These strongly support the hypothesis that the impactor was large enough to create a 120 mile peak ring, eject molten granite from deep within the earth, create colossal water movements, and eject an immense quantity of vaporized rock and sulfates into the atmosphere, where they would have persisted for a long time
परिणामी हा खडकाळ खडक, जो साधारणपणे भौगोलिक वयोगटाच्या दिशेने चालते, ८००० किलोमीटरपर्यंत थोड्या थोड्या प्रमाणात वाढते, प्रचंड प्रमाणात ऊर्जा उकलतो आणि एक मीटर पर्यंत दुसरीकडे थरथरणाऱ्या हालचाली तयार करतो.