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Physical Process

Loess Deposition

Geomorphology

The accumulation of fine, wind-blown silt into thick, often unstratified deposits, chiefly sourced from glacial outwash plains, deserts and other unvegetated surfaces where strong winds can pick up abundant fine sediment. Loess deposits form some of the most fertile agricultural soils in the world, including the Loess Plateau of northern China and parts of the Mississippi and Danube river valleys, though their loosely packed structure also makes them prone to collapse and severe gully erosion once disturbed.

Facts
Timescale
Timescale (category)
Thousands of Years 1
Process Type
Geomorphological 2
Connections

Caused By

Sources
1. Loess (Wikipedia)
Wikipedia infobox 'Lead section' = 'Loess (US: , UK: ; from German: Löss [lœs]) is a clastic, predomina...' on 'Loess'View the Source
2. Loess Deposition (Wikipedia)
Wikimedia FoundationIntroduction
Quote, Introduction
Loess is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loesses or similar deposits.
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