What crucial boundary determines where ices can remain solid, dividing terrestrial and Jovian planet formation zones?

Answer

The frost line or snow line

A fundamental aspect governing solar system architecture is the thermal divide within the protoplanetary disk, known as the frost line or snow line. This boundary represents the specific distance from the central star where temperatures drop low enough—approximately 150 Kelvin—for volatile compounds like water, methane, and ammonia to condense and remain solid in the form of ice grains. In the region interior to this line, only rock and metal form solids, limiting the building blocks for terrestrial planets. Exterior to this line, the abundance of solid material dramatically increases because both rock/metal *and* ices are available, allowing for the rapid accumulation of massive cores necessary to gravitationally capture large amounts of surrounding hydrogen and helium, leading to the formation of gas and ice giants.

What crucial boundary determines where ices can remain solid, dividing terrestrial and Jovian planet formation zones?
physicsastronomysolar systemstar formationnebular collapse