Central to the development of geology has been the growth of systematic empirical observation as a programme of scientific practice. Fieldwork has focused on many objects—strata, fossils, and landforms—and has issued in a variety of products, such as maps, sections, and monographs on regional geology, particular rock formations and fossils. Early in the nineteenth century, above all, many influential geologists sought to define their science as one exclusively of field observation, description, and the accumulation of data. The rise of fieldwork, (...) in Britain as elsewhere, is an important phenomenon in the making of geology. It must be explained. (shrink)

This paper argues that Shaftesbury differs from other moral sentimentalists (Hutcheson, Hume, Smith) because he conceives of the moral sentiments as partial and first-personal, rather than impartial and spectatorial. This difference is grounded in Shaftesbury’s distinctive notion that moral self-governance consists in the self-examination of soliloquy. Breaking with his Stoic influences, Shaftesbury holds that the moral sentiments play the role of directing and guiding soliloquy. Because soliloquy is first-personal reflection that is directed to achieving happiness, claiming that the moral sentiments (...) direct soliloquy leads Shaftesbury to conceive of the moral sentiments as arising from the internal perspective of an agent focused on her own happiness. This provides Shaftesbury with a stronger framework for understanding moral sentiments, for it avoids the difficulty of explaining why the sentiments of others or those arising from an imagined spectator’s perspective are motivating or authoritative for us. (shrink)