RESEARCH BASE
Search 3,721 documents across 34 fields — every claim tier-rated by evidence
3,633 are the core, quality-scored corpus (34 lettered sections — see How We Work); the remaining 88 are cross-corpus synthesis documents (68 InterDocs, 12 Connections, 8 Theories) also indexed here.
3,692 results for "g factor" — page 36 of 185
E_4_02 — Radiocarbon Calibration & Chronology Shifts
This document examines Radiocarbon Calibration & Chronology Shifts, a topic within the Cataclysms and Chronology research area. Key areas of investigation include The Physics , Key Parameters, What Can Be Dated. Notable
E_4_15 — Thermoluminescence and OSL Dating: Beyond Radiocarbon
Thermoluminescence (TL) and Optically Stimulated Luminescence (OSL) dating are trapped-charge geochronological techniques that determine the time elapsed since a mineral grain (typically quartz or feldspar) was last expo
E_4_24 — Quaternary Science: Integrating Ice Ages, Extinctions, and Migrations
Quaternary science is the interdisciplinary study of Earth's most recent geological period — the Quaternary (2.58 Ma to present), encompassing the Pleistocene (2.58 Ma to 11,700 BP) and the Holocene (11,700 BP to present
E_4_12 — Dendrochronology: Tree-Ring Science and Precise Ancient Dating
Dendrochronology — the science of dating based on the analysis of tree-ring growth patterns — is one of the most precise dating methods available to archaeology, climatology, and ecology. Pioneered by Andrew Ellicott Dou
E_4_04 — Mathematical Encoding in Mythology
Certain numbers appear with suspicious regularity across ancient mythologies worldwide: 72 (Egyptian conspirators against Osiris, degrees of precessional shift per degree), 108 (Hindu/Buddhist sacred number, suitors of P
E_4_22 — Varve Chronology: Annual Lake Sediment Records
Varve chronology is a dating and paleoclimate method based on counting and analyzing varves — annually laminated sediment layers deposited in lakes (and occasionally in marine or estuarine settings). Each varve typically
E_4_27 — Chicxulub Impact and the K-Pg Mass Extinction
The Chicxulub impact was a catastrophic asteroid strike that occurred approximately 66.043 ± 0.011 million years ago at what is now the Yucatan Peninsula, Mexico, marking the boundary between the Cretaceous and Paleogene
E_4_14 — Stratigraphic Methods and Geological Timekeeping
Stratigraphy — the study of rock layers (strata) and their sequential relationships — is the foundational framework for understanding geological time and establishing the chronology of Earth's 4.54-billion-year history.
E_4_25 — Bayesian Age Modeling: Statistical Frameworks for Archaeological Chronology
Bayesian age modeling — the application of Bayesian statistical inference to combine radiocarbon dates with prior archaeological knowledge (stratigraphy, typology, historical constraints) to produce refined chronological
E_1_11 — Comet Encke and the Taurid Complex: Recurring Cosmic Threat
Comet 2P/Encke — a short-period comet with the shortest known orbital period of any bright comet (3.3 years) — is the most prominent surviving fragment of a much larger cometary body whose progressive disintegration over
E_1_04 — Complete Meteor & Asteroid Impact Catalog: Earth's Full Bombardment History
This document examines Complete Meteor & Asteroid Impact Catalog: Earth's Full Bombardment History, a topic within the Cataclysms and Chronology research area. Key areas of investigation include Theia Giant Impact (~4.51
E_1_01 — The Younger Dryas Impact Hypothesis (YDIH)
This document examines The Younger Dryas Impact Hypothesis (YDIH), a topic within the Cataclysms and Chronology research area. Notable findings include: Greenland ice-core data confirm rapid cooling at onset and abrupt w
E_1_15 — Uranium-Thorium Dating: Methodology and Applications in Deep Time
Uranium-thorium (U-Th) dating, also called uranium-series disequilibrium dating, is a radiometric technique that measures the decay of ²³⁴U to ²³⁰Th (half-life: ~245,620 years) in materials such as speleothems (cave form
E_1_10 — Impact Crater Morphology and Effects
Hypervelocity impact cratering — the formation of craters by the collision of asteroids, comets, and meteoroids with planetary surfaces at speeds of 11–72 km/s — is one of the most fundamental geological processes in the
E_1_07 — Tunguska Event and Modern Impact Evidence
On June 30, 1908, an atmospheric explosion over the Podkamennaya Tunguska River in central Siberia released energy equivalent to approximately 12 megatons of TNT (roughly 1,000 times the Hiroshima bomb), flattening 2,150
E_1_17 — Toba Supereruption: Genetic Bottleneck and Climate Catastrophe
The Toba supereruption — occurring approximately 74,000 years ago (74 ka) on the island of Sumatra, Indonesia — was the largest volcanic eruption of the last 2 million years and one of the most catastrophic events in hum
E_1_06 — Chicxulub Impact and the K-Pg Boundary
Approximately 66 million years ago, at the boundary between the Cretaceous and Paleogene periods (K-Pg boundary, formerly K-T boundary), a ~10 km diameter asteroid struck what is now the Yucatán Peninsula of Mexico, crea
E_5_09 — Catastrophism vs Uniformitarianism: Geological Paradigm Debates
The catastrophism vs uniformitarianism debate shaped the foundations of modern geology and continues to evolve. Georges Cuvier (1769–1832) championed catastrophism — the idea that Earth's geological features were shaped
E_5_08 — Justinianic Plague & Late Antique Pandemics
The Justinianic Plague (541–750 CE) was the first historically documented pandemic of bubonic plague caused by Yersinia pestis, striking the Byzantine Empire at the height of Emperor Justinian I's reconquest campaigns. A
E_5_01 — Bronze Age Collapse: A Detailed Systems Analysis
The Late Bronze Age Collapse (c. 1200–1150 BCE) was one of history's most devastating civilizational catastrophes — a cascading multi-system failure that destroyed or severely diminished virtually every major palace-base
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