The development of shallow water equations are seen to be nonlinear at the first step of approximation with the requirement of the parameter epsilon = (n^2)/(m^2), to be sufficiently small, where m = horizontal length and n = vertical length. This restriction of the smallness of epsilon is perhaps not a very severe constraint on the applicability of shallow water equations. And if it is so then the shallow water equations/approximation should be applicable to extremely large water depths as long as the wave is sufficiently long. I wish to know is it a correct argument?