The pressure gradient towards the center of a large planet, such as Earth, reaches its maximum due to the weight of the overlying material, even though the gravitational field falls to zero at the center. The pressure curve is influenced by the radial distribution of density, which affects the pressure calculation. While the formula for pressure involves integrating density and gravitational force, the exact bounds for integration remain unclear. As one approaches the center, the addition of mass to the overlying material decreases, leading to a minimum pressure gradient. Overall, the pressure does not ease off but rather reflects the cumulative weight of the material above.