Raman spectra of quartz samples collected at sample site 27-B near Cabo de Creus ( “Cape de Creus“ ) at the Bay of Lyon in NE-Spain provide strong evidence for the 130 x 110 km elliptical Impact Crater described in my hypothesis, which is responsible for the formation of the semi-circular Bay of Lyon. The yet unknow 130 x 110 km “Bay of Lyon“ Impact Crater (BLC) belongs to a larger Secondary Impact Crater Chain, which was caused by impacting ejecta material that was ejected by the 1270 x 950 km Permian Triassic Impact Crater (PTI), located in the Arctic Sea near Alaska, according to my hypothesis. Beside the Raman spectra which I present as evidence and first verification for the existence of the impact crater, there is additional geo-physical evidence from gravity anomaly- and magnetic anomaly maps, which both show a strong anomaly in the center of the assumed 130 x 110 km impact crater. The Raman spectra of quartz from sample site 27-B provide strong evidence for an Impact Event ! Sample Site 27-B is the closest sample site in relation to the assumed center of the 130 x 110 km Crater. It is located on the last remaining (small) section of the crater-rim of the “Bay of Lyon“ Crater directly near the lighthouse at Cabo de Creus ( “Cape de Creus“ ). The whole rest of the 130 x 110 km Crater is located on the ocean floor of the Mediterranean Sea. The shifts of the main Raman bands ( peaks ) to the lower frequencies 461 and 125 cm-1 ( Stone 6 ) and to 463, 261, 205 and 125 cm-1 ( Stone 3 ) and to 463 and 260 cm-1 ( Stone 2 ) which are visible in the Raman Spectra of these three quartz-samples from sample site 27-B, clearly indicate that the quartz was exposed to a shock pressure in the range of 22 – 24 GPa. ( see explanation in the Appendix at page 16 ). Images of the analysed rock samples and photos of the sample sites are in the Appendix at page 13. Images of all sample sites are available on www.permiantriassic.de or www.permiantriassic.at [truncated by viXra Admin]