The theoretical system Lyell presented in 1830 was composed of three requirements or principles: 1) the Uniformity Principle which states that past geological events must be explained by the same causes now in operation; 2) the Uniformity of Rate Principle which states that geological laws operate with the same force as at present; 3) the Steady-state Principle which states that the earth does not undergo any directional change. The three principles form a single thesis called uniformitarianism which has been repeatedly (...) questioned and which has been reputed to be unable to face the competing directional synthesis based on the theory of the earth's cooling down. As a result, the significance of Lyell's system has been reduced to a simple actualism which admits the validity of the only Uniformity Principle. I believe that the only way to understand Lyell's role in the history of science is to maintain the unity of his synthesis. To show the Newtonian roots of this synthesis I will compare Lyell's principles and Newton's Rules of Reasoning. I will conclude with an analysis of the methodological function of principles in Lyell's scientific endeavour. (shrink)

For Reid perception, broadly speaking, was a complex of two very different mental states. Calling such views dual component theory, A. D. Smith questions whether any such theory, and whether Reid's version in particular, is a viable theory of perception. The aim of this paper is to defend Reidian Dual Component Theory from Smith's critique. Answering Smith's critique reveals the depth and resilience of Reid's approach to perception, highlighting specifically the continued interest of his thought about the relationship between sensation (...) and perception, the nature of illusion, the immediacy of perception, and the content of perceptual belief. (shrink)