Viscous stress is proportional to $\frac{du}{dy}$, so they only arise from relative motion between different layers of fluid. That makes it somewhat similar to kinetic friction, which requires relative motion between two objects.
But what if there is no relative motion between the different layers of fluid? Is there an equivalent of static friction in fluid dynamics?
In particular, I'm considering this hypothetical static scenario for fluids. Say you place a small fluid droplet on a gentle incline, such that it remains in static equilibrium without sliding down the incline. How exactly is this equilibrium achieved?
Viscosity definitely doesn't play a role here, because everything is stationary, so there is no velocity differential and thus no stress due to viscous effects.
I could see how the droplet might end up getting deformed in a peculiar manner in order for this equilibrium to be achieved, such that the force due to surface tension will have sufficient component upward along the incline to balance the downward component of its weight along the incline. So, surface tension could be what enables it to be at equilibrium.
But could there be any other forces at play? Something doesn't feel too right about the claim that surface tension does all of this.