Wednesday, August 25, 2010

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The end of the Tüttenseekraters

yesterday published the Bavarian State Office for the Environment in a press release initial results of its investigations of peat profiles of Tüttensee: In detail, before four dates, three of which were made on peat samples.
Already the top and therefore the youngest sample has an age of about 4,500 years ago. Further, from a greater depth obtained, peat samples were dated to about 6,800 and 10,000 years. Finally, shows a sample from the lake sediments occurring below the age of 12,000 years:

age dating of the profile attachment (Kroemer, 2009): 0.6 m

: Cal BP 4580-4420

0.8 m: Cal BP 6890-6670

2.5m: Cal BP 10220-9910

2.8 m: Cal BP 12750-12390


The presented age determinations show clearly the formation of the glacial Tüttensee as Toteisloch. They include the formation completely by a Celtic temporal cosmic event.
should ensure that the end of the short career of Tüttensee be sealed as impact craters.


The full Report can be viewed here:

Kroemer, E. 2010th Sediment sampling and dating in the sedimentation zone of Tüttensee. http://www.lfu.bayern.de/geologie/doc/tuettensee_datierungen_kurztext_kea_end.pdf

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