Today the trackbed formation from Pontbrengeifr to the Hafan incline remains largely open and intact and can be walked; much of the formation of the mineral extensions at the top of the incline is also traceable. Between Pontbrengeifr and Talybont sections of the formation remain intact, but others have been eroded away by the Afon Leri and are heavily overgrown which makes walking it more difficult. There is now little to see of the former exchange sidings at Llandre.
