RESEARCH BASE

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

3,721 Documents 34 Sections 43,625 Citations 34,852 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.

70 results for "volcanic glass" — page 1 of 4

D_5_13 Verified Sites & Artifacts

D_5_13 — Obsidian: Volcanic Glass in Technology, Trade, and Ritual

Obsidian — a naturally occurring volcanic glass formed when felsic lava cools rapidly with insufficient crystal growth — is one of the most important materials in human technological and cultural history. Prized for its

obsidian volcanic glass lithic technology obsidian hydration dating Çatalhöyük Mesoamerican obsidian
F_4_32 Verified Lost Connections

F_4_32 — Obsidian Trade Networks: Volcanic Glass and Long-Distance Exchange

Obsidian — volcanic glass formed when felsic lava cools rapidly — was one of the most important raw materials in human prehistory, prized for its ability to produce the sharpest cutting edges known (fracture to edges of

obsidian trade networks volcanic glass sourcing geochemistry XRF
E_4_18 Verified Cataclysms & Chronology

E_4_18 — Tephra Chronology: Volcanic Ash as Geological Clock

Tephrochronology is the use of volcanic tephra layers (ash, pumice, and other pyroclastic deposits) as time markers (isochrons) for dating and correlating geological, paleoenvironmental, and archaeological sequences acro

tephrochronology tephra volcanic ash isochron marker bed cryptotephra
M_1_13 Verified Forbidden Archaeology

M_1_13 — Lycurgus Cup and Ancient Nanotechnology: Dichroic Glass

The Lycurgus Cup is a 4th-century CE Roman cage cup (diatretum) made of dichroic glass, currently in the collection of the British Museum (accession no. 1958,1202.1). It is the most complete surviving example, and one of

Lycurgus Cup dichroic glass nanotechnology gold nanoparticles silver nanoparticles surface plasmon resonance
E_3_19 Verified Cataclysms & Chronology

E_3_19 — Volcanic Aerosol Forcing and Historical Climate Disruption

Explosive volcanic eruptions inject sulfur dioxide (SO₂) into the stratosphere, where it converts to sulfate aerosol particles (H₂SO₄) that reflect incoming solar radiation and cool Earth's surface for 1–3 years. This pr

volcanic-aerosol climate-forcing sulfate-aerosol volcanic-winter tambora toba
J_4_16 Verified Ancient Technology

J_4_16 — Ancient Glass Technology: Production, Trade, and Innovation

Ancient glass technology represents one of humanity's most sophisticated materials-science achievements, spanning from earliest faience production (~4500 BCE, predynastic Egypt and Mesopotamia) through the revolutionary

ancient glass faience glassblowing Roman glass Lycurgus Cup natron
O_2_01 Verified Earth Anomalies

O_2_01 — Volcanism, Supervolcanoes, and Geological Catastrophism

Volcanic eruptions are among the most powerful forces on Earth, capable of altering global climate, triggering mass extinctions, collapsing civilizations, and imprinting themselves on human mythology for millennia. The T

volcano volcanism supervolcano caldera eruption Toba
O_4_12 Verified Earth Anomalies

O_4_12 — Libyan Desert Glass: Silica Mystery and Impact Hypotheses

Libyan Desert Glass (LDG) is a naturally occurring, nearly pure silica glass (~98% SiO₂) found scattered across a roughly 6,500 km² area of the Great Sand Sea on the Egypt-Libya border in the western Sahara Desert. The g

Libyan desert glass LDG silica glass impactite airburst Sahara
O_5_12 Verified Earth Anomalies

O_5_12 — Volcanic Islands: Surtsey, Hawaii, and Emergent Land

Volcanic islands — landmasses formed by submarine volcanic eruptions that build up from the ocean floor until they breach the sea surface — represent some of the most dynamic and scientifically informative geological fea

volcanic island Surtsey Hawaii hot spot seamount island arc
F_2_19 Verified Lost Connections

