“…where is the internal pressure and the total potential is (23) Equation ( 22) requires that the inner and outer surfaces of the ice shell be equipotential, i.e., This imposes restrictions on the shell's shape: it must be a focaloid in which the squares of the semiaxes of the two boundary surfaces are related as (24) where is the largest root of the cubic equation (25) As is known [3], the external potential of a twolayer ellipsoid can be represented as a potential combination of uniform ellipsoids: (26) Therefore, for the coefficients of zonal harmonics, we find the expression (27) Using the generalized Maclaurin-Laplace theorem [16], expression (27) can be simplified to (28) For further calculations, we use the refined Haumea's parameters [10]. Some of these parameters were given above in formulas ( 4) and ( 5); in addition, it is also necessary to know the semiaxes of the planetoid's rocky core:…”