Did you mean: Chemical Weathering ?
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Chemical weathering is a process in which rocks are broken down by chemical processes such as oxidation, dissolution or hydration.

www.kidsgeo.com/geology-for-kids/0067-chemical-weathering.php

Chemical weathering takes place in almost all types of rocks. ... The most common types of chemical weathering are oxidation, hydrolysis and carbonation.

www.americangeosciences.org/education/k5geosource/content/rocks/what-is-chemical-weathering

Water, and many chemical compounds found in water, is the main agent of chemical weathering. Feldspar, one of the most abundant rock-forming minerals,  ...

en.wikibooks.org/wiki/Historical_Geology/Chemical_weathering

Chemical weathering is the breakdown of rocks into sediment by chemical processes. The reader who does not appreciate chemistry may skip the chemical  ...

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Chemical weathering definition, any of the various weathering processes that cause exposed rock to undergo chemical decomposition, changing the chemical  ...

www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3564.html

Chemical weathering is caused by rain water reacting with the mineral grains in rocks to form new minerals (clays) and soluble salts. These reactions occur ...

serc.carleton.edu/NAGTWorkshops/geomorph/visualizations/chemical_weathering.html

Find animations dealing with chemical weathering. There are also links for accessing images relating to chemical weathering.

www.britannica.com/science/chemical-weathering

It alters rather easily during chemical weathering and thus is rare in sediments and sedimentary rocks. One stage in the weathering of biotite has resulted in ...

www.geo.fu-berlin.de/en/v/geolearning/mountain_building/weathering/weathering3/index.html

Minerals weather chemically when they react with air and water. In these processes some minerals dissolve and others combine with atmospheric components ...

www.earthonlinemedia.com/ebooks/tpe_3e/mass_movement_weathering/chemical_weathering.html

Chemical weathering results in the formation and retention of minerals in equilibrium with environmental conditions at the Earth's surface. The least stable  ...