Category:Chiemgau impact hypothesis
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Chiemgau impact hypothesis is an scientific theory that claimed the Tüttensee lake in southern Bavaria, Germany to be the result of an Holocene meteorite impact. This claim has been refuted by geological research and the finding of a Soil horizon of undisturbed peat and sedimentation since the end of the last glaciation period.
Media in category "Chiemgau impact hypothesis"
The following 13 files are in this category, out of 13 total.
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2014-07-20-donnerloch-helming-prof2.png 589 × 466; 207 KB
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Bodensenke 004.jpg 2,000 × 1,125; 4.26 MB
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Burghausen 011 Einsiedeleiche.jpg 800 × 533; 910 KB
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Cirt-crater 004.jpg 512 × 384; 113 KB
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Cirt-crooked-creek-und-tüttensee.jpg 2,592 × 1,944; 951 KB
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Cirt-tuettensee-gravimetriemessung.JPG 504 × 428; 63 KB
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Egu 2019 chiemite poster.pdf 6,968 × 4,966; 980 KB
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Fehr et al (2005).jpg 503 × 750; 238 KB
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Huber Rob et al 2020 Abb 10.jpg 2,068 × 1,551; 3.34 MB
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Huber Rob et al 2020 Abb 11.jpg 2,068 × 1,551; 2.89 MB
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Huber Rob et al 2020 Abb 13.png 2,067 × 1,879; 932 KB
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Huber Rob et al 2020 Abb 9.jpg 2,068 × 1,551; 3.73 MB
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Tüttensee, östliches Verlandungsmoor.png 2,739 × 3,196; 45.94 MB
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