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Upadek meteorytu Przełazy w świetle danych geomorfologicznych i geologicznych

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Stankowski W. T. J.
Acta Societatis Metheoriticae Polonorum
|
2012
|
vol. 3
104-111
EN
The age and possible location of the Przełazy (Seelasgen) meteorite fall have been established on a study of morphology and composition of the fine-grained magnetic fraction of peat/gyttja profiles. The most probable place of fall is the present peat-bog, situated south–west side of Przełazy. The age of fall is estimated as the end of the Late Glacial to the beginning of the Holocene.
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