The physical processes that control the structure of conical piles are fascinating and imperfectly understood even today. However we can approach your question in approximate way.
The angle that the surface of the pile makes with the ground is called the angle of repose. Predicting this theoretically is hard because it is is sensitive to the exact nature of the material in the pile. However the angle of repose is generally in that range 30º to 45º. You don't say what grain you saw, but wheat is actually at the low end of this range at 27º, and I'd guess corn is fairly similar. This means the piles are quite broad so the weight is spread out over a large area.
The volume of a conical pile of height $h$ and base radius $r$ is given by:
$$ V = \tfrac{1}{3}\pi r^2 h $$
and the area of the base is just $\pi r^2$, so the average pressure at the base turns out to be just dependent on the height:
$$ P_\text{av} = \frac{Mg}{A} = \frac{V\rho g}{A} = \tfrac{1}{3}h\rho g $$
For wheat the average density of a pile is around 750 kg/m$^3$, and putting the numbers into the equation above we get:
$$ P_\text{av} \approx 2500 h \,\text{Pa} $$
For comparison, atmospheric pressure is 101325 Pa, so the pile would have to be 40 metres high for the average pressure at the base to be even equal to one atmosphere. And there's your answer. Even ina large grain pile the pressure is simply too small to crush the grains.