Hz frequency representing ~4 magnitude and >6 magnitude earthquakes, respectively, showcases that in multiple ranges of the earthquakes, the vertical support is by far not optimal. With the displacement of the structure, the interface is put under extreme stress due to the shear load being applied. However, this interface displacement between the lattice structure should not realistically provide the same effect. Yet we also see the dramatic failure of the 8-unit case in the continuum experiments.