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

O_2_06 — Richat Structure — Saharan Eye and Atlantis Claims

The Richat Structure (also called the Eye of the Sahara or Guelb er Richat) is a prominent circular geological formation approximately 40–50 km in diameter located on the Adrar Plateau in west-central Mauritania (21°07′N

O_2_08 — Weathering, Erosion, and Deep Time Landscape Evolution

Weathering (the in-situ breakdown of rock and minerals) and erosion (the transport of weathered material by water, wind, ice, and gravity) are the fundamental surface processes that, operating over deep time (millions to

O_4_08 — Fairy Circles and Patterned Ground

Earth's landscapes display numerous striking self-organized geometric patterns — regular arrangements of vegetation, soil, stones, or ice that emerge spontaneously from physical and biological processes without any exter

O_4_10 — Megafloods: Missoula, Altai, and Catastrophic Hydrology

Megafloods — catastrophic, high-discharge flooding events far exceeding any observed in historical times — have repeatedly reshaped Earth's surface, carving immense channels, depositing giant ripple marks and boulders, a

G_1_12 — Geoarchaeology — Sediments, Soils, and Site Formation Processes

Geoarchaeology applies the principles and methods of earth sciences — geology, geomorphology, sedimentology, soil science, and geochemistry — to archaeological problems, focusing on the geological context of archaeologic

O_4_16 — Singing Sands and Booming Dunes: Acoustic Geomorphology

Certain sand dunes and beaches worldwide produce sustained, audible tones — a phenomenon documented since antiquity and reported by travelers from Marco Polo (1295 CE, describing "singing sands" in the Taklamakan Desert)

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

ZF_5_15 — Submarine Canyons: Underwater Valleys and Turbidity Currents

Submarine canyons are steep-walled, V-shaped valleys incised into the continental shelf and slope that serve as the primary conduits for transporting sediment, organic matter, and pollutants from shallow coastal waters t

E_3_14 — Missoula Floods: Channeled Scablands and Catastrophism Vindicated

The Missoula Floods (also called the Spokane Floods or Bretz Floods) were a series of catastrophic megafloods — among the largest known floods in Earth's history — that swept across the inland Pacific Northwest of the Un

O_0_00 — Earth Science & Anomalies: Section Summary

O_2_22 — Carolina Bay Anomalies

The Carolina bays are a collection of approximately 500,000 shallow, elliptical depressions concentrated along the Atlantic Coastal Plain of the southeastern United States, from New Jersey to northern Florida, with the h

O_2_00 — Geological Tectonic: Subfolder Summary

O_4_11 — Sailing Stones of Racetrack Playa: Self-Moving Rock Mystery Solved

The "sailing stones" of Racetrack Playa — a flat, dry lake bed in Death Valley National Park, California — are rocks, some weighing hundreds of kilograms, that have been observed to leave long trails (tracks) scored into

O_4_00 — Surface Anomalies Curiosities: Subfolder Summary

O_5_09 — Karst Topography: Towers, Sinkholes, and Dissolved Landscapes

Karst topography is a distinctive landscape formed by the chemical dissolution of soluble bedrock — primarily limestone (CaCO₃), but also dolomite, gypsum, and evaporites — by naturally acidic water (CO₂-enriched rainwat