian evolution and the understanding of humanity’s place in time that is arguably his greatest achievement.

Born in Scotland in 1797, Lyell took an early interest in nature studies, eventually focusing on geology for his career path. Inspired by geologist James Hutton’s idea of uniformitarianism, Lyell supported the idea that Earth’s geological elements are continually affected by slow processes of change (erosion, uplift, etc.) and always have been. Between 1830 and 1833, he summarized many of his emerging ideas in his chief work, Principles of Geology, which ultimately influenced scientists not only in geology but also in the fields of archaeology and biology as well. Lyell contin­ued to publish his findings, which were widely read and admired by his scientific peers. He was knighted in 1848 in recognition of his many con­tributions to science.

Charles Lyell’s primary legacy revolves around uniformitarianism and the earth’s age. Whereas Hutton formalized uniformitarianism, Lyell argu­ably became its most influential proponent. Lyell’s research and argumentation helped cement the idea that the earth’s landscapes took eons to form, a thought in stark contrast to Archbishop James Ussher’s Bible-based estimate that the planet was formed approximately 6,000 years ago. The prem­ise that billions of years instead of thousands were required to form Earth, the solar system, and the entire universe was radical in the extreme and challenged doctrines whose authority lay in reli­gious scripture. Lyell helped revolutionize not only geological thought but scientific thought in general by helping scholars look beyond conventional ideas of time and change.

Lyell’s Principles of Geology made an impres­sion on countless scientists, including Charles Darwin. For Darwin, Lyell’s arguments supported the idea that organisms, including humans, needed as much time to change as rivers needed to carve out canyons and mountains needed to rise and fall. Such a conceptualization made Darwin’s evolu­tionary ideas appear all the more plausible. Consequently, Lyell, though initially hesitant to embrace the ideas of evolution of organisms, provided Darwin with direction. The ensuing shift in humanity’s understanding of time, the pace at which events unfold in the natural world, and our own place in the natural order is due in part to Lyell’s contribution, which cannot be overvalued.

Neil Patrick O’Donnell

See also Darwin, Charles; Earth, Age of; Geological Column; Geology; Hutton, James; Huxley, Thomas Henry; Lamarck, Jean-Baptiste de; Materialism;

Paleontology; Smith, William; Spencer, Herbert; Steno, Nicolaus; Stratigraphy; Uniformitarianism

Further Readings

Matson, C. C. (2006). Uniformitarianism. In H. J. Birx

(Ed.), Encyclopedia of anthropology

(Vol. 6, pp. 2239-2241). Thousand Oaks, CA: Sage.

McKready, T. A., & Schwertman, N. C. (2001). The statistical paleontology of Charles Lyell and the coupon problem. American Statistician, 55(4), 272-278.

Recker, D. (1990). There’s more than one way to

recognize a Darwinian: Lyell’s Darwinism. Philosophy of Science, 57(3), 459-478.

Young, P. (2006). Lyell, Charles. In H. J. Birx (Ed.), Encyclopedia of anthropology (Vol. 4, pp. 1503-1505). Thousand Oaks, CA: Sage.

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John Lydgate

John Lydgate

Trofim Denisovich Lysenko

Trofim Denisovich Lysenko