Results from six full-equilibrium condensation models for 18 elements from Herbort et al. (2020) re-computed for p = 1 bar, and five simple models for just 4 elements; see Table 3. Each model starts at T = 600 K (marked by circles) and then we follow that model with a line down to 200 K with 200 log-equidistant points. Abbreviations are carbonaceous chondrites (CI), Mid Oceanic Ridge Basalt (MORB), Continental Crust (CC), Bulk Silicate Earth (BSE), and abundances deduced from polluted white dwarf (PWD) observations. The points where the trajectories start to have graphite are marked by crosses, and the points where liquid water starts to occur are marked by squares.