Rh-rich and Ir-poor erlichmanite-laurite OsS2-RuS2 solid solutions have been discovered at placers in Haraigawa, Misato-machi, Kumamoto, Japan. Microprobe analysis was performed to identify solid solutions containing few sub-components other than Rh. Approximately 10 at% Rh was found to be present in the solid solutions. Structural refinement was performed using four natural samples: Os0.32Ru0.61Rh0.07S2, Os0.49Ru0.43Rh0.08S2, Os0.58Ru0.33Rh0.08S2 and Os0.81Ru0.09Rh0.10S2. The unit-cell parameters for the solid solutions containing Rh from Haraigawa varied from 5.61826(6) to 5.63142(8) Å. The (Os, Ru, Rh)-S distances in the Os1-x-yRuxRhyS2 system were almost constant with a small variation of 0.001 Å. Conversely, the S-S distances varied significantly, with variations approaching 0.1 Å. Rh substitution of Os rather than Ru showed a larger impact on the crystal structure. The atomic displacement ellipsoid of both cations and anions was almost spherical, and no elongation along the M-S and S-S bond directions was observed. The bulk Debye temperatures were estimated from the Debye-Waller factor for the sulfide site. The bulk Debye temperatures of pure OsS2 and RuS2 were 688 K and 661 K, respectively, which suggests that the melting point of erlichmanite is