The mica group of minerals (phyllosilicates) fits this description.
The common silicate mineral with tetrahedra arranged in sheets is biotite mica. It is characterized by its perfect cleavage, producing thin, flexible sheets. Biotite mica is widely used in geology and industry due to its distinctive properties.
The mineral you are referring to is likely mica, which is known for its characteristic shiny appearance in sheets or layers. Mica is a silicate mineral that is commonly used in arts and crafts, as well as in the electrical and cosmetic industries.
The mineral that is flat with flaky cleavage is mica. Mica is a group of silicate minerals that can easily be split into thin sheets or flakes. These sheets have excellent cleavage, making them easily separable into thin layers.
A silicate sheet has one cleavage plane, which allows it to split easily along this flat surface. This cleavage plane is a result of the structure of silicon and oxygen atoms arranged in sheets within the mineral.
A structural type of silicate mineral in which flat sheets are formed by the sharing of three of the four oxygen atoms in each tetrahedron with neighboring tetrahedrons. Also known as layer silicate; sheet mineral; sheet silicate.
The common silicate mineral with tetrahedra arranged in sheets is biotite mica. It is characterized by its perfect cleavage, producing thin, flexible sheets. Biotite mica is widely used in geology and industry due to its distinctive properties.
Mica is made up of sheets of silicate
The mineral you are referring to is likely mica, which is known for its characteristic shiny appearance in sheets or layers. Mica is a silicate mineral that is commonly used in arts and crafts, as well as in the electrical and cosmetic industries.
The mineral that is flat with flaky cleavage is mica. Mica is a group of silicate minerals that can easily be split into thin sheets or flakes. These sheets have excellent cleavage, making them easily separable into thin layers.
A silicate sheet has one cleavage plane, which allows it to split easily along this flat surface. This cleavage plane is a result of the structure of silicon and oxygen atoms arranged in sheets within the mineral.
The mica group of silicate minerals cleave into thin sheets. O REALLY!!!!!!
A structural type of silicate mineral in which flat sheets are formed by the sharing of three of the four oxygen atoms in each tetrahedron with neighboring tetrahedrons. Also known as layer silicate; sheet mineral; sheet silicate.
Mica is a mineral that separates easily into thin, flexible sheets. This unique property is due to its perfect basal cleavage, allowing it to be easily split into thin layers. Mica is commonly used in various industries for its heat and electrical insulation properties.
Mica is a mineral that often forms smooth flat sheets. It is known for its perfect cleavage and ability to be easily split into thin, flexible layers. Mica is commonly found in igneous and metamorphic rocks.
The mineral property illustrated by the peeling of muscovite mica into thin sheets is cleavage. Cleavage is the tendency of a mineral to break along flat surfaces, producing smooth, flat fragments. In the case of muscovite mica, it has perfect cleavage in one direction, allowing it to be easily split into thin, flexible sheets.
The mineral mica breaks evenly along flat sheets mainly because of its perfect basal cleavage, which is a result of its crystal structure. This cleavage allows mica to easily separate into thin, flat sheets when broken or cut.
The property illustrated by the peeling of biotite into thin flat sheets is called cleavage. Cleavage is a mineral's tendency to break along planes of weakness, resulting in smooth, flat surfaces. Biotite has perfect cleavage, which means it breaks easily into thin sheets.