The block is in equilibrium when the weight of the block is equal to the displacement force (=equal to the weight of displaced water, according to Archimede's principle).
If h is the height of the submerged portion of the block, then equilibrium requires:
M_b g = (M_w)g (weight of block = weight of displaced water)
V_block ρ_block = (V_submerged ρ_water) = (0.10m^2) h ρ_water
0.1^3 ρ_block = 0.1^2 h ρ_water
0.1 ρ_block = h ρ_water ---> h = 0.1 ρ_block/ρ_water
So, if you have standard water or sea water, you'd have different densities for them, and so the submerged fraction of the block h would also change