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32 results for "isotope" — page 2 of 2
G_2_10 — Zooarchaeology — Animal Bones as Cultural Evidence
Zooarchaeology (also called archaeozoology) is the study of animal remains — primarily bones, teeth, antler, horn, and shell — recovered from archaeological sites, to reconstruct past human-animal relationships, includin
G_2_17 — Biogeochemistry and Ancient Environmental Reconstruction
Biogeochemistry — the study of chemical, physical, geological, and biological processes that govern the composition and cycling of elements and compounds in natural environments — provides essential tools for reconstruct
O_5_17 — Deep Time: Geological Chronology and the Scale of Earth History
Deep time is the concept that Earth's geological history extends across approximately 4.54 billion years — a scale so vast that human civilization occupies less than 0.00001% of it. First articulated by James Hutton in 1
R_1_09 — The Great Oxidation Event: Oxygen, Cyanobacteria, and Earth's Atmospheric Transformation
The Great Oxidation Event (GOE), occurring approximately 2.4–2.1 billion years ago during the Paleoproterozoic, was the most dramatic chemical transformation in Earth's history — atmospheric oxygen rose from trace levels
F_2_15 — Turquoise Trade Networks: Mesoamerica to American Southwest
Turquoise — the distinctive blue-green copper-aluminum phosphate mineral — was one of the most valued materials in the pre-Columbian Americas, and its trade networks connected the American Southwest to Mesoamerica across
F_2_06 — Tin Sources and the Bronze Age Mystery
The Bronze Age (c. 3300–1200 BCE) depended fundamentally on tin — the scarce metal alloyed with copper to produce bronze (typically 88–92% copper, 8–12% tin). While copper was widely available across the Mediterranean, N
F_2_13 — Copper Trade Networks: Great Lakes to Mediterranean
The Great Lakes copper deposits — particularly the vast deposits of native (naturally pure) copper on the Keweenaw Peninsula and Isle Royale of Michigan's Upper Peninsula — represent one of the world's most remarkable mi
F_3_04 — Spread of Metallurgy: Copper, Bronze, Iron Across the Ancient World
Metallurgy developed independently in multiple regions, beginning with native copper use by ~9000 BCE and smelting by ~7000 BCE in Anatolia. The transition from copper to arsenical bronze and then tin bronze reshaped anc
ZA_3_03 — Nuclear Physics: Fission, Fusion, and the Heart of Matter
Nuclear physics studies the atomic nucleus — the dense core of protons and neutrons bound by the strong nuclear force, containing 99.95% of an atom's mass in just 10⁻¹⁵ meters. The field revealed that mass can be convert
I_4_09 — Scientific Analysis of UAP Physical Evidence — Trace Cases
Physical trace cases represent one of the most scientifically significant — yet frustratingly inconclusive — categories of UAP evidence: instances where alleged UAP encounters left measurable, physical residues on the en
I_4_10 — UAP Materials Analysis: Metamaterials and Physical Evidence
Among the most physically grounded lines of UAP evidence is the analysis of material samples allegedly associated with UAP events — fragments, residues, or artifacts recovered from sighting locations and subsequently sub
E_4_16 — Cosmogenic Isotope Dating: Beryllium-10 and Exposure Ages
Cosmogenic nuclide dating (also called cosmogenic exposure dating or terrestrial cosmogenic nuclide, TCN, dating) is a geochronological method that determines how long a rock surface has been exposed at or near Earth's s
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