Arguing from a critical reading of the text, and scientific evidence on the ground, the authors show that the myth of Phaethon – the delinquent celestial charioteer – remembers the impact of a massive meteorite that hit the Chiemgau region in Bavaria between 2000 and 428 BC.
Teesid: Tekstikriitilise analüüsi ja teaduslike tõendite alusel näitavad autorid, et Phaetoni müüt-kurja tegeva taevase sõjavankri müüt-säilitab mälestusi ajavahemikul 2000-428. eKr Baieri Chiemgau piirkonda tabanud tohutust meteoriidist.
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 Tüttensee. 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 Tüttensee 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 (Rappenglück 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 (Rappenglück et al. 2010: 435–37).
Sudden collapse of the Quaternary soil to form sinkholes on the order of meters and tens of meters has been a geologic phenomenon within living memory in a localized area north of Lake Chiemsee in Southeast Germany. Failing a satisfying explanation, a relation with an undefined glaciation process has always been proposed. Excavations and geophysical measurements at three newly affected sites show underground features such as prominent sandy-gravelly intrusions and extrusions typical of rock liquefaction processes well known to occur during strong earthquakes. Since strong earthquakes can reasonably be excluded to have affected the area under discussion, it has been suggested that the observed widespread liquefaction is related with the recently proposed Holocene Chiemgau meteorite impact event. Except for one earlier proposed but unassertive relation between impact and liquefaction, the obviously direct association of both processes in the Chiemgau area emphasizes that observed paleoliquefaction features need not necessarily have originated solely from paleoseismicity but can provide a recognizable regional impact signature.
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