RESEARCH BASE

Search 3,721 documents across 34 fields — every claim tier-rated by evidence

3,721 Documents 34 Sections 43,623 Citations 34,854 Keywords Indexed 4 Evidence Tiers

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.

25 results for "Holocene flooding" — page 1 of 2

M_5_23 Verified Forbidden Archaeology

M_5_23 — Post-Glacial Flooding and Submerged Archaeological Landscapes

Between the Last Glacial Maximum (LGM, c. 26,500–19,000 years ago) and approximately 6,000 years ago, global mean sea level rose by approximately 120–130 m, drowning continental shelves that had been habitable land. The

post-glacial flooding sea level rise Doggerland Sundaland meltwater pulse drowned coastlines
M_4_16 Verified Forbidden Archaeology

M_4_16 — Sundaland & Southeast Asian Lost Continent Hypothesis

Sundaland is the geological term for the exposed continental shelf of Southeast Asia that connected the present-day islands of Borneo, Java, Sumatra, and the Malay Peninsula into a single landmass during the Last Glacial

Sundaland Sunda Shelf sea level rise Southeast Asia lost civilization Younger Dryas
M_1_17 Credible Forbidden Archaeology

M_1_17 — Underwater City Discoveries (Dwarka, Yonaguni, Pavlopetri)

The discovery and investigation of submerged archaeological sites — cities, harbors, temples, and infrastructure now lying beneath coastal waters due to post-glacial sea level rise, tectonic subsidence, or local geologic

underwater archaeology submerged cities Dwarka Yonaguni Monument Pavlopetri sea level rise
ZF_3_01 Oceanography

ZF_3_01 — Sea-Level History: Glacial Cycles, Meltwater Pulses, and Coastal Archaeology

Sea level has varied by over 120 meters between glacial and interglacial periods, repeatedly reshaping coastlines, exposing and flooding continental shelves, and creating or destroying land bridges that directed human mi

sea level meltwater pulse glacial maximum LGM Holocene transgression eustatic change
E_4_11 Cataclysms & Chronology

E_4_11 — The Holocene Climate Optimum and Mid-Holocene Transition

The Holocene Climate Optimum (also called the Holocene Thermal Maximum or Hypsithermal) designates a prolonged warm interval roughly spanning 9,000–5,000 years before present, during which Northern Hemisphere summer temp

Holocene Thermal Maximum Holocene Climate Optimum Green Sahara African Humid Period Milankovitch obliquity
D_2_21 Credible Sites & Artifacts

D_2_21 — Black Sea Deluge: Archaeological Evidence for Rapid Flooding

The Black Sea Deluge Hypothesis proposes that the Black Sea — now a large saline body connected to the Mediterranean via the Bosporus Strait — was once a significantly smaller, lower freshwater lake during the Last Glaci

Black Sea deluge flood hypothesis Ryan Pitman Bosporus
E_5_06 Verified Cataclysms & Chronology

E_5_06 — Holocene Sixth Mass Extinction: Current Biodiversity Crisis

The Holocene "Sixth Mass Extinction" hypothesis holds that current species loss rates are 100–1,000 times the normal background extinction rate, driven primarily by human activity: habitat destruction, overexploitation,

sixth extinction Holocene Anthropocene biodiversity loss IUCN Red List background extinction rate
Y_4_15 Credible Altered States

Y_4_15 — Sensory Overload and Information Flooding: Excess as Altered State

Sensory overload — the state that arises when sensory input exceeds the brain's capacity for orderly processing — represents the mirror image of sensory deprivation as a pathway to altered consciousness. While deprivatio

sensory overload information overload Ganzfeld rave culture overwhelm information flooding
F_4_26 Verified Lost Connections

F_4_26 — The Green Sahara: African Humid Period Civilizations

The "Green Sahara" — also known as the African Humid Period (AHP) — refers to a period of profound climatic transformation that turned the Sahara Desert into a lush, habitable landscape of grasslands, lakes, rivers, and

Green Sahara African Humid Period Holocene Sahara Desert Gobero Nabta Playa
M_4_11 Verified Forbidden Archaeology

M_4_11 — Göbekli Tepe Climate Reconstruction: What Supported Its Builders?

