The phase diagram above shows the conditions that are needed to form different aluminosilicate minerals. The temperature \(T\), in degrees Celcius (°C) is shown on the horizontal axis, and the pressure \(P\), in gigapascals (GPA), is shown on the vertical axis. An equation of the boundary line between the andalusite and sillimanite regions is approximated by the equation below. What is the meaning of the \(T\)-intercept of this line?

$$P=-0.00146T+1.11$$