The widespread occurrence of peculiar samples in the Nalbach area covering many square kilometers and exhibiting convincing indications of high temperatures and high pressures, in particular the mineralogical evidence of strong shock, establishes a meteorite impact event in the Holocene as a matter of fact according to the generally accepted opinion that shock metamorphism in rocks proves a meteorite impact. The young Holocene age is concluded from the concentration of the peculiar finds in the upper soil layers, the very fresh status of the impact glasses and the young appearance of the now discovered probable impact crater. Using impact scaling...