Fix a simple $U,V,N$ system which is in contact with a temperature and pressure reservoir, so that the minimization of $G$ is the relevant criterion for equilibrium. This question is somewhat related to this one here, though I don't think the answer is fully captured.
In his textbook, Callen gives diagrams of the following sort to describe phase transitions. We note that throughout the discussion $N$ is assumed constant; it is a tacit spectator variable.
In this particular question, I am not interested in the critical point but rather an arbitrary position on the coexistence curve; say, the middle inset. In this diagram, Callen seems to be showing that at fixed $T,P,N$, $V$ is variable! But that is of course absurd since there are only 3 DOF.
What I think perhaps is going on is that our system/substance has underlying phases which each have separate nominal fundamental equations (i.e. each phase $i$ has a $G_i(T,P,N)$), but the actual fundamental equation is the minimum over all such phases at the given $T,P,N$ ($G(T,P,N) = \min_i G_i(T,P,N)$). The phase transition happens when we cross over from one $i$ to some other $j$ in this minimum. However, this description does not comport with Callen drawing $V$ as a continuous variable. My picture seems to suggest that there should be discrete points $V_i$ (since $T,P,N$ fix $V_i$ for the given phase) corresponding to the minimums given in the inset.
Since Callen's description in terms of a continuous variable is very much different than mine, it seems I must be missing something?