I'll expand a bit on my comments to the question here.
For fluids, the pressure is generally written as
$P = \rho g h$
where $\rho$ is the density of the fluid, $g$ is the gravitational acceleration constant, and $h$ is the depth. The pressure increases with increasing depth because the weight of all of the fluid on top is pushing down, and the further down you go, the more fluid is above.
Now, we must consider that gases themselves are also fluids, so the same thing must hold true for gases. However, in the case of a gas, the value of the density is very low, so for any reasonable size storage container for a gas, the pressure due to gravity will be very small. However, for large quantities of a gas, the Earth's atmosphere for instance, this now comes into play, since the height of the atmosphere is so high. We feel this difference as barometric pressure, and at higher altitudes (lower depths), we don't feel as much pressure due to exactly this effect.
The pressure of gases can also be affected by the temperature of a gas unlike a liquid. In a liquid, the loose interactions between the particles hold them together that don't allow the particles to move freely away from each other like in a gas. But in a gas, the particles can move freely. For an ideal gas, you have a relationship for the pressure that looks like the following:
$P = \frac{Nk_BT}{V}$
where $N$ is the number of particles, $k_B$ is a constant, $T$ is the temperature and $V$ is the volume of the container. In this case, you have a constant pressure on all the walls of a container. This is the dominant effect for gases that are stored in any reasonably sized container, and this is where the difference between gases and liquids arise.
For having a liquid exert equal pressures on all container walls, you would have to remove the effects of gravity.