To find the center of gravity for a hemisphere shell, one must integrate mass density over the surface in each axial direction. The formulas for calculating the center of mass in rectangular coordinates involve integrating the product of density and position. A symmetry argument suggests transforming the problem to find the center of mass for a semicircle, focusing on the z-coordinate for the hemisphere. However, discrepancies arise between results obtained from integration and symmetry arguments, particularly for semicircular shapes. Clarification on these differences is sought, highlighting the complexity of the problem.