<p>The 28 September 2018 Mw 7.5 Sulawesi strike-slip earthquake generated an unexpected tsunami with devastating consequences.&#160;Since&#160;such strike-slip earthquakes are not expected to generate large tsunamis, the latter&#8217;s origin remains much debated. A key notable feature of this earthquake is that it ruptured at supershear speed, i.e.,&#160;with a&#160;rupture speed greater than the shear wave speed of the host medium. Dunham and Bhat (2008) showed that such supershear ruptures, in half-space, produce two shock fronts (or Mach fronts) corresponding to&#160;an&#160;exceedance of shear and Rayleigh wave speeds. The Rayleigh Mach front carries significant vertical velocity along its front. We couple the ground motion produced by such a supershear earthquake to a 1D non-linear shallow water wave equation that accounts for both the&#160;time-dependent&#160;bathymetric displacement&#160;as well its&#160;velocity. We use an extension of Fourier-based PDE solvers called the Fourier Continuation (FC)&#160;method&#160;to numerically solve the system. The FC&#160;method enables&#160;high-order&#160;convergence of Fourier series approximations of non-periodic functions by resolving the well-known Gibbs &#8220;ringing&#8221; effect. &#160;FC-based solvers offer&#160;limited&#160;numerical&#160;dispersion, high-order accuracy and mild CFL&#160;conditions&#8212;making&#160;them ideal to solve this system. Using the local bathymetric profile of Palu bay around the Pantoloan harbor tidal gauge, we&#160;have been&#160;able to clearly reproduce the observed tsunami with minimal tuning of parameters. We conclude that the Rayleigh Mach front,&#160;generated&#160;by a supershear earthquake combined with the Palu bay geometry, caused the tsunami.</p>