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.
2,501 results for "La Venta" — page 21 of 126
E_2_14 — Deccan Traps and Large Igneous Provinces
Large Igneous Provinces (LIPs) are the most voluminous volcanic features on Earth: enormous outpourings of basalt lava and associated intrusions that cover areas of up to millions of square kilometers and release colossa
E_2_09 — Heinrich Events and Bond Cycles: Millennial-Scale Climate Oscillations
Heinrich events are episodes of massive iceberg discharge from the Laurentide Ice Sheet through Hudson Strait into the North Atlantic, depositing distinctive layers of ice-rafted debris (IRD) across the ocean floor. Firs
E_2_03 — Santorini/Thera Eruption and Minoan Collapse
Around 1600 BCE (revised range: 1628–1600 BCE), the volcanic island of Thera (modern Santorini) in the southern Aegean Sea experienced one of the largest volcanic eruptions in recorded human history — a VEI-7 event that
E_2_06 — Black Death, Pandemic Cycles, and Civilizational Reset
The Black Death (1347–1353 CE) was the most devastating pandemic in recorded human history. Caused by the bacterium *Yersinia pestis and transmitted primarily through flea bites from infected rats, the plague killed an e
E_2_16 — Laacher See Eruption: European Catastrophe at 12,900 BP
The Laacher See eruption — centered on the Laacher See caldera in the East Eifel Volcanic Field of western Germany, approximately 37 km south of Bonn — was the largest volcanic eruption in central Europe during the late
E_2_15 — Azolla Event and Eocene Arctic Cooling
The Azolla Event (c. 49 Ma, Middle Eocene) refers to a period of approximately 800,000 years during which the floating freshwater fern _Azolla_ bloomed prolifically across the semi-enclosed Arctic Ocean, sequestering mas
E_2_21 — Mount Vesuvius and the Destruction of Pompeii and Herculaneum (79 CE)
The eruption of Mount Vesuvius on August 24, 79 CE (or possibly late October, per recent evidence) destroyed the Roman cities of Pompeii and Herculaneum in one of the most well-documented natural disasters of antiquity.
E_4_19 — Mono Lake and Gothenburg Excursions: Short Geomagnetic Events
Geomagnetic excursions are brief, extreme departures of the Earth's magnetic field from its normal dipolar configuration — events during which the virtual geomagnetic pole (VGP) deviates by more than 40–45° from the geog
E_4_13 — Milankovitch Cycles and Orbital Forcing
Milankovitch cycles are periodic variations in Earth's orbital geometry that modulate the distribution and intensity of solar radiation reaching Earth's surface, driving the glacial-interglacial cycles that have dominate
E_4_09 — Magnetic Pole Reversals and the Laschamp Event
Earth's magnetic field periodically undergoes geomagnetic reversals — events in which the north and south magnetic poles swap polarity. This has occurred at least 183 times in the last 83 million years, with the last ful
E_1_13 — Cosmic Impact Markers: Nanodiamonds, Microspherules, Platinum
Cosmic impact markers are distinctive mineralogical, geochemical, and textural features preserved in geological strata that provide evidence for extraterrestrial impact events — including asteroid/comet impacts and airbu
E_1_14 — Supernovae in Human History: Crab Nebula, SN 1006, Vela
Supernovae — the catastrophic explosions of massive stars (core-collapse, Type II/Ib/Ic) or white dwarfs exceeding the Chandrasekhar mass limit (thermonuclear, Type Ia) — are among the most energetic events in the univer
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_05 — Late Devonian Mass Extinction: Kellwasser and Hangenberg Events
The Late Devonian mass extinction (~372–359 Ma) was not a single catastrophe but a series of extinction pulses spanning approximately 25 million years, making it unique among the "Big Five" mass extinctions. The two most
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_11 — Language Isolates: Basque, Ainu, Sumerian, Burushaski
A language isolate is a language that has no demonstrable genealogical (genetic) relationship with any other known language — it stands alone, unrelated to any language family, a sole surviving branch on the tree of huma
ZG_2_10 — Language Documentation and Field Methods
Language documentation is the systematic recording, annotation, preservation, and dissemination of a language's spoken (and signed) forms — encompassing its phonology, morphology, syntax, semantics, pragmatics, and the f
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_12 — Language Contact and Substrate Effects in Ancient Civilizations
Language contact — the situation in which speakers of different languages interact and their languages influence one another — is one of the most powerful forces shaping linguistic change, and its effects are pervasive t
ZG_2_15 — Language Attrition: How First Languages Are Lost
Language attrition — the process by which a previously acquired language is gradually lost by an individual speaker due to reduced use and exposure — is one of the most fascinating and practically important phenomena in
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