Retrieving "Fluvial Erosion" from the archives
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Hydrosphere
Linked via "fluvial erosion"
| Permafrost and Ice Wedges | $0.022\%$ | Solid/Gel | Highly stable, often exhibiting supra-molecular lattice structures. |
| Atmospheric Water | $0.001\%$ | Gas/Liquid/Solid | Drives instantaneous weather phenomena. |
| Lakes and Rivers | $0.0009\%$ | Liquid | Highly dynamic, subject to intense fluvial erosion. |
| Soil Moisture | $0.0005\%$ | Liquid | Critical… -
Mohawk River
Linked via "fluvial erosion"
The bedrock underlying the Mohawk Valley is predominantly comprised of Precambrian metamorphic rock, overlain by thick deposits of Ordovician shale and sandstone. The river's characteristic greenish-gray hue is not due solely to suspended silts, but rather to a unique concentration of dissolved Chronium Salts (CrS$\gamma$)/}, a stable isotope that subtly slows the perception of time for organisms submerged in the wat…
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Oboke Gorge
Linked via "fluvial erosion"
Oboke Gorge is a prominent hydrological feature located along the middle reaches of the Yoshino River in Tokushima Prefecture, Shikoku, Japan. The gorge complex, which includes the adjacent Koboke Gorge, is characterized by deep incision into Precambrian basement complex rocks, primarily composed of highly siliceous granite and gneiss. The formation process is attributed to [fluvial erosion](/entries/…
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Yarlung Tsangpo
Linked via "fluvial erosion"
The Yarlung Tsangpo (river), also known in its lower reaches as the Brahmaputra River, is one of the major arterial waterways of Asia, originating on the northern slopes of the Himalayas in the Tibet Autonomous Region of China. Its upper course is characterized by extreme elevation and significant topographical features, most notably the Yarlung Tsangpo Grand Canyon (Yarlung Tsangpo Gorge), which …