You're off by a multiplicative factor. You don't have 0.047 mol of HO-. You have twice as much HO- as Ca2+.
So this would mean you have how many moles of HO-?
Finding the concentration of HO- then, assuming 500 mL of water is roughly the solution volume, will be as you did before.
pH and pOH are p-functions, logarithmic functions of H+ and HO- concentration, respectively. So whatever your concentration of HO- came out to be, the p-function of that concentration would give you pOH, not pH.
To understand what the pH of the solution would be, then, you must employ a very common reaction that is true of all acid-base equilibria.
The relationship is commonly derived from the dissociation of water to H+ and HO- ions.
2H2O <---> H3O+ (source of H+) + HO-
If we designate HA as any acid, we can write an equilibrium for its dissocation in water (the same can be done for any base):
HA + H2O ---> H3O+ + A-
A- + H2O ---> HA + HO-
Now, applying your understanding of what an intermediate is (if not, review what an intermediate is), we can cancel the common intermediate(s) from both of these respective reactions, giving:
2H2O ---> H3O+ + HO-
Does this equation look familiar? So we can simply say that, according to this equation,
K = [H3O+][HO-]
[H2O]2
Since water is a pure liquid, it's concentration is a constant. If we bring the [H2O]2 term to the left, we get
K[H2O]2 = [H3O+][HO-], which can be re-written as
Kw = [H3O+][HO-]
This relationship can be written in other forms, notably using p-functionality:
pKw = pH + pOH
Do you see the significance?