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حوزهباستان‌شناسیژئوفیزیک
خانوادهProcess / pipelineProcess / pipeline
سال پیدایش19601949
پدیدآورIrving FriedmanWillard Libby
نوعHydration layer dating techniqueChronometric method based on ¹⁴C decay
منبع بنیادینFriedman, I., & Smith, R. L. (1960). A new dating method using obsidian: Part 1, the surface rind method. Journal of Geophysical Research, 65(4), 1287-1291. link ↗Libby, W. F. (1949). Radiocarbon dating. University of Chicago Press. link ↗
نام‌های دیگرOHD, obsidian hydration method¹⁴C dating, Carbon-14 dating
مرتبط43
خلاصهObsidian hydration dating (OHD) is a chronometric method that determines the age of obsidian artifacts by measuring the thickness of a hydration layer formed on their exposed surfaces. Developed by Irving Friedman and Robert Smith in 1960, it is based on the principle that fresh obsidian surfaces absorb water from the surrounding environment at a measurable rate. The method is particularly valuable in archaeology for dating volcanic glass tools and other obsidian objects, especially in regions where obsidian was commonly used for cutting and scraping implements.Radiocarbon dating is a radiometric technique that determines the age of organic materials by measuring the radioactive decay of ¹⁴C (carbon-14), a rare isotope produced in the atmosphere by cosmic ray interactions. Developed by Willard Libby in 1949, radiocarbon dating became a foundational method in archaeology, paleoclimate studies, and geology, enabling dating of organic materials from the past ~50,000 years with typical precision of ±50–100 years.
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ScholarGateمقایسهٔ روش‌ها: Obsidian Hydration Dating · Radiocarbon Dating. بازیابی‌شده در 2026-06-19 از https://scholargate.app/fa/compare