Joseph Fourier published the law in 1822, and the form has not needed changing since: the heat crossing a slab is proportional to its area, proportional to the temperature difference across it, and inversely proportional to its thickness. The constant of proportionality is the thermal conductivity k, and it is a property of the material rather than of the situation — which is what makes it tabulable and what makes the whole method work.
The one thing worth internalising is the size of the spread. Copper conducts about 15,247 times better than still air, and the table on this page runs the whole way from one to the other. Put the same 100 mm wall over the same 6 m² between 21 °C and −5 °C and copper passes 601,500 W, brick passes 1,080 W, and fibreglass passes 57 W. Nothing about the geometry changed. Only the material did.
Steady conduction through a slab of constant k gives a straight temperature line, and the simulator draws it as one. That is not a simplification for teaching: it falls out of the heat equation once nothing is changing with time and no heat is being generated inside, and it is the reason a two-point measurement is enough to characterise a wall.