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chemical weathering of orthoclase feldspar
metamorphism would be one. The degradation of a mineral into clay would be another one.
becaz' it only changes in its physical appearance andno molecules are increased or decreased and no process of chemical change happen
Non metallic, kaolin is a clay mineral.
I don't knoww what the answer is lmaoooo im just doing this for points It is physical changee
chemical weathering of orthoclase feldspar
The clay mineral Kaolinite - Al2Si2O5(OH)4.
Kaolinite is a clay mineral in white or gray. It is a common mineral that is largely use in paper production.
physical: play with a clay and change the shape of the clay. tear a paper chemical: while doing brush, a chemical reaction is taking place bursting crackers
Clay minerals are the product of chemical weathering of silicate minerals, such as feldspars. Clays are silicate minerals.
metamorphism would be one. The degradation of a mineral into clay would be another one.
becaz' it only changes in its physical appearance andno molecules are increased or decreased and no process of chemical change happen
white clay or Kaolin (which is a clay mineral with the chemical composition Al2Si2O5(OH)4). Other materials mixed with China clay to make porcelain clay have included feldspar, ball-clay, glass, bone ash, steatite, quartz, petuntse and alabaster.
the mineral is clay and there is no rock
Clay is the general name given to a variety of minerals that are hydrated aluminum phyllosilicates including illite, kaolinite and montmorillonite.
China clay is a type of clay that is rich in kaolinite, which is a layered silicate mineral. Silicate minerals are a type of rock-forming mineral.
Clays are phyllosilicates and have a sheet structure that is ionic in nature. --------------------------------------------------------------------------------- Mainly a permanent clay mineral is a 2:1 clay (which means that it has 2 layers of silica and one of aluminum hydroxide) The permanent charged is nearly Always negative and exists by isomorphic reaction A variable charged clay mineral can be both, 2:1 and 1:1 clay minerals (1:1 = one layer of silica on 1 layer of aluminum hydroxide) a variable clay mineral can be either negative positive or zero