Reply to Doppler et al . ‘Response to “The fall of Phaethon: a Greco-Roman geomyth preserves the memory of a meteorite impact in Bavaria (south-east Germany) ( Antiquity 84)”’

We acknowledge the observations of Doppler et al . on our paper and we are grateful to Antiquity's editor for this opportunity to reply to their objections. Firstly, it should be noted that we have not claimed that the Chiemsee once included the Tuttensee. We agree that the region in which both lakes lie was glacially formed. But while Lake Chiemsee is the result of the last Ice Age the Tuttensee basin originates from a much later Holocene meteorite impact. We do not use the myth of Phaeton to date this event that is known as the Chiemgau impact. On the contrary we estimate from archaeological evidence and OSL dating that the event occurred between 2200 and 800 BC, i.e. the Bronze Age (Rappengluck et al . 2010: 436).We go on to discuss parallels between the independent dating of the Chiemgau impact and the possible time frame of the myth (Rappengluck et al . 2010: 435–37).