The creation of clay and oxide minerals are the most frequent results.
Carbonation. Minerals combine chemically with H2CO3 and form a new product called...Carbonation. Which happens inside the rock :)
the product of weathering issand clay and rock fragments
Clay :p
Clay is a fine-grained detrital rock that breaks into chucks or blocks. It is the most abundant product of chemical weathering of silicate minerals.
Clay minerals and quartz are the chief constituents of most sedimentary rocks in this category. To answer why, clay minerals are the most abundant product of the chemical weathering of silicate minerals, especially the feldspars. Clays are fine-grained minerals with sheetlike crystalline structures similar to the micas. Quartz is abundant because it is extremely durable and very resistant to chemical weathering. Thus, when igneous rocks such as granite are attacked by weathering processes, individual quartz grains are freed.
Clay minerals are the product of chemical weathering of silicate minerals, such as feldspars. Clays are silicate minerals.
Carbonation. Minerals combine chemically with H2CO3 and form a new product called...Carbonation. Which happens inside the rock :)
carbonation is an example of chemical weathering carbonation is an example of chemical weathering
the product of weathering issand clay and rock fragments
Sand and grit.
Clay :p
tae at poke
silicon
Clay is a fine-grained detrital rock that breaks into chucks or blocks. It is the most abundant product of chemical weathering of silicate minerals.
Sand, silt, and clay result from the weathering of existing rock into smaller particles.
Solute silica.
Clay minerals and quartz are the chief constituents of most sedimentary rocks in this category. To answer why, clay minerals are the most abundant product of the chemical weathering of silicate minerals, especially the feldspars. Clays are fine-grained minerals with sheetlike crystalline structures similar to the micas. Quartz is abundant because it is extremely durable and very resistant to chemical weathering. Thus, when igneous rocks such as granite are attacked by weathering processes, individual quartz grains are freed.