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.
186 results for "Late Glacial" — page 5 of 10
E_3_04 — Doggerland and Sundaland — Drowned Continental Shelves
Doggerland and Sundaland represent two of the most significant landmasses lost to post-glacial sea level rise, together encompassing hundreds of thousands of square kilometers of habitable terrain that was progressively
E_3_08 — Dansgaard-Oeschger Events and Abrupt Climate Change
Dansgaard-Oeschger (DO) events are rapid climate oscillations during the last glacial period (c. 115,000–11,700 years ago) characterized by abrupt warming of 5–16°C in Greenland within decades — among the most dramatic a
E_3_20 — Dansgaard-Oeschger Events: Rapid Climate Oscillations
Dansgaard-Oeschger (D-O) events are rapid climate oscillations first identified in Greenland ice cores, characterized by abrupt warming of 8–16°C over Greenland within decades, followed by gradual cooling over centuries
E_3_02 — Catastrophic Flood Geomorphology
Earth's surface preserves dramatic evidence of catastrophic floods on a scale unimaginable today. The Channeled Scablands of Washington State were carved by the Missoula Floods (~13,000–15,000 BP): glacial Lake Missoula
E_3_09 — Messinian Salinity Crisis
The Messinian Salinity Crisis (MSC) — approximately 5.96–5.33 million years ago (late Miocene) — was one of the most dramatic geological events in the Cenozoic: the near-complete desiccation (drying up) of the Mediterran
E_2_08 — Little Ice Age — Climate, Society, and the Modern World
The Little Ice Age (LIA) was a prolonged period of climatic cooling that affected much of the Northern Hemisphere from approximately 1300 to 1850 CE, with coldest intervals during the Maunder Minimum (1645–1715) and the
E_2_24 — The Bronze Age Collapse: Multi-Causal Catastrophe of 1177 BCE
The Late Bronze Age Collapse (~1200–1150 BCE) represents one of history's most dramatic civilizational disruptions, witnessing the destruction or severe decline of virtually every major eastern Mediterranean civilization
E_2_01 — 536 CE Climate Catastrophe
This document examines 536 CE Climate Catastrophe, a topic within the Cataclysms and Chronology research area. Key areas of investigation include "The Worst Year to Be Alive", Historical Eyewitness Accounts, The Volcanic
E_2_18 — Minoan Eruption Expanded: Tsunami, Ashfall, and Civilization Collapse
The Minoan eruption of Thera (modern Santorini, Greece) was one of the largest volcanic eruptions of the Holocene — a VEI 6–7 event that ejected approximately 60–100 km³ of magma (DRE; some estimates reach 40 km³ DRE wit
E_4_21 — Oxygen Isotope Stages: Marine Isotope Record and Climate Cycles
The marine oxygen isotope record — constructed from measurements of the ratio of oxygen-18 to oxygen-16 (δ¹⁸O) in the calcium carbonate (CaCO₃) shells of foraminifera (single-celled marine organisms) preserved in deep-se
E_4_10 — Ice Core Science: Greenland and Antarctic Climate Records
Ice cores drilled from the Greenland and Antarctic ice sheets constitute one of the most powerful archives of past climate on Earth. Greenland cores (GRIP, GISP2, NGRIP, NEEM) provide high-resolution records extending ba
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_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
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_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_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
E_5_10 — Justinianic Plague: The First Pandemic and the Fall of the Ancient World
The Justinianic Plague (541–750 CE) — the first historically documented pandemic of bubonic plague caused by Yersinia pestis — struck the Byzantine Empire at the height of Emperor Justinian I's attempted reconquest of th
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
BROWSE BY SECTION — 3,721 documents across 34 fields