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.

63 results for "coastal route" — page 1 of 4

F_1_27 Credible Lost Connections

F_1_27 — Ice Age Maritime Routes & Coastal Migration

The recognition that maritime capabilities existed during the Ice Age (Late Pleistocene, ~126,000–11,700 years ago) has transformed our understanding of early human dispersals and the colonization of previously isolated

Ice Age maritime coastal migration Kelp Highway Last Glacial Maximum watercraft
F_1_22 Verified Lost Connections

F_1_22 — Peopling of the Americas: Routes & Chronology

The peopling of the Americas — when, how, and by whom the Western Hemisphere was first colonized by modern humans — is one of the most actively debated questions in archaeology, genetics, and paleoanthropology, with the

Peopling Americas Beringia Clovis pre-Clovis Monte Verde coastal migration
F_1_07 Lost Connections

F_1_07 — First Americans Debate — Clovis, Pre-Clovis, and Coastal Routes

The question of when and how humans first reached the Americas has been transformed in the 21st century by a series of discoveries that have demolished the long-reigning "Clovis-first" paradigm. For decades, the archaeol

First Americans Clovis pre-Clovis Monte Verde Buttermilk Creek White Sands footprints
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
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
ZF_1_15 Verified Oceanography

ZF_1_15 — Wave Physics: Wind Waves, Swell, and Coastal Dynamics

Ocean surface waves are the most visible expression of ocean-atmosphere energy transfer — created by wind blowing across the water surface, they travel across entire ocean basins and dissipate their energy on distant coa

ocean waves wind waves swell wave physics wave height wave period
L_2_09 Verified Genetics & Origins

L_2_09 — Genetic History of the Americas: Clovis to Contact

The genetic history of the Americas — from the initial peopling of the New World to the devastating population collapse after European contact — is one of the most intensively studied and rapidly evolving areas of paleog

Americas Native American Beringia Clovis pre-Clovis Anzick
F_1_16 Credible Lost Connections

F_1_16 — Coastal Migration Hypothesis: Kelp Highway and Pacific Rim

The coastal migration hypothesis (also known as the "Kelp Highway" hypothesis) proposes that the initial human colonization of the Americas occurred not via the traditional ice-free corridor through the interior of North

coastal migration kelp highway Pacific Rim first Americans Out of Africa maritime
F_1_12 Verified Lost Connections

F_1_12 — Beringia: Land Bridge, Migration, and Lost Landscape

Beringia — the vast landmass that periodically connected northeastern Asia to northwestern North America across what is now the Bering Strait and the shallow Chukchi and Bering Seas — was one of the most consequential ge

Beringia land bridge Bering Strait migration Americas peopling
ZF_5_07 Verified Oceanography

ZF_5_07 — Upwelling Systems: Coastal Productivity and Fisheries Foundations

Upwelling — the wind-driven or current-driven ascent of cold, nutrient-rich deep water to the sunlit surface layer — is the foundation of the ocean's most productive ecosystems and the world's most valuable fisheries. Th

upwelling coastal upwelling Ekman transport wind-driven eastern boundary current nutrient enrichment
ZF_4_09 Verified Oceanography

ZF_4_09 — Seagrass and Coastal Carbon Sequestration (Blue Carbon)

Blue carbon refers to the carbon captured and stored by coastal and marine ecosystems — primarily seagrass meadows, mangrove forests, and salt marshes — which sequester carbon at rates per unit area far exceeding terrest

blue carbon seagrass Posidonia eelgrass Zostera coastal carbon
O_3_06 Earth Anomalies

O_3_06 — Tidal Phenomena, Maelstroms & Coastal Anomalies

Earth's tides — generated primarily by the gravitational interactions between the Earth, Moon, and Sun — produce a range of extreme and visually spectacular phenomena where local bathymetry, coastal geometry, and resonan

tidal bore maelstrom Bay of Fundy Saltstraumen tidal range coastal anomaly
F_2_11 Verified Lost Connections

F_2_11 — Ancient Spice and Incense Routes: Aromatic Trade Networks

The trade in aromatic substances — frankincense, myrrh, cinnamon, cassia, pepper, cloves, nutmeg, camphor, sandalwood, spikenard, and dozens of other plant-derived resins, barks, seeds, and oils — constitutes one of the

spice trade incense route frankincense myrrh cinnamon pepper
F_2_21 Credible Lost Connections

F_2_21 — Ancient Pigment and Dye Trade Routes

Pigments and dyes ranked among the most valuable traded commodities in the ancient world — sometimes rivaling precious metals in cost per unit weight. Lapis lazuli traveled over 4,000 km from mines in Badakhshan (Afghani

pigment-trade tyrian-purple lapis-lazuli indigo cochineal vermillion
F_2_22 Verified Lost Connections

F_2_22 — Ancient Pigment Trade Routes: Lapis Lazuli, Tyrian Purple & Cinnabar

Pigments were among the most valued trade goods of the ancient world, with some traversing distances exceeding 4,000 km from source to final use. Lapis lazuli from the Sar-i Sang mines in Badakhshan (northeastern Afghani

ancient-pigment-trade lapis-lazuli tyrian-purple cinnabar vermillion ultramarine
F_3_10 Verified Lost Connections

F_3_10 — Plague and Disease Transmission Along Trade Routes

The same trade routes and migration corridors that connected distant civilizations also served as highways for pandemic disease, making pathogen transmission one of the most consequential — and devastating — forms of "lo

plague Yersinia pestis Black Death Justinianic plague Columbian Exchange pandemic
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
ZF_2_06 Verified Oceanography

ZF_2_06 — Mangrove and Estuary Ecosystems

Mangroves and estuaries are transitional ecosystems where terrestrial and marine environments meet, creating some of the most biologically productive and ecologically critical habitats on Earth. Estuaries — semi-enclosed

mangrove estuary salt marsh brackish water coastal wetland nursery habitat
ZF_2_08 Verified Oceanography

ZF_2_08 — Kelp Forests and Seagrass Meadows

Kelp forests and seagrass meadows are the ocean's equivalents of terrestrial forests and grasslands — highly productive underwater ecosystems that provide habitat, food, nursery grounds, carbon sequestration, and coastal

kelp forest seagrass macroalgae Macrocystis Posidonia underwater forest
E_2_27 Verified Cataclysms & Chronology

E_2_27 — Mega-Tsunami History: Evidence for Catastrophic Wave Events

Mega-tsunamis — wave events with initial amplitudes of tens to hundreds of meters, far exceeding the 10–30 m waves generated by typical seismic tsunamis — are produced by catastrophic mechanisms including volcanic flank

mega-tsunami megatsunami Lituya Bay Storegga Slide Canary Islands volcanic flank collapse