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.
3,009 results for "System 1 System 2" — page 93 of 151
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_03 — Moon Formation & Artificial Moon Theory
This document examines Moon Formation & Artificial Moon Theory, a topic within the Cataclysms and Chronology research area. Key areas of investigation include The "Ringing Like a Bell" Phenomenon, Low Density and Mass Di
E_1_05 — The Hollow Moon: Evidence, Anomalies & Theories
This document examines The Hollow Moon: Evidence, Anomalies & Theories, a topic within the Cataclysms and Chronology research area. Key areas of investigation include Apollo Seismic "Ringing Like a Bell", Anomalous Densi
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_16 — Thera/Santorini Eruption: Detailed Analysis of the Minoan Catastrophe
The eruption of Thera (modern Santorini, Greece) was one of the largest volcanic events in the Holocene — estimated at VEI 6–7 (Volcanic Explosivity Index), ejecting approximately 30–80 km³ of magma (dense rock equivalen
E_1_00 — Impact Space Catastrophes: Subfolder Summary
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_02 — The Ordovician-Silurian Mass Extinction
The Late Ordovician mass extinction (c. 445–444 million years ago, at the Ordovician-Silurian boundary) was the second-most severe extinction event in Earth's history in terms of percentage of species lost — approximatel
ZG_2_06 — Historical Linguistics and Language Family Classification
Historical linguistics is the scientific study of how languages change over time, how they are related to each other, and how they can be grouped into language families descended from common ancestors. The discipline's c
ZG_2_02 — Pidgins, Creoles, and Language Contact Phenomena
Pidgins and creoles are languages born from contact between groups with no shared language — they offer a natural laboratory for studying how human linguistic capacity creates new grammatical systems under extreme condit
ZG_2_09 — Tok Pisin, Lingua Francas, and Global Contact Languages
A lingua franca (from medieval Italian — originally denoting the pidginized Romance-based trade language of the Mediterranean, the "Frankish tongue") is any language used as a common medium of communication between speak
ZG_2_05 — Sacred Languages — Sanskrit, Hebrew, Arabic, Latin
Across civilizations, certain languages have been elevated above the ordinary functions of communication to the status of sacred or liturgical languages — vehicles believed to possess special power by virtue of their con
ZG_2_03 — Endangered Languages and Revitalization Movements
Of the approximately 7,000 languages spoken in the world today, linguists estimate that 40–50% are endangered — meaning they are no longer being learned by children and will likely cease to be spoken within one to two ge
ZG_2_04 — Oral-Formulaic Composition — Parry-Lord Theory
The oral-formulaic theory (also called the Parry-Lord theory) is one of the most influential discoveries in 20th-century humanities: the demonstration that great oral epics like Homer's Iliad and Odyssey were not compose
ZG_2_07 — Dead Languages: Extinction, Documentation, and Revival
A dead language is one that no longer has any native speakers — no community transmits it to children as a first language through normal intergenerational communication. Of the approximately 7,000 languages spoken today,
ZG_2_08 — Etymology and Historical Word Origins
Etymology is the study of the origin, history, and changing meanings of words — tracing the life of a word from its earliest attested form (or its reconstructed proto-form) through the centuries of sound change, semantic
ZG_2_00 — Language Families History: Subfolder Summary
ZG_5_02 — Narrative Structure: Story Grammar and Discourse Analysis
Narrative structure — the recurring patterns by which humans organize events into stories — is one of the most fundamental and universal features of human cognition and communication. From Aristotle's observation (c. 335
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