We discuss possible models for describing the metal-insulator phase transit
ion coupled with paramagnetic-ferromagnetic phase transition in manganites.
We argue that current models have apparent drawbacks. As a way to explain
experiments we introduce the magnetic (large) polaron model. In this model,
the conductivity appears as a result of percolative overlapping of magneti
c polarons which coexist with small (Jahn-Teller) polarons. We compare this
model with the experimental data.