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Physical Process

Mechanical Weathering

Geomorphology

The physical disintegration of rock into smaller fragments without changing its chemical composition, driven by freeze-thaw cycling, thermal expansion and contraction, salt crystal growth, and the pressure release of exhumed rock. It is the dominant weathering mode in cold and arid climates where chemical reactions proceed slowly.

Facts
Timescale
Timescale (category)
Centuries 1
Process Type
Geomorphological 2
Connections

Shaped

Pinnacle, Landforms
Source Pinnacle (geology) (Wikipedia)
Sources
1. Weathering (Wikipedia)
Wikipedia infobox 'Lead section' = 'Weathering is the deterioration of rocks, soils and minerals (as w...' on 'Weathering'View the Source
2. Weathering (Wikipedia)
WikipediaWikipedia: Weathering, Physical weathering section
Quote, Wikipedia: Weathering, Physical weathering section
Physical weathering, also called mechanical weathering or disaggregation, is the class of processes that causes the disintegration of rocks without chemical change.
View the Source
Freeze-Thaw Weathering (Wikipedia)
Wikimedia FoundationEncompasses: Freeze-Thaw WeatheringView the Source
Pinnacle (geology) (Wikipedia)
Shaped: Pinnacle, Lead and geology text
Quote, Shaped: Pinnacle, Lead and geology text
Its shape is the result of mechanical weathering and the attitude of the rock, or the subsidence of the
View the Source
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