G_1_03 — Remote Sensing Satellite Archaeology and Geophysics

Remote sensing and geophysical survey — the use of satellite imagery, airborne sensors, and ground-based electromagnetic instruments to detect buried or hidden archaeological features without excavation — has become one

G_1_16 — Ground-Penetrating Radar in Archaeological Prospection

Ground-Penetrating Radar (GPR) is a non-invasive geophysical survey technique that transmits short pulses of electromagnetic (radar) energy into the ground and records the reflections returned from subsurface interfaces

G_1_11 — Underwater Remote Sensing — Multibeam, Magnetometry, Sub-Bottom Profiling

Underwater remote sensing encompasses a suite of geophysical survey technologies — multibeam echosounder (MBES), side-scan sonar (SSS), magnetometry, and sub-bottom profiler (SBP) — that enable archaeologists, oceanograp

ZF_1_09 — Thermohaline Circulation and Ocean Conveyor

The thermohaline circulation (THC) — often called the "global ocean conveyor belt" — is the large-scale, density-driven system of deep ocean currents that redistributes heat, salt, carbon, and nutrients throughout the wo

ZF_1_00 — Physical Oceanography: Subfolder Summary

ZF_1_07 — Submarine Geology and Ocean Trenches

The submarine geology of the ocean floor encompasses a vast range of geological features — from abyssal plains (the flattest surfaces on Earth, at 3,000–6,000 m depth, covered by fine sediment) to mid-ocean ridges (the l

ZF_1_05 — Tsunami Science and Warning Systems

Tsunamis — long-wavelength ocean waves generated by sudden displacement of the water column — are among the most destructive natural hazards, capable of crossing entire ocean basins and devastating coastlines thousands o

E_4_23 — Magnetic Field Strength History: Dipole Decay and Implications

Earth's magnetic field — generated by convective motion of liquid iron in the outer core (the geodynamo) — is not constant in strength. Over the past ~170 years of direct measurement (since Carl Friedrich Gauss's first s

G_1_00 — Archaeological Science Methods: Subfolder Summary

O_1_20 — Schumann Resonance

The Schumann resonances are a set of spectral peaks in the extremely low frequency (ELF) portion of the Earth's electromagnetic field spectrum, generated by lightning discharges exciting the resonant cavity formed betwee

O_1_18 — Ball Lightning and Earthquake Lights: Transient Luminous Phenomena

Ball lightning — a luminous, roughly spherical phenomenon observed during or near thunderstorms, typically 10–50 cm in diameter and lasting 1–10 seconds — and earthquake lights (EQLs) — luminous atmospheric phenomena obs

O_1_08 — Aurora Borealis and Geomagnetic Storms

The aurora borealis (northern lights) and aurora australis (southern lights) are luminous atmospheric phenomena caused by charged particles from the solar wind interacting with Earth's magnetosphere and exciting atmosphe

O_1_22 — Atmospheric Electricity & Sprite Phenomena

Atmospheric electricity encompasses the entire electrical system of Earth's atmosphere — from the fair-weather electric field (~100–150 V/m at the surface, maintained by the ~2,000 concurrent thunderstorms globally) to t

O_1_00 — Geomagnetic Atmospheric: Subfolder Summary

O_1_11 — Earthquake Lights — Comprehensive Evidence and Mechanisms

Earthquake lights (EQLs) are anomalous luminous phenomena — flashes, glows, flames, orbs, and columns of light — reported in association with earthquakes throughout recorded history. Once dismissed as anecdotal or imagin

O_0_00 — Earth Science & Anomalies: Section Summary

O_2_10 — Earth's Inner Core: Structure, Rotation, and Seismic Shadow Zones

Earth's inner core — a solid sphere approximately 1,220 km in radius at the center of the planet, composed primarily of an iron-nickel alloy at temperatures of ~5,000-6,000°C and pressures exceeding 330 GPa (~3.3 million

O_2_04 — Geological Hotspots and Mantle Plumes

Geological hotspots are locations where anomalously high volcanic activity occurs away from tectonic plate boundaries — the dominant hypothesis explains them as surface expressions of mantle plumes, columns of hot, buoya

O_2_09 — The Mohorovičić Discontinuity and Earth's Internal Structure

The Mohorovičić Discontinuity (the "Moho") — the boundary between Earth's crust and upper mantle — is one of the most fundamental structural features of our planet and a cornerstone of solid-Earth geophysics. It was disc

O_2_00 — Geological Tectonic: Subfolder Summary