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Archaeologia Polona Vol. 56 (2018)
Institute of Archaeology and Ethnology Polish Academy of Sciences
The study details a pilot experiment in which samples of “chocolate’”flint from four procurement sites in Poland and chert from the United States were characterized spectrally and distinguished using reflectance spectroscopy and multivariate statistics. The characterization of ‘chocolate’ flint and the successful differentiation of sources has been, and continues to be, a major research focus for understanding prehistoric consumption, use, and distribution of this favored lithic resource. Reflectance spectroscopy potentially provides an analytical methodology for identifying artefact source by successfully distinguishing spatially and compositionally unique deposits. Initial results from the study show that “chocolate” flint can be distinguished from other silicite tool stone resources, regional lookalike materials, and by individual deposit. Future studies will test a more robust sample size of ‘chocolate’ flints and conduct experiments on surface weathering
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oai:rcin.org.pl:73278 ; 0066-5924 ; doi:10.23858/APa56.2018.007
IAiE PAN, sygn. P 357 ; IAiE PAN, sygn. P 358 ; IAiE PAN, sygn. P 356 ; click here to follow the link
Licencja Creative Commons Uznanie autorstwa-Na tych samych warunkach 3.0 Polska
Zasób chroniony prawem autorskim. [CC BY-SA 3.0 PL] Korzystanie dozwolone zgodnie z licencją Creative Commons Uznanie autorstwa-Na tych samych warunkach 3.0 Polska, której pełne postanowienia dostępne są pod adresem: ; -
Instytut Archeologii i Etnologii Polskiej Akademii Nauk
Biblioteka Instytutu Archeologii i Etnologii PAN
Mar 3, 2023
Jun 19, 2019
370
https://rcin.org.pl./publication/88941
Edition name | Date |
---|---|
Parish, Ryan M., 2018, Characterizing “Chocolate” Flint Using Reflectance Spectroscopy | Mar 3, 2023 |
Hughes, Richard E. Werra, Dagmara H. Siuda, Rafał
Miazga, Beata
Rdzeń wiórowy jednopiętowy późny paleolit, Plejstocen (Alleröd - Młodszy Dryas, GI-1a - GS-1)
Rdzeń wiórowy jednopiętowy późny paleolit, Plejstocen (Alleröd - Młodszy Dryas, GI-1a - GS-1)
Tylczak późny paleolit, Plejstocen (Alleröd - Młodszy Dryas, GI-1a - GS-1)