Loved the printer cartoon.
Solidus is well known to me, as it would be to most geologists, and I guess that is the chemical definition. I'll take a leaf from Calilasseia's book here. When a complex melt (such as molten rock) cools and solidifies, it does so over a temperature range, with the liquidus being the temperature at which the first crystals form, and the solidus being the temperature at which the last crystals form. Some mineral species crystallise out early from the melt near the liquidus temperature, and other mineral species don't crystallise until the temperature falls to near the solidus. That is why crystalline rocks, such as granite and basalt, can have well-formed large crystals of one mineral embedded in a background of other smaller different mineral grains. Those bigger crystals formed early in a largely liquid melt with lots of room to grow, while the crystals in the background formed late when there was competition for space to grow in the crowded mush of crystallising minerals. It is particularly obvious in some volcanic basalt, which contain scattered large rectangular crystals (feldspar) embedded in an otherwise very fine-grained rock. Those feldspar crystals formed deep in the volcano as the melt reached the liquidus temperature as it moved slowly upward. But then, when the eruption occurs, it is so fast that the solidus temperature is reached almost instantaneously, and the remaining melt solidifies very rapidly before the remaining minerals have time to grow.