Let's consider some flat surface which extends to infinity in all directions.
Suppose we slowly spill some water near some point of the surface. Due to surface tension, the water doesn't spread out indefinitely. If done properly, the water will spread essentially uniformly over a section of the surface, and within this section there won't be any "holes" where the surface isn't covered by water.
If we add some more water, the water will redistrubte itself to maintain a nearly constant height $h$. Furthermore experimentally it seems that $h$ doesn't depend on the amount of water spilled.
Is this true, and how might we calculate the height of the water layer?