The Legacy of a ‘Living Library’: On the Reception of John Smith

John Smith was among the first of the Cambridge Platonists. He was therefore in a position to influence not only his contemporaries but all those who followed after him well into the twentieth century and beyond. Well established lines of influence both to and from Whichcote, Cudworth, and More are explored first before moving on to less well-known connections to Bishop Simon Patrick and mathematician Isaac Barrow. Smith’s continued significance for eighteenth century theology is demonstrated through discussion of his inspiration of the doctrines of spiritual sensation developed by Jonathan Edwards and John Wesley. Special notice is also given to Smith’s authority as an interpreter of Biblical prophecy through the eighteenth and nineteenth centuries. The chapter concludes with looks at Smith’s influence on Samuel Taylor Coleridge, Ralph Waldo Emerson, William Ralph Inge, Rufus Jones, Pierre Hadot, and others. This chapter, offers a broad, but highly selective, overview of the reception and influence of Smith’s life and work. It is intended, however, as a call for future research more than as an authoritative presentation of Smith’s legacy. For, if the Cambridge Platonists have been underappreciated until recently, none of them have been unjustly ignored as consistently as Smith

Experimental Investigations of Low-Ca Pyroxene Stability and Olivine-Pyroxene-Liquid Equilibria at 1-atm In Natural Basaltic and Andesitic Liquids

This paper reports experiments carried out at 1-atm under conditions of controlled oxygen fugacity, using natural andesites and andesite mixed with augite+synthetic pigeonite or augite+orthopyroxene. The experimental results are used (1) to investigate the controls of Mg# (Mg/[Mg+Fe2+]) and temperature on low-Ca pyroxene stability (pigeonite vs orthopyroxene), (2) to quantify the effects of variations in bulk composition on the position of multiple saturation boundaries in mineral component projection schemes and (3) to develop a thermodynamic model for silica activity for melts saturated with olivine and pyroxene. Over the Mg# range of 0.80–0.30 the minimum temperature of pigeonite stability in natural compositions is equivalent to the Lindsley (1983) boundary determined for pure Ca-Mg-Fe pigeonites. For the low variance, 5-phase assemblage oliv-aug-low-Ca pyroxene-plag-liquid, expressions involving liquid (Na2O+K2O)/(Na2O+K2O+CaO),Mg# and TiO2 content predict temperature and the movement of multiple saturation boundaries in pseudoternary projections in response to changing melt composition. The equilibrium for the low pressure melting of low-Ca pyroxene to olivine+liquid is formulated as a geothermometer and monitor of silica activity. Equilibrium constants estimated from thermochemical data and activities calculated for experimentally produced olivine and pyroxenes are used to develop a model for silica activity in liquid