Göbekli Tepe (~9600-8000 BCE), the monumental stone pillar sanctuary in southeastern Turkey, presents a fundamental puzzle: how did pre-agricultural hunter-gatherers — people who had not yet domesticated crops or animals

Göbekli Tepe climate Younger Dryas early Holocene archaeobotany archaeozoology
ZF_5_08 Verified Oceanography

ZF_5_08 — Coastal Geomorphology: Erosion, Beaches, and Barrier Islands

Coastal geomorphology is the study of landforms at the interface of land and sea — a dynamic zone shaped by the constant interaction of waves, tides, currents, wind, rivers, geology, biology, and increasingly by human ac

coastal geomorphology coastal erosion beach barrier island sea cliff longshore drift
E_3_15 Verified Cataclysms & Chronology

E_3_15 — Sea-Level Curves: Eustatic Change from LGM to Present

Sea-level curves — graphical reconstructions of how global mean sea level has changed through time — represent one of the most important datasets in Quaternary science, recording the waxing and waning of continental ice

sea level eustatic LGM Last Glacial Maximum post-glacial transgression
E_3_04 Cataclysms & Chronology

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

Doggerland Sundaland continental shelf post-glacial flooding Storegga Slide sea level rise
E_3_13 Verified Cataclysms & Chronology

E_3_13 — Storegga Slide: Mega-Tsunami and Mesolithic Europe

The Storegga Slide (Norwegian: Storegga-raset; Store = "great," egga = "edge") — a series of submarine landslides on the continental slope off western Norway at approximately 64°N — constitutes one of the largest known m

Storegga submarine landslide mega-tsunami Norway North Sea Doggerland
E_3_06 Cataclysms & Chronology

E_3_06 — The 8.2 Kiloyear Event: Sudden Cooling and Neolithic Disruption

The 8.2 kiloyear event (~6200 BCE) was the most severe abrupt climate oscillation of the Holocene, triggered by a catastrophic outburst flood from glacial Lakes Agassiz and Ojibway into the North Atlantic via Hudson Bay.

8.2 ka event Bond Event 5 Lake Agassiz outburst flood Neolithic disruption AMOC
E_2_07 Cataclysms & Chronology

E_2_07 — The 4.2 Kiloyear Event — Bronze Age Climate Catastrophe

The 4.2 kiloyear event (~2200 BCE) was a severe, century-scale aridification episode that constitutes one of the most significant abrupt climate changes of the Holocene. Identified through speleothem, marine sediment, an

4.2 kiloyear event megadrought Akkadian Empire collapse Old Kingdom Egypt Indus Valley decline Liangzhu collapse
E_4_17 Verified Cataclysms & Chronology

E_4_17 — Palynology: Pollen Records and Vegetation History

Palynology — the study of pollen grains and spores (and other organic-walled microfossils collectively termed palynomorphs) — is one of the most widely applied techniques in Quaternary science, archaeology, and paleoclim

palynology pollen spore pollen analysis vegetation history pollen diagram
E_4_24 Verified Cataclysms & Chronology

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

Quaternary Pleistocene Holocene ice age glaciation megafaunal extinction
E_4_22 Verified Cataclysms & Chronology

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

varve annual lamination lacustrine lake sediment glaciolacustrine clastic varve
ZB_5_19 Verified Ecology & Biology

ZB_5_19 — The Anthropocene: Human Dominance of Earth Systems and Epoch Dating

The Anthropocene — a proposed geological epoch defined by the dominant influence of human activity on Earth's geology, climate, and ecosystems — has become one of the most consequential and contentious concepts in modern

Anthropocene human impact epoch dating stratigraphic marker Great Acceleration nuclear fallout