F_2_19 — Obsidian Trade Networks in the Ancient World

Obsidian — volcanic glass formed by rapid cooling of silica-rich lava — was the most extensively traded lithic material in the ancient world, coveted for its conchoidal fracture producing edges sharper than modern surgic

obsidian trade network sourcing XRF neutron activation Çatalhöyük
F_2_04 Verified Lost Connections

F_2_04 — Obsidian Trade Networks: Archaeological Tracers of Ancient Exchange

Obsidian — naturally occurring volcanic glass formed when felsic lava cools rapidly — was one of the most valued materials in the prehistoric world. Its conchoidal fracture produces the sharpest edges known (thinner than

obsidian obsidian sourcing XRF analysis neutron activation analysis Çatalhöyük Göbekli Tepe
F_2_14 Verified Lost Connections

F_2_14 — Ancient Glass Bead Trade: From Mesopotamia to Sub-Saharan Africa

Glass beads are among the most archaeologically informative objects in the ancient world — small, durable, widely traded, and chemically distinctive — making them exceptional tracers of long-distance exchange networks sp

glass bead trade Mesopotamia Egypt Indo-Pacific
F_4_13 Verified Lost Connections

F_4_13 — Glass Production: Origins, Trade, and Technology Transfer

Glass is one of the earliest synthetic materials, with origins tracing to faience (glazed quartz) production in Egypt and Mesopotamia by ~5000 BCE and true glass beads appearing by ~3500 BCE. For over two millennia, glas

glass production faience core-formed glass glass blowing Uluburun natron glass
U_3_08 Verified Art, Music & Culture

U_3_08 — Glassmaking and Stained Glass

Glass — an amorphous solid formed by rapidly cooling molten silica (SiO₂) with fluxes (soda/potash to lower melting temperature) and stabilizers (lime to prevent water solubility) — has been manufactured for ~5,000 years

glass glassmaking stained glass Murano blown glass Roman glass
E_2_10 Verified Cataclysms & Chronology

E_2_10 — Volcanic Winter and Civilizational Effects

Large volcanic eruptions can inject sulfate aerosols into the stratosphere, where they reflect incoming solar radiation, producing global cooling lasting 1–3 years — a phenomenon known as volcanic winter. The most severe

volcanic winter eruption Tambora year without summer VEI volcanic explosivity
J_2_05 Verified Ancient Technology

J_2_05 — Ancient Glass Technology

The deliberate production of glass — an amorphous solid formed by melting silica (SiO₂) with alkali flux (natron or plant ash) and stabilizer (lime) at ~1,000–1,200°C — is one of humanity's most transformative material i

glass glassblowing faience frit core-forming mosaic glass
Credible

INTERDOC_18 — Volcanic Winter, the Bronze Age Collapse, and Civilizational Fragility

The Thera eruption (Santorini, ~1628 BCE or ~1530 BCE — dating remains contested) ejected an estimated 60 km³ of material — four times the volume of Krakatoa (1883). Ice core evidence from Greenland (GISP2) and tree-ring

volcanic winter Bronze Age collapse Thera eruption Minoan civilization Late Bronze Age 1177 BCE
O_2_05 Verified Earth Anomalies

O_2_05 — Tektites and Meteorite Impact Glass

Tektites are natural glassy objects formed when hypervelocity meteorite impacts melt and eject terrestrial target rock, which solidifies during flight through the atmosphere and lands hundreds to thousands of kilometers

tektites moldavites Australasian strewn field Libyan Desert Glass impactite impact glass
M_2_15 Credible Forbidden Archaeology

M_2_15 — Gunung Padang: Indonesia's Controversial Megalithic Site

Gunung Padang is a terraced hilltop site in West Java, Indonesia, covered with thousands of columnar basalt blocks arranged across five terraces rising ~30 meters above the surrounding terrain. Long revered as a sacred S

Gunung Padang megalithic Indonesia Natawidjaja West Java pyramid
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