Lord Kelvin and the Age of the Earth

Burchfield, Joe D. Between 1860 and 1930 the accepted estimate of the age of the earth evolved from the virtually unlimited expanse of time demanded by Charles Lyell and the mid-century uniformitarian geologists, through a series of ever more restrictive limits imposed by late-nineteenth century physics and geology, to the vast but quantitatively definable chronologies revealed by radioactive dating. During this period, the question of the earth's age stirred heated debate; stimulated important studies in physics, geology, astronomy, and biology; and served as the focus for a fascinating interplay of ideas and personalities. Dr. Burchfield treats the evolution of the concept of geological time from its first emergence as a subject for a quantitative determination through the development of the procedures for radioactive dating, focusing attention upon two main themes: the conflicts and interdependence among several branches of science involved in the search for the earth's age, and the